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Mount Grant (Montana)
Mount Grant is an 8,590-foot-elevation (2,618 meter) mountain summit located in Flathead County in the U.S. state of Montana. Description Mount Grant is situated in the Great Bear Wilderness on land managed by Flathead National Forest. Mount Grant is in the Flathead Range, west of the Continental Divide, and the nearest higher peak is Great Northern Mountain, one mile to the northwest. Topographic relief is significant as the west aspect rises above Hungry Horse Reservoir in four miles, and the east aspect rises the same in five miles above the Middle Fork Flathead Valley. Precipitation runoff from the mountain drains east into Tunnel Creek, which is a tributary of Middle Fork Flathead River, and the west slope drains to Hungry Horse Reservoir. Climate According to the Köppen climate classification system, the mountain is located in an alpine subarctic climate zone with long, cold, snowy winters, and cool to warm summers. This climate supports the Grant Glacier on t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Great Northern Mountain
Great Northern Mountain is a prominent mountain summit located in Flathead County in the U.S. state of Montana. It is situated in the Flathead National Forest, in the Flathead Range, west of the Continental Divide. Great Northern Mountain is the highest point in the Great Bear Wilderness, and the nearest higher peak is Mount Saint Nicholas, 10.56 miles to the east-northeast in Glacier National Park. Topographic relief is significant as the west aspect rises above Hungry Horse Reservoir in four miles, and the east aspect rises the same in five miles above the Middle Fork Flathead Valley. The Great Northern Railway is the namesake of the mountain, and the mountain is the namesake of the Great Northern Brewing Company.Ryan Newhouse, ''Montana Beer: A Guide to Breweries in Big Sky Country'', 2013, Arcadia Publishing Incorporated, Climate According to the Köppen climate classification system, the mountain is located in an alpine subarctic climate zone with long, cold, sn ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hungry Horse Reservoir
Hungry Horse Dam is an arch dam in the western United States, on the South Fork Flathead River The South Fork Flathead River is a major river in Northwestern Montana in the northwest United States. It is one of the three main forks of the Flathead River, a tributary of the Clark Fork River (the Pend Oreille River). The north-northwest trend ... in the Rocky Mountains of northwest Montana. It is located in Flathead National Forest in Flathead County, Montana, Flathead County, about south of the west entrance to Glacier National Park (U.S.), Glacier National Park, southeast of Columbia Falls, Montana, Columbia Falls, and northeast of Kalispell, Montana, Kalispell. The Hungry Horse project, dam, and powerplant are operated by the United States Bureau of Reclamation, U.S. Bureau of Reclamation. The entrance road leading to the dam is located in Hungry Horse, Montana, Hungry Horse. The purposes of the Hungry Horse Project authorized by law are irrigation, flood control, navigation ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Flathead County, Montana
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geology Of The Rocky Mountains
The geology of the Rocky Mountains is that of a discontinuous series of mountain ranges with distinct geological origins. Collectively these make up the Rocky Mountains, a mountain system that stretches from Northern British Columbia through central New Mexico and which is part of the great mountain system known as the North American Cordillera. The rocky cores of the mountain ranges are, in most places, formed of pieces of continental crust that are over one billion years old. In the south, an older mountain range was formed 300 million years ago, then eroded away. The rocks of that older range were reformed into the Rocky Mountains. The Rocky Mountains took shape during an intense period of plate tectonic activity that resulted in much of the rugged landscape of the western North America. The Laramide orogeny, about 80–55 million years ago, was the last of the three episodes and was responsible for raising the Rocky Mountains. Subsequent erosion by glaciers has created t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Looking At Mount Grant And Friends From Tunnel Ridge
Looking is the act of intentionally focusing visual perception on someone or something, for the purpose of obtaining information, and possibly to convey interest or another sentiment. A large number of troponyms exist to describe variations of looking at things, with prominent examples including the verbs "stare, gaze, gape, gawp, gawk, goggle, glare, glimpse, glance, peek, peep, peer, squint, leer, gloat, and ogle".Anne Poch Higueras and Isabel Verdaguer Clavera, "The rise of new meanings: A historical journey through English ways of ''looking at''", in Javier E. Díaz Vera, ed., ''A Changing World of Words: Studies in English Historical Lexicography, Lexicology and Semantics'', Volume 141 (2002), p. 563-572. Additional terms with nuanced meanings include viewing,Madeline Harrison Caviness, ''Visualizing Women in the Middle Ages: Sight, Spectacle, and Scopic Economy'' (2001), p. 18. watching,John Mowitt, ''Sounds: The Ambient Humanities'' (2015), p. 3. eyeing,Charles John Smit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Grant Glacier (Montana)
Grant Glacier is located in the US state of Montana in Flathead National Forest. The glacier is situated in a cirque and lies below the east slopes of Mount Grant (). Grant Glacier is southeast of Stanton Glacier and both west of Glacier National Park (U.S.). Images taken of the glacier in 1902 and from the same vantage point in 1998 indicate that the glacier retreated substantially during the 20th Century. See also *List of glaciers in the United States This is a list of glaciers existing in the United States, currently or in recent centuries. These glaciers are located in nine states, all in the Rocky Mountains or farther west. The southernmost named glacier among them is the Lilliput Glacier ... References Glaciers of Flathead County, Montana Glaciers of Montana {{FlatheadCountyMT-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Subarctic Climate
The subarctic climate (also called subpolar climate, or boreal climate) is a climate with long, cold (often very cold) winters, and short, warm to cool summers. It is found on large landmasses, often away from the moderating effects of an ocean, generally at latitudes from 50° to 70°N, poleward of the humid continental climates. Subarctic or boreal climates are the source regions for the cold air that affects temperate latitudes to the south in winter. These climates represent Köppen climate classification ''Dfc'', ''Dwc'', ''Dsc'', ''Dfd'', ''Dwd'' and ''Dsd''. Description This type of climate offers some of the most extreme seasonal temperature variations found on the planet: in winter, temperatures can drop to below and in summer, the temperature may exceed . However, the summers are short; no more than three months of the year (but at least one month) must have a 24-hour average temperature of at least to fall into this category of climate, and the coldest month should a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Köppen Climate Classification
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notably in 1918 and 1936. Later, the climatologist Rudolf Geiger (1894–1981) introduced some changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification system. The Köppen climate classification divides climates into five main climate groups, with each group being divided based on seasonal precipitation and temperature patterns. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Middle Fork Flathead River
The Middle Fork Flathead River is a river in western Montana in the United States, forming the southwestern boundary of Glacier National Park. Its drainage basin lies to the east of the South Fork Flathead River and the Hungry Horse Reservoir. Towns along the river include West Glacier, Nyack, Pinnacle, Essex, and Nimrod. The river's headwaters lie in the Bob Marshall Wilderness at the confluence of two small streams, Strawberry Creek and Bowl Creek. From there, it runs north, receiving many tributaries from glacial valleys to the east and west, most of them inside Glacier National Park. The river begins to parallel U.S. Highway 2 as it winds north-northwest, and after a long and narrow course, the river enters a wider valley and begins to spread out and braid between meadows and forested slopes. It then enters another narrow gorge, turning generally westwards, then passing the southwestern entrance of the national park, receives a tributary from Lake McDonald, a large glacia ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Surface Runoff
Surface runoff (also known as overland flow) is the flow of water occurring on the ground surface when excess rainwater, stormwater, meltwater, or other sources, can no longer sufficiently rapidly infiltrate in the soil. This can occur when the soil is saturated by water to its full capacity, and the rain arrives more quickly than the soil can absorb it. Surface runoff often occurs because impervious areas (such as roofs and pavement) do not allow water to soak into the ground. Furthermore, runoff can occur either through natural or man-made processes. Surface runoff is a major component of the water cycle. It is the primary agent of soil erosion by water. The land area producing runoff that drains to a common point is called a drainage basin. Runoff that occurs on the ground surface before reaching a channel can be a nonpoint source of pollution, as it can carry man-made contaminants or natural forms of pollution (such as rotting leaves). Man-made contaminants in runoff i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Topographic Relief
Terrain or relief (also topographical relief) involves the vertical and horizontal dimensions of land surface. The term bathymetry is used to describe underwater relief, while hypsometry studies terrain relative to sea level. The Latin word (the root of ''terrain'') means "earth." In physical geography, terrain is the lay of the land. This is usually expressed in terms of the elevation, slope, and orientation of terrain features. Terrain affects surface water flow and distribution. Over a large area, it can affect weather and climate patterns. Importance The understanding of terrain is critical for many reasons: * The terrain of a region largely determines its suitability for human settlement: flatter alluvial plains tend to have better farming soils than steeper, rockier uplands. * In terms of environmental quality, agriculture, hydrology and other interdisciplinary sciences; understanding the terrain of an area assists the understanding of watershed boundaries, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Flathead County, Montana
Flathead County is in the U.S. state of Montana. At the 2020 census, its population was 104,357, making it the state's fourth most populous county. Its county seat is Kalispell. Its numerical designation (used in the issuance of license plates) is 7. Its northern border is on the state's north border, making it contiguous with the Canada–US border, facing British Columbia. Flathead County comprises the Kalispell, Montana Micropolitan Statistical Area, with neighboring Lake County following soon after. History Flathead County was founded in 1893. Some sources cite the supposed practice of the Salish tribe flattening infants' heads as the origin of the name Flathead, but there is no record of Salish Indians ever having that appearance. Geography The county includes much of Flathead Lake, the Flathead Valley, and the Flathead River. These natural treasures, originated by glaciers, are named for the unique geological formation of a broad flat valley surrounded by mountains ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
