Editing Coast Mountains

{{short description|Mountain range in Canada and the United States}}
{{About|the mountain ranges of the west coast of North America|other uses|Coast Range (disambiguation){{!}}Coast Range}}
{{Infobox mountain
| name = Coast Mountains
| other_name = Coast Range
| photo = ISS046-E-3699.JPG
| photo_caption = Coast Mountains taken from the [[International Space Station]] from outer space, the [[Canadian Rockies]] can be seen at the right
| country = [[Canada]] and [[United States]]
| region = [[Alaska]], [[British Columbia]] and [[Yukon]]
| length_km = 1600
| length_orientation = north–south
| width_km = 300
| width_orientation = east–west
| parent = [[Pacific Coast Ranges]]
| area_km2 = 336962
| highest = [[Mount Waddington]]
| highest_location = [[British Columbia]]
| elevation_m = 4019
| coordinates = {{coord|51|22|30|N|125|15|30|W|type:mountain_region:CA|format=dms|display=inline}}
| range_coordinates = {{coord|54|N|128|W|type:mountain_region:CA|format=dms|display=inline,title}}
| map_image = Rannikkovuoret sijainti.png
| map_caption = Locator map of the Coast Mountains
}}
The '''Coast Mountains''' ({{langx|fr|La chaîne Côtière}}) are a major [[mountain range]] in the [[Pacific Coast Ranges]] of western [[North America]], extending from southwestern [[Yukon]] through the [[Alaska Panhandle]] and virtually all of the [[British Columbia Coast|Coast of British Columbia]] south to the [[Fraser River]].<ref>[https://archive.today/20140426052451/http://apps.gov.bc.ca/pub/bcgnws/names/21188.html BC Names/GeoBC entry "Coast Mountains"]</ref> The mountain range's name derives from its proximity to the sea coast, and it is often referred to as the '''Coast Range'''.<ref name="SD">{{cite web|publisher=Government of British Columbia|url=http://www.ilmb.gov.bc.ca/bcgn-bin/bcg10?name=21188 |title=BCGNIS Query Results|access-date=2008-11-13}} {{Dead link|date=September 2010|bot=H3llBot}}</ref> The range includes volcanic and non-volcanic mountains and the extensive [[ice field]]s of the [[Pacific Ranges|Pacific]] and [[Boundary Ranges]], and the northern end of the [[volcano|volcanic]] system known as the [[Cascade Volcanoes]]. The Coast Mountains are part of a larger mountain system called the [[Pacific Coast Ranges]] or the Pacific Mountain System, which includes the [[Cascade Range]], the [[Insular Mountains]], the [[Olympic Mountains]], the [[Oregon Coast Range]], the [[California Coast Ranges]], the [[Saint Elias Mountains]] and the [[Chugach Mountains]]. The Coast Mountains are also part of the [[American Cordillera]]{{emdash}}a Spanish term for an extensive chain of mountain ranges{{emdash}}that consists of an almost continuous sequence of mountain ranges that form the western backbone of [[North America]], [[Central America]], [[South America]] and [[Antarctica]].

The Coast Mountains are approximately {{convert|1600|km|-2}} long and average {{convert|300|km}} in width.<ref name="SD"/> The range's southern and southeastern boundaries are surrounded by the [[Fraser River]] and the [[Interior Plateau]] while its far northwestern edge is delimited by the [[Kelsall River|Kelsall]] and [[Tatshenshini River]]s at the north end of the Alaska Panhandle, beyond which are the Saint Elias Mountains, and by [[Champagne, Yukon|Champagne Pass]] in the [[Yukon Territory]].<ref>[http://www.empr.gov.bc.ca/Mining/Geoscience/PublicationsCatalogue/BulletinInformation/BulletinsAfter1940/Documents/Bull48-txt.pdf S. Holland, ''Landforms of British Columbia'', Province of British Columbia, 1976, pp 41] {{webarchive |url=https://web.archive.org/web/20160304185301/http://www.empr.gov.bc.ca/Mining/Geoscience/PublicationsCatalogue/BulletinInformation/BulletinsAfter1940/Documents/Bull48-txt.pdf |date=March 4, 2016 }}</ref><ref>[http://www.empr.gov.bc.ca/Mining/Geoscience/PublicationsCatalogue/BulletinInformation/BulletinsAfter1940/Documents/Bull48-physiographic-map.pdf map from ''Bulletin 48: Landforms of British Columbia''] {{webarchive |url=https://web.archive.org/web/20160303182612/http://www.empr.gov.bc.ca/Mining/Geoscience/PublicationsCatalogue/BulletinInformation/BulletinsAfter1940/Documents/Bull48-physiographic-map.pdf |date=March 3, 2016 }}</ref> Covered in dense [[temperate rainforest]] on its western exposures, the range rises to heavily [[glacier|glaciated]] peaks, including the largest temperate-latitude ice fields in the world. On its eastern flanks, the range tapers to the dry Interior Plateau and the subarctic [[Taiga|boreal forests]] of the [[Skeena Mountains]] and [[Stikine Plateau]].

The Coast Mountains are part of the [[Pacific Ring of Fire]]{{emdash}}the ring of volcanoes and associated mountains around the [[Pacific Ocean]]{{emdash}}and contain some of British Columbia's highest mountains. [[Mount Waddington]] is the highest mountain of the Coast Mountains and the highest that lies entirely within British Columbia, located northeast of the head of [[Knight Inlet]] with an elevation of {{convert|4019|m}}.<ref>{{cite web|publisher=Government of British Columbia|url=https://apps.gov.bc.ca/pub/bcgnws/names/38556.html |archive-url=https://archive.today/20070815193807/http://ilmbwww.gov.bc.ca/bcgn-bin/bcg10?name=38556 |url-status=live |archive-date=2007-08-15 |title=BCGNIS Query Results|access-date=2008-11-13}}</ref>

==Geography==
The Coast Mountains consists of three subdivisions known as the [[Pacific Ranges]], the [[Kitimat Ranges]], and the [[Boundary Ranges]]. The Pacific Ranges are the southernmost subdivision of the Coast Mountains, extending from the lower stretches of the [[Fraser River]] to [[Bella Coola, British Columbia|Bella Coola]]. Included in this subdivision is four of the five major coastal icecaps in the southern Coast Mountains. These are the largest temperate-latitude icecaps in the world and fuel a number of major [[river]]s. Other than logging and a large ski resort at the [[resort town]] of [[Whistler, British Columbia|Whistler]], most of the land in the range is completely undeveloped. [[Mount Waddington]], the highest mountain of the Coast Mountains, lies in the [[Waddington Range]] of the Pacific Ranges.

Just north of the Pacific Ranges lies the central subdivision known as the Kitimat Ranges. This subdivision extends from the [[Bella Coola River]] and [[Burke Channel]] in the south to the [[Nass River]] in the north.

[[File:A040, Coast Mountains, Alaska Panhandle, USA, 2002.jpg|thumb|left|[[Kakuhan Range]] between Juneau and Haines, Alaska]]
The third and northernmost subdivision of the Coast Mountains is the [[Boundary Ranges]], extending from the Nass River in the south to the [[Kelsall River]] in the north. It is also the largest subdivision of the Coast Mountains, spanning the British Columbia-Alaska border and northwards into [[Yukon]] flanking the west side of the [[Yukon River]] drainage as far as [[Champagne Pass]], north of which being the [[Yukon Ranges]]. The Boundary Ranges include several large icefields, including the [[Juneau Icefield]] between [[Juneau, Alaska]] and [[Atlin Lake]] in British Columbia, and the [[Stikine Icecap]], which lies between the lower [[Stikine River]] and the [[Whiting River]].

Because the Coast Mountains are just east of the [[Pacific Ocean]], they have a profound effect on British Columbia's climate by forcing moisture-laden air off the Pacific Ocean to rise, dropping heavy rainfalls on the western slopes where lush forests exist.<ref name="SD"/> This precipitation is among the heaviest in North America.<ref name="SD"/> The eastern slopes are relatively dry and less steep and protect the [[British Columbia Interior]] from the Pacific weather systems, resulting in dry warm summers and dry cold winters.<ref name="SD"/>

Beyond the eastern slopes is a {{convert|154635|km2|mi2|abbr=on}} plateau occupying the southern and central portions of British Columbia called the [[Interior Plateau]]. Included within the Interior Plateau is a coalescing series of layered [[flood basalt]] lava flows. These sequences of fluid [[volcanic rock]] cover about {{convert|25000|km2|mi2|abbr=on}} of the Interior Plateau and have a volume of about {{convert|1800|km3|mi3|abbr=on}}, forming a large [[volcanic plateau]] constructed atop of the Interior Plateau. North of the Interior Plateau on the range's northeastern slopes lies a huge mountainous area known by geographers as the [[Interior Mountains]], which includes the neighbouring [[Skeena Mountains|Skeena]], [[Cassiar Mountains|Cassiar]] and [[Hazelton Mountains]].

==Geology==
===Origins and growth===
The Coast Mountains consist of deformed [[igneous rock|igneous]] and [[metamorphic rock|metamorphosed]] structurally complex pre-[[Tertiary]] rocks. These originated in diverse locations around the globe: the area is built of several different [[terrane]]s of different ages with a broad range of tectonic origins. In addition, [[oceanic crust]] under the [[Pacific Ocean]] is being [[subduction|subducted]] at the southern portion of the range to form a north–south line of volcanoes called the [[Garibaldi Volcanic Belt]], a northern extension of the [[Cascade Volcanoes]] in the northwestern [[United States]], and contains the most explosive young volcanoes in Canada. Further north the northwesterly structural trend of the Coast Mountains lies partly in a large continental [[rift]] responsible for the creation of several volcanoes. These volcanoes form part of the [[Northern Cordilleran Volcanic Province]], the most volcanically active area in Canada.

====Insular and Omineca Arc eruptive periods====
[[Image:Insular Omineca arcs.png|thumb|right|Bridge River Ocean between North America and the Insular Islands]]
{{Main|Insular Islands|Omineca Arc}}
The first event began 130 million years ago when a group of active volcanic islands approached a pre-existing [[continental margin]] and coastline of North America.<ref name="AD">{{cite web|publisher=Burke Museum of Natural History and Culture|url=http://www.washington.edu/burkemuseum/geo_history_wa/Coast%20Range%20Episode.htm |title=The Coast Range Episode (115 to 57 million years ago)|access-date=2008-04-09}}</ref> These volcanic islands, known as the [[Insular Islands]] by geoscientists, were formed on a pre-existing [[plate tectonics|tectonic plate]] called the [[Insular Plate]] by [[subduction]] of the former [[Farallon Plate]] to the west during the early [[Paleozoic]] era.<ref name="AD"/> This subduction zone records another subduction zone to the east under an ancient [[ocean basin]] between the Insular Islands and the former continental margin of North America called the [[Bridge River Ocean]].<ref name="AD"/> This arrangement of two parallel subduction zones is unusual in that very few twin subduction zones exist on Earth; the [[Philippine Mobile Belt]] off the southeastern coast of [[Asia]] is an example of a modern twin subduction zone.<ref name="AD"/> As the Insular Plate drew closer to the pre-existing continental margin by ongoing subduction under the Bridge River Ocean, the Insular Islands drew closer to the former continental margin and coastline of western North America, supporting a pre-existing volcanic arc on the former continental margin of North America called the [[Omineca Arc]].<ref name="AD"/> As the [[North American Plate]] drifted west and the Insular Plate drifted east to the old continental margin of western North America, the Bridge River Ocean eventually closed by ongoing subduction under the Bridge River Ocean.<ref name="AD"/> This subduction zone eventually jammed and shut down completely 115 million years ago, ending the Omineca Arc and the Insular Islands collided, forming the [[Insular Belt]].<ref name="AD"/> Compression resulting from this collision crushed, fractured and [[fold (geology)|folded]] rocks along the old continental margin.<ref name="AD"/> The Insular Belt then welded onto the pre-existing continental margin by magma that eventually cooled to create a large mass of [[igneous rock]], creating a new continental margin.<ref name="AD"/> This large mass of igneous rock is the largest [[granite]] outcropping in North America.<ref name="AD"/>

[[Image:Coast_Range_Arc_tectonics.png|thumb|left|Plate tectonics of the Coast Range Arc about 100 million years ago]]

====Coast Range Arc eruptive period====
{{Main|Coast Range Arc}}
The final event began when the [[Farallon Plate]] continued to subduct under the new continental margin after the Insular Plate and Insular Islands collided with the old continental margin, supporting a new continental volcanic arc called the [[Coast Range Arc]] about 100 million years ago during the [[Late Cretaceous]] period.<ref name="KO">{{cite book | last = Stowell | first = Harold H. |author2=McClelland William C. | title = Tectonics of the Coast Mountains, Southeastern Alaska and British Columbia |publisher = [[Geological Society of America]] |page = 101 |url = https://books.google.com/books?id=5SgAthT0MuAC&q=tectonics+of+the+Coast+Mountains+southeastern+Alaska+and+British+Columbia |isbn = 0-8137-2343-4 |access-date =2008-09-04| date = 2000-01-01 }}</ref> Magma rising from the Farallon Plate under the new continental margin ascended through the newly accreted Insular Belt, injecting huge quantities of granite into older igneous rocks of the Insular Belt.<ref name="AD"/> At the surface, new volcanoes were built along the continental margin.<ref name="AD"/> Named after the Coast Mountains, the basement of this arc was likely Early Cretaceous and [[Late Jurassic]] intrusions from the Insular Islands.<ref name="KO"/>

[[Image:Late Cretaceous Coast Mountains plate tectonics.jpg|thumb|right|Plate tectonics of the Coast Range Arc about 75 million years ago]]
One of the major aspects that changed early during the Coast Range Arc was the status of the northern end of the Farallon Plate, a portion now known as the [[Kula Plate]].<ref name="AD"/> About 85 million years ago, the Kula Plate broke off from the Farallon Plate to form a [[mid-ocean ridge]] known to geoscientists as the [[Kula-Farallon Ridge]].<ref name="AD"/> This change apparently had some important ramifications for regional geologic evolution. When this change was completed, Coast Range Arc volcanism returned and sections of the arc were uplifted considerably in latest Cretaceous time.<ref name="SI">[https://web.archive.org/web/20170420060002/https://books.google.com/books?id=AAZBokqaWj8C&pg=PA66&lpg=PA66&dq=Coast+Mountains+origins&source=web&ots=Gjg_FBlH2R&sig=mHwPx7nmsQV2KxRG-YW7tQ9_e5o&hl=en&sa=X&oi=book_result&resnum=1&ct=result Geology of a Transpressional Orogen Developed During Ridge-Trench ... - Google Books]. Books.google.ca. Retrieved on 2013-07-21.</ref> This started a period of mountain building that affected much of western North America called the [[Laramide orogeny]].<ref name="AV">{{cite web | title = Laramide orogeny | publisher = [[Encyclopædia Britannica, Inc.]] | year = 1998 | url = http://tlacaelel.igeofcu.unam.mx/~GeoD/colision/figs/orogeny/laramide.html | access-date = November 16, 2008 | url-status = dead | archive-url = https://web.archive.org/web/20090526224324/http://tlacaelel.igeofcu.unam.mx/~GeoD/colision/figs/orogeny/laramide.html | archive-date = May 26, 2009 }}</ref> In particular a large area of dextral transpression and southwest-directed thrust faulting was active from 75 to 66 million years ago.<ref name="SI"/> Much of the record of this deformation has been overridden by [[Tertiary]] age structures and the zone of Cretaceous dextral thrust faulting appears to have been widespread.<ref name="SI"/> It was also during this period when massive amounts of molten granite intruded highly deformed ocean rocks and assorted fragments from pre-existing island arcs, largely remnants of the Bridge River Ocean.<ref name="AD"/> This molten granite burned the old oceanic sediments into a glittering medium-grade [[metamorphic rock]] called [[schist]].<ref name="AD"/> The older intrusions of the Coast Range Arc were then deformed under the heat and pressure of later intrusions, turning them into layered metamorphic rock known as [[gneiss]].<ref name="AD"/> In some places, mixtures of older intrusive rocks and the original oceanic rocks have been distorted and warped under intense heat, weight and stress to create unusual swirled patterns known as [[migmatite]], appearing to have been nearly melted in the procedure.<ref name="AD"/>

Volcanism began to decline along the length of the arc about 60 million years ago during the [[Albian]] and [[Aptian]] [[faunal stage]]s of the Cretaceous period.<ref name="KO"/> This resulted from the changing geometry of the Kula Plate, which progressively developed a more northerly movement along the [[Pacific Northwest]].<ref name="AD"/> Instead of subducting beneath the Pacific Northwest, the Kula Plate began subducting underneath southwestern Yukon and Alaska and during the early [[Eocene]] period.<ref name="AD"/> Volcanism along the entire length of the Coast Range Arc shut down about 50 million years ago and many of the volcanoes have disappeared from erosion.<ref name="AD"/> What remains of the Coast Range Arc to this day are outcrops of granite when magma intruded and cooled at depth beneath the volcanoes, forming the present Coast Mountains.<ref name="AD"/> During construction of intrusions 70 and 57&nbsp;million years ago, the northern motion of the Kula Plate might have been between {{convert|140|mm|in|0|abbr=on}} and {{convert|110|mm|in|0|abbr=on}} per year.<ref name="KC">{{cite web|publisher=[[University of Arizona]]|url=http://www.geo.arizona.edu/tectonics/Ducea/Batholiths/Tectonics.htm|title=Tectonic overview of the CPC|access-date=2008-09-07}}</ref> However, other geologic studies determined the Kula Plate moved at a rate as fast as {{convert|200|mm|in|0|abbr=on}} per year.<ref name="KC"/>

== High-prominence peaks ==
{{GeoGroup|section=High-prominence peaks}}
{| class="wikitable sortable"
|- style="background:#ffc;"
! style="text-align:left;"|Mountain/Peak  ||colspan=2|Height (m/ft)||colspan=2|Prom. (m/ft) ||Location
|-
|[[Mount Waddington]]
|{{elevation_cells|4019|m}}
|{{elevation_cells|3289|m}}
|{{Coord|51|22.3|N|125|15.7|W|type:mountain_region:CA|name=Mount Waddington}}
|-
|[[Monarch Mountain (British Columbia)|Monarch Mountain]]
|{{elevation_cells|3555|m}}
|{{elevation_cells|2930|m}}
|{{Coord|51|54.0|N|125|52.6|W|type:mountain_region:CA|name=Monarch Mountain}}
|-
|[[Skihist Mountain]]
|{{elevation_cells|2968|m}}
|{{elevation_cells|2463|m}}
|{{Coord|50|11.3|N|121|54.2|W|type:mountain_region:CA|name=Skihist Mountain}}
|-
|[[Mount Ratz]]
|{{elevation_cells|3090|m}}
|{{elevation_cells|2430|m}}
|{{Coord|57|23.6|N|132|18.2|W|type:mountain_region:CA|name=Mount Ratz}}
|-
|[[Mount Queen Bess]]
|{{elevation_cells|3298|m}}
|{{elevation_cells|2355|m}}
|{{Coord|51|16.3|N|124|34.1|W|type:mountain_region:CA|name=Mount Queen Bess}}
|-
|[[Razorback Mountain (British Columbia)|Razorback Mountain]]
|{{elevation_cells|3183|m}}
|{{elevation_cells|2253|m}}
|{{Coord|51|35.4|N|124|41.5|W|type:mountain_region:CA|name=Razorback Mountain}}
|-
|[[Wedge Mountain]]
|{{elevation_cells|2892|m}}
|{{elevation_cells|2249|m}}
|{{Coord|50|08.0|N|122|47.6|W|type:mountain_region:CA|name=Wedge Mountain}}
|-
|[[Otter Mountain]]
|{{elevation_cells|2692|m}}
|{{elevation_cells|2242|m}}
|{{Coord|56|00.4|N|129|41.6|W|type:mountain_region:CA|name=Otter Mountain}}
|-
|[[Kwatna Peak]]
|{{elevation_cells|2290|m}}
|{{elevation_cells|2225|m}}
|{{Coord|52|04.2|N|126|57.6|W|type:mountain_region:CA|name=Kwatna Peak}}
|-
|[[Scud Peak]]
|{{elevation_cells|2987|m}}
|{{elevation_cells|2172|m}}
|{{Coord|57|14.5|N|131|10.1|W|type:mountain_region:CA|name=Scud Peak}}
|}
[[File:Coast mountains.jpg|thumb|right|upright=1.13|North Shore Mountains near Vancouver]]
[[File:Juneau Icefield.jpg|thumb|right|upright=1.13|Juneau Icefield]]

==Mountain ranges==
{| class="wikitable sortable" 2" cellspacing="width:100%" style="border-style:solid; border-width:1px; border-color:grey"
|- style="background:#efefef;"
! style="text-align:left;"| Range Name !! Parent !! Region(s) !! Country
|-
| [[Boundary Ranges]] || Coast Mountains || British Columbia, Yukon, Alaska || Canada, United States
|-
| [[Boundary Range]] || Boundary Ranges || British Columbia, Alaska || Canada, United States
|-
|[[Adam Mountains]] || Boundary Ranges || Alaska || United States
|-
|[[Ashington Range]] || Boundary Ranges || British Columbia || Canada
|-
|[[Burniston Range]] || Boundary Ranges || British Columbia || Canada
|-
|[[Dezadeash Range]] || Boundary Ranges || Yukon || Canada
|-
|[[Florence Range]] || Boundary Ranges || British Columbia || Canada
|-
|[[Halleck Range]] || Boundary Ranges || Alaska || United States
|-
|[[Juneau Icefield]] || Boundary Ranges || British Columbia, Alaska || Canada, United States
|-
|[[Sawtooth Range (Alaska)|Sawtooth Range]] || Juneau Icefield || Alaska || United States
|-
|[[Kakuhan Range]] || Boundary Ranges || Alaska || United States
|-
|[[Lincoln Mountains]]  || Boundary Ranges || Alaska || United States
|-
|[[Longview Range]] || Boundary Ranges || British Columbia || Canada
|-
|[[Peabody Mountains]] || Boundary Ranges || Alaska || United States
|-
|[[Rousseau Range]] || Boundary Ranges || Alaska || United States
|-
|[[Seward Mountains (Alaska)|Seward Mountains]] || Boundary Ranges || Alaska || United States
|-
|[[Snowslide Range]] || Boundary Ranges || British Columbia || Canada
|-
|[[Spectrum Range]] || Boundary Ranges || British Columbia || Canada
|-
|[[Stikine Icecap]] || Boundary Ranges || British Columbia, Alaska || Canada, United States
|-
|[[Chechidla Range]] || Stikine Icecap || British Columbia || Canada
|-
|[[Cheja Range]] || Stikine Icecap || British Columbia || Canada
|-
|[[Kitimat Ranges]] || Coast Mountains || British Columbia || Canada
|-
|[[Bare Top Range]] || Kitimat Ranges || British Columbia || Canada
|-
|[[Countess of Dufferin Range]] || Kitimat Ranges || British Columbia || Canada
|-
|[[Kitlope Range]] || Kitimat Ranges || British Columbia || Canada
|-
|[[North Coastal Archipelago]] || Kitimat Ranges || British Columbia || Canada
|-
|[[Bell Range]] || North Coastal Archipelago || British Columbia || Canada
|-
|[[Burnaby Range]] || North Coastal Archipelago || British Columbia || Canada
|-
|[[Cape Range]] || North Coastal Archipelago || British Columbia || Canada
|-
|[[Chismore Range]] || North Coastal Archipelago || British Columbia || Canada
|-
|[[Murphy Range (Canada)|Murphy Range]] || North Coastal Archipelago || British Columbia || Canada
|-
|[[Richardson Range]] || North Coastal Archipelago || British Columbia || Canada
|-
|[[Spiller Range]] || North Coastal Archipelago || British Columbia || Canada
|-
|[[Williams Range]] || North Coastal Archipelago || British Columbia || Canada
|-
|[[Wimbledon Range]] || North Coastal Archipelago || British Columbia || Canada
|-
|[[Tenaiko Range]] || Kitimat Ranges || British Columbia || Canada
|-
|[[Pacific Ranges]] || Coast Mountains || British Columbia || Canada
|-
|[[Ashlu-Elaho Divide]] || Pacific Ranges || British Columbia || Canada
|-
|[[Bazalgette Range]] || Pacific Ranges || British Columbia || Canada
|-
|[[Bendor Range]] || Pacific Ranges || British Columbia || Canada
|-
|[[Bridge-Lillooet Divide]] || Pacific Ranges || British Columbia || Canada
|-
|[[Broughton Archipelago]] || Pacific Ranges || British Columbia || Canada
|-
|[[Calliope Range]] || Broughton Archipelago || British Columbia || Canada
|-
|[[Georgina Range]] || Broughton Archipelago || British Columbia || Canada
|-
|[[Bunster Range]] || Pacific Ranges || British Columbia || Canada
|-
|[[Cadwallader Range]] || Pacific Ranges || British Columbia || Canada
|-
|[[Caren Range]] || Pacific Ranges || British Columbia || Canada
|-
|[[Charlotte Alplands]] || Pacific Ranges || British Columbia || Canada
|-
|[[Douglas Ranges]] || Pacific Ranges || British Columbia || Canada
|-
|[[Chilcotin Ranges]] || Pacific Ranges || British Columbia || Canada
|-
|[[Camelsfoot Range]] || Chilcotin Ranges || British Columbia || Canada
|-
|[[Dickson Range]] || Chilcotin Ranges || British Columbia || Canada
|-
|[[Leckie Range (British Columbia)|Leckie Range]] || Chilcotin Ranges || British Columbia || Canada
|-
|[[Pantheon Range]] || Chilcotin Ranges || British Columbia || Canada
|-
|[[Potato Range (British Columbia)|Potato Range]] || Chilcotin Ranges || British Columbia || Canada
|-
|[[Shulaps Range]] || Chilcotin Ranges || British Columbia || Canada
|-
|[[Clendinning Range]] || Pacific Ranges || British Columbia || Canada
|-
|[[Colville Range]] || Pacific Ranges || British Columbia || Canada
|-
|[[Conical Range]] || Pacific Ranges || British Columbia || Canada
|-
|[[Earle Range]] || Pacific Ranges || British Columbia || Canada
|-
|[[Edwards Range]] || Pacific Ranges || British Columbia || Canada
|-
|[[Florence Range]] || Pacific Ranges || British Columbia || Canada
|-
|[[Franklyn Range]] || Pacific Ranges || British Columbia || Canada
|-
|[[Fraser Range]] || Pacific Ranges || British Columbia || Canada
|-
|[[Garibaldi Ranges]] || Pacific Ranges || British Columbia || Canada
|-
|[[Garibaldi Névé]] || Garibaldi Ranges || British Columbia || Canada
|-
|[[Fitzsimmons Range]] || Garibaldi Ranges || British Columbia || Canada
|-
|[[McBride Range]] || Garibaldi Ranges || British Columbia || Canada
|-
|[[Spearhead Range]] || Garibaldi Ranges || British Columbia || Canada
|-
|[[Golden Ears Group|Golden Ears]] || Garibaldi Ranges || British Columbia || Canada
|-
|[[Misty Icefield]] || Garibaldi Ranges || British Columbia || Canada
|-
|[[Bastion Range]] || Garibaldi Ranges || British Columbia || Canada
|-
|[[Gastineau Range]] || Pacific Ranges || British Columbia || Canada
|-
|[[Ha-Iltzuk Icefield]] || Pacific Ranges || British Columbia || Canada
|-
|[[Homathko Icefield]] || Pacific Ranges || British Columbia || Canada
|-
|[[Koeye Range]] || Pacific Ranges || British Columbia || Canada
|-
|[[Lewis Range (Coast Mountains)|Lewis Range]] || Pacific Ranges || British Columbia || Canada
|-
|[[Lillooet Icecap]] || Pacific Ranges || British Columbia || Canada
|-
|[[Compton Névé]] || Lillooet Icefield || British Columbia || Canada
|-
|[[Lillooet Ranges]] || Pacific Ranges || British Columbia || Canada
|-
|[[Cantilever Range]] || Lillooet Ranges || British Columbia || Canada
|-
|[[Cayoosh Range]] || Lillooet Ranges || British Columbia || Canada
|-
|[[Mission Ridge (British Columbia)|Mission Ridge]] || Pacific Ranges || British Columbia || Canada
|-
|[[Monarch Icefield]] || Pacific Ranges || British Columbia || Canada
|-
|[[North Shore Mountains]] || Pacific Ranges || British Columbia || Canada
|-
|[[Fannin Range]] || North Shore Mountains || British Columbia || Canada
|-
|[[Britannia Range (Canada)|Britannia Range]] || North Shore Mountains || British Columbia || Canada
|-
|[[Namu Range]] || Pacific Ranges || British Columbia || Canada
|-
|[[Nicholl Range]] || Pacific Ranges || British Columbia || Canada
|-
|[[Niut Range]] || Pacific Ranges || British Columbia || Canada
|-
|[[Pemberton Icefield]] || Pacific Ranges || British Columbia || Canada
|-
|[[Pembroke Range]] || Pacific Ranges || British Columbia || Canada
|-
|[[Powell Divide]] || Pacific Ranges || British Columbia || Canada
|-
|[[Sir Harry Range]] || Pacific Ranges || British Columbia || Canada
|-
|[[Squamish-Cheakamus Divide]] || Pacific Ranges || British Columbia || Canada
|-
|[[Tantalus Range]] || Pacific Ranges || British Columbia || Canada
|-
|[[The Tahumming]] || Pacific Ranges || British Columbia || Canada
|-
|[[Tottenham Range]] || Pacific Ranges || British Columbia || Canada
|-
|[[Unwin Range]] || Pacific Ranges || British Columbia || Canada
|-
|[[Waddington Range]] || Pacific Ranges || British Columbia || Canada
|-
|[[Wharncliffe Range]] || Pacific Ranges || British Columbia || Canada
|-
|[[Whitemantle Range]] || Pacific Ranges || British Columbia || Canada
|}

==See also==
{{Portal|Geography|Canada}}
*[[Coast Range Arc]]
*[[Pandemonium Creek slide]] (1959)
*[[Geography of British Columbia]]
*[[Geology of British Columbia]]
*[[Volcanism of Canada]]
*[[Volcanism of Western Canada]]
*[[List of mountain ranges]]
*[[Rocky Mountains]]
*[[Columbia Mountains]]
* {{portal-inline|Pacific Northwest}}

==References==
{{Reflist}}

{{Coast Mountains}}
{{Canada topics}}
{{Authority control}}

[[Category:Coast Mountains| ]]
[[Category:Pacific Coast Ranges]]
[[Category:Mountain ranges of British Columbia]]
[[Category:Mountain ranges of Yukon]]
[[Category:Mountain ranges of Alaska]]
[[Category:Coast of British Columbia]]