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Sperry Glacier
Sperry Glacier is a glacier on the north slopes of Gunsight Mountain west of the Continental Divide in Glacier National Park in the U.S. state of Montana. Although many geologic features of Glacier National Park were formed during the much longer period of glaciation ending over 10,000 years ago, Sperry Glacier — like all the glaciers in the park today — is a product of the recent Little Ice Age, the period of cooler average temperatures starting in about the 13th century and concluding in the mid-19th century. Once one of the largest glaciers in the park, the surface area of Sperry Glacier has retreated 75 percent since the mid-19th century. 2005 measurements of the surface area of the glacier resulted in an estimated area of , whereas the glacier is estimated to have covered an area of at the end of the Little Ice Age in the mid-19th century. The glacier lost almost 35 percent of its surface area between 1966 and 2005. The glacier is named for Lyman B. Sperry, a pro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gunsight Mountain (Montana)
Gunsight Mountain () is located in the Lewis Range, Glacier National Park in the U.S. state of Montana. Gunsight Mountain is named after the adjacent Gunsight Pass, which was named by George Bird Grinnell in 1891. Geology Like other mountains in Glacier National Park, Gunsight Mountain is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks thick, wide and long over younger rock of the cretaceous period. See also * Mountains and mountain ranges of Glacier National Park (U.S.) Mountains in Glacier National Park (U.S.) are part of the Rocky Mountains. There are at least 150 named mountain peaks over in Glacier in three mountain ranges--the Clark Range, Lewis Range, Livingston Range. Mount Cleveland at is the high ... References External links * Gunsight ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sperry Glacier
Sperry Glacier is a glacier on the north slopes of Gunsight Mountain west of the Continental Divide in Glacier National Park in the U.S. state of Montana. Although many geologic features of Glacier National Park were formed during the much longer period of glaciation ending over 10,000 years ago, Sperry Glacier — like all the glaciers in the park today — is a product of the recent Little Ice Age, the period of cooler average temperatures starting in about the 13th century and concluding in the mid-19th century. Once one of the largest glaciers in the park, the surface area of Sperry Glacier has retreated 75 percent since the mid-19th century. 2005 measurements of the surface area of the glacier resulted in an estimated area of , whereas the glacier is estimated to have covered an area of at the end of the Little Ice Age in the mid-19th century. The glacier lost almost 35 percent of its surface area between 1966 and 2005. The glacier is named for Lyman B. Sperry, a pro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake McDonald
Lake McDonald is the largest lake in Glacier National Park. It is located at in Flathead County in the U.S. state of Montana. Lake McDonald is approximately 10 miles (16 km) long, and over a mile (1.6 km) wide and 472 feet (130 m) deep, filling a valley formed by a combination of erosion and glacial activity. Lake McDonald lies at an elevation of and is on the west side of the Continental Divide. Going-to-the-Sun Road parallels the lake along its southern shoreline. The surface area of the lake is 6,823 acres (27.6 km2). The lake is home to numerous native species of trout, and other game fish. Catchable species include: westslope cutthroat trout, rainbow trout, bull trout (char), lake trout (char), Lake Superior whitefish, mountain whitefish, kokanee salmon (landlocked sockeye), and suckers. However, the lake is nutrient-poor and is not considered a prime fishing destination. Grizzly bears, black bear, moose, and mule deer are found in many places ne ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Going-to-the-Sun Road
Going-to-the-Sun Road is a scenic mountain road in the Rocky Mountains of the western United States, in Glacier National Park in Montana. The Sun Road, as it is sometimes abbreviated in National Park Service documents, is the only road that traverses the park, crossing the Continental Divide through Logan Pass at an elevation of 6,646 feet (2,026 m), which is the highest point on the road. Construction began in 1921 and was completed in 1932 with formal dedication in the following summer on July 15, 1933. Prior to the construction of the road, visitors would need to spend several days traveling through the central part of the park, an area which can now be traversed within a few hours, excluding any stops for sightseeing or construction. The road is the first to have been registered in all of the following categories: National Historic Place, National Historic Landmark and Historic Civil Engineering Landmark. The road is approximately 50 miles (80 km) long and spans the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bearhat Mountain
Bearhat Mountain () is located in the Lewis Range, Glacier National Park in the U.S. state of Montana. Bearhat Mountain is immediately west of Hidden Lake. The mountain was named after a Kootenai Native American, and was officially adopted by the U.S. Board on Geographic Names in 1932. Based on the Köppen climate classification, Bearhat Mountain has an alpine climate characterized by long, usually very cold winters, and short, cool to mild summers. Temperatures can drop below −10 °F with wind chill factors below −30 °F. Geology Like other mountains in Glacier National Park, Bearhat Mountain is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks thick, wide and long over younger rock of the cretaceous period. See also * Geology of the Rocky Mounta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hidden Lake (Flathead County, Montana)
Hidden Lake is located in Glacier National Park, in the U. S. state of Montana. Hidden Lake is surrounded by numerous peaks, including Bearhat Mountain to the southwest, Dragons Tail to the south, Clements Mountain to the north, and Reynolds Mountain to the east. Hidden Lake is a popular day hike destination, with the Hidden Lake overlook a hike from Logan Pass, and the lakeshore adding another one way. See also *List of lakes in Flathead County, Montana (A-L) There are at least 269 named lakes and reservoirs in Flathead County, Montana. Lakes * Abbot Lake, , el. * Aeneas Lake, , el. * Akaiyan Lake, , el. * Akokala Lake, , el. * Alcove Lake, , el. * Almeda Lake, , el. * Alpha Lake, , el. ... References Lakes of Glacier National Park (U.S.) Lakes of Flathead County, Montana Going-to-the-Sun Road {{FlatheadCountyMT-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Logan Pass
Logan Pass (elevation ) is located along the Continental Divide in Glacier National Park, in the U.S. state of Montana. It is the highest point on the Going-to-the-Sun Road. The pass is named after Major William R. Logan, the first superintendent of the park. The Logan Pass Visitor Center is open during the summer season just east of the pass. The pass is a popular starting point for hiking and backpacking trips. The most popular trail is the Highline Trail which heads north along the west side of the continental divide, through an area known as the Garden Wall, due to the proliferation of wildflowers which grow there during the summer. Just east of the pass, an area known as Big Drift often records over 100 feet (30 m) of snowfall, much of which has been pushed over the continental divide by the prevailing westerly winds during the winter. The pass is closed during the winter due to avalanche hazards and the virtual impossibility of keeping the Going-to-the-Sun Road open, yet is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cairn
A cairn is a man-made pile (or stack) of stones raised for a purpose, usually as a marker or as a burial mound. The word ''cairn'' comes from the gd, cà rn (plural ). Cairns have been and are used for a broad variety of purposes. In prehistoric times, they were raised as markers, as memorials and as burial monuments (some of which contained chambers). In modern times, cairns are often raised as landmarks, especially to mark the summits of mountains. Cairns are also used as trail markers. They vary in size from small stone markers to entire artificial hills, and in complexity from loose conical rock piles to elaborate megalithic structures. Cairns may be painted or otherwise decorated, whether for increased visibility or for religious reasons. A variant is the inuksuk (plural inuksuit), used by the Inuit and other peoples of the Arctic region of North America. History Europe The building of cairns for various purposes goes back into prehistory in Eurasia, ranging in s ... [...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 Provenà ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Edwards Mountain
Edwards Mountain () is located in the Lewis Range, Glacier National Park in the U.S. state of Montana. Edwards Mountain rises just to the west of Sperry Glacier. Based on the Köppen climate classification, Edwards Mountain has an alpine climate characterized by long, usually very cold winters, and short, cool to mild summers. Temperatures can drop below −10 °F with wind chill factors below −30 °F. Geology Like other mountains in Glacier National Park, Edwards Mountain is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks thick, wide and long over younger rock of the cretaceous period. See also * Mountains and mountain ranges of Glacier National Park (U.S.) * Geology of the Rocky Mountains References Mountains of Flathead County, Montana Edwa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Brown (Montana)
Mount Brown () is located in the Lewis Range, Glacier National Park in the U.S. state of Montana. There are conflicting claims about who Mount Brown was named after. A US Park Service publication states it was: "named for William Brown of Chicago, then Solicitor General for the Chicago and Alton Railroad, by some members of his party on a camping and fishing trip to the area around Lake McDonald in 1894. The companions, Charles H. Russell (not the artist) and Frank A. Johnson, climbed this mountain that arose back of their camp, and so named it." However this naming story does not explain how the campers were able make their naming decision known to the public. The 1929 US Geographic Board decision card states that the Board accepted the name Mount Brown in accordance with existing local usage, and states that it was probably named for Louis Brown, a Montana pioneer. Below the summit on the southwestern slopes of Mount Brown is the historic Mount Brown Fire Lookout which was bu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Comeau Pass
Comeau may refer to: People * Anselm-François Comeau, 19th Century Nova Scotia politician * Andy Comeau, actor * Ashley Comeau, actor, improviser, producer * Blake Comeau, hockey player * Carol Comeau, teacher * Chuck Comeau, drummer for Simple Plan * Ed Comeau, former coach of the Orlando Titans * Fredric Gary Comeau, Writer and singer-songwriter * Gerald Comeau, Canadian Senator * Joseph Willie Comeau, Nova Scotia politician * Joey Comeau, writer * Marcel Comeau, Canadian ice hockey coach and NHL executive * Michael G. Comeau, American attorney and politician * Phil Comeau, film director * Rey Comeau, National Hockey League player Fictional characters * Michael Comeau, a fictional character in the ''Scott Pilgrim'' franchise Places * Comeau's Hill, Nova Scotia, a community in Nova Scotia, Canada * Comeau Building, a building in West Palm Beach, Florida * Baie-Comeau, a city in Quebec Other * Comeau C/C++, a code compiler In computing, a compiler is a computer prog ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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