Sheep Mountain (Alaska)
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Sheep Mountain (Alaska)
Sheep Mountain is a elevation summit located northeast of Palmer, Alaska, Palmer in the southern Talkeetna Mountains of the U.S. state of Alaska. This landmark is set midway between Palmer and Glennallen, Alaska, Glennallen, with the Glenn Highway traversing the southern base of this mountain at mile 113. The mountain is situated west-southwest of Gunsight Mountain, and northeast of Mount Wickersham. The mountain's local name was reported in 1906 by U.S. Geological Survey. It is called ''Beznae'', meaning ''"(a type of) Stone"'', in the Ahtna language.James Kari and James A. Fall, ''Shem Pete's Alaska'', 2nd Ed. 2003, page 308. Climate Based on the Köppen climate classification, Sheep Mountain is located in a subarctic climate zone with long, cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. The months May through June offer the most favorable weather for climbing or viewing. Precipitation Surface runoff, run ...
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Ahtna Language
Ahtna or Ahtena (, from'' ''"Copper River") is the Na-Dené language of the Ahtna ethnic group of the Copper River area of Alaska. The language is also known as Copper River or Mednovskiy. The Ahtna language consists of four different dialects: Upper, Central, Lower, and Western. Three of the four are still spoken today. Ahtna is closely related to Dena'ina. The similar name Atnah occurs in the journals of Simon Fraser and other early European diarists in what is now British Columbia as a reference to the Tsilhqot'in people, another Northern Athapaskan group. Classification Eyak-Athabaskan, Athabaskan, Northern Athabaskan. History Ahtna is one of the eleven Athabaskan languages native to Alaska. The Ahtna language comes from the proto-Athabaskan language possibly evolving 5,000 to 10,000 years ago when humans migrated from Eurasia to The New World over the Bering Sea floor (Beringia) when it was dried up and exposed creating a natural land bridge. Many indigenous Nativ ...
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Mountains Of Alaska
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 ...
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Geography Of Alaska
Alaska occupies the northwestern portion of the North American continent and is bordered only by Canada on the east. It is one of two U.S. states not bordered by another state; Hawaii is the other. Alaska has more ocean coastline than all of the other U.S. states combined. About of Canadian territory separate Alaska from Washington state. Alaska is thus an exclave of the United States that is part of the continental U.S. and the U.S. West Coast, but is not part of the contiguous U.S. Alaska is also the only state, other than Hawaii, whose capital city is accessible only via ship or air, because no roads connect Juneau to the rest of the continent. The state is bordered by Yukon and British Columbia, Canada to the east, the Gulf of Alaska and the Pacific Ocean to the south, Russia ( Chukotka Autonomous Okrug), Bering Sea, the Bering Strait, and Chukchi Sea to the west, and the Beaufort Sea and the Arctic Ocean to the north. Because it extends into the Eastern Hemisphere ...
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Matanuska Formation
The Matanuska Formation consists of more than of sedimentary strata exposed in the northern Chugach Mountains, Matanuska Valley, and southern Talkeetna Mountains of South-Central Alaska. The Matanuska Formation contains strata from Early Cretaceous (Albian) to Late Cretaceous ( Maestrichtian). Parts of the formation contain abundant marine mollusks, foraminifera, and radiolaria. Fossils of non-marine plants are found in some beds. Fossils of two dinosaurs have been recovered from marine mudstones in the formation. The lower Matanuska Formation (MF) is several hundred meters thick and includes non-marine and marine sediments. Campanian-Maastrichtian graded sandstone, conglomerate, and mudstone comprise the upper 2000 meters of the Formation. Invertebrate paleofauna Annelida Calcareous worm tube fossils are known from the formation. Bivalves Cephalopods The formation's thin shelled heteromorphic ammonites probably lived at depths of 36–183 m. The formation's ammonites gen ...
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Matanuska River
The Matanuska River ( Dena'ina: ''Ch'atanhtnu''; Ahtna: ''Ts'itonhna’'') is a 75-mile (121 km) long river in Southcentral Alaska, United States. The river drains a broad valley south of the Alaska Range eponymously known as the Matanuska Valley. Course Formed by the confluence of its east and south forks, the Matanuska River flows generally southwest to the Knik Arm of Cook Inlet. Downstream of its source, the river is joined by meltwater from Matanuska Glacier in the northern Chugach Mountains. From there it continues through the Matanuska Valley, between the Chugach Mountains to the south and the Talkeetna Mountains to the north. Population centers along its course include Chickaloon, Sutton, Palmer, and Butte. It enters the Knik Arm of Cook Inlet about southwest of Palmer and about northeast of Anchorage. The Glenn Highway runs roughly parallel to the river for much of its length. Highway bridges over the river, listed from source to mouth, include Glacier Park B ...
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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 ...
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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 ave ...
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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'' indi ...
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Mount Wickersham
Mount Wickersham is a elevation mountain summit located east of Palmer, in the northern Chugach Mountains of the U.S. state of Alaska. This landmark of the Matanuska Valley is set midway between Anchorage and Glennallen, at mile 101 of the Glenn Highway. It is situated immediately west of Matanuska Glacier, and east of Amulet Peak. The mountain was named in 1960 by Senator Bob Bartlett and Secretary of the Interior Fred A. Seaton, to remember James Wickersham (1857–1939), attorney, District Judge, and Territorial Delegate to Congress from Alaska.''Dictionary of Alaska Place Names'', Donald J. Orth author, United States Government Printing Office (1967), page 1046. In June 1903, Wickersham was also leader of the (unsuccessful) first attempt to climb Denali (Mount McKinley at that time). His attempt was stymied by steep cliffs which also now bear his name, Wickersham Wall. Climate Based on the Köppen climate classification, Mount Wickersham is located in a subarctic c ...
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Matanuska-Susitna Borough, Alaska
Matanuska-Susitna Borough (often referred to as the Mat-Su Borough) is a borough located in the U.S. state of Alaska. Its county seat is Palmer, and the largest community is the census-designated place of Knik-Fairview. The borough is part of the Anchorage Metropolitan Statistical Area, along with the municipality of Anchorage on its south. The Mat-Su Borough is so designated because it contains the entire Matanuska and Susitna Rivers. They empty into Cook Inlet, which is the southern border of the Mat-Su Borough. It is one of the few agricultural areas of Alaska. Geography The borough seat is Palmer, and the largest community is the census-designated place of Knik-Fairview, Alaska. As of the 2020 census, the population was 107,081, up from 88,995 in 2010. It is the fastest growing subdivision in Alaska. According to the U.S. Census Bureau, the borough has a total area of , of which is land and (2.6%) is water. Adjacent boroughs and census areas * Denali Borough, ...
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Gunsight Mountain
Gunsight Mountain is a prominent elevation summit located northeast of Palmer in the Talkeetna Mountains of the U.S. state of Alaska. This landmark is set midway between Palmer and Glennallen, with the Glenn Highway traversing the southern base of this mountain. This remote mountain is situated at the east end of Sheep Mountain, and northeast of Mount Wickersham, its nearest higher peak. The mountain's descriptive local name was reported in 1952 by U.S. Geological Survey, and derives from a conspicuous deep notch in the summit ridge which has the appearance of a gunsight. This mountain is called ''Siz'aani'', meaning ''"Heart"'', in the Ahtna language.James Kari and James A. Fall, ''Shem Pete's Alaska'', 2nd Ed. 2003, page 309. Climate Based on the Köppen climate classification, Gunsight Mountain is located in a subarctic climate zone with long, cold, snowy winters, and mild summers. Winter temperatures can drop below −20 °C with wind chill factors below −30  ...
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