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{{short description|Group of lakes in North America}} {{about|the lakes in North America|the lakes in Africa|African Great Lakes|the region|Great Lakes region|other uses of this term|Great Lakes (disambiguation)}} {{pp-move|small=yes}} {{Use mdy dates|date=March 2024}} {{Infobox body of water | name = Great Lakes of North America | other_name = Great Lakes | image = Great Lakes, No Clouds (4968915002) Brighter.jpg | alt = Five continent-sized lakes | caption = The Great Lakes seen from NASA's [[Aqua (satellite)|Aqua]] satellite in August 2010. From left to right: [[Lake Superior]], [[Lake Michigan|Michigan]], [[Lake Huron|Huron]], [[Lake Erie|Erie]], [[Lake Ontario|Ontario]] | image_bathymetry = Great Lakes bathymetry map.png | alt_bathymetry = | caption_bathymetry = [[Bathymetry]] map of the Great Lakes | location = Eastern [[North America]] | coordinates = {{coord|45|N|84|W|region:US_type:waterbody_scale:7500000}} | type = group of interconnected [[freshwater lake]]s | part_of = [[Great Lakes Basin]] | inflow = Past: [[precipitation]] and [[meltwater]]<br />Now: [[river]]s, precipitation, and [[Spring (hydrology)|groundwater spring]]s | outflow = Evaporation, [[St. Lawrence River]] to the [[Atlantic Ocean]] | catchment = <!-- {{convert|VALUE|UNITS}} must be used --> | basin_countries = [[Canada]], [[United States]] | agency = | area = {{convert|94250|sqmi|0}} | depth = {{cvt|60–480|ft|m}} depending on the lakes | max-depth = {{cvt|210–1300|ft|m}} depending on the lakes | volume = {{convert|5439|cumi|0}} (lowest) | salinity = | shore = <!-- {{convert|VALUE|UNITS}} must be used --> | elevation = <!-- {{convert|VALUE|UNITS}} must be used --> | temperature_high = <!-- {{convert|VALUE|UNITS}} must be used --> | temperature_low = <!-- {{convert|VALUE|UNITS}} must be used --> | frozen = around January to March | islands = | trenches = | cities = <!-- Map --> | website = | reference = <!-- In the article --> }} The '''Great Lakes''', also called the '''Great Lakes of North America''', are a series of large interconnected [[freshwater]] [[lake]]s spanning the [[Canada–United States border]]. The five lakes are [[Lake Superior|Superior]], [[Lake Michigan|Michigan]], [[Lake Huron|Huron]], [[Lake Erie|Erie]], and [[Lake Ontario|Ontario]] (though hydrologically, [[Lake Michigan–Huron|Michigan and Huron]] are a single body of water, joined at the [[Straits of Mackinac]]). The [[Great Lakes Waterway]] enables modern travel and shipping by water among the lakes. The lakes connect to the [[Atlantic Ocean]] via the [[Saint Lawrence River]], and to the [[Mississippi River]] basin through the [[Illinois Waterway]]. The Great Lakes are the largest group of freshwater lakes on Earth by total area and the second-largest by total volume. They contain 21% of the world's surface fresh water by volume.<ref>{{cite web |title=Great Lakes |url=http://www.epa.gov/glnpo/basicinfo.html |publisher=[[U.S. Environmental Protection Agency]] |date=June 28, 2006 |access-date=February 19, 2011}}</ref><ref>{{cite web |title=LUHNA Chapter 6: Historical Landcover Changes in the Great Lakes Region |publisher=USGS: Ecosystems |date=November 20, 2003 |access-date=February 19, 2011 |archive-url=https://web.archive.org/web/20120111122929/http://biology.usgs.gov/luhna/chap6.html |url=http://biology.usgs.gov/luhna/chap6.html |archive-date=January 11, 2012}}</ref><ref>{{cite book |last=Ghassemi |first=Fereidoun |title=Inter-basin water transfer |publisher=Cambridge University Press |location=Cambridge |year=2007 |isbn=978-0-521-86969-0}}</ref> The total surface is {{convert|94250|sqmi|0}}, and the total volume (measured at the low water datum) is {{convert|5439|cumi|0}},<ref name="EPAphysical">{{cite web |title=Great Lakes: Basic Information: Physical Facts |url=http://www.epa.gov/glnpo/physfacts.html |publisher=U.S. Environmental Protection Agency |date=May 25, 2011 |access-date=November 9, 2011 |archive-url=https://web.archive.org/web/20120529233616/http://www.epa.gov/glnpo/physfacts.html |archive-date=May 29, 2012}}</ref> slightly less than the volume of [[Lake Baikal]] ({{cvt|23615|km3|order=flip|disp=or|}}, 22–23% of the world's surface fresh water). Because of their sea-like characteristics, such as rolling waves, sustained winds, strong currents, great depths, and distant horizons, the five Great Lakes have long been called [[inland seas]].<ref>{{cite book |last=Williamson |first=James |title=The inland seas of North America: and the natural and industrial productions ... |url=https://books.google.com/books?id=ydMNAQAAMAAJ&pg=PA7 |publisher=John Duff Montreal Hew Ramsay Toronto AH Armour and Co. |year=2007 |access-date=January 5, 2014 |isbn=9780665341281}}</ref> Depending on how it is measured, by surface area, either Lake Superior or [[Lake Michigan–Huron]] is the [[List of lakes by area|second-largest lake in the world]] and the largest freshwater lake. Lake Michigan is the largest lake, by surface area, that is entirely within one country, the United States.<ref>{{cite web |title=The Top Ten: The Ten Largest Lakes of the World |url=http://www.infoplease.com/toptens/largelakes.html |work=infoplease.com}}</ref><ref>{{cite book |last=Hough |first=Jack |chapter=Great Lakes |title=Encyclopædia Britannica |publisher=William Benton |location=Chicago |edition=Commemorative Edition for Expo'70 |volume=10 |year=1970 |orig-date=1763 |page=774 |isbn=978-0-85229-135-1}}</ref><ref>{{cite web |title=Large Lakes of the World |url=http://www.factmonster.com/ipka/A0001777.html |work=factmonster.com}}</ref> The Great Lakes began to form at the end of the [[Last Glacial Period]] around 14,000 years ago, as retreating ice sheets exposed the basins they had carved into the land, which then filled with meltwater.<ref name="CordellLightfoot2008">{{cite book |last1=Cordell |first1=Linda S. |last2=Lightfoot |first2=Kent |last3=McManamon |first3=Francis |last4=Milner |first4=George |title=Archaeology in America: An Encyclopedia |url=https://books.google.com/books?id=arfWRW5OFVgC&pg=RA1-PA25 |publisher=ABC-CLIO |year=2008 |page=1 |isbn=978-0-313-02189-3}}</ref> The lakes have been a major source for transportation, migration, trade, and fishing, serving as a habitat to many aquatic species in a region with much [[biodiversity]]. The surrounding region is called the [[Great Lakes region]], which includes the [[Great Lakes Megalopolis]].<ref>{{cite web |title=Great Lakes |url=http://www.america2050.org/great_lakes.html |website=America 2050 |access-date=December 7, 2016 |archive-url=https://web.archive.org/web/20200220180833/http://www.america2050.org/great_lakes.html |archive-date=February 20, 2020}}</ref> Major cities within the region include, on the American side, from east to west, [[Buffalo, NY|Buffalo]], [[Cleveland]], [[Detroit]], [[Chicago]], and [[Milwaukee]]; and, on the Canadian side, [[Toronto]], [[Hamilton, Ontario|Hamilton]] and [[Mississauga]]. ==Geography== [[File:Sub-basins Great Lakes Basin.png|thumb|right|upright=1.1|A map of the Great Lakes Basin showing the five sub-basins. Left to right they are: Superior (magenta); Michigan (cyan); Huron (green); Erie (yellow); Ontario (red).]] Though the five lakes lie in separate basins, they form a single, naturally interconnected body of fresh water, within the [[Great Lakes Basin]]. As a chain of lakes and rivers, they connect the east-central interior of North America to the Atlantic Ocean. From the interior to the outlet at the Saint Lawrence River, water flows from Superior to Huron and Michigan, southward to Erie, and finally northward to Lake Ontario. The lakes [[Drainage system (geomorphology)|drain a large watershed]] via many rivers and contain approximately 35,000 islands.<ref name="Bennett1999as">{{cite book |last=Bennett |first=Tom |title=State of the Great Lakes: 1997 Annual Report |url=https://books.google.com/books?id=uN2nhumNsiAC&pg=PA1991-IA7 |publisher=Diane Publishing |year=1999 |page=1991 |isbn=978-0-7881-4358-8}}</ref> There are also several thousand smaller lakes, often called "inland lakes", within the basin.<ref name="Likens2010at">{{cite book |last=Likens |first=Gene E. |title=Lake Ecosystem Ecology: A Global Perspective |url=https://books.google.com/books?id=OzJOqh90RuwC&pg=PA326 |publisher=Academic Press |year=2010 |page=326 |isbn=978-0-12-382003-7}}</ref> The surface area of the five primary lakes combined is roughly equal to the size of the United Kingdom, while the surface area of the entire basin (the lakes and the land they drain) is about the size of the UK and France combined.<ref name="Grady" /> Lake Michigan is the only one of the Great Lakes that is entirely within the United States; the others form a water boundary between the United States and Canada. The lakes are divided among the jurisdictions of the Canadian province of [[Ontario]] and the U.S. states of [[Michigan]], [[Wisconsin]], [[Minnesota]], [[Illinois]], [[Indiana]], [[Ohio]], [[Pennsylvania]], and [[New York (state)|New York]]. Both the province of Ontario and the state of Michigan include in their boundaries portions of four of the lakes. The province of Ontario does not border Lake Michigan, and the state of Michigan does not border Lake Ontario. New York and Wisconsin's jurisdictions extend into two lakes, and each of the remaining states into one of the lakes. ===Bathymetry=== {| border="0" cellspacing="2" cellpadding="0" style="width:600px; font-size:smaller;" |+ Relative elevations, average depths, maximum depths, and volumes of the Great Lakes |- |colspan=2| <timeline> ImageSize = width:595 height:250 PlotArea = width:525 height:200 left:50 bottom:15 AlignBars = justify Period = from:-1000 till:600 TimeAxis = orientation:vertical ScaleMajor = unit:year increment:500 start:-1000 ScaleMinor = unit:year increment:100 start:-1000 Colors = id:blue1 value:rgb(0.0,0.0,0.75) id:blue2 value:rgb(0.1,0.1,0.8) id:blue3 value:rgb(0.2,0.2,0.85) id:blue4 value:rgb(0.3,0.3,0.9) id:blue5 value:rgb(0.4,0.4,0.95) id:textinbar value:yelloworange id:textoutsidebar value:redorange Define $elevation = shift:(0,15) mark:(line,textoutsidebar) textcolor:textoutsidebar Define $avgdepth = mark:(line,textinbar) textcolor:textinbar Define $maxdepth = shift:(0,-11) mark:(line,textoutsidebar) textcolor:textoutsidebar PlotData= align:center bar:Superior from:-732 till:600 width:194 color:blue1 $elevation at:600 text:"600 ft (183 m)" $avgdepth at:117 shift:(0,1) text:"483 ft (147 m)" $maxdepth at:-732 text:"1,332 ft (406 m)" bar:Michigan from:-348 till:577 width:113 color:blue5 $elevation at:577 text:"577 ft (176 m)" $avgdepth at:298 shift:(0,2) text:"279 ft (85 m)" $maxdepth at:-348 text:"925 ft (282 m)" bar:Huron from:-173 till:577 width:101 color:blue3 $elevation at:577 text:"577 ft (176 m)" $avgdepth at:382 shift:(0,1) text:"195 ft (59 m)" $maxdepth at:-173 text:"750 ft (229 m)" bar:Erie from:359 till:569 width:49 color:blue2 $elevation at:569 text:"569 ft (173 m)" $avgdepth at:507 align:left shift:(30,2) text:"62 ft (19 m)" $maxdepth at:359 text:"210 ft (64 m)" bar:Ontario from:-559 till:243 width:44 color:blue4 $elevation at:243 text:"243 ft (74 m)" $avgdepth at:-40 shift:(0,2) text:"283 ft (86 m)" $maxdepth at:-559 text:"802 ft (244 m)" align:left shift:(35,0) textcolor:green at:243 text:"surface~elevation" at:-40 text:"average~depth" at:-559 text:"maximum~depth" </timeline> |- valign=top !align=right| Notes: | The area of each rectangle is proportional to the volume of each lake. All measurements at Low Water Datum. |- valign=top !align=right| Source: | United States Environmental Protection Agency<ref name=EPA>{{cite web |url = http://www.epa.gov/glnpo/atlas/gl-fact1.html |title = Great Lakes Atlas: Factsheet #1 |access-date = December 3, 2007 |date = March 9, 2006 |website = U.S. Environmental Protection Agency |url-status = dead |archive-url = https://web.archive.org/web/20080328170959/http://www.epa.gov/glnpo/atlas/gl-fact1.html |archive-date = March 28, 2008 }}</ref> |} {| class="wikitable" style="text-align:center;" cellpadding="5" |- ! ![[Lake Erie]] ![[Lake Huron]] ![[Lake Michigan]] ![[Lake Ontario]] ![[Lake Superior]] |- ! Surface area<ref name="EPAphysical"/> | {{convert|9910|sqmi|km2|abbr=on|order=flip}} | {{convert|23000|sqmi|km2|abbr=on|order=flip}} | {{convert|22300|sqmi|km2|abbr=on|order=flip}} | {{convert|7340|sqmi|km2|abbr=on|order=flip}} | {{convert|31700|sqmi|km2|abbr=on|order=flip}} |- ! Water volume<ref name="EPAphysical"/> | {{convert|116|cumi|km3|abbr=on|order=flip}} | {{convert|850|cumi|km3|abbr=on|order=flip}} | {{convert|1180|cumi|km3|abbr=on|order=flip}} | {{convert|393|cumi|km3|abbr=on|order=flip}} | {{convert|2900|cumi|km3|abbr=on|order=flip}} |- ! Elevation<ref name=EPA/> | {{convert|571|ft|m|abbr=on|order=flip}} | {{convert|577|ft|m|abbr=on|order=flip}} | {{convert|577|ft|m|abbr=on|order=flip}} | {{convert|246|ft|m|abbr=on|order=flip}} | {{convert|600.0|ft|m|abbr=on|order=flip}} |- ! Average depth<ref name="Grady" /> | {{convert|62|ft|m|abbr=on|order=flip}} | {{convert|195|ft|m|abbr=on|order=flip}} | {{convert|279|ft|m|abbr=on|order=flip}} | {{convert|283|ft|m|abbr=on|order=flip}} | {{convert|483|ft|m|abbr=on|order=flip}} |- ! Maximum depth<ref name="dep">{{cite web |title = Great Lakes Map |url = http://www.michigan.gov/deq/0,1607,7-135-3313_3677-15926--,00.html |publisher = Michigan Department of Environmental Quality |access-date = November 27, 2011 |archive-url = https://web.archive.org/web/20111114034432/http://www.michigan.gov/deq/0,1607,7-135-3313_3677-15926--,00.html |archive-date = November 14, 2011 |url-status = dead }}</ref> | {{convert|210|ft|m|abbr=on|order=flip}} | {{convert|748|ft|m|abbr=on|order=flip}} | {{convert|925|ft|m|abbr=on|order=flip}} | {{convert|804|ft|m|abbr=on|order=flip}} | {{convert|1333|ft|m|abbr=on|order=flip}} |- ! Major settlements<ref>See [[List of cities on the Great Lakes]] for a complete list.</ref> | [[Buffalo, New York|Buffalo, NY]]<br />[[Erie, Pennsylvania|Erie, PA]]<br />[[Cleveland|Cleveland, OH]]<br />[[Detroit|Detroit, MI]]<br/>[[Lorain, Ohio|Lorain, OH]]<br />[[Toledo, Ohio|Toledo, OH]]<br />[[Sandusky, Ohio|Sandusky, OH]] | [[Alpena, Michigan|Alpena, MI]]<br />[[Bay City, Michigan|Bay City, MI]]<br />[[Collingwood, Ontario|Collingwood, ON]]<br />[[Owen Sound|Owen Sound, ON]]<br />[[Port Huron, Michigan|Port Huron, MI]]<br />[[Sarnia|Sarnia, ON]] | [[Chicago|Chicago, IL]]<br />[[Waukegan|Waukegan, IL]]<br />[[Gary, Indiana|Gary, IN]]<br />[[Green Bay, Wisconsin|Green Bay, WI]]<br />[[Sheboygan, Wisconsin|Sheboygan, WI]]<br />[[Milwaukee|Milwaukee, WI]]<br />[[Kenosha, Wisconsin|Kenosha, WI]]<br />[[Racine, Wisconsin|Racine, WI]]<br />[[Muskegon, Michigan|Muskegon, MI]]<br />[[Traverse City, Michigan|Traverse City, MI]] | [[Hamilton, Ontario|Hamilton, ON]]<br />[[Kingston, Ontario|Kingston, ON]]<br />[[Mississauga|Mississauga, ON]]<br />[[Oshawa|Oshawa, ON]]<br />[[Rochester, New York|Rochester, NY]]<br />[[Toronto|Toronto, ON]] | [[Duluth, Minnesota|Duluth, MN]]<br />[[Marquette, Michigan|Marquette, MI]]<br />[[Sault Ste. Marie, Michigan|Sault Ste. Marie, MI]]<br />[[Sault Ste. Marie, Ontario|Sault Ste. Marie, ON]]<br />[[Superior, Wisconsin|Superior, WI]]<br />[[Thunder Bay|Thunder Bay, ON]] |}As the surfaces of Lakes Superior, Huron, Michigan, and Erie are all approximately the same elevation above sea level, while Lake Ontario is significantly lower, and because the [[Niagara Escarpment]] precludes all natural navigation, the four upper lakes are commonly called the "upper great lakes". This designation is not universal. Those living on the shore of Lake Superior often refer to all the other lakes as "the lower lakes", because they are farther south. Sailors of [[Bulk carrier|bulk freighters]] transferring cargoes from Lake Superior and northern Lake Michigan and Lake Huron to ports on Lake Erie or Ontario commonly refer to the latter as the lower lakes and Lakes Michigan, Huron, and Superior as the upper lakes. This corresponds to thinking of lakes Erie and Ontario as "down south" and the others as "up north". Vessels sailing north on Lake Michigan are considered "upbound" even though they are sailing toward its effluent current.<ref name="Bowlus2010">{{cite book |first = W. Bruce |last = Bowlus |title = Iron Ore Transport on the Great Lakes: The Development of a Delivery System to Feed American Industry |url = https://books.google.com/books?id=nyGjHG1PaUEC&pg=PA215 |year = 2010 |publisher = McFarland |isbn = 978-0-7864-8655-7 |page = 215 }}</ref>{{clear}} [[File:Great Lakes.svg|upright=1.8|thumb|left|System profile of the Great Lakes]] {{clear}} ===Primary connecting waterways=== [[File:2009-09-18 3060x2040 chicago skyline.jpg|thumb|right|Chicago on Lake Michigan is in the western part of the lakes megalopolis and the site of the waterway linking the lakes to the Mississippi River valley]] * The [[Chicago River]] and [[Calumet River]] systems connect the Great Lakes Basin to the [[Mississippi River]] System through human-made alterations and canals. * The [[St. Marys River (Michigan–Ontario)|St. Marys River]], including the [[Soo Locks]], connects Lake Superior to Lake Huron, via the [[North Channel (Ontario)|North Channel]]. * The [[Straits of Mackinac]] connect Lake Michigan to Lake Huron (the two are hydrologically one lake). * The [[St. Clair River]] connects Lake Huron to [[Lake St. Clair]]. * The [[Detroit River]] connects Lake St. Clair to Lake Erie. * The [[Niagara River]], including [[Niagara Falls]], connects Lake Erie to Lake Ontario. * The [[Welland Canal]], bypassing the Niagara River, connects Lake Erie to Lake Ontario. * The [[Saint Lawrence River]] and the [[Saint Lawrence Seaway]] connect Lake Ontario to the [[Gulf of Saint Lawrence]], which connects to the [[Atlantic Ocean]]. ===Lake Michigan–Huron=== {{main|Lake Michigan–Huron}} [[File:ISS067-E-14016 Lake Michigan–Huron.jpg|thumb|Lake Michigan–Huron with north oriented to the right; taken on April 14, 2022, during [[Expedition 67]] of the International Space Station. {{nowrap|Green Bay}} is at the upper right and Saginaw Bay is on the left.]] Lakes Huron and Michigan are sometimes considered a single lake, called Lake Michigan–Huron, because they are one hydrological body of water connected by the Straits of Mackinac.<ref>{{cite web |url = http://www.infoplease.com/ipa/A0001804.html |title = Michigan and Huron: One Lake or Two? |publisher = Pearson Education |website = Information Please Database |year = 2007 }}</ref> The straits are {{convert|5|mi|km|0|spell=in}} wide<ref name="Grady" /> and {{convert|120|ft|m}} deep; the water levels rise and fall together,<ref name=nyt>{{cite book |editor-first = John W. |editor-last = Wright |year = 2006 |title = The New York Times Almanac |url = https://archive.org/details/newyorktimes200600wrig |url-access = registration |edition = 2007 |publisher = Penguin Books |location = New York |isbn = 978-0-14-303820-7 |page = [https://archive.org/details/newyorktimes200600wrig/page/64 64] }}</ref> and the flow between Michigan and Huron frequently reverses direction. ===Large bays and related significant bodies of water=== * [[Lake Nipigon]], connected to Lake Superior by the [[Nipigon River]], is surrounded by [[layered intrusion|sill-like formations]] of [[mafic]] and [[ultramafic rock|ultramafic]] [[igneous rock]] hundreds of meters high. The lake lies in the [[Nipigon Embayment]], a [[Aulacogen|failed arm]] of the [[triple junction]] (centered beneath Lake Superior) in the [[Midcontinent Rift System]] event, estimated at 1.1 billion years ago. * [[Thunder Bay (Ontario)|Thunder Bay]] is a large bay on the north shore of Lake Superior bordered to the east by the [[Sibley Peninsula]] in northern Ontario. * [[Chequamegon Bay]] is an inlet of Lake Superior south of the [[Apostle Islands]] and the [[Bayfield Peninsula]] in northern Wisconsin. * [[Keweenaw Bay]] is an arm of Lake Superior southeast of the [[Keweenaw Peninsula]]. * [[Whitefish Bay]] is a large bay on the eastern end of Lake Superior which leads to the outflow of the lake into the [[St. Marys River (Michigan–Ontario)|St. Marys River]]. * [[Lake Winnebago]], connected to Green Bay by the [[Fox River (Green Bay tributary)|Fox River]], serves as part of the [[Fox–Wisconsin Waterway]] and is part of a larger system of lakes in Wisconsin known as the [[Winnebago Pool]]. * [[Green Bay (Lake Michigan)|Green Bay]] is an arm of Lake Michigan along the south coast of the [[Upper Peninsula of Michigan]] and the east coast of Wisconsin. It is separated from the rest of the lake by the [[Door Peninsula]] in Wisconsin, the [[Garden Peninsula]] in Michigan, and the chain of islands between them, all of which were formed by the [[Niagara Escarpment]]. The north end of Green Bay consists of [[Big Bay de Noc]] and [[Little Bay de Noc]]. * [[Grand Traverse Bay]] is an arm of Lake Michigan on Michigan's west coast and is one of the largest natural harbors in the Great Lakes. The bay is divided into east and west arms by the [[Old Mission Peninsula]].<ref>{{cite web |url = http://www.peninsulatownship.com |title = Home |publisher = Peninsula Township |access-date = December 7, 2016 }}</ref> The bay has one major island, [[Power Island]]. Its name is derived from [[Jacques Marquette|Jacques Marquette's]] crossing of the bay from [[Norwood, Michigan|Norwood]] to [[Northport, Michigan|Northport]] which he called ''La Grande Traversee''.{{citation needed|date=May 2016}} * [[Georgian Bay]] is an arm of Lake Huron, extending northeast from the lake entirely within Ontario. The bay, along with its narrow westerly extensions of the [[North Channel (Ontario)|North Channel]] and [[Mississagi Strait]], is separated from the rest of the lake by the [[Bruce Peninsula]], [[Manitoulin Island]], and [[Cockburn Island (Ontario)|Cockburn Island]], all of which were formed by the Niagara Escarpment. * [[Lake Nipissing]], connected to Georgian Bay by the [[French River (Ontario)|French River]], contains two [[volcanic pipe]]s, which are the [[Manitou Islands (Lake Nipissing)|Manitou Islands]] and [[Callander Bay]].<ref>{{cite web |url = http://home.cogeco.ca/~nananne/backgroundgeology/070211-BackgroundGeology-w.html |title = Background Geology of the North Bay area |archive-url = https://web.archive.org/web/20100724012748/http://home.cogeco.ca/~nananne/backgroundgeology/070211-BackgroundGeology-w.html |archive-date = July 24, 2010 |access-date = September 24, 2007 }}{{self-published inline|certain=yes|date=March 2024}}</ref> These pipes were formed by a violent, [[supersonic eruption]] of deep origin. The lake lies in the [[Ottawa-Bonnechere Graben]], a [[Mesozoic]] [[rift valley]] that formed 175 million years ago. * [[Lake Simcoe]], connected to Georgian Bay by the [[Severn River (central Ontario)|Severn River]], serves as part of the [[Trent–Severn Waterway]], a canal route traversing [[Southern Ontario]] between Lakes Ontario and Huron. * [[Thunder Bay (Michigan)|Thunder Bay]] is a bay on the west side of Lake Huron in Michigan. * [[Saginaw Bay]], an extension of Lake Huron into the [[Lower Peninsula of Michigan]], fed by the [[Saginaw River|Saginaw]] and other rivers, has the largest contiguous freshwater [[wetland]] in the United States.<ref>{{Cite web |url = https://www.epa.gov/greatlakes |title = The Great Lakes |id = REG 05 |date = August 20, 2015 |publisher = Environmental Protection Agency }}</ref> * [[Lake St. Clair]], connected with Lake Huron to its north by the [[St. Clair River]] and with Lake Erie to its south by the [[Detroit River]]. Although it is 17 times smaller in area than Lake Ontario and only rarely included in the listings of the Great Lakes,<ref name=LakeStClair>{{cite web |url = http://www.great-lakes.net/lakes/stclairReport/summary_00.pdf |title = Lake St. Clair summary report |archive-url = https://web.archive.org/web/20160416124842/http://www.great-lakes.net/lakes/stclairReport/summary_00.pdf |archive-date = April 16, 2016 |website = Great Lakes.net |access-date = December 2, 2007 }}</ref><ref name="U.S.Army">{{cite web |url = http://www.lre.usace.army.mil/_kd/Items/actions.cfm?action=Show&item_id=4310&destination=ShowItem |title = Chapter 1:Introduction to Lake St. Clair and the St. Clair River |access-date = June 8, 2008 |publisher = U.S. government U.S. Army |date = June 2004 |archive-url = https://web.archive.org/web/20090110202934/http://www.lre.usace.army.mil/_kd/Items/actions.cfm?action=Show&item_id=4310&destination=ShowItem |archive-date = January 10, 2009 }}</ref> proposals for its official recognition as a Great Lake are occasionally made, which would affect its inclusion in scientific research projects designated as related to "The Great Lakes".<ref>{{cite news |url = https://www.latimes.com/archives/la-xpm-2002-oct-20-na-stclair20-story.html |title = Movement Would Thrust Greatness on Lake St. Clair |newspaper = [[Los Angeles Times]] |date = October 20, 2002 }}</ref> * [[Sandusky Bay]] is a bay on Lake Erie in northern Ohio. * [[Long Point, Ontario|Long Point Bay]] is a bay on the north shore of Lake Erie in Ontario. * [[Hamilton Harbour]] is a harbor on the western tip of Lake Ontario. * The [[Bay of Quinte]] is a long and narrow bay on the north shore of Lake Ontario. ===Islands=== [[File:Put-in-Bay Airport.jpg|thumb|[[South Bass Island]] in Lake Erie]] Dispersed throughout the Great Lakes are approximately [[List of islands of the Great Lakes|35,000 islands]].<ref name="Bennett1999as"/> The largest among them is [[Manitoulin Island]] in Lake Huron, the largest island in any inland body of water in the world.<ref name="Dunn1996bv">{{cite book |last = Dunn |first = Gary A |title = Insects of the Great Lakes Region |url = https://books.google.com/books?id=HWHXdlPF-7cC&pg=PA3 |year = 1996 |publisher = [[University of Michigan Press]] |isbn = 978-0-472-06515-8 |page = 3 }}</ref> The second-largest island is [[Isle Royale]] in Lake Superior.<ref name="Huber(U.S.)1975">{{cite book |last1 = Huber |first1 = Norman King |author2 = United States Geological Survey |author3 = United States National Park Service |title = The geologic story of Isle Royale National Park |url = https://books.google.com/books?id=Te8sAQAAMAAJ&pg=PA41 |year = 1975 |publisher = Government Printing Office |page = 41 |isbn = 9780932212313 }}</ref> Both of these islands are large enough to contain multiple lakes themselves—for instance, Manitoulin Island's [[Lake Manitou]] is the world's largest lake on a freshwater island.<ref name="Manivanan2008">{{cite book |last = Manivanan |first = R. |title = Water Quality Modeling: Rivers, Streams, and Estuaries |url = https://books.google.com/books?id=KneEuR09lsQC&pg=PA114 |year = 2008 |publisher = New India Publishing |isbn = 978-81-89422-93-6 |page = 114 }}</ref> Some of these lakes even have their own islands, like [[Treasure Island (Ontario)|Treasure Island]] in [[Lake Mindemoya]] in Manitoulin Island. ===Peninsulas=== [[File:Skyline of Toronto viewed from Harbour.jpg|thumb|right|[[Toronto]] on Lake Ontario is in the eastern section of the [[Great Lakes Megalopolis]]]] The Great Lakes have several peninsulas between them, most prominently the [[Upper Peninsula of Michigan|Upper Peninsula]], the [[Lower Peninsula of Michigan|Lower Peninsula]], and the [[Ontario Peninsula]]. Population centers on these peninsulas include [[Grand Rapids, Michigan|Grand Rapids]], [[Flint, Michigan|Flint]], and [[Detroit, Michigan|Detroit]] in Michigan along with [[London, Ontario|London]], [[Hamilton, Ontario|Hamilton]], [[Brantford, Ontario|Brantford]], and [[Toronto, Ontario|Toronto]] in Ontario. Other significant peninsulas in the Great Lakes include the [[Sibley Peninsula|Sibley]], [[Bayfield Peninsula|Bayfield]], [[Keweenaw Peninsula|Keweenaw]], [[Door Peninsula|Door]], [[Garden Peninsula|Garden]], [[Leelanau Peninsula|Leelanau]], [[The Thumb|Thumb]], [[Bruce Peninsula|Bruce]], and [[Niagara Peninsula|Niagara]] peninsulas. ===Shipping connection to the ocean=== Although the Saint Lawrence Seaway and Great Lakes Waterway make the Great Lakes accessible to ocean-going vessels,<ref name="McCalla1994">{{cite book |first = Robert |last = McCalla |title = Water Transportation in Canada |url = https://archive.org/details/watertransportat0000mcca |url-access = registration |date = January 1, 1994 |publisher = Formac Publishing Company |isbn = 978-0-88780-247-8 |pages = [https://archive.org/details/watertransportat0000mcca/page/159 159]–162 }}</ref> shifts in shipping to wider ocean-going [[container ship]]s—which do not fit through the [[Lock (water navigation)|locks]] on these routes—have limited container shipping on the lakes. Most Great Lakes trade is of bulk material, and bulk freighters of [[Seawaymax]]-size or less can move throughout the entire lakes and out to the Atlantic.<ref name="Coastal Sediments '07">{{cite book |title = Coastal Sediments '07 |url = https://books.google.com/books?id=iMt2BQ0R628C&pg=PA2215 |access-date = April 16, 2013 |year = 2007 |publisher = ASCE Publications |isbn = 978-0-7844-7194-4 |page = 2215 }}</ref> Larger ships are confined to working within the lakes. Only barges can access the [[Illinois Waterway]] system providing access to the [[Gulf of Mexico]] via the Mississippi River. Despite their vast size, large sections of the Great Lakes freeze over in winter, interrupting most shipping from January to March. Some [[icebreaker]]s ply the lakes, keeping the shipping lanes open through other periods of ice on the lakes. The Great Lakes are connected by the [[Chicago Sanitary and Ship Canal]] to the Gulf of Mexico via the [[Illinois River]] (from the [[Chicago River]]) and the Mississippi River. An alternate track is via the Illinois River (from Chicago), to the Mississippi, up the Ohio, and then through the [[Tennessee–Tombigbee Waterway]] (a combination of a series of rivers and lakes and canals), to [[Mobile Bay]] and the Gulf of Mexico. Commercial [[Tugboat|tug]]-and-[[barge]] traffic on these waterways is heavy.<ref name="Census1908">{{cite book |author = United States Bureau of the Census |title = Transportation by water. 1906 |url = https://archive.org/details/transportationb00censgoog |year = 1908 |publisher = Government Printing Office |page = [https://archive.org/details/transportationb00censgoog/page/n252 220] }}</ref> Pleasure boats can enter or exit the Great Lakes by way of the [[Erie Canal]] and [[Hudson River]] in New York. The Erie Canal connects to the Great Lakes at the east end of Lake Erie (at [[Buffalo, New York]]) and at the south side of Lake Ontario (at [[Oswego, New York]]). ===Water levels=== The lakes were originally fed by both precipitation and [[meltwater]] from glaciers which are no longer present. In modern times, only about 1% of volume per year is "new" water, originating from rivers, precipitation, and groundwater springs. In the post-glacial period, [[evaporation]], and drainage have generally been balanced, making the levels of the lakes relatively constant.<ref name=Grady/> Intensive [[World population|human population]] growth began in the region in the 20th century and continues today.<ref name=Grady/> At least two human water use activities have been identified as having the potential to affect the lakes' levels: diversion (the transfer of water to other watersheds) and consumption (substantially done today by the use of lake water to power and cool electric generation plants, resulting in evaporation).<ref>{{cite web |url = http://www.epa.gov/glnpo/solec/index.html |title = State of the Great Lakes 2009 Highlights |publisher = [[Environment Canada]] and Environmental Protection Agency |access-date = July 7, 2013 |pages = 7–8 }}</ref> Outflows through the Chicago Sanitary and Ship Canal is more than balanced by artificial inflows via the [[Ogoki River]] and Long Lake/[[Kenogami River]] diversions.<ref>{{cite web |title = An Overview of Great Lakes Diversions |url = https://ijc.org/en/lsbc/watershed/great-lakes-diversions |publisher = [[International Joint Commission]] |date = May 14, 2020 |access-date = September 29, 2021 }}</ref> Fluctuation of the water levels in the lakes has been observed since records began in 1918.<ref name="auto">{{cite web |url = https://lre-wm.usace.army.mil/ForecastData/GLBasinConditions/LTA-GLWL-Graph.pdf |archive-url = https://web.archive.org/web/20190711121842/http://lre-wm.usace.army.mil/ForecastData/GLBasinConditions/LTA-GLWL-Graph.pdf |archive-date = July 11, 2019 |url-status = live |title = Great Lakes Water Levels (1918–2021) |publisher = United States Army Corps of Engineers |access-date = June 26, 2021 }}</ref> The water level of Lake Michigan–Huron had remained fairly constant over the 20th century.<ref name="BolsengaHerdendorf1993">{{cite book |last1 = Bolsenga |first1 = Stanley J. |last2 = Herdendorf |first2 = Charles E. |title = Lake Erie and Lake Saint Clair Handbook |url = https://books.google.com/books?id=nndmmFTWkVEC&pg=PA67 |year = 1993 |publisher = Wayne State University Press |isbn = 978-0-8143-2470-7 |page = 67 }}</ref> Recent lake levels include record low levels in 2013 in Lakes Superior, Erie, and Michigan-Huron,<ref name=jsonline>{{cite web |url = http://www.jsonline.com/news/wisconsin/lakes-michigan-huron-hit-record-low-level-dq8loc2-189903561.html |work = Milwaukee Journal Sentinel |title = Lakes Michigan, Huron hit record low water level |last = Egan |first = Dan |date = February 5, 2013 |access-date = June 26, 2021 }}</ref> followed by record high levels in 2020<ref>{{cite web |url = https://www.glerl.noaa.gov/data/wlevels/data/miHuronLevelsFeet.png |title = Lake Michigan-Huron Water Levels from Harbor Beach, MI - 9075014 2020 – 2021 |publisher = National Oceanic and Atmospheric Administration |access-date = June 26, 2021 }}</ref> in the same lakes. The water level in Lake Ontario has remained relatively constant in the same time period, hovering around the historical average level.<ref name="auto"/> [[File:Great lakes water level.png|thumb|upright=1.1|Water levels of Lakes Michigan and Huron in the United States, 1918 to 2019]] Although "true tides—changes in water level caused by the gravitational forces of the sun and moon—do occur in a semi-diurnal (twice daily) pattern", such changes are quite small and generally obscured by other forces.<ref>{{Cite web |last=US Department of Commerce |title=Do the Great Lakes have tides? |url=https://oceanservice.noaa.gov/facts/gltides.html# |access-date=2024-11-27 |website=National Oceanic and Atmospheric Administration |language=EN-US}}</ref> The lake levels are affected primarily by changes in regional meteorology and climatology. The outflows from Lakes Superior and Ontario are regulated, while the outflows of Michigan-Huron and Erie are not regulated at all. Ontario is the most tightly regulated, with its outflow controlled by the [[Moses-Saunders Power Dam]], which explains its consistent historical levels.<ref>{{cite news |last = Armstrong |first = Leslie |title = Great Lakes Water Levels Rebound Thanks to Prolonged Winter |newspaper = Toronto Star |date = August 14, 2014 }}</ref> ===Ice cover=== The annual ice coverage on the Great Lakes varies greatly from year to year due to weather patterns and long-term climate trends. Ice typically begins forming in December and reaches its peak in February or early March.<ref name="eonasa">{{cite web |title=New Lows for Great Lakes Ice Cover |url=https://earthobservatory.nasa.gov/images/152502/new-lows-for-great-lakes-ice-cover |website=Earth Observatory |publisher=NASA |access-date=5 April 2025 |language=en |date=29 February 2024}}</ref> The extent of ice cover can vary from as little as 10% to over 90% depending on winter severity. For example, during the particularly cold winter of 2013–2014, ice coverage peaked at over 92% across the five lakes, while in milder years like 2023–2024, coverage remained below 20%.<ref name="noaaice">{{cite web |title=Great Lakes Ice Cover |url=https://www.glerl.noaa.gov/data/ice/ |website=Great Lakes Environmental Research Laboratory |publisher=National Oceanic and Atmospheric Administration |access-date=5 April 2025 |language=EN-US}}</ref> Long-term data from the [[National Oceanic and Atmospheric Administration]]'s [[Great Lakes Environmental Research Laboratory]] (NOAA GLERL) indicate a general decline in maximum ice cover over the past few decades, aligning with broader patterns of warming in the region.<ref name="eonasa"/><ref>{{cite web |title=Great Lakes Ice |url=https://www.climatecentral.org/climate-matters/great-lakes-ice-2024 |date=7 February 2024 |website=Climate Central |access-date=5 April 2025 |language=en}}</ref> ==Etymology== [[File:1675ayer48Bernou.jpg|thumb|upright=1.1|1675 French map, published shortly before the voyage of ''[[Le Griffon]]''. Lake Michigan is named Lake Illinois (the name change is first recorded in 1681<ref name="Ducar may 1890 64">{{cite book |last1 = Dunbar |first1 = W.F. |url = https://books.google.com/books?id=zP-AEAAAQBAJ&pg=PT64 |title = Michigan: A History of the Wolverine State |last2 = May |first2 = G.S. |publisher = Wm. B. Eerdmans Publishing Company |year = 1995 |isbn = 978-1-4674-3517-8 |page = 64 |quote = By 1681, a map published in Paris, obviously based on this new information, shows the Mississippi River and the western shore of Lake Michigan. Earlier maps had called the lake Lac des Illinois; this was the first to call it Lac de Michigami, thus introducing an early variation of the future state's name. |access-date = September 7, 2022 }}</ref>), and Lake Ontario is named Lake Frontenac, after [[Louis de Buade de Frontenac|the then-governor of New France]].]] [[File:Great Lakes Superior, Michigan, Huron, and Erie.jpg|thumb|upright=1.1|Lakes Superior, Michigan, Huron, and Erie, photographed from the [[Sentinel-3B]] satellite in June 2022, Lake Ontario is not visible in this image.]] ;[[Lake Erie]] : From the [[Erie (tribe)|Erie tribe]], a shortened form of the [[Iroquoian]] word {{lang|iro|erielhonan}} 'long tail'.<ref name="Room2006">{{cite book |last = Room |first = A. |title = Placenames of the World: Origins And Meanings of the Names for 6,600 Countries, Cities, Territories, Natural Features And Historic Sites |url = https://books.google.com/books?id=M1JIPAN-eJ4C&pg=PA150 |year = 2006 |publisher = McFarland |isbn = 978-0-7864-2248-7 |page = 150 }}</ref> ;[[Lake Huron]] :Named for the inhabitants of the area, the [[Wyandot people|Wyandot]] (or "Hurons"), by the first French explorers .<ref name= "Room2006b">{{harvp|Room|2006|p=[https://books.google.com/books?id=M1JIPAN-eJ4C&pg=PA171 171]}}.</ref> The Wyandot originally referred to the lake by the name {{lang|wyn|karegnondi}}, a word which has been variously translated as "Freshwater Sea", "Lake of the Hurons", or simply "lake".<ref>{{cite book |url = https://books.google.com/books?id=U_14tuSMUBcC&q=Karegnondi&pg=PA221 |access-date = March 12, 2009 |title = Huron-Wendat |last1 = Sioui |first1 = Georges E. |others = [[Jane Brierley]] |publisher = UBC Press |isbn = 978-0-7748-0715-9 |year = 1999 }}</ref><ref name=fj6>{{cite news |last = Fonger |first = Ron |title = Genesee, Oakland counties adopt historic name for water group |url = http://blog.mlive.com/flintjournal/newsnow/2007/05/genesee_oakland_counties_adopt.html |access-date = December 6, 2011 |newspaper = The Flint Journal |date = May 3, 2007 }}</ref> ;[[Lake Michigan]] : From the [[Ojibwe language|Ojibwe]] word {{lang|oj|mishi-gami}} "great water" or "large lake".<ref name="WeilandWilsey2010">{{cite book |last1 = Weiland |first1 = Matt |last2 = Wilsey |first2 = Sean |title = State by State |url = https://books.google.com/books?id=BywaW1f4iQ4C&pg=PA226 |year = 2010 |publisher = HarperCollins |isbn = 978-0-06-204357-3 |page = 226 }}</ref> ;[[Lake Ontario]] : From the Wyandot word {{lang|wyn|ontarí'io}} "lake of shining waters".<ref name="Ylvisaker2004">{{cite book |last = Ylvisaker |first = Anne |title = Lake Ontario |url = https://archive.org/details/lakeontario0000ylvi |url-access = registration |year = 2004 |publisher = Capstone |isbn = 978-0-7368-2211-4 |page = [https://archive.org/details/lakeontario0000ylvi/page/12 12] }}</ref> ;[[Lake Superior]] : English translation of the French term {{lang|fr|lac supérieur}} "upper lake", referring to its position north of Lake Huron. The indigenous [[Ojibwe]] call it {{lang|oj|gichi-gami}} (from Ojibwe {{lang|oj|gichi}} "big, large, great"; {{lang|oj|gami}} "water, lake, sea"). Popularized in French-influenced transliteration as ''Gitchigumi'' as in [[Gordon Lightfoot]]'s 1976 story song "[[The Wreck of the Edmund Fitzgerald|The Wreck of the ''Edmund Fitzgerald'']]", or ''Gitchee Gumee'' as in [[Henry Wadsworth Longfellow]]'s 1855 epic poem, ''[[The Song of Hiawatha]]'').<ref name="dep" /> ==Statistics== The Great Lakes contain 21% of the world's surface fresh water: {{convert|5472|cumi|km3}}, or 6.0×10<sup>15</sup> U.S. gallons, that is 6 quadrillion U.S. gallons, (2.3×10<sup>16</sup> liters). The lakes contain about 84% of the surface freshwater of North America;<ref name="epa2">{{cite web |date = August 20, 2015 |title = The Great Lakes |url = http://www.epa.gov/greatlakes/basicinfo.html |publisher = Environmaal Protection Agency }}</ref> if the water were evenly distributed over the entire continent's land area, it would reach a depth of 5 feet (1.5 meters).<ref name="Grady2">{{cite book |last = Grady |first = Wayne |title = The Great Lakes |publisher = Greystone Books and [[David Suzuki Foundation]] |year = 2007 |isbn = 978-1-55365-197-0 |location = Vancouver |pages = 13, 21–26, 42–43 }}</ref> This is enough water to cover the 48 contiguous U.S. states to a uniform depth of {{convert|9.5|ft|m}}. Although the lakes contain a large percentage of the world's fresh water, the Great Lakes supply only a small portion of U.S. drinking water on a national basis.<ref name="CaytonSisson2006">{{cite book |last1 = Cayton |first1 = Andrew R.L. |last2 = Sisson |first2 = Richard |last3 = Zacher |first3 = Chris |title = The American Midwest: An Interpretive Encyclopedia |url = https://books.google.com/books?id=n3Xn7jMx1RYC&pg=PA161 |year = 2006 |publisher = [[Indiana University Press]] |isbn = 978-0-253-00349-2 |page = 161 }}</ref> The total [[surface area]] of the lakes is approximately {{convert|94250|sqmi|km2}}—nearly the same size as the United Kingdom, and larger than the U.S. states of [[New York (state)|New York]], [[New Jersey]], [[Connecticut]], [[Rhode Island]], [[Massachusetts]], [[Vermont]], and [[New Hampshire]] combined.<ref name="Taylor/Schechter/Wolfson">{{cite book |last1 = Taylor |first1 = William W. |last2 = Schechter |first2 = Michael G. |last3 = Wolfson |first3 = Lois G. |title = Globalization: Effects on Fisheries Resources |url = https://books.google.com/books?id=HT4Ck7ivIekC&pg=PA85 |publisher = Cambridge University Press |isbn = 978-1-139-46834-3 |page = 85 |year = 2007 }}</ref> The Great Lakes coast measures approximately {{convert|10500|mi|km}},<ref name="Grady" /> but [[Coastline paradox|the length of a coastline is impossible to measure exactly]]. Canada borders approximately {{convert|5200|mi|km}} of coastline, while the remaining {{convert|5300|mi|km}} are bordered by the United States. Michigan has the longest shoreline of the United States, bordering roughly {{convert|3288|mi|km}} of lakes, followed by Wisconsin ({{convert|820|mi|km}}), New York ({{convert|473|mi|km}}), and Ohio ({{convert|312|mi|km}}).<ref>{{cite web |title = Shorelines of the Great Lakes |url = http://www.michigan.gov/deq/0,4561,7-135-3313_3677-15959--,00.html |publisher = Michigan Department of Environmental Quality |access-date = July 8, 2014 |archive-url = https://web.archive.org/web/20140714132403/http://www.michigan.gov/deq/0%2C4561%2C7-135-3313_3677-15959--%2C00.html |archive-date = July 14, 2014 }}</ref> Traversing the shoreline of all the lakes would cover a distance roughly equivalent to travelling half-way around the world at the equator.<ref name="Grady">{{cite book |last = Grady |first = Wayne |title = The Great Lakes |publisher = Greystone Books and [[David Suzuki Foundation]] |location = Vancouver |year = 2007 |isbn = 978-1-55365-197-0 |pages = 13, 21–26, 42–43 }}</ref> A notable modern phenomenon is the formation of [[ice volcano]]es over the lakes during wintertime. Storm-generated waves carve the lakes' ice sheet and create conical mounds through the eruption of water and slush. The process is only well-documented in the Great Lakes, and has been credited with sparing the southern shorelines from worse rocky erosion.<ref name="Fahnestock19732">{{cite journal |last1 = Fahnestock |first1 = R. K. |last2 = Crowley |first2 = D. J. |last3 = Wilson |first3 = M. |last4 = Schneider |first4 = H. |date = 1973 |title = Ice Volcanoes of the Lake Erie Shore Near Dunkirk, New York, U.S.A. |url = https://www.igsoc.org/journal/12/64/igs_journal_vol12_issue064_pg93-99.pdf |archive-url = https://web.archive.org/web/20170828222836/https://www.igsoc.org/journal/12/64/igs_journal_vol12_issue064_pg93-99.pdf |archive-date = August 28, 2017 |url-status = live |journal = Journal of Glaciology |volume = 12 |issue = 64 |pages = 93–99 |doi = 10.3189/S0022143000022735 |access-date = May 25, 2018 |doi-access = free }}</ref> ==Geology== [[File:Glacial lakes.jpg|thumb|right|upright=1.5|A diagram of the formation of the Great Lakes]] [[File:Champlain Sea 1.png|thumb|upright=1.5|The [[Champlain Sea]] - The best evidence of this former sea is the vast clay plain deposited along the [[Ottawa River|Ottawa]] and [[St. Lawrence River|St. Lawrence Rivers]].<ref>Chapman, L.J. and D.F. Putnam. 1984. ''The Physiography of Southern Ontario''. Third edition. Ontario Geological Survey, Special Volume No.2. Government of Ontario, Toronto.</ref> ]] It has been estimated that the foundational geology that created the conditions shaping the present day upper Great Lakes was laid from 1.1 to 1.2 billion years ago,<ref name="Grady" /><ref name=Schmus>{{cite journal |last1 = Van Schmus |first1 = W.R. |last2 = Hinze |first2 = W. J. |title = The Midcontinent Rift System |journal = Annual Review of Earth and Planetary Sciences |volume = 13 |issue = 1 |pages = 345–83 |date = May 1985 |url = https://kuscholarworks.ku.edu/dspace/bitstream/1808/104/1/fac6cit13.pdf |doi = 10.1146/annurev.ea.13.050185.002021 |access-date = October 6, 2008 |hdl = 1808/104 |bibcode = 1985AREPS..13..345V |hdl-access = free }}</ref> when two previously fused [[tectonic plates]] split apart and created the [[Midcontinent Rift System|Midcontinent Rift]], which crossed the [[Great Lakes Tectonic Zone]]. A valley was formed providing a basin that eventually became modern day Lake Superior. When a second fault line, the [[Saint Lawrence rift system|Saint Lawrence rift]], formed approximately 570 million years ago,<ref name="Grady" /> the basis for Lakes Ontario and Erie was created, along with what would become the Saint Lawrence River. The Great Lakes are estimated to have been formed at the end of the [[Last Glacial Period]] (the [[Wisconsin glaciation]] ended 10,000 to 12,000 years ago), when the [[Laurentide Ice Sheet]] receded.<ref name="CordellLightfoot2008"/> The retreat of the ice sheet left behind a large amount of meltwater ([[Lake Algonquin]], [[Lake Chicago]], [[Glacial Lake Iroquois]], and [[Champlain Sea]]) that filled up the basins that the glaciers had carved, thus creating the Great Lakes as they are today.<ref>{{cite journal |last1 = Larson |first1 = Grahame |last2 = Schaetzl |first2 = R. |title = Origin and evolution of the Great Lakes |journal = Journal of Great Lakes Research |volume = 27 |issue = 4 |pages = 518–546 |year = 2001 |url = http://www.geo.msu.edu/schaetzl/PDFs/Larson-Great_lakes.pdf |doi = 10.1016/S0380-1330(01)70665-X |bibcode = 2001JGLR...27..518L |access-date = March 4, 2009 |archive-url = https://web.archive.org/web/20081031073825/http://www.geo.msu.edu/schaetzl/PDFs/Larson-Great_lakes.pdf |archive-date = October 31, 2008 }}</ref> Because of the uneven nature of glacier [[erosion]], some higher hills became Great Lakes islands. The Niagara Escarpment follows the contour of the Great Lakes between New York and Wisconsin. Land below the glaciers [[Post-glacial rebound|"rebounded"]] as it was uncovered.<ref>{{cite web |url = http://greatlakesecho.org/2009/06/08/lake-levels-report-weighs-great-lakes-basins-glacial-legacy/ |title = Lake levels report weighs Great Lakes basin's glacial legacy |publisher = Great Lakes Echo |date = June 8, 2009 |access-date = February 19, 2011 }}</ref> Since the glaciers covered some areas longer than others, this glacial rebound occurred at different rates. ==Climate== The Great Lakes have a humid continental climate, [[Köppen climate classification]] Dfa (in southern areas) and Dfb (in northern parts)<ref name="epa-atlas-ch2">{{cite web |url = http://www.epa.gov/greatlakes/atlas/glat-ch2.html |work = The Great Lakes: An Environmental Atlas and Resource Book |title = Natural Processes in the Great Lakes |access-date = November 27, 2011 |date = July 24, 2008 |publisher = Environmental Protection Agency }}</ref> with varying influences from air masses from other regions including dry, cold Arctic systems, mild Pacific air masses from the west, and warm, wet tropical systems from the south and the Gulf of Mexico.<ref name="king">{{cite web |url = https://www.sciencedaily.com/releases/2009/01/090113101122.htm |title = Great Lakes Water Levels Sensitive To Climate Change |access-date = April 14, 2010 |date = January 14, 2009 |website = Science Daily }}</ref> The lakes have a moderating effect on the climate; they can also increase precipitation totals and produce [[lake effect snow]]fall.<ref name="epa-atlas-ch2"/> ===Lake effect=== [[File:Lake effect snow wind direction bands1.png|thumb|upright=1.0|The location of common lake effect bands on the Great Lakes]] {{Main|Lake-effect snow#Great Lakes region}} {{More citations needed section|date=February 2021}} The Great Lakes can have an effect on regional weather called ''[[lake-effect snow]]'', which is sometimes very localized. Even late in winter, the lakes often have no icepack in the middle. The prevailing winds from the west pick up the air and moisture from the lake surface, which is slightly warmer in relation to the cold surface winds above. As the slightly warmer, moist air passes over the colder land surface, the moisture often produces concentrated, heavy snowfall that sets up in bands or "streamers". This is similar to the effect of warmer air dropping snow as it passes over mountain ranges. During freezing weather with high winds, the "[[snowbelt]]s" receive regular snow fall from this localized weather pattern, especially along the eastern shores of the lakes. Snowbelts are found in Wisconsin, Indiana, Michigan, Ohio, Pennsylvania, New York, and Ontario. Related to the lake effect is the regular occurrence of fog, particularly along the shorelines of the lakes. This is most noticeable along Lake Superior's shores. The lakes tend to moderate seasonal temperatures to some degree but not with as large an influence as do large oceans; they absorb heat and cool the air in summer, then slowly radiate that heat in autumn. They protect against frost during transitional weather and keep the summertime temperatures cooler than further inland. This effect can be very localized and overridden by offshore wind patterns. This temperature buffering produces areas known as "[[fruit belt]]s", where fruit can be produced that is typically grown much farther south. For instance, [[western Michigan]] has apple orchards, and cherry orchards are cultivated adjacent to the lake shore as far north as the [[Grand Traverse Bay]]. Near [[Collingwood, Ontario]], commercial fruit orchards, including a few wineries, exist near the shoreline of southern [[Nottawasaga Bay]]. The eastern shore of Lake Michigan and the southern shore of Lake Erie have many successful wineries because of the lakes' moderating effects, as do the large commercial fruit and wine growing areas of the Niagara Peninsula located between Lake Erie and Lake Ontario. A similar phenomenon allows wineries to flourish in the [[Finger Lakes]] region of New York, as well as in [[Prince Edward County, Ontario]], on Lake Ontario's northeast shore. The Great Lakes have been observed to help intensify storms, such as [[Hurricane Hazel]] in 1954, and the [[2011 Goderich, Ontario tornado]], which moved onshore as a tornadic [[waterspout]]. In 1996, a rare tropical or subtropical storm was observed forming in Lake Huron, dubbed the [[1996 Lake Huron cyclone]]. Rather large severe thunderstorms covering wide areas are well known in the Great Lakes during mid-summer; these [[Mesoscale convective complex]]es or MCCs<ref>{{cite web |url = http://www.weather.gov/glossary/index.php?letter=m |title = Glossary |publisher = National Weather Service }}</ref> can cause damage to wide swaths of forest and shatter glass in city buildings. These storms mainly occur during the night, and the systems sometimes have small embedded tornadoes, but more often straight-line winds accompanied by intense lightning. ==Ecology== {{stack|[[File:USGS image cropped.jpg|thumb|upright=1.5|Generalized schematic of Great Lakes waterline ecosystem]]}} Historically, the Great Lakes, in addition to their [[lake ecology]], were surrounded by various [[forest]] ecoregions (except in a relatively small area of southeast Lake Michigan where [[savanna]] or [[prairie]] occasionally intruded). Logging, urbanization, and agriculture uses have changed that relationship. In the early 21st century, Lake Superior's shores are 91% forested, Lake Huron 68%, Lake Ontario 49%, Lake Michigan 41%, and Lake Erie, where logging and urbanization has been most extensive, 21%. Some of these forests are second or third growth (i.e. they have been logged before, changing their composition). At least 13 wildlife species are documented as becoming extinct since the arrival of Europeans, and many more are threatened or endangered.<ref name=Grady/> Meanwhile, exotic and invasive species have also been introduced. ===Fauna=== {{see also|Great Lakes Areas of Concern#Invasive species|Category:Fauna of the Great Lakes region (North America)|Category:Fish of the Great Lakes|Asian carp in North America}} [[File:Lakesturgeon public U.S.Fish&Wildlife.jpg|thumb|[[Lake sturgeon]], the largest native fish in the Great Lakes and the subject of extensive commercial fishing in the 19th and 20th centuries is listed as a threatened species<ref>{{cite web |url = http://www.fws.gov/midwest/sturgeon/biology.htm |title = Great Lakes Lake Sturgeon Web Site |author = U.S. Fish and Wildlife Service }}</ref>]] While the organisms living on the bottom of shallow waters are similar to those found in smaller lakes, the deep waters contain organisms found only in deep, cold lakes of the northern latitudes. These include the delicate opossum shrimp (order [[mysida]]), the deepwater scud (a crustacean of the order [[amphipoda]]), two types of [[copepod]]s, and the [[deepwater sculpin]] (a spiny, large-headed fish).<ref>{{cite web |url = https://www.britannica.com/place/Great-Lakes |title = Great Lakes |last1 = Beeton |first1 = Alfred |website = Encyclopædia Britannica |access-date = January 31, 2016 }}</ref> The Great Lakes are an important source of [[fishing]]. Early European settlers were astounded by both the variety and quantity of fish; there were 150 different species in the Great Lakes.<ref name="Grady" /> Throughout history, fish populations were the early indicator of the condition of the Lakes and have remained one of the key indicators even in the current era of sophisticated analyses and measuring instruments. According to the bi-national (U.S. and Canadian) resource book, ''The Great Lakes: An Environmental Atlas and Resource Book'': "The largest Great Lakes fish harvests were recorded in 1889 and 1899 at some {{convert|67000|t|ton}} [147 million pounds]."<ref name="glearb">{{cite book |author = Anon |year = 1972 |title = The Great Lakes: An Environmental Atlas and Resource Book }} Bi-national (U.S. and Canadian) resource book.{{full citation needed|date=March 2024}}</ref> By 1801, the [[New York State Legislature|New York Legislature]] found it necessary to pass regulations curtailing obstructions to the natural migrations of [[Atlantic salmon]] from Lake Erie into their spawning channels. In the early 19th century, the government of [[Upper Canada]] found it necessary to introduce similar legislation prohibiting the use of weirs and nets at the mouths of Lake Ontario's tributaries. Other protective legislation was passed, but enforcement remained difficult.<ref name="Bogue2001m">{{cite book |first = Margaret Beattie |last = Bogue |title = Fishing the Great Lakes: An Environmental History, 1783–1933 |url = https://books.google.com/books?id=Pn7IlRl8DhsC&pg=PA180 |year = 2001 |publisher = Univ of Wisconsin Press |isbn = 978-0-299-16763-9 |page = 180 }}</ref> On both sides of the Canada–United States border, the proliferation of [[dam]]s and impoundments have multiplied, necessitating more regulatory efforts. Concerns by the mid-19th century included obstructions in the rivers which prevented salmon and [[lake sturgeon]] from reaching their spawning grounds. The Wisconsin Fisheries Commission noted a reduction of roughly 25% in general fish harvests by 1875. The states have removed dams from rivers where necessary.{{Clarify|date=September 2012}}<ref name="Commission">{{cite book |author = Atlantic States Marine Fisheries Commission |title = Special report ... of the Atlantic States Marine Fisheries Commission |publisher = The Commission |page = 23 }}</ref> Overfishing has been cited as a possible reason for a decrease in population of various [[freshwater whitefish|whitefish]], important because of their culinary desirability and, hence, economic consequence. Moreover, between 1879 and 1899, reported whitefish harvests declined from some 24.3 million pounds (11 million kg) to just over 9 million pounds (4 million kg).<ref name="MacdonaldService2009"/> By 1900, commercial fishermen on Lake Michigan were hauling in an average of 41 million pounds of fish annually.<ref name=js2/> By 1938, Wisconsin's commercial fishing operations were motorized and mechanized, generating jobs for more than 2,000 workers, and hauling 14 million pounds per year.<ref name=js2/> The population of giant freshwater mussels was eliminated as the mussels were harvested for use as buttons by early Great Lakes entrepreneurs.<ref name="MacdonaldService2009">{{cite book |editor1-last = Macdonald |editor1-first = David |editor2-last = Service |editor2-first = Katrina |title = Key Topics in Conservation Biology |url = https://books.google.com/books?id=flEwoquwpGUC&pg=PA188 |year = 2009 |publisher = John Wiley & Sons |isbn = 978-1-4443-0906-5 |page = 188 }}</ref> ''The Great Lakes: An Environmental Atlas and Resource Book'' (1972) notes: "Only pockets remain of the once large commercial fishery."<ref name="glearb" /> Water quality improvements realized during the 1970s and 1980s, combined with successful salmonid stocking programs, have enabled the growth of a large recreational fishery.<ref name="Agency1998">{{cite book |title = Great Minds?, Great Lakes! Don't Miss The Boat With Environmental Education |date = March 1997 |url = https://books.google.com/books?id=SlD57QnxOb0C&pg=PA7 |publisher = Environmental Protection Agency |page = 7 }}</ref> The last commercial fisherman left Milwaukee in 2011 because of overfishing and anthropogenic changes to the [[biosphere]].<ref name="js2">{{cite news |url = http://www.jsonline.com/news/wisconsin/127610953.html |title = The lake left me. It's gone |work = Milwaukee Journal Sentinel |date = August 13, 2011 }}</ref> [[File:Lake Superior North Shore(v2).jpg|thumb|Cliffs at [[Palisade Head]] on Lake Superior in Minnesota near Silver Bay.]] === Invasive species === Since the 19th century, an estimated 160 new species have found their way into the Great Lakes ecosystem; many have become invasive; the overseas ship ballast and ship hull parasitism are causing severe economic and ecological impacts.<ref>{{cite news |title=New EPA rules to target invasive species; Invaders have plagued Great Lakes for years |newspaper=The Blade|id = {{ProQuest|380761083}}}}</ref><ref name="ISEA">{{cite web |url = http://www.greatlakeseducation.org/about_isea/?id=204 |archive-url = https://web.archive.org/web/20130403134459/http://www.greatlakeseducation.org/about_isea/?id=204 |archive-date = April 3, 2013 |title = Our Threatened Great Lakes |access-date = November 30, 2007 |publisher = Inland Seas Education Association }}</ref> According to the Inland Seas Education Association, on average a new species enters the Great Lakes every eight months.<ref name="ISEA" /> Introductions into the Great Lakes include the [[zebra mussel]], which was first discovered in 1988, and [[quagga mussel]] in 1989. Since 2000, the invasive quagga mussel has smothered the bottom of Lake Michigan almost from shore to shore, and their numbers are estimated at 900 trillion.<ref name="js2"/> The [[Mollusca|mollusks]] are efficient filter feeders, competing with native mussels and reducing available food and spawning grounds for fish. In addition, the mussels may be a nuisance to industries by clogging pipes. The [[U.S. Fish and Wildlife Service]] estimated in 2007 that the economic impact of the zebra mussel could be about $5 billion over the next decade.<ref>{{cite web |url = http://www.glc.org/ans/ |title = Great Lakes Aquatic Nuisance Species |access-date = November 30, 2007 |publisher = Great Lakes Commission |date = March 27, 2007 |url-status = deviated |archive-url = https://web.archive.org/web/20070415222144/http://www.glc.org/ans/ |archive-date = April 15, 2007 }}</ref>{{Update inline|date=September 2021}} The state of Michigan has had to develop legislation and regulations to help protect against these invasive species. [[Aquatic invasive species regulations in Michigan]] have been put in place to combat the influx of species. [[File:Zebra mussel GLERL 3.jpg|thumb|upright|A zebra mussel–encrusted vector-averaging [[current meter]] from Lake Michigan.]] The [[alewife (fish)|alewife]] first entered the system west of Lake Ontario via 19th-century canals. By the 1960s, the small silver fish had become a familiar nuisance to beach goers across Lakes Michigan, Huron, and Erie. Periodic mass die-offs result in vast numbers of the fish washing up on shore; estimates by various governments have placed the percentage of Lake Michigan's biomass which was made up of alewives in the early 1960s as high as 90%. In the late 1960s, the various state and federal governments began stocking several species of salmonids, including the native lake trout as well as non-native [[Chinook salmon|chinook]] and [[Coho salmon|coho]] salmon; by the 1980s, alewife populations had dropped drastically.<ref>{{cite web |last = Smith |first = Paul |title = Gobies up, alewives down in Lake Michigan |url = http://www.jsonline.com/blogs/sports/40240287.html |publisher = Miwaukee Journal Sentinel |access-date = August 6, 2010 |date = February 24, 2009 |url-status = dead |archive-url = https://web.archive.org/web/20110605165415/http://www.jsonline.com/blogs/sports/40240287.html |archive-date = June 5, 2011 }}</ref> The [[ruffe]], a small [[percid]] fish from Eurasia, became the most abundant fish species in Lake Superior's [[Saint Louis River (Lake Superior tributary)|Saint Louis River]] within five years of its detection in 1986. Its range, which has expanded to Lake Huron, poses a significant threat to the lower lake fishery.<ref>{{cite web |title = Predicting Invasive Species in the Great Lakes |url = http://www.epa.gov/ord/sciencenews/scinews_great_lakes.htm |publisher = Environmental Protection Agency |archive-url = https://web.archive.org/web/20110205183050/http://www.epa.gov/ord/sciencenews/scinews_great_lakes.htm |archive-date = February 5, 2011 |url-status = dead }}</ref> Five years after first being observed in the St. Clair River, the [[round goby]] can now be found in all of the Great Lakes. The goby is considered undesirable for several reasons: it preys upon bottom-feeding fish, overruns optimal habitat, spawns multiple times a season, and can survive poor water quality conditions.<ref>{{cite web |last = Glassner-Shwayder |first = Katherine |title = Briefing Paper: Great Lakes Nonindigenous Invasive Species |url = http://www.glc.org/ans/pdf/briefpapercomplete.pdf |archive-url = https://web.archive.org/web/20051227060749/http://www.glc.org/ans/pdf/briefpapercomplete.pdf |archive-date = December 27, 2005 |publisher = Great Lakes Nonindigenous Invasive Species Workshop |access-date = August 6, 2010 |date = July 2000 }}</ref> The influx of parasitic [[lamprey]] populations after the development of the Erie Canal and the much later Welland Canal led to the two federal governments of the United States and Canada working on joint proposals to control it. By the mid-1950s, the [[lake trout]] populations of Lakes Michigan and Huron were reduced, with the lamprey deemed largely to blame. This led to the launch of the bi-national [[Great Lakes Fishery Commission]]. Several species of exotic [[Cladocera|water fleas]] have accidentally been introduced into the Great Lakes, such as the spiny waterflea, ''[[Bythotrephes longimanus]]'', and the fishhook waterflea, ''[[Cercopagis pengoi]]'', potentially having an effect on the [[zooplankton]] population. Several species of [[crayfish]] have also been introduced that may contend with native crayfish populations. More recently an electric fence has been set up across the Chicago Sanitary and Ship Canal in order to keep several species of invasive [[Asian carp]] out of the lakes. These fast-growing planktivorous fish have heavily colonized the Mississippi and Illinois river systems.<ref>{{cite web |title = Risk Assessment for Asian Carps in Canada |url = http://www.dfo-mpo.gc.ca/csas/Csas/DocREC/2004/RES2004_103_E.pdf |archive-url = https://web.archive.org/web/20060301092522/http://www.dfo-mpo.gc.ca/csas/Csas/DocREC/2004/RES2004_103_E.pdf |archive-date = March 1, 2006 |url-status = live |publisher = CSAS |date = 2004 }}</ref> Invasive species, particularly zebra and quagga mussels, may be at least partially responsible for the collapse of the deepwater demersal fish community in Lake Huron,<ref>{{cite journal |last1 = Riley |first1 = S.C. |year = 2008 |title = Deepwater demersal fish community collapse in Lake Huron |journal = Transactions of the American Fisheries Society |volume = 137 |issue = 6 |pages = 1879–90 |url = http://www.glsc.usgs.gov/_files/publications/1457.pdf |archive-url = https://web.archive.org/web/20130603123219/http://www.glsc.usgs.gov/_files/publications/1457.pdf |archive-date = June 3, 2013 |doi = 10.1577/T07-141.1 |last2 = Roseman |first2 = Edward F. |last3 = Nichols |first3 = S. Jerrine |last4 = O'Brien |first4 = Timothy P. |last5 = Kiley |first5 = Courtney S. |last6 = Schaeffer |first6 = Jeffrey S. |bibcode = 2008TrAFS.137.1879R }}</ref> as well as drastic unprecedented changes in the zooplankton community of the lake.<ref>{{cite journal |year = 2009 |title = Recent shifts in the crustacean zooplankton community of Lake Huron |doi = 10.1139/F09-036 |journal = Canadian Journal of Fisheries and Aquatic Sciences |volume = 66 |pages = 816–828 |last1 = Barbiero |first1 = Richard P. |last2 = Balcer |first2 = Mary |last3 = Rockwell |first3 = David C. |last4 = Tuchman |first4 = Marc L. |issue = 5 }}</ref> ===Microbiology=== Scientists understand that the micro-aquatic life of the lakes is abundant but know very little about some of the most plentiful microbes and their environmental effects in the Great Lakes. Although a drop of lake water may contain 1 million [[bacteria]] cells and 10 million [[viruses]], only since 2012 has there been a long-term study of the lakes' micro-organisms. Between 2012 and 2019 more than 160 new species have been discovered.<ref>{{cite news |url = https://www.chicagotribune.com/news/environment/ct-lake-michigan-microbes-20190705-ihsj56fbs5d4ngvyljsjsg5ao4-story.html |title = Minuscule microbes wield enormous power over the Great Lakes. But many species remain a mystery. |last = Briscoe |first = Tony |date = July 5, 2019 |work = Chicago Tribune |access-date = July 5, 2019 }}</ref> ===Flora=== {{category see also|Flora of the Great Lakes region (North America)}} Native habitats and ecoregions in the Great Lakes region include: * [[Alvar]] * [[Fen#Rich fens|Boreal rich fen]] (such as in [[Flora of Door County, Wisconsin#Plant communities unique to the area|Door County]]) * [[Eastern forest-boreal transition]] * [[Eastern Great Lakes lowland forests]] * [[Southern Great Lakes forests]] * [[Central forest-grasslands transition]] * [[Upper Midwest forest-savanna transition]] * [[Western Great Lakes forests]] * [[Central Canadian Shield forests]] * [[Laurentian Mixed Forest Province]] * [[Beech-maple forest]] * [[Habitats of the Indiana Dunes]] Plant lists include: * [[List of Michigan flowers]] * [[List of Minnesota wild flowers]] * [[List of Minnesota trees]] ==== Logging ==== [[Logging]] of the extensive forests in the Great Lakes region removed [[riparian zone|riparian]] and adjacent tree cover over rivers and streams, which provide shade, moderating water temperatures in fish spawning grounds. Removal of trees also destabilized the soil, with greater volumes washed into stream beds causing siltation of gravel beds, and more frequent flooding. Running cut logs down the tributary rivers into the Great Lakes also dislocated sediments. In 1884, the New York Fish Commission determined that the dumping of sawmill waste (chips and sawdust) had impacted fish populations.<ref name="Dempsey2004">{{cite book |last = Dempsey |first = Dave |title = On the Brink: The Great Lakes in the 21st Century |year = 2004 |publisher = Michigan State University Press |isbn = 978-0-87013-705-1 |page = [https://archive.org/details/onbrinkgreatlake0000demp/page/48 48] |url-access = registration |url = https://archive.org/details/onbrinkgreatlake0000demp/page/48 }}</ref> ===Pollution=== The first U.S. [[Clean Water Act]], passed by a Congressional override after being vetoed by U.S. President [[Richard Nixon]] in 1972, was a key piece of legislation,<ref>{{cite book |title = Evolution of the Great Lakes Water Quality Agreement |first1 = Paul |last1 = Muldoon |first2 = Lee |last2 = Botts |publisher = Michigan State University Press |year = 2005 }}</ref> along with the bi-national [[Great Lakes Water Quality Agreement]] signed by Canada and the U.S. A variety of steps taken to process industrial and municipal pollution discharges into the system greatly improved water quality by the 1980s, and Lake Erie in particular is significantly cleaner.<ref>{{cite web |url = http://www.michigan.gov/dnr/0%2C1607%2C7-153--145852--%2C00.html |archive-url = https://web.archive.org/web/20130830182201/http://www.michigan.gov/dnr/0%2C1607%2C7-153--145852--%2C00.html |archive-date = August 30, 2013 |title = Recovery of Lake Erie Walleye a Success Story |publisher = Michigan Department of Natural Resources |date = June 8, 2006 }}</ref> Discharge of toxic substances has been sharply reduced. Federal and state regulations control substances like [[Polychlorinated biphenyl|PCBs]]. The first of 43 "[[Great Lakes Areas of Concern]]" to be formally "de-listed" through successful cleanup was Ontario's Collingwood Harbour in 1994; Ontario's Severn Sound followed in 2003.<ref>{{cite web |work = binational.net |url = http://binational.net/ourgreatlakes/ourgreatlakes.pdf |archive-url = https://web.archive.org/web/20051227162745/http://binational.net/ourgreatlakes/ourgreatlakes.pdf |archive-date = December 27, 2005 |title = Our Great Lakes }}</ref> [[Presque Isle Bay]] in Pennsylvania is formally listed as in recovery, as is Ontario's Spanish Harbour. Dozens of other Areas of Concern have received partial cleanups such as the [[River Rouge (Michigan)|Rouge River (Michigan)]] and Waukegan Harbor (Illinois).<ref>{{cite web |url = http://www.epa.state.il.us/environmental-progress/v22/n1/waukegan-harbor.html |archive-url = https://web.archive.org/web/20141129040321/http://www.epa.state.il.us/environmental-progress/v22/n1/waukegan-harbor.html |archive-date = November 29, 2014 |title = Milestone in Waukegan Harbor PCB Cleanup |publisher = Illinois Environmental Protection Agency |date = Spring 1997 }}</ref> Phosphate detergents were historically a major source of nutrient to the Great Lakes algae blooms in particular in the warmer and shallower portions of the system such as Lake Erie, [[Saginaw Bay]], [[Green Bay (Lake Michigan)|Green Bay]], and the southernmost portion of Lake Michigan. By the mid-1980s, most jurisdictions bordering the Great Lakes had controlled phosphate detergents.<ref>{{cite web |last = Knud-Hansen |first = Chris |date = February 1994 |url = http://www.colorado.edu/conflict/full_text_search/AllCRCDocs/94-54.htm |title = Historical Perspective of the Phosphate Detergent Conflict |archive-url = https://web.archive.org/web/20100528155811/http://www.colorado.edu/conflict/full_text_search/AllCRCDocs/94-54.htm |archive-date = May 28, 2010 |id = Working Paper 94-54 |via = Colorado.edu |access-date = December 7, 2016 }}</ref> Blue-green algae, or [[cyanobacteria]] blooms,<ref>{{cite web |url = https://www.weather.gov/cle/LakeErieHAB |title = Lake Erie Harmful Algal Bloom |publisher = National Weather Service }}</ref> have been problematic on Lake Erie since 2011.<ref>{{cite news |url = https://www.nytimes.com/2013/03/15/science/earth/algae-blooms-threaten-lake-erie.html |title = Spring Rain, Then Foul Algae in Ailing Lake Erie |date = March 14, 2013 |work = The New York Times }}</ref> "Not enough is being done to stop fertilizer and phosphorus from getting into the lake and causing blooms," said Michael McKay, executive director of the Great Lakes Institute for Environmental Research (GLIER) at the [[University of Windsor]]. The largest Lake Erie bloom to date occurred in 2015, exceeding the severity index at 10.5 and in 2011 at a 10.<ref name="windsorstar.com">{{cite news |url = https://windsorstar.com/news/local-news/large-lake-erie-algal-bloom-nearing-colchester-tested-for-toxicity |archive-url = https://web.archive.org/web/20190811140408/https://windsorstar.com/news/local-news/large-lake-erie-algal-bloom-nearing-colchester-tested-for-toxicity |archive-date = August 11, 2019 |title = Large Lake Erie algal bloom nearing Colchester tested for toxicity |work = Windsor Star |date = August 7, 2019 |first = Sharon |last = Hill |access-date = August 12, 2019 }}</ref> In early August 2019, satellite images depicted a bloom stretching up to 1,300 square kilometers on Lake Erie, with the heaviest concentration near [[Toledo, Ohio]]. A large bloom does not necessarily mean the cyanobacteria ... will produce toxins", said Michael McKay, of the University of Windsor. Water quality testing was underway in August 2019.<ref>{{cite news |url = http://www.uwindsor.ca/dailynews/2019-08-07/uwindsor-researchers-test-waters-harmful-algae-bloom |archive-url = https://web.archive.org/web/20190812145246/http://www.uwindsor.ca/dailynews/2019-08-07/uwindsor-researchers-test-waters-harmful-algae-bloom |archive-date = August 12, 2019 |title = UWindsor researchers test the waters for harmful algae bloom }}</ref><ref name="windsorstar.com" /> ==== Mercury ==== Until 1970, [[Mercury (element)|mercury]] was not listed as a harmful chemical, according to the United States Federal Water Quality Administration. In the 21st century, mercury has become more apparent in water tests. Mercury compounds have been used in paper mills to prevent slime from forming during their production, and chemical companies have used mercury to separate chlorine from brine solutions. Studies conducted by the [[United States Environmental Protection Agency|Environmental Protection Agency]] have shown that when the mercury comes in contact with many of the bacteria and compounds in the fresh water, it forms the compound [[Methylmercury|methyl mercury]], which has a much greater impact on human health than elemental mercury due to a higher propensity for absorption. This form of mercury is not detrimental to a majority of fish types, but is very detrimental to people and other wildlife animals who consume the fish. Mercury has been known for health related problems such as birth defects in humans and animals, and the near extinction of eagles in the Great Lakes region.<ref>{{cite web |url = http://www.idph.state.il.us/envhealth/factsheets/mercuryspills.htm |title = Mercury Spills |publisher = Idph.state.il.us |access-date = February 19, 2011 }}</ref> ==== Sewage ==== The amount of raw sewage dumped into the waters was the primary focus of both the first Great Lakes Water Quality Agreement and federal laws passed in both countries during the 1970s. Implementation of secondary treatment of municipal sewage by major cities greatly reduced the routine discharge of untreated sewage during the 1970s and 1980s.<ref>{{cite web |url = http://ohioseagrant.osu.edu/_documents/publications/FS/FS-046%20Lake%20Erie%20water%20quality%20past%20present%20future.pdf |archive-url = https://web.archive.org/web/20060902100228/http://ohioseagrant.osu.edu/_documents/publications/FS/FS-046%20Lake%20Erie%20water%20quality%20past%20present%20future.pdf |archive-date = September 2, 2006 |url-status = live |title = Lake Erie Water Quality Past Present and Future |access-date = December 4, 2013 }}</ref> The [[International Joint Commission]] in 2009 summarized the change: "Since the early 1970s, the level of treatment to reduce pollution from waste water discharges to the Great Lakes has improved considerably. This is a result of significant expenditures to date on both infrastructure and technology, and robust regulatory systems that have proven to be, on the whole, quite effective."<ref name="ijc.org">{{Cite book |url = http://www.ijc.org/php/publications/pdf/ID1631.pdf |archive-url = https://web.archive.org/web/20100924165650/http://ijc.org/php/publications/pdf/ID1631.pdf |archive-date = September 24, 2010 |url-status = live |title = 14th Biennial Report on Great Lakes Water Quality }}</ref> The commission reported that all urban sewage treatment systems on the U.S. side of the lakes had implemented secondary treatment, as had all on the Canadian side except for five small systems.{{Citation needed|date=September 2012}} Though contrary to federal laws in both countries, those treatment system upgrades have not yet eliminated [[combined sewer]] overflow events.{{citation needed|date=December 2013}} This describes when older sewerage systems, which combine storm water with sewage into single sewers heading to the treatment plant, are temporarily overwhelmed by heavy rainstorms. Local sewage treatment authorities then must release untreated effluent, a mix of rainwater and sewage, into local water bodies. While enormous public investments such as the [[Deep Tunnel]] projects in Chicago and [[Milwaukee]] have greatly reduced the frequency and volume of these events, they have not been eliminated. The number of such overflow events in Ontario, for example, is flat according to the International Joint Commission.<ref name="ijc.org"/> Reports about this issue on the U.S. side highlight five large municipal systems (those of Detroit, Cleveland, Buffalo, Milwaukee and [[Gary, Indiana|Gary]]) as being the largest current periodic sources of untreated discharges into the Great Lakes.<ref>{{cite web |url = http://healthylakes.org/press-releases/new-report-solving-region%E2%80%99s-sewage-crisis-will-create-jobs-restore-great-lakes/ |title = New Report: Solving Region's Sewage Crisis Will Create Jobs, Restore Great Lakes |archive-url = https://web.archive.org/web/20141129035802/http://healthylakes.org/press-releases/new-report-solving-region%E2%80%99s-sewage-crisis-will-create-jobs-restore-great-lakes/ |archive-date = November 29, 2014 |work = Healthylakes.org |date = August 9, 2010 |access-date = December 7, 2016 }}</ref> [[File:Diatoms_through_the_microscope.jpg|thumb|upright=1.3|Diatoms of different sizes seen through the microscope. These minuscule [[phytoplankton]] are encased within a [[silicate]] [[cell wall]].]] The fish of the Great Lakes have anti-depressant drugs meant for humans in their brains, which has caused concerns. The number of American adults who take anti-depressant drugs rose from 7.7% of all American adults in 1999–2002 to 12.7% in 2011–2014. As the anti-depressant drugs pass out of human bodies and through sanitation systems into the Great Lakes, this has resulted in fish in the Great Lakes with twenty times the level of anti-depressants in their brains than what is in the water, leading to the fish being exceedingly happy and hence less risk-averse, to the extent of damaging the fish populations.<ref name="The Economist">{{cite news |title = Antidepressants are finding their way into fish brains |url = https://www.economist.com/united-states/2018/02/08/antidepressants-are-finding-their-way-into-fish-brains |access-date = January 15, 2023 |newspaper = The Economist |date = February 8, 2018 }}</ref> ==== Plastic ==== Researchers have found that more than {{convert|22|e6lb}} of plastic end up in the Great Lakes each year.<ref name=agl>{{cite web |title = Great Lakes Plastic Pollution |url = https://greatlakes.org/great-lakes-plastic-pollution-fighting-for-plastic-free-water/ |access-date = April 21, 2023 |publisher = Alliance for the Great Lakes |language = en-US }}</ref> Plastics in the water break up into very small particles known as [[microplastics]]. Microplastics can also come from synthetic clothing washed down our drains.<ref name=varsity>{{cite news |first = Nicole |last = Szabo |date = September 5, 2021 |title = U of T researchers discover microplastics in all samples of Great Lakes fish |url = https://thevarsity.ca/2021/09/04/ontario-freshwater-microplastics-lakes/ |access-date = April 21, 2023 |website = The Varsity |language = en-US }}</ref> [[Plastic waste]] found in the lakes include [[single-use plastic]]s, plastics used in packaging, takeout containers as well as [[Plastic pellet pollution|pre-production pellets]] produced by [[plastics industry]].<ref>{{cite news |first1 = Inayat |last1 = Singh |first2 = Alice |last2 = Hopton |date = October 1, 2021 |title = Industrial plastic is spilling into Great Lakes, and no one's regulating it, experts warn |publisher = CBC News |url = https://www.cbc.ca/news/science/plastics-waste-great-lakes-water-1.6185621 |access-date = April 21, 2023 }}</ref> High concentrations of microplastics were discovered in 100 percent of the fish that were studied by researchers from the Rochman Lab. About {{convert|50|e6lb}} of fish is harvested each year from Great Lakes which has raised concerns on how this might affect human health.<ref name=varsity/> Microscopic pieces of plastic have also been found in drinking water coming from Great Lakes. It is estimated that nearly 40 million people in the region rely on drinking water from the Great Lakes.<ref name=agl/> A number of self-operating floating devices called Seabin, were put in the Great Lakes to capture plastic trash as part of the Great Lakes Plastic Cleanup project. The project captured 74,000 pieces of trash using this technology between 2020 and 2021; however, it does not claim to catch up with {{convert|22|e6lb}} of plastic that ends up in Great Lakes every year. The production, consumption, and throwing away of plastics seems to remain the core of Great Lakes trash problem.<ref>{{Cite web |last = Redelmeier |first = Rebecca |date = October 14, 2022 |title = How a fleet of robots could help solve the Great Lakes plastic pollution problem |url = https://www.theverge.com/2022/10/14/23401381/great-lakes-plastic-pollution-cleanup-tech-robots |access-date = April 21, 2023 |website = The Verge |language = en-US }}</ref> === Impacts of climate change on algae === Algae such as [[diatom]]s, along with other [[phytoplankton]], are [[photosynthetic]] [[primary producers]] supporting the [[food web]] of the Great Lakes,<ref>{{cite web |url = https://www.glc.org/lakes/ |title = About the Lakes |publisher = Great Lakes Commission }}</ref> and have been [[Effects of global warming|affected by global warming]].<ref>{{cite web |url = https://greatlakesecho.org/2019/02/13/monitoring-algal-blooms-in-the-great-lakes-basin/ |title = Monitoring algal blooms in the Great Lakes Basin |first = Kurt |last = Williams |date = February 13, 2019 |website = Great Lakes Echo }}</ref> The changes in the size or in the function of the primary producers may have a direct or an indirect impact on the food web. Photosynthesis carried out by diatoms constitutes about one fifth of the total photosynthesis.{{Where|date=February 2021}} By taking {{CO2 |link=yes}} out of the water to photosynthesize, diatoms help to stabilize the [[pH]] of the water, as {{CO2}} would react with water to produce [[Carbon dioxide#In aqueous solution|carbonic acid]]. :{{chem2|CO2 + H2O <-> HCO3- + H+}} Diatoms acquire [[Inorganic compound|inorganic]] carbon through passive diffusion of {{CO2}} and [[Bicarbonate|{{chem2|HCO3-}}]], and use [[carbonic anhydrase]] mediated active transport to speed up this process.<ref>{{cite journal |last1 =Burkhardt |first1 = Steffen |last2 = Amoroso |first2 = Gabi |last3 = Riebesell |first3 = Ulf |last4 = Sültemeyer |first4 = Dieter |date = September 2001 |title = CO<sub>2</sub> and {{chem|HCO|3|-}} uptake in marine diatoms acclimated to different CO<sub>2</sub> concentrations |journal =Limnology and Oceanography |volume = 46 |issue = 6 |pages = 1378–1391 |doi=10.4319/lo.2001.46.6.1378}}</ref> Large diatoms require more carbon uptake than smaller diatoms.<ref name=":0">{{cite journal |first1 = Brian N. |last1 = Popp |first2 = Edward A. |last2 = Laws |first3 = Robert R. |last3 = Bidigare |first4 = John E. |last4 = Dore |first5 = Kristi L. |last5 = Hanson |first6 = Stuart G. |last6 = Wakeham |journal = Geochimica et Cosmochimica Acta |year = 998 |title = Effect of Phytoplankton Cell Geometry on Carbon Isotopic Fractionation |volume = 62 |issue = |pages = 69–77 |doi = 10.1016/S0016-7037(97)00333-5 }}</ref> There is a [[Correlation and dependence|positive correlation]] between the surface area and the chlorophyll concentration of diatom cells.<ref>{{cite journal |last = Durbin |first = E.G. |year = 1977 |title = Studies on the Autecology of the Marine Diatom ''Thalassiosira nordenskioeldii'' II. The Influence of Cell Size on Growth Rate, and Carbon, Nitrogen, Chlorophyll ''a'' and Silica Content |journal = Journal of Phycology |volume = 13 |issue = 2 |pages = 150–155 |doi = 10.1111/j.1529-8817.1977.tb02904.x |bibcode = 1977JPcgy..13..150D }}</ref> ==History== [[File:Le-griffon.jpg|thumb|upright=1.3|A woodcut of ''Le Griffon'']] Several Native American populations ([[Paleo-indians]]) inhabited the region around 10,000 BC, after the end of the Wisconsin glaciation.<ref>{{cite journal |last1 = O'Shea |first1 = John |last2 = Meadows |first2 = Guy |date = June 23, 2009 |title = Evidence for early hunters beneath the Great Lakes |journal = Proceedings of the National Academy of Sciences |volume = 106 |issue = 25 |pages = 10120–10123 |quote = The earliest human occupation in the upper Great Lakes is associated with the regional fluted-point Paleoindian tradition, which conventionally ends with the drop in water level to the Lake Stanley stage |pmc = 2700903 |pmid = 19506245 |doi = 10.1073/pnas.0902785106 |bibcode = 2009PNAS..10610120O |doi-access = free }}</ref><ref>{{cite web |url = https://www.wisconsinhistory.org/Records/Article/CS3584 |title = Ancient Land and First Peoples |publisher = Wisconsin Historical Society |date = February 6, 2013 |access-date = February 13, 2020 }}</ref> The peoples of the Great Lakes traded from around 1000 AD, as copper nuggets have been extracted from the region and fashioned into ornaments and weapons in the mounds of Southern Ohio. The [[Rush–Bagot Treaty]] signed in 1818, after the [[War of 1812]] and the later [[Treaty of Washington (1871)|Treaty of Washington]] eventually led to a complete disarmament of naval vessels in the Great Lakes. Nonetheless, both nations maintained coast guard vessels in the Great Lakes. The brigantine {{ship||Le Griffon}}, which was commissioned by [[René-Robert Cavelier, Sieur de La Salle]], was built at Cayuga Creek, near the southern end of the [[Niagara River]], and became the first known sailing ship to travel the upper Great Lakes on August 7, 1679.<ref name="Woodford1991">{{cite book |last = Woodford |first = Arthur M. |title = Charting the Inland Seas: A History of the U.S. Lake Survey |url = https://books.google.com/books?id=PjcUrS0vZGcC&pg=PA4 |year = 1991 |publisher = Wayne State University Press |isbn = 978-0-8143-2499-8 |page = 4 }}</ref> During settlement, the Great Lakes and its rivers were the only practical means of moving people and freight. Barges from middle North America were able to reach the Atlantic Ocean from the Great Lakes when the [[First Welland Canal|Welland Canal]] opened in 1824 and the later Erie Canal opened in 1825.<ref name="Bernstein2010oi">{{cite book |last = Bernstein |first = Peter L. |title = Wedding of the Waters: The Erie Canal and the Making of a Great Nation |url = https://books.google.com/books?id=94edBai9RDoC&pg=PA349 |year = 2010 |publisher = W.W. Norton |isbn = 978-0-393-32795-3 |page = 349 }}</ref> By 1848, with the opening of the [[Illinois and Michigan Canal]] at Chicago, direct access to the Mississippi River was possible from the lakes.<ref name="Danzer2011re">{{cite book |last = Danzer |first = Gerald A. |title = Illinois: A History in Pictures |url = https://books.google.com/books?id=VulYOvM4f48C&pg=PA90 |year = 2011 |publisher = [[University of Illinois Press]] |isbn = 978-0-252-03288-2 |page = 90 }}</ref> With these two canals an all-inland water route was provided between New York City and [[New Orleans]]. The main business of many of the passenger lines in the 19th century was transporting immigrants. Many of the larger cities owe their existence to their position on the lakes as a freight destination as well as for being a magnet for immigrants. After railroads and surface roads developed, the freight and passenger businesses dwindled and, except for ferries and a few foreign cruise ships, have now vanished. The immigration routes still have an effect today. Immigrants often formed their own communities, and some areas have a pronounced ethnicity, such as Dutch, German, Polish, Finnish, and many others. Since many immigrants settled for a time in New England before moving westward, many areas on the U.S. side of the Great Lakes also have a New England feel, especially in home styles and accent. [[File:Eastland Christopher Columbus leaving Chicago ca1912.jpg|thumb|upright=1.3|The passenger ship {{SS|Eastland}} (foreground) leaving Chicago, c. 1909]] Since general freight these days is transported by railroads and trucks, domestic ships mostly move bulk cargoes, such as [[iron ore]], [[coal]] and [[limestone]] for the [[steel]] industry. The domestic bulk freight developed because of the nearby mines. It was more economical to transport the ingredients for steel to centralized plants rather than to make steel on the spot. Grain exports are also a major cargo on the lakes. In the 19th and early 20th centuries, iron and other ores such as copper were shipped south on (downbound ships), and supplies, food, and coal were shipped north (upbound). Because of the location of the coal fields in Pennsylvania and [[West Virginia]], and the general northeast track of the [[Appalachian Mountains]], railroads naturally developed shipping routes that went due north to ports such as [[Erie, Pennsylvania]] and [[Ashtabula, Ohio]]. Because the lake maritime community largely developed independently, it has some distinctive vocabulary. Ships, no matter the size, are called "boats". When the sailing ships gave way to steamships, they were called "steamboats"—the same term used on the Mississippi. The ships also have a distinctive design; ships that primarily trade on the lakes are known as "[[Lake freighter|lakers]]". Foreign boats are known as "salties". One of the more common sights on the lakes has been since about 1950 the {{convert|1000|by|105|ft|adj=on}}, {{convert|78850|LT|metric ton|adj=on}} self-unloader. This is a laker with a conveyor belt system that can unload itself by swinging a crane over the side.<ref>{{cite web |last = Wharton |first = George |title = Great Lakes Fleet Page Vessel Feature – Burns Harbor |url = http://www.boatnerd.com/pictures/fleet/burnsharbor.htm |work = Boatnerd |access-date = August 6, 2010 }}</ref> Today, the Great Lakes fleet is much smaller in numbers than it once was because of the increased use of overland freight, and a few larger ships replacing many small ones. During World War II, the risk of submarine attacks against coastal training facilities motivated the [[United States Navy]] to operate two aircraft carriers on the Great Lakes, {{USS|Sable|IX-81|6}} and {{USS|Wolverine|IX-64|6}}. Both served as training ships to qualify naval aviators in carrier landing and takeoff.<ref name="Gonzalez2008o">{{cite book |last = Gonzalez |first = Therese |title = Great Lakes Naval Training Station |url = https://books.google.com/books?id=CbX3WAOPaHIC&pg=PA71 |year = 2008 |publisher = Arcadia Publishing |isbn = 978-0-7385-5193-7 |page = 71 }}</ref> [[Lake Champlain]] briefly became the sixth Great Lake of the United States on March 6, 1998, when [[Bill Clinton|President Clinton]] signed Senate Bill 927. This bill, which reauthorized the [[National Sea Grant Program]], contained a line declaring Lake Champlain to be a Great Lake. Not coincidentally, this status allows neighboring states to apply for additional federal research and education funds allocated to these national resources. Following a small uproar, the Senate voted to revoke the designation on March 24 (although New York and Vermont universities would continue to receive funds to monitor and study the lake).<ref>{{cite news |last = Seelye |first = Katharine Q. |url = https://www.nytimes.com/1998/03/25/us/lakes-are-born-great-5-sniff-so-upstart-is-ousted.html |title = Lakes Are Born Great, 5 Sniff, So Upstart Is Ousted |work = The New York Times |date = March 25, 1998 |access-date = November 14, 2013 }}</ref> Alan B. McCullough has written that the fishing industry of the Great Lakes got its start "on the American side of Lake Ontario in [[Chaumont Bay]], near the [[Maumee River]] on Lake Erie, and on the [[Detroit River]] at about the time of the War of 1812". Although the region was sparsely populated until the 1830s, so there was not much local demand and transporting fish was prohibitively costly, there were economic and infrastructure developments that were promising for the future of the fishing industry going into the 1830s. Particularly, the 1825 opening of the Erie Canal and the Welland Canal a few years later. The fishing industry expanded particularly in the waters associated with the [[fur trade]] that connect Lake Erie and Lake Huron. In fact, two major suppliers of fish in the 1830s were the fur trading companies [[Hudson's Bay Company]] and the [[American Fur Company]].<ref name="bogue3">{{cite book |last1 = Bogue |first1 = Magaret Beattie |title = Fishing the Great Lakes: An Environmental History, 1783–1933 |date = 2000 |publisher = The University of Wisconsin Press |pages = 29–31 }}</ref> The catch from these waters was sent to the growing market for [[salted fish]] in Detroit, where merchants involved in the fur trade had already gained some experience handling salted fish. One such merchant was [[John P. Clark]], a [[shipbuilder]] and merchant who began selling fish in the area of [[Manitowoc, Wisconsin]] where whitefish was abundant. Another operation cropped up in [[Georgian Bay]], Canadian waters plentiful with trout as well as whitefish. In 1831, Alexander MacGregor from [[Goderich, Ontario]] found whitefish and [[herring]] in abundant supply around the Fishing Islands. A contemporary account by [[Methodist]] missionary John Evans describes the fish as resembling a "bright cloud moving rapidly through the water".<ref name="bogue3" /> From 1844 through 1857, [[palace steamer]]s carried passengers and cargo around the Great Lakes.<ref name="Thompson19912">{{cite book |last = Thompson |first = Mark L. |url = https://books.google.com/books?id=KRLZDXIEWCsC&pg=PA210 |title = Steamboats & Sailors of the Great Lakes |publisher = Wayne State University Press |year = 1991 |isbn = 978-0-8143-2359-5 |page = 210 }}</ref> In the first half of the 20th century [[Great Lakes passenger steamers|large luxurious passenger steamers]] sailed the lakes in opulence.<ref name="KoutskyKoutsky20062">{{cite book |last1 = Strand |first1 = Kathryn Koutsky |url = https://books.google.com/books?id=Z_zmhDMlWrIC&pg=PA34 |title = Minnesota Vacation Days: An Illustrated History |last2 = Koutsky |first2 = Linda |publisher = Minnesota Historical Society |year = 2006 |isbn = 978-0-87351-526-9 |page = 34 }}</ref> The [[Detroit and Cleveland Navigation Company]] had several vessels at the time and hired workers from all walks of life to help operate these vessels.<ref>{{cite book |url = https://books.google.com/books?id=ABuzV44QuUkC&pg=PA30 |title = Toast of the Town: The Life and Times of Sunnie Wilson |publisher = Wayne State University Press |year = 2005 |isbn = 978-0-8143-2696-1 |page = 30 }}</ref> Several ferries currently operate on the Great Lakes to carry passengers to various islands. As of 2007, four car ferry services cross the Great Lakes, two on Lake Michigan: a steamer from [[Ludington, Michigan]], to Manitowoc, Wisconsin, and a high speed catamaran from Milwaukee to [[Muskegon, Michigan]], one on Lake Erie: a boat from [[Kingsville, Ontario]], or [[Leamington, Ontario]], to [[Pelee, Ontario|Pelee Island, Ontario]], then onto [[Sandusky, Ohio]], and one on Lake Huron: the MS ''Chi-Cheemaun''<ref>{{cite web |title = MS Chi-Cheemaun About Us |url = http://www.ontarioferries.com/ontarioferries/english/aboutus.html |archive-url = https://web.archive.org/web/20141129135305/http://www.ontarioferries.com/ontarioferries/english/aboutus.html |archive-date = November 29, 2014 |access-date = June 29, 2014 |publisher = Ontario Ferries }}</ref> runs between Tobermory and South Baymouth, Manitoulin Island, operated by the Owen Sound Transportation Company. [[HSC Virgen de Coromoto|An international ferry]] across Lake Ontario from [[Rochester, New York]], to [[Toronto]] ran during 2004 and 2005 but is no longer in operation. === Shipwrecks === {{See also|List of shipwrecks in the Great Lakes|Great Storms of the North American Great Lakes|Great Lakes Storm of 1913}} The large size of the Great Lakes increases the risk of water travel; [[storm]]s and [[reef]]s are common threats. The lakes are prone to sudden and severe storms, in particular in the autumn, from late October until early December. Hundreds of ships have met their end on the lakes. The greatest concentration of shipwrecks lies near [[Thunder Bay (Michigan)]], beneath Lake Huron, near the point where eastbound and westbound shipping lanes converge. The Lake Superior shipwreck coast from [[Grand Marais, Michigan]], to [[Whitefish Point]] became known as the "[[Graveyard of the Great Lakes]]". More vessels have been lost in the Whitefish Point area than any other part of Lake Superior.<ref>{{cite book |last = Stonehouse |first = Frederick |orig-date = 1985 |year = 1998 |title = Lake Superior's Shipwreck Coast |page = 267 |publisher = Avery Color Studios |location = Gwinn, Michigan |isbn = 0-932212-43-3 }}</ref> The [[Whitefish Point Underwater Preserve]] serves as an underwater museum to protect the many shipwrecks in this area. The first ship to sink in Lake Michigan was ''Le Griffon'', also the first ship to sail the Great Lakes. Caught in a 1679 storm while trading furs between Green Bay and Michilimacinac, she was lost with all hands aboard.<ref name="ledger0411042">{{cite news |url = http://www.ledgersentinel.com/article.asp?a=3448 |last = Matile |first = Roger |date = April 11, 2004 |title = Has a famed Great Lakes mystery been solved? |archive-url = https://web.archive.org/web/20160101014314/http://www.ledgersentinel.com/article.asp?a=3448 |archive-date = January 1, 2016 |newspaper = Ledger-Sentinel |location = Oswego, Illinois }}</ref> Its wreck may have been found in 2004,<ref>{{cite news |url = http://www.canada.com/technology/France+claims+historic+Great+Lakes+wreck/1299362/story.html |title = France claims historic Great Lakes wreck |first = Randy |last = Boswell |publisher = Canwest News Service |date = February 17, 2009 }}</ref> but a wreck subsequently discovered in a different location was also claimed in 2014 to be ''Le Griffon''.<ref>{{cite news |url = https://news.yahoo.com/explorer-says-griffin-shipwreck-may-found-014242419.html |title = Explorer says Griffin shipwreck may be found |work = Yahoo! News |agency = Associated Press |date = June 24, 2014 }}</ref> The largest and last major freighter wrecked on the lakes was the {{SS|Edmund Fitzgerald}}, which sank on November 10, 1975, just over {{convert|17|mi|km|sigfig=1}} offshore from Whitefish Point on Lake Superior. The largest loss of life in a shipwreck out on the lakes may have been that of {{PS|Lady Elgin||2}}, wrecked in 1860 with the loss of around 400 lives on Lake Michigan. In an incident at a Chicago dock in 1915, the {{SS|Eastland}} rolled over while loading passengers, killing 844. In 2007, the [[Great Lakes Shipwreck Museum|Great Lakes Shipwreck Historical Society]] announced that it had found the wreckage of ''Cyprus'', a {{convert|420|ft|m|adj=on}} long, century-old [[ore]] carrier. ''Cyprus'' sank during a Lake Superior storm on October 11, 1907, during its second voyage while hauling iron ore from [[Superior, Wisconsin]], to Buffalo, New York. The entire crew of 23 drowned, except one, Charles Pitz, who floated on a life raft for almost seven hours.<ref>{{cite news |date = September 10, 2007 |title = Century-old shipwreck discovered |publisher = NBC News |agency = Associated Press |url = https://www.nbcnews.com/id/wbna20679934 |access-date = December 3, 2007 }}</ref> In 2008, [[Deep sea diving|deep sea divers]] in Lake Ontario found the wreck of the 1780 [[Royal Navy]] warship {{HMS|Ontario|1780|6}} in what has been described as an "archaeological miracle".<ref>{{cite news |date = June 14, 2008 |title = Divers find 1780 British warship |publisher = BBC News |url = http://news.bbc.co.uk/1/hi/uk/7454578.stm |access-date = June 15, 2008 }}</ref> There are no plans to raise her as the site is being treated as a war grave. In 2010, ''[[L.R. Doty]]'' was found in Lake Michigan by an exploration diving team led by dive boat Captain Jitka Hanakova from her boat ''Molly V''.<ref>{{cite news |date = June 24, 2010 |title = L.R. Doty, ship that sank in Lake Michigan 112 years ago, found largely intact near Milwaukee |newspaper = [[Star Tribune]] |location = Minneapolis |url = http://www.startribune.com/local/97084514.html |access-date = June 28, 2010 |archive-url = https://web.archive.org/web/20100627120140/http://www.startribune.com/local/97084514.html |archive-date = June 27, 2010 }}</ref> The ship sank in October 1898, probably attempting to rescue a small schooner, ''Olive Jeanette'', during a terrible storm. Still missing are the two last warships to sink in the Great Lakes, the French minesweepers [[French minesweepers Inkerman and Cerisoles|''Inkerman'' and ''Cerisoles'']], which vanished in Lake Superior during a blizzard in 1918. 78 people died, making it the largest loss of life in Lake Superior and the greatest unexplained loss of life in the Great Lakes. The [[Wisconsin Shipwreck Coast National Marine Sanctuary]] was established in 2021 in the waters of Lake Michigan off Wisconsin. It is the site of a large number of historically significant [[shipwreck]]s.<ref>{{cite web |url = https://www.federalregister.gov/documents/2021/06/23/2021-12846/wisconsin-shipwreck-coast-national-marine-sanctuary-designation-final-regulations |title = Wisconsin Shipwreck Coast National Marine Sanctuary Designation; Final Regulations |author = National Oceanographic and Atmospheric Administration |work = Federal Register |date = June 23, 2021 |access-date = June 29, 2021 }}</ref><ref>{{cite web |url = https://sanctuaries.noaa.gov/media/docs/wisconsin-shipwreck-coast-national-marine-sanctuary.pdf |title = National Marine Sanctuaries media document: Wisconsin Shipwreck Coast National Marine Sanctuary |access-date = June 29, 2021 }}</ref><ref>{{cite web |url = https://www.noaa.gov/news-release/noaa-designates-new-national-marine-sanctuary-in-wisconsin-s-lake-michigan |work = NOAA News |title = NOAA designates new national marine sanctuary in Wisconsin's Lake Michigan |date = June 22, 2021 |access-date = June 29, 2021 }}</ref> ==Economy== [[File: Great Lakes and St. Lawrence Seaway map 1959.png|upright=2.4|center|thumb|Map of the Great Lakes, [[Great Lakes Waterway]], [[St. Lawrence Seaway]] depicting the entire length.]] [[File:Overview of the Great Lakes from orbit.jpg|thumb|upright=1.3|Photograph of, closest to farthest, Lakes Ontario, Erie and Huron (North is to the right) plus the [[Finger Lakes]] of upstate New York, near Lake Ontario, June 14, 2012, taken aboard the [[International Space Station]], with lake names added]] ===Shipping=== Except when the water is frozen during winter, more than 100 lake freighters operate continuously on the Great Lakes,<ref name="clui">{{Cite web |url = http://www.clui.org/section/united-divide-a-linear-portrait-usacanada-border-3 |title = Chapter 4: The Watery Boundary |website = United Divide: A Linear Portrait of the USA/Canada Border |publisher = The Center for Land Use Interpretation |date = Winter 2015 }}</ref> which remain a major [[water transport]] corridor for bulk goods. The [[Great Lakes Waterway]] connects all the lakes; the shorter [[Saint Lawrence Seaway]] connects the lakes to the Atlantic Ocean. Some lake freighters are too large to use the Seaway and operate only on the Waterway and lakes. In 2002, 162 million net [[ton]]s of dry bulk cargo were moved on the Lakes. This was, in order of volume: iron ore, grain and [[potash]].<ref>{{cite web |url = http://www.greatlakesports.org/industry-overview/cargoes/ |title = Great Lake Seaway Cargoes – American Great Lakes Ports Association |website = www.greatlakesports.org |access-date = May 18, 2017 |archive-date = May 9, 2021 |archive-url = https://web.archive.org/web/20210509142250/https://www.greatlakesports.org/industry-overview/cargoes/ |url-status = dead }}</ref> The iron ore and much of the stone and coal are used in the steel industry. There is also some shipping of liquid and containerized cargo. Major ports on the Great Lakes include [[Twin Ports|Duluth-Superior]], Chicago, Detroit, Cleveland, Twin Harbors, [[Hamilton-Oshawa Port Authority|Hamilton]] and [[Thunder Bay Port Authority|Thunder Bay]]. ===Recreation=== [[File:Marina Fest.jpg|thumb|upright=1.3|[[Escanaba, Michigan|Escanaba]]'s Ludington Park in Michigan]] Tourism and recreation are major industries on the Great Lakes.<ref name="GroverKrantzberg2012">{{cite book |last1 = Grover |first1 = Velma I. |last2 = Krantzberg |first2 = Gail |title = Great Lakes: Lessons in Participatory Governance |url = https://books.google.com/books?id=P-HMjx9tgoEC&pg=PA334 |year = 2012 |publisher = CRC Press |isbn = 978-1-57808-769-3 |page = 334 }}</ref> A few small cruise ships operate on the Great Lakes including some [[sailing|sailing ships]]. Sport fishing, commercial fishing, and Native American fishing represent a U.S.$4 billion a year industry with [[salmon]], [[Coregonus|whitefish]], [[smelt (fish)|smelt]], lake trout, [[Bass (fish)|bass]] and [[walleye]] being major catches. Many other [[List of water sports|water sports]] are practiced on the lakes such as [[yachting]], [[sea kayak]]ing, [[Recreational diving|diving]], [[kitesurfing]], [[powerboat]]ing, and [[lake surfing]]. The [[Great Lakes Circle Tour]] is a designated scenic road system connecting all of the Great Lakes and the Saint Lawrence River.<ref>{{cite web |url = http://www.great-lakes.net/tourism/circletour/ |title = Great Lakes Circle Tour |publisher = Great-lakes.net |date = July 5, 2005 |access-date = February 19, 2011 |archive-url = https://web.archive.org/web/20100725204133/http://www.great-lakes.net/tourism/circletour/ |archive-date = July 25, 2010 }}</ref> ==Legislation== [[File:Great Lakes 1.PNG|thumb|upright=1.3|Various national, state, provincial, and municipal jurisdictions govern the Great Lakes]] In 1872, a treaty gave access to the St. Lawrence River to the United States and access to Lake Michigan to the [[Canadian Confederation|Dominion of Canada]].<ref>{{cite book |url = https://books.google.com/books?id=nyGjHG1PaUEC&q=false&pg=PA227 |title = Iron Ore Transport on the Great Lakes: The Development of a Delivery System to Feed American Industry |last = Bowlus |first = W. Bruce |publisher = McFarland |year = 2010 |isbn = 978-0-7864-8655-7 |page = 227, n.35 }}</ref> The International Joint Commission was established in 1909 to help prevent and resolve disputes relating to the use and quality of boundary waters, and to advise Canada and the United States on questions related to water resources. Concerns over diversion of Lake water are of concern to both Americans and Canadians. Some water is diverted through the Chicago River to operate the Illinois Waterway, but the flow is limited by treaty. Possible schemes for [[bottled water]] plants and diversion to dry regions of the continent raise concerns. Under the U.S. "Water Resources Development Act of 1986",<ref>{{cite web |url = http://www.dnr.state.oh.us/tabid/4053/default.aspx |title = Federal Statute on Great Lakes. Water Diversions. Water Resources Development Act |access-date = October 29, 2007 |archive-url = https://web.archive.org/web/20071029172833/http://www.dnr.state.oh.us/tabid/4053/default.aspx |archive-date = October 29, 2007 |publisher = Ohio Department of Natural Resources }}</ref><ref>United States. Water Resources Development Act of 1986. {{uspl|99|662}}, approved November 17, 1986. {{USC|42|1962d-20}}</ref> diversion of water from the Great Lakes Basin requires the approval of all eight Great Lakes governors through the [[Great Lakes Commission]], which rarely occurs. International treaties regulate large diversions. In 1998, the Canadian company Nova Group won approval from the Province of Ontario to withdraw {{convert|158000000|U.S.gal|m3}} of Lake Superior water annually to ship by tanker to Asian countries. Public outcry forced the company to abandon the plan before it began. Since that time, the eight Great Lakes Governors and the Premiers of Ontario and Quebec have negotiated the Great Lakes-Saint Lawrence River Basin Sustainable Water Resources Agreement<ref>{{cite web |url = http://www.cglg.org/projects/water/docs/12-13-05/Great_Lakes-St_Lawrence_River_Basin_Sustainable_Water_Resources_Agreement.pdf |archive-url = https://web.archive.org/web/20060308043903/http://www.cglg.org/projects/water/docs/12-13-05/Great_Lakes-St_Lawrence_River_Basin_Sustainable_Water_Resources_Agreement.pdf |archive-date = March 8, 2006 |url-status = live |title = Great Lakes—St. Lawrence River Basin Sustainable Water Resources Agreement |access-date = February 19, 2011 }}</ref> and the Great Lakes-St. Lawrence River Basin Water Resources Compact<ref>{{cite web |url = http://www.cglg.org/projects/water/docs/12-13-05/Great_Lakes-St_Lawrence_River_Basin_Water_Resources_Compact.pdf |title = Agreement. Great Lakes-St Lawrence River Basin Water Resources |publisher = cglg.org |date = December 13, 2005 }}</ref> that would prevent most future diversion proposals and all long-distance ones. The agreements strengthen protection against abusive water withdrawal practices within the Great Lakes basin. On December 13, 2005, the Governors and Premiers signed these two agreements, the first of which is between all ten jurisdictions. It is somewhat more detailed and protective, though its legal strength has not yet been tested in court. The second, the [[Great Lakes Compact]], has been approved by the state legislatures of all eight states that border the Great Lakes as well as the U.S. Congress, and was signed into law by President [[George W. Bush]] on October 3, 2008.<ref>{{cite web |url = http://www.greatlakes.org/Page.aspx?pid=526 |title = Great Lakes Compact |publisher = Alliance for the Great Lakes }}</ref> The Great Lakes Restoration Initiative,<ref>United States. Federal Water Pollution Control Act (commonly the [[Clean Water Act]]), as amended by the Water Quality Act of 1987 ({{uspl|100|4}}, approved February 4, 1987), and the Consolidated Appropriations Act, 2016 ({{uspl|114|113}}, approved December 18, 2015). {{USC|33|1268}}</ref><ref>{{cite web |url = http://greatlakesrestoration.us/ |title = Great Lakes Restoration Initiative home page |archive-url = https://web.archive.org/web/20160206222143/http://greatlakesrestoration.us/ |archive-date = February 6, 2016 }}</ref> was funded at $475 million in the U.S. federal government's Fiscal Year 2011 budget, and $300 million in the Fiscal Year 2012 budget. Through the program a coalition of federal agencies is making grants to local and state entities for toxics cleanups, wetlands and coastline restoration projects, and invasive species-related projects. The Great Lakes Restoration Initiative Act of 2019 passed as {{uspl|116|294}} on January 5, 2021, reauthorizing the program through Fiscal Year 2026. ==See also== {{portal|Lakes}} {{div col}} * [[Alliance for the Great Lakes]] * [[Boundary Waters Treaty of 1909]] * [[Eastern Continental Divide]] * [[Great Lakes census statistical areas]] * [[Great Lakes Protection Fund]] * [[Great Lakes WATER Institute]] * [[Great Recycling and Northern Development Canal]] * [[Lake Ontario National Marine Sanctuary]] * [[List of municipalities on the Great Lakes]] * [[Michigan Islands National Wildlife Refuge]] * [[Thunder Bay National Marine Sanctuary]] * [[Wisconsin Shipwreck Coast National Marine Sanctuary]] * [[Populated islands of the Great Lakes]] * [[Sixty Years' War]] for control of the Great Lakes{{div col end}} ==References== {{Reflist|refs= <!-- <ref name="GLBathEr">[https://www.ncei.noaa.gov/products/great-lakes-bathymetry National Geophysical Data Center] (1999). Bathymetry of Lake Erie and Lake Saint Clair. National Geophysical Data Center, NOAA. {{doi|10.7289/V5KS6PHK}}</ref> <ref name="GLBathHur"> [https://www.ncei.noaa.gov/products/great-lakes-bathymetry National Geophysical Data Center] (1999). Bathymetry of Lake Huron. National Geophysical Data Center, NOAA. {{doi|10.7289/V5G15XS5}}</ref> <ref name="GLBathMich">[https://www.ncei.noaa.gov/products/great-lakes-bathymetry National Geophysical Data Center] (1999). Bathymetry of Lake Michigan. National Geophysical Data Center, NOAA. {{doi|10.7289/V5B85627}}</ref> <ref name="GLBathOnt">[https://www.ncei.noaa.gov/products/great-lakes-bathymetry National Geophysical Data Center] (1999). Bathymetry of Lake Ontario. National Geophysical Data Center, NOAA. {{doi|10.7289/V56H4FBH}}</ref> <ref name="GLBathSup">[https://www.ncei.noaa.gov/products/great-lakes-bathymetry National Geophysical Data Center] (1999). Bathymetry of Lake Superior. National Geophysical Data Center, NOAA.<br />(the general reference to NGDC because this lake was never published, compilation of Great Lakes Bathymetry at NGDC has been suspended).</ref> <ref name="GLOBE">National Geophysical Data Center (1999). Global Land One-kilometer Base Elevation (GLOBE) v. 1. Hastings, D. and P.K. Dunbar. National Geophysical Data Center, NOAA. {{doi|10.7289/V52R3PMS}}</ref> -->}} ==Further reading== {{refbegin}} * {{cite book |first = Peter |last = Annin |title = The Great Lakes Water Wars |url = https://books.google.com/books?id=VzMeZHaLP_gC&pg=PP1 |year = 2006 |publisher = Island Press |isbn = 978-1-61091-077-4 }} * {{cite book |last = Beltran |first = R. |display-authors = etal |url = http://www.epa.gov/glnpo/atlas/glat-ch2.html |title = The Great Lakes: An Environmental Atlas and Resource Book |publisher = Environmental Protection Agency |year = 1995 |isbn = 0-662-23441-3 }} * {{cite book |last1 = Coon |first1 = W.F. |first2 = R.A. |last2 = Sheets |url = http://pubs.usgs.gov/sir/2006/5180/ |title = Estimate of Ground Water in Storage in the Great Lakes Basin |series = Scientific Investigations Report 2006-5180 |publisher = United States Geological Survey |year = 2006 }} * {{cite book |title = The Death and Life of the Great Lakes |last = Egan |first = Dan |isbn = 978-0-393-35555-0 |publisher = W.W. Norton & Company |year = 2018 }} * {{cite book |last = Holling |first = Holling Clancy |year = 2019 |orig-date = 1941 |title = [[Paddle-to-the-Sea]] |location = Boston |publisher = Houghton Mifflin |isbn = 978-0-395-15082-5 }} (an illustrated children's book about the Great Lakes and their environment). * {{cite book |first = Helen |last = Hornbeck Tanner |title = Atlas of Great Lakes Indian History |url = https://archive.org/details/nby_e78_g7_a87_1987 |year = 1987 |publisher = [[University of Oklahoma Press]] |isbn = 978-0-8061-2056-0 }} * {{cite book |last = Riley |first = John L. |year = 2013 |title = The Once and Future Great Lakes Country: An Ecological History |publisher = [[McGill-Queen's University Press]] }} (traces environmental change in the region since the last ice age.) {{refend}} ==External links== {{wikivoyage}} {{Commons category|Great Lakes}} * Eric W. Morse 1968, ''[http://parkscanadahistory.com/publications/fur-trade-canoe-routes.pdf Fur Trade Canoe Routes of Canada /Then and Now]'', pp 121 * {{Cite NIE|wstitle=Great Lakes|short=x}} * {{Cite PSM|wstitle=How the Great Lakes Were Built|volume=49|month-and-year=June 1896}} * [http://www.ec.gc.ca/grandslacs-greatlakes/default.asp?lang=En&n=70283230-1 Great Lakes website] of the [[Environment Canada|Canadian Department of the Environment]] * [http://www.epa.gov/glnpo/ Great Lakes website] of the [[United States Environmental Protection Agency]] * [http://binational.net/ Binational website of USEPA and Environment Canada for Great Lakes Water Quality] {{Webarchive|url=http://arquivo.pt/wayback/20160518092315/http://binational.net/ |date=May 18, 2016 }} * [http://www.glerl.noaa.gov/ Great Lakes Environmental Research Laboratory website] (an arm of the American [[National Oceanic and Atmospheric Administration]]) * [https://web.archive.org/web/20060126235433/http://www.great-lakes.net/ Great Lakes Information Network], sponsored by the [http://www.glc.org/ Great Lakes Commission], an official American [[interstate compact]] agency. * [http://greatlakesecho.org/ Great Lakes Echo, a publication covering Great Lakes environmental issues] * [http://www.MaritimeHistoryOfTheGreatLakes.ca/ ''Maritime History of the Great Lakes''], digital library covering Great Lakes history. ===Dynamically updated data=== * [http://www.coastwatch.msu.edu/ Surface temperatures] {{Webarchive|url=https://web.archive.org/web/20080511230142/http://www.coastwatch.msu.edu/ |date=May 11, 2008 }} * [http://www.glerl.noaa.gov/data/wlevels/ Water levels] * [http://www.glerl.noaa.gov/res/glcfs/currents/glcfs-currents-avg.html Currents] {{Webarchive|url=https://web.archive.org/web/20170707093015/https://www.glerl.noaa.gov//res/glcfs/currents/glcfs-currents-avg.html |date=July 7, 2017 }} * [http://ais.boatnerd.com/ Ship locations] * [https://web.archive.org/web/20160304093823/http://www.waterlevels.gc.ca/C%26A/NetworkMeans2014.pdf Water levels since 1918] {{greatlakes}} {{Authority control}} [[Category:Great Lakes| ]] [[Category:Central Canada]] [[Category:Eastern Canada]] [[Category:Great Lakes region (U.S.)]] [[Category:Lake groups]]
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