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Garnet Canyon
Garnet Canyon is located in Grand Teton National Park in the U.S. state of Wyoming. The canyon was formed by retreating glaciers which reached their last glacial maximum around 15,000 years ago. While Garnet Canyon is a less popular destination for recreational hikers than nearby Cascade Canyon or Death Canyon, it is an important approach to many significant and popular mountaineering climbs including routes found on Grand Teton, Middle Teton, South Teton and Disappointment Peak. The trailhead for Garnet Canyon is found at Lupine Meadows, and the canyon itself is reached after several miles of hiking through forest and switchbacks which climb a large lateral moraine. The entrance to the canyon is guarded by a boulderfield that requires some Class 3 scrambling to cross. Beyond the boulderfield is the popular camping area known as the Meadows, above which the canyon divides into north and south forks. The north fork leads up to the lower saddle between Middle Teton and Gra ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nez Perce Peak
Nez Perce Peak () is located in the Teton Range, Grand Teton National Park, Wyoming, immediately southeast of Grand Teton. The peak is in the central portions of the range, immediately east of Cloudveil Dome and is sometimes considered to be part of what is collectively known as the Cathedral Group. Nez Perce rises to the south of Garnet Canyon and is a dramatic peak that dominates the skyline to the west of Bradley and Taggart Lakes. When viewed from the western section of Jackson Hole Jackson Hole (originally called Jackson's Hole by mountain men) is a valley between the Gros Ventre and Teton mountain ranges in the U.S. state of Wyoming, near the border with Idaho, in Teton County, one of the richest counties in the Unit ..., Nez Perce often obscures the view of Cloudveil Dome as well as South Teton, even though both summits are higher. References {{Mountains of Wyoming Mountains of Grand Teton National Park Mountains of Wyoming Mountains of Teton County, Wyom ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
South Teton
South Teton () is the fifth-highest peak in the Teton Range, Grand Teton National Park, in the U.S. state of Wyoming. The peak is south of Middle Teton and just west of Cloudveil Dome and is part of the Cathedral Group of high Teton peaks. The Teton Range is the youngest mountain chain in the Rocky Mountains, and began their uplift 9 million years ago, during the Miocene. Several periods of glaciation have carved South Teton and the other peaks of the range into their current shapes. Climbing South Teton was first climbed on August 29, 1923 by Albert R. Ellingwood and Eleanor Davis. Ellingwood made the first ascent of Middle Teton the same day. Davis was the first woman to ascend Grand Teton. The easiest climbing route is via Garnet Canyon to an altitude of . From there a trail leads southwest towards a pass between South and Middle Teton. Most ascents of the summit are made from this pass. A number of more difficult ascents are also done by experienced climbers, with diffic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canyons Of The Teton Range
The canyons of the Teton Range lie almost entirely within Grand Teton National Park in the U.S. state of Wyoming. Ranging from to less than in length and up to deep, the canyons were carved primarily by glaciers over the past 250,000 years. The canyons in the Teton Range descend in altitude generally west to east and many have lakes at their outlets. The lakes were created by terminal moraines left behind by the now retreated glaciers. A few of the canyons have small glaciers that were created mostly during the Little Ice Age (1550-1850). Fast retreating Schoolroom Glacier is a tiny glacier located at the head of the South Cascade Canyon. Most of the canyons have streams from which rain and snowmelt flow towards Jackson Hole valley, and due to the sometimes rapid altitude descent, waterfalls are common. The canyons offer the easiest hiking access into the Teton Range. Teton Range canyons within Grand Teton National Park *Webb Canyon is long and originates at several alpine l ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jenny Lake Ranger Station Historic District
The Jenny Lake Ranger Station Historic District comprises an area that was the main point of visitor contact in Grand Teton National Park from the 1930s to 1960. Located near Jenny Lake, the buildings are a mixture of purpose-built structures and existing buildings that were adapted for use by the National Park Service. The ranger station was built as a cabin by Lee Mangus north of Moose, Wyoming about 1925 and was moved and rebuilt around 1930 for Park Service use. A store was built by a concessioner, and comfort stations were built to Park Service standard plans. All buildings were planned to the prevailing National Park Service Rustic style, although the ranger station and the photo shop were built from parts of buildings located elsewhere in the park. Ranger station The ranger station was reconstructed from a cabin originally built by Lee Manges about 1925 which was acquired by the National Park Service in 1930 and moved to the present site. The small rectangular log cabin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
National Park Service
The National Park Service (NPS) is an agency of the United States federal government within the U.S. Department of the Interior that manages all national parks, most national monuments, and other natural, historical, and recreational properties with various title designations. The U.S. Congress created the agency on August 25, 1916, through the National Park Service Organic Act. It is headquartered in Washington, D.C., within the main headquarters of the Department of the Interior. The NPS employs approximately 20,000 people in 423 individual units covering over 85 million acres in all 50 states, the District of Columbia, and US territories. As of 2019, they had more than 279,000 volunteers. The agency is charged with a dual role of preserving the ecological and historical integrity of the places entrusted to its management while also making them available and accessible for public use and enjoyment. History Yellowstone National Park was created as the first national par ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Middle Teton
Middle Teton () is the third-highest peak in the Teton Range, in the U.S. state of Wyoming. Located within Grand Teton National Park, the peak is immediately southwest of Grand Teton, from which it is separated by a broad high ridge at , known to local climbers as the Lower Saddle. The Middle Teton Glacier is located on the eastern slopes of the peak. Middle Teton is a classic pyramidal alpine peak and is sometimes included as part of the Cathedral Group of high Teton peaks. The Teton Range is the youngest mountain chain in the Rocky Mountains, beginning its uplift 9 million years ago, during the Miocene. Several periods of glaciation have carved Middle Teton and the other peaks of the range into their current shapes. From the Lower Saddle, a distinctive feature known as the black dike appears as a straight line running from near the top of the mountain down . The black dike is a basaltic intrusion that occurred long after the surrounding rock was formed. Climbing The first re ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Pass
A mountain pass is a navigable route through a mountain range or over a ridge. Since many of the world's mountain ranges have presented formidable barriers to travel, passes have played a key role in trade, war, and both Human migration, human and animal migration throughout history. At lower elevations it may be called a hill pass. A mountain pass is typically formed between two volcanic peaks or created by erosion from water or wind. Overview Mountain passes make use of a gap (landform), gap, saddle (landform), saddle, col or notch (landform), notch. A topographic saddle is analogous to the mathematical concept of a saddle surface, with a saddle point marking the highest point between two valleys and the lowest point along a ridge. On a topographic map, passes are characterized by contour lines with an hourglass shape, which indicates a low spot between two higher points. In the high mountains, a difference of between the summit and the mountain is defined as a mountain pas ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scrambling
Scrambling is a mountaineering term for ascending steep terrain using one's hands to assist in holds and balance.''New Oxford American Dictionary''. It is also used to describe terrain that falls between hiking and rock climbing (as a “scramble”). Sure-footedness and a head for heights are essential. Canyoning and stream climbing are other types of scrambling. Overview Scrambling is ascending or traversing a grade without technical apparatus. Unroped ascent in exposed situations is potentially one of the most dangerous of mountaineering activities. As soon as an ascent involves a rope, going up or down, it is no longer a scramble. Alpine scrambling Alpine scrambling is scrambling in high mountains and may not follow a defined or waymarked path. The Seattle Mountaineers climbing organization defines alpine scrambling as follows: Alpine Scrambles are off-trail trips, often on snow or rock, with a 'non-technical' summit as a destination. A non-technical summit is one ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moraine
A moraine is any accumulation of unconsolidated debris (regolith and rock), sometimes referred to as glacial till, that occurs in both currently and formerly glaciated regions, and that has been previously carried along by a glacier or ice sheet. It may consist of partly rounded particles ranging in size from boulders (in which case it is often referred to as boulder clay) down to gravel and sand, in a groundmass of finely-divided clayey material sometimes called glacial flour. Lateral moraines are those formed at the side of the ice flow, and terminal moraines were formed at the foot, marking the maximum advance of the glacier. Other types of moraine include ground moraines (till-covered areas forming sheets on flat or irregular topography) and medial moraines (moraines formed where two glaciers meet). Etymology The word ''moraine'' is borrowed from French , which in turn is derived from the Savoyard Italian ("mound of earth"). ''Morena'' in this case was derived from Proven ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Trailhead
A trailhead is the point at which a trail begins, where the trail is often intended for hiking, biking, horseback riding, or off-road vehicles. Modern trailheads often contain rest rooms, maps, sign posts and distribution centers for informational brochures about the trail and its features, and parking areas for vehicles and trailers. The United States Access Board states "A trailhead is defined as an outdoor space that is designated by an entity responsible for administering or maintaining a trail to serve as an access point to the trail." The intersection of two trails is a trail junction and does not constitute a trailhead. Historically, the cities located at the terminus of major pathways for foot traffic such as the Natchez Trace and the Chisholm Trail were also known as trailheads. For mountain climbing and hiking, the elevation of the trailhead above sea level is posted to give an idea of how high the mountain is above the Height above average terrain, average terrain. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Disappointment Peak (Wyoming)
Disappointment Peak () is in the Teton Range of Wyoming, in Grand Teton National Park and immediately southeast of Grand Teton. The peak is part of the Cathedral Group, a region of the Tetons noted for particularly rugged mountains. Disappointment Peak rises to the north of Garnet Canyon and to the west of Amphitheater and Surprise lakes. The peak has a variety of mountaineering Mountaineering or alpinism, is a set of outdoor activities that involves ascending tall mountains. Mountaineering-related activities include traditional outdoor climbing, skiing, and traversing via ferratas. Indoor climbing, sport climbing, a ... routes, including the most difficult in the range. Disappointment Peak was given its name in 1925 when four Colorado climbers, led by Phil Smith (who was soon to become the first park ranger), set out to climb the Grand, but found an impasse on this peak where a drop is encountered to the saddle between the two summits. After a failed rappel attempt, they ga ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountaineering
Mountaineering or alpinism, is a set of outdoor activities that involves ascending tall mountains. Mountaineering-related activities include traditional outdoor climbing, skiing, and traversing via ferratas. Indoor climbing, sport climbing, and bouldering are also considered variants of mountaineering by some. Unlike most sports, mountaineering lacks widely applied formal rules, regulations, and governance; mountaineers adhere to a large variety of techniques and philosophies when climbing mountains. Numerous local alpine clubs support mountaineers by hosting resources and social activities. A federation of alpine clubs, the International Climbing and Mountaineering Federation (UIAA), is the International Olympic Committee-recognized world organization for mountaineering and climbing. The consequences of mountaineering on the natural environment can be seen in terms of individual components of the environment (land relief, soil, vegetation, fauna, and landscape) and location/z ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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