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| Bow Glacier Falls | |
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| Coordinates | 51°39′23″N116°29′48″W / 51.656397°N 116.49663°W |
| Type | Tiered |
| Total height | 410 feet (120 m) |
| Total width | 75 feet (23 m) |
| Watercourse | Bow River |
Bow Glacier Falls is located near Banff, AB. The falls originates from melt water from the Bow Glacier and flows into Bow Lake. [1]
Yosemite Valley is a glacial valley in Yosemite National Park in the western Sierra Nevada mountains of Central California, United States. The valley is about 7.5 mi (12.1 km) long and 3,000–3,500 ft (910–1,070 m) deep, surrounded by high granite summits such as Half Dome and El Capitan, and densely forested with pines. The valley is drained by the Merced River, and a multitude of streams and waterfalls flow into it, including Tenaya, Illilouette, Yosemite and Bridalveil Creeks. Yosemite Falls is the highest waterfall in North America and is a big attraction, especially in the spring, when the water flow is at its peak. The valley is renowned for its natural environment and is regarded as the centerpiece of Yosemite National Park.
Scouting in Montana has a long history, from the 1910s to the present day, serving thousands of youth in programs that suit the environment in which they live.
Banff National Park is Canada's oldest national park, established in 1885 as Rocky Mountains Park. Located in Alberta's Rocky Mountains, 110–180 kilometres (68–112 mi) west of Calgary, Banff encompasses 6,641 square kilometres (2,564 sq mi) of mountainous terrain, with many glaciers and ice fields, dense coniferous forest, and alpine landscapes. Provincial forests and Yoho National Park are neighbours to the west, while Kootenay National Park is located to the south and Kananaskis Country to the southeast. The main commercial centre of the park is the town of Banff, in the Bow River valley.
Mount Forbes is the seventh tallest mountain in the Canadian Rockies and the tallest within the boundaries of Banff National Park. It is located in southwestern Alberta, 18 km (11 mi) southwest of the Saskatchewan River Crossing in Banff. The mountain was named by James Hector in 1859 after Edward Forbes, Hector's natural history professor at the University of Edinburgh during the mid-19th century.
Mendenhall Glacier is a glacier about 13.6 miles (21.9 km) long located in Mendenhall Valley, about 12 miles (19 km) from downtown Juneau in the southeast area of the U.S. state of Alaska. The glacier and surrounding landscape is protected as part of the 5,815 acres (2,353 ha) Mendenhall Glacier Recreation Area, a federally designated unit of the Tongass National Forest.
The Medicine Bow Mountains are a mountain range in the Rocky Mountains that extend 100 miles (160 km) from northern Colorado into southern Wyoming. The northern extent of this range is the sub-range the Snowy Range. From the northern end of Colorado's Never Summer Mountains, the Medicine Bow mountains extend north from Cameron Pass along the border between Larimer and Jackson counties in Colorado and northward into south central Wyoming. In Wyoming, the range sits west of Laramie, in Albany and Carbon counties to the route of the Union Pacific Railroad and U.S. Interstate 80. The mountains often serve as a symbol for the city of Laramie. The range is home to Snowy Range Ski Area.
Peyto Lake is a glacier-fed lake in Banff National Park in the Canadian Rockies. The lake itself is near the Icefields Parkway. It was named for Bill Peyto, an early trail guide and trapper in the Banff area.
Bow Valley Provincial Park is a provincial park in Alberta, Canada. Established in 1959 in the arch of the Bow River at its confluence with the Kananaskis River, the park is one park of many within the Kananaskis Country park system.
Bow Glacier is located in Banff National Park, Alberta, Canada, approximately 37 km (23 mi) northwest of Lake Louise. It can be viewed from the Icefields Parkway. Bow Glacier is an outflow glacier from the Wapta Icefield, which rests along the Continental Divide, and runoff from the glacier supplies water to Bow Lake and the Bow River. The glacier is credited for creating the Bow Valley before retreating at the end of the last glacial maximum.
The Waputik Icefield is located on the Continental divide in the Canadian Rocky Mountains, in the provinces of British Columbia and Alberta. It is developed on the heights of the Waputik Range in the Central Main Ranges.
The Wapta Icefield is a series of glaciers located on the Continental Divide in the Waputik Mountains of the Canadian Rockies, in the provinces of British Columbia and Alberta, in Yoho National Park in the Canadian Rockies. The icefield is shared by Banff and Yoho National Parks and numerous outlet glaciers extend from the icefield, including the Vulture, Bow and Peyto Glaciers. Runoff from the icefields and outlet glaciers supply water to both the Kicking Horse and Bow Rivers, as well as numerous streams and lakes.
The Stanley Mitchell hut is an alpine hut located at an altitude of 2,060 metres (6,759 ft) in the Little Yoho Valley in Yoho National Park, British Columbia, Canada. It sits in a small meadow not far from the base of a mountain called The President. It serves as a base for hiking, scrambling, ski-touring and climbing the nearby mountains. The hut is maintained by the Alpine Club of Canada.
Bow Lake is a small lake in western Alberta, Canada. It is located on the Bow River, in the Canadian Rockies, at an altitude of 1920 m.
The Bow Range is a mountain range of the Canadian Rockies in Alberta and British Columbia, Canada. The range is named in association with the Bow River and was officially adopted on March 31, 1917 by the Geographic Board of Canada.
Blood Falls is an outflow of an iron oxide–tainted plume of saltwater, flowing from the tongue of Taylor Glacier onto the ice-covered surface of West Lake Bonney in the Taylor Valley of the McMurdo Dry Valleys in Victoria Land, East Antarctica.
Nugget Falls, also known as Nugget Creek Falls or Mendenhall Glacier Falls, is a waterfall downstream of the Nugget Glacier, at the base of Bullard Mountain, in the U.S. state of Alaska. Formed by the creek from the Nugget Glacier, the waterfall drops 377 feet (115 m) in two tiers of 99 feet (30 m) and 278 feet (85 m) onto a sandbar in Mendenhall Lake, which is the freshwater pool at the face of the Mendenhall Glacier. The lake then drains via Mendenhall River into the Inside Passage. The waterfall is fed by Nugget Creek, which is in turn fed by the Nugget Glacier, a tributary glacier on the mountainside east of Auke Bay. The creek cascades down towards Mendenhall Lake, forming a hanging valley, then plunges over the falls to the lake. Prior to the recession of Mendenhall Glacier, it was said that the falls would drop "directly on the glacier", or that the "glacier covered the waterfall".
Ahern Glacier is in Glacier National Park in the U.S. state of Montana. The glacier was named after George Patrick Ahern. Ahern Glacier is situated on a ridge between Ipasha Peak to the north and Ahern Peak to the south at an elevation between 8,800 feet (2,700 m) and 8,000 feet (2,400 m) above sea level, immediately east of the Continental Divide. Meltwater from the glacier feeds Ahern Glacier Falls, a waterfall which descends an estimated 1,680 feet (510 m) in one sheer drop to a talus slope below en route to Helen Lake. Between 1966 and 2005, Ahern Glacier lost 13 percent of its surface area.
The Regional designations of Montana vary widely within the U.S state of Montana. The state is a large geographical area that is split by the Continental Divide, resulting in watersheds draining into the Pacific Ocean, Gulf of Mexico and Hudson's Bay. The state is approximately 545 miles (877 km) east to west along the Canada–United States border and 320 miles (510 km) north to south. The fourth largest state in land area, it has been divided up in official and unofficial ways into a variety of regions. Additionally, Montana is part of a number of larger federal government administrative regions.
Bow Mountain is located in the northern Wind River Range in the U.S. state of Wyoming. Situated 1 mi (1.6 km) west of American Legion Peak, Bow Mountain is in the Bridger Wilderness of Bridger-Teton National Forest. Stroud Glacier lies just to the north of the peak. Bow Mountain is the 29th tallest peak in Wyoming.
Lake Jordan was a glacial lake formed during the late Pleistocene along the Jordan River. After the Laurentide Ice Sheet retreated, water melting off the glacier accumulated between the Rocky Mountains and the ice sheet. The lake drained along the front of the ice sheet, eastward towards the Yellowstone River and Glacial Lake Glendive.
| Authority control databases: Geographic |
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