Crater Lake National Park

Template:Use American English Template:Use mdy dates Template:Short description Template:About Template:Infobox protected area Crater Lake National Park is a national park of the United States located in southern Oregon. Established in 1902, Crater Lake is the fifth-oldest national park in the United States and the only national park in Oregon.<ref name="nps">Template:Cite web</ref> The park encompasses the caldera of Crater Lake, a remnant of Mount Mazama, a destroyed volcano, and the surrounding hills and forests.

The lake is Template:Convert deep at its deepest point,<ref name="deepest">Bacon, Charles R.; James V. Gardner; Larry A. Mayer; Mark W. Buktenica; Peter Darnell; David W. Ramsey; Joel E. Robinson (June 2002). "Morphology, volcanism, and mass wasting in Crater Lake, Oregon". Geological Society of America Bulletin 114 (6): 675–692. doi:10.1130/0016-7606(2002)114<0675:MVAMWI>2.0.CO;2. ISSN 0016-7606.</ref> which makes it the deepest lake in the United States, the second-deepest in North America and the tenth-deepest in the world.<ref name="deepest"/> Crater Lake is often referred to as the seventh-deepest lake in the world, but this former listing excludes the approximately Template:Convert depth of subglacial Lake Vostok in Antarctica, which resides under nearly Template:Convert of ice, and the recent report of a Template:Convert maximum depth for Lake O'Higgins/San Martin, located on the border of Chile and Argentina. However, when comparing its average depth of Template:Convert to the average depth of other deep lakes, Crater Lake becomes the deepest in the Western Hemisphere and the third-deepest in the world. The impressive average depth of this volcanic lake is due to the nearly symmetrical Template:Convert caldera formed 7,700 years ago (about 8 kya) during the violent climactic eruptions and subsequent collapse of Mount Mazama and the relatively moist climate that is typical of the crest of the Cascade Range.

The caldera rim ranges in elevation from Template:Convert. The United States Geological Survey benchmark elevation of the lake surface is Template:Convert. The national park encompasses Template:Convert.<ref name="area"/> Crater Lake has no streams flowing into or out of it. All water that enters the lake is eventually lost from evaporation or subsurface seepage. The lake's water commonly has a striking blue hue, and the lake is refilled entirely from direct precipitation in the form of snow and rain.

Park purpose

As stated in the foundation document:<ref>Template:Cite web</ref> Template:Blockquote

Geology

Template:Details Template:Stack Volcanic activity in this area is fed by subduction off the coast of Oregon as the Juan de Fuca Plate slips below the North American Plate (see plate tectonics). Heat and compression generated by this movement has created a mountain chain topped by a series of volcanoes, which together are called the Cascade Range. The large volcanoes in the range are called the High Cascades. The range has many other volcanoes, however, most of which are much smaller.Template:Fact

About 400,000 years ago (400 kya), Mount Mazama began its existence in much the same way as the other mountains of the High Cascades, as overlapping shield volcanoes. Over time, alternating layers of lava flows and pyroclastic flows built Mazama's overlapping cones until it reached about Template:Convert in height.Template:Fact

As the young stratovolcano grew, many smaller volcanoes and volcanic vents were built in the area of the park and just outside what are now the park's borders. Chief among these were cinder cones. Although the early examples are gone, since cinder cones erode easily, the park features at least 13 much younger cinder cones, as well as at least another 11 or so outside its borders, that still retain their distinctive cinder cone appearance. Debate has continued as to whether these minor volcanoes and vents were parasitic to Mazama's magma chamber and system or whether they were related to background Oregon Cascade volcanism.Template:Fact

After a period of dormancy, Mazama became active again. Then, around 5700 BCE, Mazama collapsed into itself during a tremendous volcanic eruption, losing Template:Convert in height. The eruption formed a large caldera that, depending on the prevailing climate, was filled in about 740 years, forming Crater Lake.<ref>

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The eruptive period that decapitated Mazama also laid waste to much of the greater Crater Lake area and deposited ash as far east as the northwest corner of what is now Yellowstone National Park, as far south as central Nevada, and as far north as southern British Columbia. It produced more than 150 times as much ash as the May 18, 1980 eruption of Mount St. Helens.Template:Fact

This ash has since developed a soil type called andisol. Soils in Crater Lake National Park are brown, dark brown or dark grayish-brown sandy loams or loamy sands which have plentiful cobbles, gravel, and stones. They are slightly to moderately acidic and their drainage is somewhat excessive.Template:Fact

Climate

Template:Stack According to the Köppen climate classification system, Crater Lake National Park has a dry-summer subarctic climate (Dsc). The plant hardiness zone at the lake is 6b with an average annual extreme minimum air temperature of Template:Convert.<ref name="USDA">Template:Cite web</ref>

Snow is relatively rare at low elevations in western Oregon, but it is common at higher elevations, especially at Crater Lake. Measurements at park headquarters, Template:Convert above sea level, show that snow falls more often here than at any other long-term weather station in Oregon. Winter, which typically begins at the park in September and runs through June, includes an average of 101 days with measurable snowfall. Up to Template:Convert of snow have fallen on the park in a single day (in 1937, 1951, and 1971), Template:Convert in a month (January 1950), and Template:Convert in a year (1950).<ref name="Taylor 39-41">Taylor and Hannan, pp. 39–41</ref>

Snow typically accumulates in the park to depths of Template:Convert by early spring. Most of the park's roads remain closed through late spring, and snow lingers into the summer. In July and August, snowfall is uncommon, and "one magnificent day typically follows another".<ref>Template:Cite web</ref>

December is the coldest month, when highs average about Template:Convert and lows average about Template:Convert. August is the warmest month, with an average high of roughly Template:Convert and an average low of about Template:Convert. The highest recorded temperature was Template:Convert and the lowest was Template:Convert. Annual precipitation averages about Template:Convert a year. December is the wettest, averaging about Template:Convert.

Although snow covers Crater Lake National Park for eight months of the year (average annual snowfall is Template:Convert), the lake rarely freezes over due, in part, to a relatively mild onshore flow from the Pacific Ocean. The last recorded year in which the lake froze over was in 1949, a very long, cold winter. A 95% surface freeze occurred in 1985. The immense depth of Crater Lake acts as a heat reservoir that absorbs and traps sunlight, maintaining the lake temperature at an average of Template:Convert on the surface and Template:Convert at the bottom throughout the year. The surface temperature fluctuates a bit, but the bottom temperature remains quite constant.

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Fauna

Mammals that are residents of this national park are Canadian lynxes, bobcats, beavers, chipmunks, pronghorns, foxes, squirrels, porcupines, black bears, coyotes, pika, badgers, deer, elk, muskrats, and martens.Template:Fact

Birds that commonly fly through this park include raptors, along with American dippers, Peregrine falcons, ravens, Clark's nutcrackers, Canada jays, bald eagles, hummingbirds, and spotted owls, while Canada geese float on its lake.Template:Citation needed

Park features

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The Pumice Desert: A very thick layer of pumice and ash leading away from Mazama in a northerly direction. Even after thousands of years, this area is largely devoid of plants due to excessive porosity (meaning water drains through quickly) and poor soil composed primarily of regolith.
The Pinnacles: When the very hot ash and pumice came to rest near the volcano, it formed Template:Convert gas-charged deposits. For perhaps years afterward, hot gas moved to the surface and slowly cemented ash and pumice together in channels and escaped through fumaroles. Erosion later removed most of the surrounding loose ash and pumice, leaving tall pinnacles and spires.

Mount Scott is a steep andesitic cone whose lava came from magma from Mazama's magma chamber; geologists call such volcano a parasitic or satellite cone. Volcanic eruptions apparently ceased on Scott sometime before the end of the Pleistocene; one remaining large cirque on Scott's northwest side was left unmodified by post-ice-age volcanism.
In the southwest corner of the park stands Union Peak, an extinct volcano whose primary remains consist of a large volcanic plug, which is lava that solidified in the volcano's neck.
Crater Peak is a shield volcano primarily made of andesite and basalt lava flows topped by andesitic and dacite tephra.
Timber Crater is a shield volcano located in the northeast corner of the park. Like Crater Peak, it is made of basaltic and andesitic lava flows but, unlike Crater, it is topped by two cinder cones.
Rim Drive is the most popular road in the park; it follows a scenic route around the caldera rim.
Llao Rock on the north side rises Template:Convert above the lake, with a Template:Convert trail from Rim Drive leading to the summit.<ref>Template:Cite news</ref>
The Pacific Crest Trail, a Template:Convert long-distance hiking and equestrian trail that stretches from the Mexican to Canadian borders, passes through the park.
Old-growth forests covering Template:Convert.<ref name = "1993OldGrowthEstimates">Template:Cite web</ref>

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History

Template:Stack Local Native Americans witnessed the collapse of Mount Mazama and kept the event alive in their legends. One ancient legend of the Klamath people closely parallels the geologic story which emerges from today's scientific research. The legend tells of two Chiefs, Llao of the Below World and Skell of the Above World, pitted in a battle which ended up in the destruction of Llao's home, Mt. Mazama.<ref>Template:Cite web</ref> The battle was witnessed in the eruption of Mt. Mazama and the creation of Crater Lake.Template:Fact

A trio of gold prospectors—John Wesley Hillman, Henry Klippel, and Isaac Skeeters—were the first American prospectors to visit the lake. On June 12, 1853, they stumbled upon the long, sloping mountain while hunting for provisions. Stunned by the vibrant blue color of the lake, they named the indigo body of water "Deep Blue Lake" and the place on the southwest side of the rim where he first saw the lake later became known as Discovery Point.<ref name="nps"/> Gold, however, was more on the minds of settlers at the time, and the discovery was soon forgotten. The suggested name later fell out of favor by locals, who preferred the name "Crater Lake".Template:Fact

William Gladstone Steel devoted his life and fortune to the establishment and management of a national park at Crater Lake. His preoccupation with the lake began in 1870. In his efforts to bring recognition to the park, he participated in lake surveys that provided scientific support. He named many of the lake's landmarks, including Wizard Island, Llao Rock, and Skell Head.Template:Fact

With the help of geologist Clarence Dutton, Steel organized a USGS expedition to study the lake in 1886. The party carried the Cleetwood, a half-ton survey boat, up the steep slopes of the mountain then lowered it to the lake. From the stern of the Cleetwood, a piece of pipe on the end of a spool of piano wire sounded the depth of the lake at 168 different points. Their deepest sounding, Template:Convert, was very close to the modern official depth of Template:Convert made in 2000 by sonar.<ref name="deepest"/> At the same time, a topographer surveyed the area and created the first professional map of the Crater Lake area.Template:Fact

Template:Infobox U.S. legislation Partly based on data from the expedition and lobbying from Steel and others, Crater Lake National Park was established May 22, 1902, by President Theodore Roosevelt.<ref name=ea>Template:Cite Americana</ref> And because of Steel's involvement, Crater Lake Lodge was opened in 1915 and the Rim Drive was completed in 1918.<ref name="nps" />

Highways were later built to the park to help facilitate tourism. The 1929 edition of O Ranger! described access and facilities available by then:

Crater Lake National Park is reached by train on the Southern Pacific Railroad lines into Medford and Klamath Falls, at which stops motor stages make the short trip to the park. A hotel on the rim of the lake offers accommodations. For the motorist, the visit to the park is a short side trip from the Pacific and Dalles-California highways. He will find, in addition to the hotel, campsites, stores, filling stations. The park is open to travel from late June or July 1 for as long as snow does not block the roads, generally until October.<ref>Template:Cite book</ref>

Activities

File:Daily trips CLNP.jpg

Daily Trips (1931).

Many hiking trails and several campgrounds are inside the park. Unlicensed fishing is allowed without any limitation of size, species, or number. The lake is believed to have no indigenous fish, but several species of fish were introduced beginning in 1888 until all fish stocking ended in 1941. Kokanee salmon (Oncorhynchus nerka) and rainbow trout (Oncorhynchus mykiss) now thrive and reproduce here naturally.<ref>

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Swimming is allowed in the lake, and the boat tours, which stop at Wizard Island, a cinder cone inside the lake, operate daily during the summer. All lake access for people is from Cleetwood Trail, a steep walking trail, and there are no roads for cars, trucks, or wagons that lead to the waterfront. All of the boats in the lake were delivered by helicopter.<ref>Template:Cite news</ref>

Numerous observation points along the caldera rim for the lake are readily accessible by automobile via the Rim Drive, which is Template:Convert long and has an elevation gain of Template:Convert.Template:Fact

The highest point in Crater Lake National Park is Mount Scott at Template:Convert. Getting there requires a fairly steep Template:Convert hike from the Rim Drive trailhead. On a clear day, visibility from the summit exceeds Template:Convert, and one can, in a single view, take in the entire caldera. Also visible from this point are the white-peaked Cascade Range volcanoes to the north, the Columbia River Plateau to the east, and the Western Cascades and the more-distant Klamath Mountains to the west.Template:Fact

The scenery of Crater Lake is fully accessible during the summer months. Heavy snowfalls in this park during the fall, winter, and spring months force many road and trail closures, including the popular Rim Drive, which is generally completely open from July to October and partially open in some other months, such as May, June, and November.Template:Fact

Trails

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Cleetwood Cove

The Cleetwood Cove Trail originates on the north side of the lake about Template:Convert east of North Junction along East Rim Drive. The trail is the only one that accesses the shoreline of the lake, descending Template:Convert from the parking lot on East Rim Drive. First opened in 1960, the Cleetwood Cove Trail is Template:Convert long with an 11% grade; it is not accessible for mobility-impaired visitors. A dock with concessionaire boats facilitates tours around the lake with a stop at Wizard Island for dropping off and picking up passengers. Swimming and fishing are permitted.<ref name=CLInst1>Template:Cite web</ref>

In 2025, the trail will be closed for a two-year repair project due to erosion issues caused by its high traffic.<ref>Template:Cite news</ref>

The Watchman

The Watchman Peak trail begins from the Watchman Overlook parking lot, about Template:Convert northwest of Rim Village.<ref name=CLInst2>Template:Cite web</ref> The trail is Template:Convert long with a Template:Convert elevation change.<ref>Template:Cite web</ref> It is a steady uphill trail on an isolated mountain on the west rim of the crater, with several switchbacks, providing wide views of Crater Lake and Wizard Island. Several nearby landmarks are visible from the summit, including Mount McLoughlin, Mount Thielsen, Union Peak, Mount Scott, and the Klamath Basin. The trail ends next to a historic fire lookout tower built in 1932.<ref name=CLInst2/>

Lightning Spring

The Lightning Spring trail starts from the Lightning Spring picnic area. It is a Template:Convert hike with an elevation gain of Template:Convert. The trail circles around several meadows up to the Lightning Spring creek. The trail is known for the frequent sight of grazing deer.Template:Fact

Castle Crest Wildflower Garden

This is considered to be the easiest trail, looping around the Castle Crest Wildflower Garden. It starts from the East Rim Road, near the park's headquarters. It received its name because of a large stretch of meadows around which the trail circles and which is bursting with wildflowers in the springtime. The trail is about Template:Convert before it reaches the wildflower meadow garden, from which other improvised routes depart.Template:Fact

Plaikni Falls

The Plaikni Falls trail is the newest trail in the Crater Lake park. It stretches Template:Convert from the trailhead located Template:Convert south from the Phantom Ship Overlook on Pinnacles Road, which spins off Rim Drive. The trail leads to Plaikni Falls. Most of the trail is wheelchair-accessible. The final stretch is fairly uphill, which may prove moderately challenging.Template:Fact

Garfield Peak

File:A064, Crater Lake National Park, Oregon, USA, Phantom Ship, 2002.jpg

Phantom Ship.

The Garfield Peak trail is a moderately challenging Template:Convert hike to Garfield Peak. The trailhead is located east of the Crater Lake Lodge and gains approximately Template:Convert of elevation. Several spots along the trail provide viewpoints overlooking the Phantom Ship island and Dutton Cliff. A few viewpoints offer unique views of Wizard island. The trail is popular in the late afternoon on account of unique shifting colors over the lake and its surroundings.Template:Fact

References

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Works cited

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External links

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Template:Crater Lake Template:National parks of the United States Template:Protected areas of Oregon

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