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Top Attractions in Wyoming

Yellowstone National Park

Yellowstone National Park is a national park located primarily in the U.S. state of Wyoming, although it also extends into Montana and Idaho. It was established by the U.S. Congress and signed into law by President Ulysses S. Grant on March 1, 1872. Yellowstone, widely held to be the first national park in the world, is known for its wildlife and its many geothermal features, especially Old Faithful Geyser, one of the most popular features in the park. It has many types of ecosystems, but the subalpine forest is most abundant. It is part of the South Central Rockies forests ecoregion. Native Americans have lived in the Yellowstone region for at least 11,000 years. The region was bypassed during the Lewis and Clark Expedition in the early 19th century. Aside from visits by mountain men during the early-to-mid-19th century, organized exploration did not begin until the late 1860s. The U.S. Army was commissioned to oversee the park just after its establishment. In 1917, administration of the park was transferred to the National Park Service, which had been created the previous year. Hundreds of structures have been built and are protected for their architectural and historical significance, and researchers have examined more than 1,000 archaeological sites. Yellowstone National Park spans an area of 3,468.4 square miles, comprising lakes, canyons, rivers and mountain ranges. Yellowstone Lake is one of the largest high-elevation lakes in North America and is centered over the Yellowstone Caldera, the largest supervolcano on the continent. The caldera is considered an active volcano. It has erupted with tremendous force several times in the last two million years. Half of the worlds geothermal features are in Yellowstone, fueled by this ongoing volcanism. Lava flows and rocks from volcanic eruptions cover most of the land area of Yellowstone. The park is the centerpiece of the Greater Yellowstone Ecosystem, the largest remaining nearly-intact ecosystem in the Earths northern temperate zone. Hundreds of species of mammals, birds, fish and reptiles have been documented, including several that are either endangered or threatened. The vast forests and grasslands also include unique species of plants. Yellowstone Park is the largest and most famous megafauna location in the Continental United States. Grizzly bears, wolves, and free-ranging herds of bison and elk live in the park. The Yellowstone Park bison herd is the oldest and largest public bison herd in the United States. Forest fires occur in the park each year; in the large forest fires of 1988, nearly one third of the park was burnt. Yellowstone has numerous recreational opportunities, including hiking, camping, boating, fishing and sightseeing. Paved roads provide close access to the major geothermal areas as well as some of the lakes and waterfalls. During the winter, visitors often access the park by way of guided tours that use either snow coaches or snowmobiles.

Upper Geyser Basin

Upper Geyser Basin has the highest concentration of geothermal features in the park. This complement of features includes the most famous geyser in the park, Old Faithful Geyser, as well as four other predictable large geysers. One of these large geysers in the area is Castle Geyser which is about 1,400 feet northwest of Old Faithful. Castle Geyser has an interval of approximately 13 hours between major eruptions, but is unpredictable after minor eruptions. The other three predictable geysers are Grand Geyser, Daisy Geyser, and Riverside Geyser. Biscuit Basin and Black Sand Basin are also within the boundaries of Upper Geyser Basin. The hills surrounding Old Faithful and the Upper Geyser Basin are reminders of Quaternary rhyolitic lava flows. These flows, occurring long after the catastrophic eruption of 640,000 years ago, flowed across the landscape like stiff mounds of bread dough due to their high silica content.

Grand Teton National Park

Grand Teton National Park is a United States National Park in northwestern Wyoming. At approximately 310,000 acresthe park includes the major peaks of the 40-mile-long Teton Range as well as most of the northern sections of the valley known as Jackson Hole. It is only 10 miles south of Yellowstone National Park, to which it is connected by the National Park Service-managed John D. Rockefeller, Jr. Memorial Parkway. Along with surrounding National Forests, these three protected areas constitute the almost 18,000,000-acre Greater Yellowstone Ecosystem, one of the largest intact mid-latitude temperate ecosystems in the world. Human history of the Grand Teton region dates back at least 11,000 years, when the first nomadic hunter-gatherer Paleo-Indians began migrating into the region during warmer months pursuing food and supplies. In the early 19th century, the first White explorers encountered the eastern Shoshone natives. Between 1810 and 1840, the region attracted fur trading companies that vied for control of the lucrative beaver pelt trade. U.S. Government expeditions to the region commenced in the mid-19th century as an offshoot of exploration in Yellowstone, with the first permanent white settlers in Jackson Hole arriving in the 1880s. Efforts to preserve the region as a national park commenced in the late 19th century, and in 1929 Grand Teton National Park was established, protecting the major peaks of the Teton Range. The valley of Jackson Hole remained in private ownership until the 1930s, when conservationists led by John D. Rockefeller, Jr. began purchasing land in Jackson Hole to be added to the existing national park. Against public opinion and with repeated Congressional efforts to repeal the measures, much of Jackson Hole was set aside for protection as Jackson Hole National Monument in 1943. The monument was abolished in 1950 and most of the monument land was added to Grand Teton National Park. Grand Teton National Park is named for Grand Teton, the tallest mountain in the Teton Range. The naming of the mountains is attributed to early 19th-century French-speaking trappers—les trois tétons was later anglicized and shortened to Tetons. At 13,775 feetGrand Teton abruptly rises more than 7,000 feet above Jackson Hole, almost 850 feet higher than Mount Owen, the second-highest summit in the range. The park has numerous lakes, including 15-mile-long Jackson Lake as well as streams of varying length and the upper main stem of the Snake River. Though in a state of recession, a dozen small glaciers persist at the higher elevations near the highest peaks in the range. Some of the rocks in the park are the oldest found in any U.S. National Park and have been dated at nearly 2.7 billion years. Grand Teton National Park is an almost pristine ecosystem and the same species of flora and fauna that have existed since prehistoric times can still be found there. More than 1,000 species of vascular plants, dozens of species of mammals, 300 species of birds, more than a dozen fish species and a few species of reptiles and amphibians exist. Due to various changes in the ecosystem, some of them human-induced, efforts have been made to provide enhanced protection to some species of native fish and the increasingly threatened whitebark pine. Grand Teton National Park is a popular destination for mountaineering, hiking, fishing and other forms of recreation. There are more than 1,000 drive-in campsites and over 200 miles of hiking trails that provide access to backcountry camping areas. Noted for world-renowned trout fishing, the park is one of the few places to catch Snake River fine-spotted cutthroat trout. Grand Teton has several National Park Service-run visitor centers, and privately operated concessions for motels, lodges, gas stations and marinas.

Moose

Moose is an unincorporated community in Teton County, Wyoming, United States, in the Jackson Hole valley. It has a US Post Office, with the zip code of 83012. The town is located within Grand Teton National Park along the banks of the Snake River. It is populated mostly by families with inholdings within the borders of the park. The name Moose can also refer to the small community of Park Service houses located immediately behind the Administration offices. These houses are exclusively inhabited by Park Service employees and their families. The National Park Service maintains the Grand Teton National Park headquarters in Moose, as well as the park visitor center. A local non-profit, the Grand Teton Association, also maintains some facilities in the area to help further the NPS mission. Olaus and Margaret Murie and Olaus' brother Adolph lived in Moose for much of their lives. Today the family ranch is home to the non-profit organization, The Murie Center, whose mission is bringing people together to inspire action that preserves nature, and is administered in partnership with the National Park. The Ranch was designated a National Historic Landmark in 2006. The residents in Moose are counted as part of the Moose–Wilson Road census-designated place, but most of the residents live on the east side of the Snake River stretching as far south as Jackson Hole Airport, and as far north as Shadow Mountain. Most of the ranches and residences along the Moose–Wilson Road have been turned over to the national park, including John D. Rockefeller, Jr.'s JY Ranch and the Murie Ranch. The commercial area in the community is centered mainly around the shops and restaurants of the Dornan family ranch inholding. Given its central location in the Jackson Hole valley, Moose has been the setting for several motion pictures, including The Far Horizons in 1955.

Rock Springs

Rock Springs is a city in Sweetwater County, Wyoming, United States. The population was 23,036 at the 2010 census. Rock Springs is the principal city of the Rock Springs micropolitan statistical area, which has a population of 37,975. Rock Springs is known as the Home of 56 Nationalities because of the influx of immigrants from all over the world who came to work in the coal mines that supplied the fuel to power the steam engines of the Union Pacific Railroad. The citys rich cultural heritage is celebrated each summer on International Day, a festival where the foods, costumes, and traditions of residents ancestors are recreated and enjoyed at Bunning Park in downtown Rock Springs. Rock Springs is the site of Western Wyoming Community College and Wyomings Big Show, a yearly event with a carnival and concerts which is held at the Sweetwater County Events Complex. Rock Springs is located in an energy-rich region with many oil and natural gas wells.

Norris Geyser Basin

The Norris Geyser Basin is the hottest geyser basin in the park and is located near the northwest edge of Yellowstone Caldera near Norris Junction and on the intersection of three major faults. The Norris-Mammoth Corridor is a fault that runs from Norris north through Mammoth to the Gardiner, Montana, area. The Hebgen Lake fault runs from northwest of West Yellowstone, Montana, to Norris. This fault experienced an earthquake in 1959 that measured 7.4 on the Richter scale (sources vary on exact magnitude between 7.1 and 7.8; see 1959 Hebgen Lake earthquake). Norris Geyser Basin is so hot and dynamic because these two faults intersect with the ring fracture zone that resulted from the creation of the Yellowstone Caldera of 640,000 years ago. The Basin consists of three main areas: Porcelain Basin, Back Basin, and One Hundred Springs Plain. Unlike most of other geyser basins in the park, the waters from Norris are acidic rather than alkaline (for example, Echinus Geyser has a pH of ~3.5). The difference in pH allows for a different class of bacterial thermophiles to live at Norris, creating different color patterns in and around the Norris Basin waters. The Ragged Hills that lie between Back Basin and One Hundred Springs Plain are thermally altered glacial kames. As glaciers receded the underlying thermal features began to express themselves once again, melting remnants of the ice and causing masses of debris to be dumped. These debris piles were then altered by steam and hot water flowing through them. Madison lies within the eroded stream channels cut through lava flows formed after the caldera eruption. The Gibbon Falls lies on the caldera boundary as does Virginia Cascades.

Moran Junction

Moran is an unincorporated community in south central Teton County, Wyoming, United States, which serves as one of the principal fee collection entrances to Grand Teton National Park. It lies in Grand Teton National Park northeast of the city of Jackson, the county seat of Teton County, at the intersection of U.S. Routes 26, 89, 191, and 287. Its elevation is 6,749 feet . As the community has had two different names, the Board on Geographic Names officially ruled in favor of "Moran" in 1970. Although Moran is unincorporated, it has a post office, with the ZIP code of 83013. Moran is part of the Jackson, WY–ID Micropolitan Statistical Area and it is known as the state's coldest continually inhabited place, with a record low of -63 °F registered in the winter of 1933. The high altitude at which the village is located, as well as the effects of radiational cooling, cause particularly severe conditions in the winter.

Old Faithful Historic District

The Old Faithful Historic District in Yellowstone National Park comprises the built-up portion of the Upper Geyser Basin surrounding the Old Faithful Inn and Old Faithful Geyser. It includes the Old Faithful Inn, designed by Robert Reamer and itself a National Historic Landmark, the upper and lower Hamiltons Stores, the Old Faithful Lodge, designed by Gilbert Stanley Underwood, the Old Faithful Snow Lodge, and a variety of supporting buildings. The Old Faithful Historic District itself lies on the 140-mile Grand Loop Road Historic District. A notable missing portion of the district is the Old Faithful Museum of Thermal Activity, which formed part of the trailside museum group that includes the Madison Museum, Norris Museum and Fishing Bridge Museum, all listed as National Historic Landmarks. The Old Faithful Museum was torn down in 1971 to make way for the Mission 66 visitor center, which in turn has been replaced by the Old Faithful Visitor Education Center.

Cirque of the Towers

The Cirque of the Towers is located in the Wind River Range Wyoming, U.S., part of which is in the Bridger Wilderness in Bridger-Teton National Forest, while the remainder is in the Popo Agie Wilderness in Shoshone National Forest. Located in the southern section of the Wind River Range , the cirque is a very popular destination for technical rock climbers. Climber Orrin Bonney gave the area its current name in 1941 after his survey of the cirque. Prior to this, few if any visitors had ventured into the cirque due to the remote location. The cirque is an almost circular hole or valley carved by a glacier that retreated over 8,000 years ago. As is true with the rest of the Winds, the mountains are composed almost entirely of granite. The Continental Divide spans the crest of the main peaks. The towers average 1,000 feet lower in altitude than the highest mountains in the northern Winds, with Lizard Head Peak (12,847 ft (3,916 m)) being the tallest. Other individual mountains in the cirque include Shark's Nose, Warbonnet, Warrior Peak, Wolf's Head and Pingora Peak. There are hundreds of routes to choose from in difficulties ranging from 5.1 to 5.11a and since the mountains are composed primarily of granite rock, there is good anchoring. These climbs include two featured in Steck and Roper's Fifty Classic Climbs of North America the Northeast Face of Pingora (IV, 5.9) and the East Ridge of the Wolf's Head (III, 5.6). For both the climber and backpacker, access to the cirque from the west from Pinedale, Wyoming requires a 55 mi (89 km) drive, partly paved and partly gravel, to the Big Sandy trailhead. There is a small National Forest campground at the trailhead. An 8.7 mi (14.0 km) hike beginning at 9,000 ft (2,700 m) above sea level is relatively level the first 7 mi (11 km) and becomes very steep the last mile (1.6 km) and ascends to Jackass Pass at 10,800 ft (3,300 m), crossing the continental divide. From there one must descend a steep half mile (800 m) to Lonesome Lake, which is one of four lakes in the cirque. Expect the trail to be busy in July and August as the cirque is the most popular hiking and climbing destination in the Wind River Range. Lonesome Lake was the first lake in the Wind River Range whose water was deemed unfit for consumption due to human waste and consequently, no camping is permitted within a quarter mile (400 m) of the lake. The granitic rocks allow poor filtration of ground water and the ability of many alpine lakes to cleanse themselves is often poorer than one might find at lower altitudes.
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