Amatusuk Hills
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Amatusuk Hills
Amatusuk Hills is a mountain range in North Slope Borough, Alaska, in the United States. It is part of the Brooks Range. Amatusuk is likely a name of Indigenous origin of unknown meaning. History In 1838, Amatusuk Hills was noted in A.F. Kashevarov's Coastal Explorations in Northwest Alaska as "the last elevation of note that a coastal traveller heading north will see in northwest Alaska". In 1920, Archdeacon Stuck published the name as 'Amahk-too-sook'. It has been variously spelled as: Amahtooscok Mountain, Amatosuk Hills, Amatusak Hills, and Amooktoosuk Hills. The inland area is known for hunting, fishing, and fur trapping. The Inupiat residents of Point Lay used the rivers as navigational points, but only during bad weather. The Kukpowruk River The Kukpowruk River is a stream, long, in the western North Slope Borough of the U.S. state of Alaska. It arises in the De Long Mountains of the western Brooks Range and flows north into Kasegaluk Lagoon of the Chukchi Sea, Arc ...
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North Slope Borough, Alaska
The North Slope Borough is the northernmost borough in the US state of Alaska and, thus, the northernmost county or equivalent of the United States as a whole. As of the 2020 census, the population was 11,031. The borough seat and largest city, comprising nearly half of the borough’s population, is Utqiaġvik (known as Barrow from 1901 to 2016), the northernmost settlement in the United States. History The borough was established in 1972 by an election of the majority Indigenous people in the region, following Congressional passage of the Alaska Native Claims Settlement Act. Most are Inupiat. The borough was named for the Alaska North Slope basin. In 1974, it adopted a Home Rule Charter, enabling it to exercise any legitimate governmental power. The borough has first-class status and exercises the powers of planning, zoning, taxation, and schools.
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United States
The United States of America (USA), also known as the United States (U.S.) or America, is a country primarily located in North America. It is a federal republic of 50 U.S. state, states and a federal capital district, Washington, D.C. The 48 contiguous states border Canada to the north and Mexico to the south, with the semi-exclave of Alaska in the northwest and the archipelago of Hawaii in the Pacific Ocean. The United States asserts sovereignty over five Territories of the United States, major island territories and United States Minor Outlying Islands, various uninhabited islands in Oceania and the Caribbean. It is a megadiverse country, with the world's List of countries and dependencies by area, third-largest land area and List of countries and dependencies by population, third-largest population, exceeding 340 million. Its three Metropolitan statistical areas by population, largest metropolitan areas are New York metropolitan area, New York, Greater Los Angeles, Los Angel ...
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Brooks Range
The Brooks Range (Gwich’in language, Gwich'in: ''Gwazhał'') is a mountain range in far northern North America stretching some from west to east across northern Alaska into Canada's Yukon Territory. Reaching a peak elevation of on Mount Isto, the range is believed to be approximately 126 million years old. In the United States, these mountains are considered a subrange of the Rocky Mountains, whereas in Canada they are considered separate, as the northern border of the Rocky Mountains is considered to be the Liard River far to the south in the province of British Columbia. While the range is mostly uninhabited, the Dalton Highway and Trans-Alaska Pipeline System run through the Atigun Pass (1,415 m, 4,643 ft) on their way to the oil fields at Prudhoe Bay on Alaska's Alaska North Slope, North Slope. The Alaska Native villages of Anaktuvuk Pass, Alaska, Anaktuvuk and Arctic Village, Alaska, Arctic Village, as well as the very small communities of Coldfoot, Alaska, Coldfoot ...
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Iñupiat
The Inupiat (singular: Iñupiaq), also known as Alaskan Inuit, are a group of Alaska Natives whose traditional territory roughly spans northeast from Norton Sound on the Bering Sea to the northernmost part of the Canada–United States border. Their current communities include 34 villages across ''Iñupiat Nunaat'' (Iñupiaq lands), including seven Alaskan villages in the North Slope Borough, affiliated with the Arctic Slope Regional Corporation; eleven villages in Northwest Arctic Borough; and sixteen villages affiliated with the Bering Straits Regional Corporation."Inupiaq (Inupiat)—Alaska Native Cultural Profile."
''www.nnlm.nlm.nih.gov'' ''National Network of Libraries of Medicine.'' Retrieved 4 Dec 2013.
They often claim to be the first people of the
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Point Lay, Alaska
Point Lay (''Kali ''in Inupiaq- "Mound") is a census-designated place (CDP) in North Slope Borough, Alaska, United States. At the 2020 census the population was 330, up from 189 in 2010. Geography and climate Point Lay is located on the shores of the Chukchi Sea. According to the United States Census Bureau, the CDP has a total area of , of which, of it is land and of it (11.66%) is water. Point Lay once was on a barrier island of Kasegaluk Lagoon, but moved to the mainland near the mouth of the Kokolik River during the 1970s. A weather station was operated from October 1949 to March 1958. Apart from its landmass that is in mainland Alaska, it also consists two peninsulas that are found on its most northwestern side. Point Lay has a tundra climate (Koppen ET) with long, very cold winters and short, cool to mild summers. Demographics Point Lay first appeared on the 1880 U.S. Census as an unincorporated Inuit village. All 30 of its residents were Inuit. It returned ag ...
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Kukpowruk River
The Kukpowruk River is a stream, long, in the western North Slope Borough of the U.S. state of Alaska. It arises in the De Long Mountains of the western Brooks Range and flows north into Kasegaluk Lagoon of the Chukchi Sea, Arctic Ocean. The river mouth is about south of Point Lay. Arctic Slope Regional Corporation is the major landowner along the river. The Inuit name for the river probably means "fairly large stream" or "a stream." A late 19th-century variant was "Kook Pow ruk." See also *List of rivers of Alaska This is a List of rivers in Alaska, which are at least fifth-order according to the Strahler stream order, Strahler method of stream classification, and an incomplete list of otherwise-notable rivers and streams. Alaska has more than 12,000 rivers, ... References Rivers of North Slope Borough, Alaska Rivers of Alaska Drainage basins of the Chukchi Sea {{Alaska-river-stub ...
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Hills Of Alaska
A hill is a landform that extends above the surrounding terrain. It often has a distinct summit, and is usually applied to peaks which are above elevation compared to the relative landmass, though not as prominent as mountains. Hills fall under the category of slope landforms. Terminology The distinction between a hill and a mountain is unclear and largely subjective, but a hill is universally considered to be not as tall, or as steep as a mountain. Geographers historically regarded mountains as hills greater than above sea level. In contrast, hillwalkers have tended to regard mountains as peaks above sea level. The ''Oxford English Dictionary'' also suggests a limit of and Whittow states "Some authorities regard eminences above as mountains, those below being referred to as hills." Today, a mountain is usually defined in the UK and Ireland as any summit at least high, while the UK government's Countryside and Rights of Way Act 2000 defined mountainous areas (for the ...
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Mountains Of North Slope Borough, 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 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 climate, mountains te ...
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