Grand Teton National Park
|Grand Teton National Park|
|IUCN Category II (National Park)|
|Nearest city:||Jackson, WY|
|Area:||309,995 acres (1,255 km²)|
|Established:||February 26 1929|
|Visitation:||2,406,476 (in 2006)|
|Governing body:||National Park Service|
Grand Teton National Park is a United States National Park located in western Wyoming, south of Yellowstone National Park. It is named after Grand Teton, which at 13,770 feet (4,197 m), is the tallest mountain in the Teton Range.
The origin of the name is controversial. The most common explanation is that "Grand Teton" means "large teat" in French, named by either French-Canadian or Iroquois members of an expedition led by Donald McKenzie of the Northwest Company. However, other historians disagree, and claim that the mountain was named after the Teton Sioux tribe of Native Americans. The park covers 484 square miles (1,255 km²) of land and water and was established as a national park on February 26, 1929. There are nearly 200 miles (320 km) of trails for hikers to enjoy in the Park.
One reason the Tetons are famous is because of their great elevation above their base. Unlike most mountain ranges the Tetons lack foothills, or lower peaks, which can obscure the view. As such, the Tetons rise sharply from 5,000 to nearly 7,000 feet above the surrounding terrain; the view is especially dramatic from the town of Jackson, formerly Jackson Hole. The absence of foothills exaggerates its abrupt vertical rise. The Park is famous throughout America for its spectacular landscape featuring majestic mountains, pristine lakes and abundant wildlife. Glacial lakes at the base of the range add to the mountains' beauty.
Part of the Rocky Mountains, the north-south-trending Teton Range rises from the floor of Jackson Hole, Wyoming without any foothills along a 40-mile (65-km) long by 7- to 9-mile (11- to 15-km) wide active fault-block mountain front system. In addition to the 13,770-foot (4,197-m) high Grand Teton, another twelve peaks are over 12,000 ft (3,660 m) above sea level. Seven of these peaks between Avalanche and Cascade canyons make up the often-photographed Cathedral Group.
Jackson Hole is a 55-mile (90-km) long by 6- to 13-mile (10- to 20-km) wide graben valley that has an average elevation of 6,800 feet (2,070 m) with its lowest point near the south park boundary at 6,350 feet (1,935 m). The valley sits east of the Teton Range and is vertically displaced downward 30,000 feet (9,100 m) from corresponding rock layers in it, making the Teton Fault and its parallel twin on the east side of the valley normal faults with the Jackson Hole block being the hanging wall and the Teton Mountain block being the footwall. Grand Teton National Park contains the major part of both blocks. A great deal of erosion of the range and sediment filling the graben, however, yields a topographic relief of only up to 7,700 feet (2,350 m).
The glaciated range is composed of a series of horns and arêtes separated by U-shaped valleys headed by cirques and ended by moraines, making the Tetons a textbook example of alpine topography. Rubble piles left by ice age alpine glaciers impounded a series of interconnected lakes at the foot of the range (Jackson, Leigh, String, Jenny, Bradley, Taggart, and Phelps). There are also over 100 alpine and backcountry lakes.
The largest lake in the valley, Jackson Lake, is one of the largest high altitude lakes in the U.S. at an elevation of 6,772 feet (2,064 m) above sea level. The lake is up to 15 miles (25 km) long, 7 miles (11.25 km) wide and 438 feet (134 m) deep. The water temperature of the lake averages below 60 degrees even during the hottest summer months and can freeze to more than 6 feet (1.8 m) thick in the winter. The lake is natural, except for the top 33 feet (10 m), which is due to the construction of Jackson Lake Dam, built in 1911.
Just to the south is Burned Ridge, the same glacier's terminal or end moraine, which runs down the center of Jackson Hole roughly perpendicular to the range and cut in two by the Snake River. After exiting its dammed outlet at the southeast corner of Jackson Lake, the Snake runs down the valley and through the 10-mile (16-km) long glacial outwash plain south of Burned Ridge. The river's headwaters are in a part of the Teton Wilderness a short distance north in Yellowstone National Park and its destination is the Columbia River far to the west, which in turn empties into the Pacific Ocean. Terraces have been cut by the river into the moraines and outwash plain in the valley. About 50 miles (80 km) of the 1,056-mile (1,699-km) long Snake River winds through the park where it is fed by three major tributaries; Pacific Creek, Buffalo Fork, and the Gros Ventre River.
The local climate is a semi-arid mountain one with a yearly extreme high of 93° F (34° C) and extreme low of −46° F (−43° C). Average annual snowfall is 191 inches (485 cm) and average rainfall is 10 inches (254 mm). The coldest temperature ever recorded in Grand Teton National Park was −63° F (−53° C), and snow often blankets the landscape from early November to late April.
The rock units that make up the east face of the Teton Range are around 2,500 million years old and made of metamorphosed sandstones, limestones, various shales, and interbeded volcanic deposits. Buried deep under Tertiary volcanic, sedimentary, and glacial deposits in Jackson Hole, these same Precambrian rocks are overlain by Paleozoic and Mesozoic formations that have long since been eroded away from atop the Tetons.
The Paleozoic-aged sediments were deposited in warm shallow seas and resulted in various carbonate rocks along with sandstones and shales. Mesozoic deposition transitioned back and forth from marine to non-marine sediments. In later Mesozoic, the Cretaceous Seaway periodically covered the region and the Sierran Arc to the west provided volcanic sediments.
A mountain-building episode known as the Laramide orogeny started to uplift western North America 70 million years ago and eventually formed the Rocky Mountains. This erased the seaway and created fault systems along which highlands rose. Sediment eroded from uplifted areas filled subsiding basins such as Jackson Hole while reverse faults created the first part of the Teton Range in the Eocene epoch. Large Eocene-aged volcanic eruptions from the north in the Yellowstone-Absaroka area along with later Pleistocene-aged Yellowstone Caldera eruptions, left thick volcanic deposits in basins.
The Teton Range started to grow along a north-south trending fault system next to Jackson Hole some nine million years ago in the Miocene epoch. Then starting in the Pliocene, Lake Teewinot periodically filled Jackson Hole and left thick lakebed sediments. The lake was dry by the time a series of glaciations in the Pleistocene epoch saw the introduction of large glaciers in the Teton and surrounding ranges. During the coldest ice age these glaciers melded together to become part of the Canadian Ice Sheet, which carried away all soil from Jackson Hole and surrounding basins. Later and less severe ice ages created enough locally deposited dirt in the form of moraines and till to repair much of this damage. Since then, mass wasting events such as the 1925 Gros Ventre landslide, along with slower forms of erosion, have continued to modify the area.
Over 1,000 species of vascular plants grow in Grand Teton National Park and the surrounding area. Some trees, such as the Whitebark Pine, Limber Pine, Subalpine fir, and Engelmann Spruce can survive the cold windy slopes and alpine zone high up in the Tetons to around 10,000 feet (~3,000 m). Other evergreens, like the Lodgepole Pine, Douglas Fir, and Blue Spruce, are more commonly found on the valley floor, while the aspens, cottonwoods, alders, and willows prefer the moist soils found along the rivers and lakeshores.
Grand Teton forests generally contain two or three different types of trees growing together in a specific habitat type. These forests merge into one another in zones called ecotones, which creates edge habitat for various species of wildlife. Some animals, like the red squirrel, pine marten, and black bear spend most of their time in the forests. Others, such as moose, elk, and wolves, seek the forest for shade and shelter during the day and move out to the sagebrush or meadows to feed in the early mornings and evenings.
Soil conditions, availability of moisture, slope, aspect, and elevation all determine where plants grow. Plants that require similar conditions are often found growing in the same area. These associations form various plant communities. It is useful to divide the plants the Park into the following communities: forests, sagebrush flats, riparian corridors and wetlands, and alpine areas.
Evergreen forests composed of seven coniferous tree species and over 900 species of flowering plants dominate the mountainous part of the Teton Range below the treeline and extend into Jackson Hole on top of moraines. These compact piles of unsorted rubble have good clay content and retain moisture better than the quartzite-rich outwash plain and are thus able to support large stands of Lodgepole Pines along with many other plants.
The loose soil of the outwash plain has a poor ability to hold moisture, resulting in a sparse vegetation cover primarily made of sagebrush and coarse grasses. Abundant aspens, cottonwoods, and willows thrive along streams in riparian zones outside of the barren outwash plain. Wet meadows provide the conditions suited to grasses, sedges, and wildflowers. Coyotes and badgers dig burrows in patches of loesses, which were blown into the valley between ice ages. Although they appear gray and lifeless, the high alpine reaches of the Park support plants specially adapted to the harsh growing conditions found there. Wind, snow, lack of soil, increased ultraviolet radiation, rapid and dramatic shifts in temperature, and a short growing season all challenge the hardy plants that survive here. Most plants adapt by growing close to the ground in mats like the Alpine Forget-me-not.
Grand Teton National Park is located in the heart of the Greater Yellowstone Ecosystem, one of the largest intact temperate zone ecosystems remaining on the planet and is considered one of the world’s foremost natural laboratories in landscape ecology and geology. This means that many of the animals in the Teton area travel between the two parks and the numerous adjacent National Forests.
- Five species of amphibians: Spotted Frog, Boreal Chorus Frog, Boreal Toad, Tiger Salamander, Northern Leopard Frog (believed to be locally extinct), and Bullfrog (introduced just outside the park).
- Six species of bats
- 300+ species of birds: including Bald Eagle, Calliope Hummingbird, Golden Eagle, Osprey, Sage Grouse, Trumpeter Swan, and Western Tanager
- 17 species of carnivores: including Grizzly, Black Bear, Mountain Lion, Wolf, and Coyote.
- 16 species of fishes: including Yellowstone cutthroat trout, Snake River cutthroat trout, Mountain Sucker, Utah Chub, and Mountain Whitefish
- Six species of hoofed mammals: including American Bison, Moose, Pronghorn, Elk, and Mule Deer
- numerous invertebrates (no poisonous spiders)
- Three species of rabbits/hares
- Four species of reptiles (none poisonous): Wandering Garter Snake, Valley Garter Snake, Rubber Boa, and Northern Sagebrush Lizard
- 22 species of rodents: including Yellow-Bellied Marmot, Least Chipmunk, Muskrat, Red Squirrel, and Uinta Ground Squirrel
Native American hunting parties from the northern Rocky Mountains camped along the shore of Jackson Lake around 12,000 years ago while following game. In modern times, tribes of Bannock, Blackfoot, Crow, Gros Ventre, and Shoshone visited the area for hunting or gathering. A year–round presence was not maintained due to the severe winters. The Shoshone were the most dominant. There is evidence that there was minimal Indian presence from about the mid-1600s to the early 1800s, in which time the area served as a "neutral zone" between tribes of the area.
There were several trade routes through the area. One followed the Snake River to its source in the Yellowstone area where abundant obsidian could be found. Another major route traversed the Teton Pass at the southern end of the range, providing a shortcut to the Pacific Northwest region of the U.S.. There was also a southern route which led to the Colorado Plateaus region and the Great Basin.
White exploration and settlement
In the eighteenth and nineteenth centuries, Caucasian fur trappers and fur traders referred to deep valleys rimmed by high mountains “holes.” One such fur trapper was named David Jackson and his favorite place to “hole-up” was named after him in 1829.
John Colter, a member of the Lewis and Clark Expedition, is the first white American known to have visited the area now known as Jackson Hole as early as 1805-1806. Geologist F.V. Hayden visited the area in 1860 as part of the Raynolds expedition. In the summer of 1871 he led the first government-sponsored scientific survey of the Yellowstone area just to the north. One part of that survey, led by geologist James Stevenson, traveled into Jackson Hole via the Teton Pass before meeting up with the other half of the expedition in Yellowstone. While passing through, the team, which included Yellowstone's first superintendent N. P. Longford, photographer William Henry Jackson, and artist William Henry Holmes, among others, mapped the area and surveyed its geology and biology. These data were later included in the Hayden Survey set of reports.
Homesteaders moved into Jackson Hole after the reports were published but the short growing season along with weeks of being snowed-in each winter kept all but the hardiest individuals away. One of those settlers, a rancher named Pierce Cunningham, circulated a petition to have Jackson Hole saved for the "education and enjoyment of the Nation as a whole."
Fight for preservation
In 1897 acting Yellowstone superintendent Colonel S.B.M. Young proposed expanding that park's borders south to encompass the northern extent of Jackson Hole in order to protect migrating herds of elk. The following year, United States Geological Survey head Charles D. Walcott suggested that the Teton Range should be included as well. Stephen Mather, director of the newly created National Park Service and his assistant Horace Albright sent a report to Secretary of the Interior Franklin Lane in 1917 stating much the same. Wyoming Representative Frank Mondell sponsored a bill that unanimously passed the United States House of Representatives in 1918 but was killed in the United States Senate when Idaho Senator John Nugent feared that the expansion of Park Service jurisdiction would threaten sheep grazing permits. Public opposition to park expansion also mounted in and around Jackson Hole. Albright, in fact, was nearly run out of Jackson, Wyoming, by angry townspeople in 1919 when he traveled there to speak in favor of park expansion.
Local attitudes began to change that same year when proposals to dam Jenny, Emma Matilda, and Two Ocean lakes surfaced. Then on July 26, 1923, local and Park Service representatives including Albright met in Maud Noble's cabin to work on a plan to buy private lands to create a recreation area to preserve the "Old West" character of the valley. Albright was the only person who supported Park Service management; the others wanted traditional hunting, grazing, and dude-ranching activities to continue. In 1927 philanthropist John D. Rockefeller, Jr. founded the Snake River Land Company so he and others could buy land in the area incognito and have it held until the National Park Service could administer it. The company launched a campaign to purchase more than 35,000 acres (142 km²) for $1.4 million, but faced 15 years of opposition by ranchers and a refusal by the Park Service to take the land.
In 1928, a Coordinating Commission on National Parks and Forests met with valley residents and reached an agreement for the establishment of a park. Wyoming Senator John Kendrick then introduced a bill to establish Grand Teton National Park. It was passed by both houses of the U.S. Congress and signed into law by U.S. President Calvin Coolidge on February 26, 1929. The 96,000-acre (388-km²) park was carved from Teton National Forest and included the Teton Range and six glacial lakes at its foot in Jackson Hole. Lobbying by cattlemen, however, meant that the original park borders did not include most of Jackson Hole (whose floor was used for grazing). Meanwhile the Park Service refused to accept the 35,000 acres (142 km²) held by the Snake River Company.
Discouraged by the stalemate, Rockefeller sent a letter to then U.S. President Franklin D. Roosevelt telling him that if the federal government did not accept the land that he intended to make some other disposition of it or to sell it on the market to any satisfactory buyers. Soon afterward on March 15, 1943, the president declared 221,000 acres (894 km²) of public land as Jackson Hole National Monument. Continued controversy over the Rockefeller gift still made it impossible for the monument to officially include that land, however.
Opposition to the monument by local residents immediately followed with criticism that the declaration was a violation of states' rights and that it would destroy the local economy and tax base. Ranchers drove 500 cattle across the newly created monument in a demonstration designed to provoke conflict. The Park Service did not respond to the stunt, but the event brought national attention to the issue nonetheless. Wyoming Representative Frank Barrett introduced a bill to abolish the monument that passed both houses of Congress but was pocket vetoed by Roosevelt. U.S. Forest Service officials did not want to cede another large part of the Teton National Forest to the Park Service so they fought against transfer. One final act was to order forest rangers to gut the Jackson Lake Ranger Station before handing it over to park rangers. Residents in the area who supported the park and the monument were boycotted and harassed.
Other bills to abolish the monument were introduced between 1945 and 1947, but none passed. Increases in tourist income following the end of World War II have been cited as a cause of the change in local attitudes. A move to merge the monument into an enlarged park gained steam and by April 1949, interested parties gathered in the Senate Appropriation Committee chambers to finalize a compromise. The Rockefeller lands were finally transferred from private to public ownership on December 16, 1949, when they were added to the monument. A bill merging most of Jackson Hole National Monument (except for its southern extent, which was added to the National Elk Refuge) into Grand Teton National Park was signed into law by President Harry S. Truman on September 14, 1950. One concession in the law modified the Antiquities Act, limiting the future power of a president to proclaim National Monuments in Wyoming. The scenic highway that extends from the northern border of Grand Teton National Park to the southern entrance of Yellowstone National Park was named the John D. Rockefeller, Jr. Memorial Parkway to recognize Rockefeller's contribution to protecting the area.
Nearly three million people visit Grand Teton National Park each year. The magnificent beauty of the three Tetons—South, Middle, and Grand—is a stunning backdrop for scenic driving and some of the best wildlife viewing anywhere. There are numerous activities to enjoy in the park such as hiking and backpacking on trails for all levels of expertise; biking on the paved and unpaved roads; fishing the waters of Snake River, one of the most popular fishing rivers in the country; and bird-watching. From the marshes along the Snake River to the forests to the alpine tundra there is much to experience.
- Daugherty, John, Stephanie Crockett, William H. Goetzmann, and Reynold G. Jackson. 1999. A place called Jackson Hole: the historic resource study of Grand Teton National Park. Moose, Wyoming: Grand Teton National Park, National Park Service.
- Harris, Ann G., Esther Tuttle, and Sherwood D. Tuttle. 1990. Geology of national parks: Fifth Edition. Dubuque, Iowa: Kendall/Hunt Pub. Co. ISBN 0840346190
All links retrieved January 8, 2014.
- National Park Service. Grand Teton National Park.
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