Chilkat Range
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Chilkat Range
The Chilkat Range is a mountain range in Haines Borough and the Hoonah-Angoon Census Area in the U.S. state of Alaska, west of the city of Juneau. The Chilkat Range is one of the principal divisors between Haines Borough and Glacier Bay National Park and Preserve. It also separates Chilkat Inlet and Lynn Canal from Muir Inlet in Glacier Bay. The northern boundary is generally considered to be the Klehini River. The unnamed ice field in the range also feeds many glaciers including the Davidson and Rainbow Glaciers. It was named Chilkat Mountains in 1879 by the USGS for the Chilkat subdivision of the Tlingit People The Tlingit ( or ; also spelled Tlinkit) are indigenous peoples of the Pacific Northwest Coast of North America. Their language is the Tlingit language (natively , pronounced ),
. These mountains were renamed as the Chilkat Range in 1891.


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Klehini River
The Klehini River is a large, glacially fed stream in the vicinity of Haines in the U.S. state of Alaska. The Klehini River is about long from its source in British Columbia to its mouth at the Chilkat River, of which it is the largest tributary. The Klehini River is renowned for its salmon runs, its biannual congregation of bald eagles—the second largest in the Haines area after the Chilkat River's Council Grounds—and for the Klehini Falls. The Klehini also delineates the northern boundary of the Chilkat Range. The name ''Klehini'' appears to be derived from the Tlingit phrase ''l’éiw héeni'', which translates to ''river with sand or gravel in it''. ''See'', The Klehini River contains abundances of both sand and gravel. The lower Klehini is located within the Alaska Chilkat Bald Eagle Preserve. Walt Disney's 1991 rendition of ''White Fang'' was filmed along the Klehini River. Klehini Falls The Klehini Falls are a series of four cataracts in far northwes ...
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Mountain Ranges 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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Landforms Of Hoonah–Angoon Census Area, Alaska
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fou ...
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Mount Golub
Mount Golub is a prominent mountain summit located in the Chilkat Range of the Saint Elias Mountains, in the U.S. state of Alaska. This peak is situated northwest of Juneau, and west of Lynn Canal, on land managed by Tongass National Forest. Although modest in elevation, relief is significant since Mount Golub rises above tidewater in less than two miles. The mountain's name was officially adopted in 1972 by the U.S. Board on Geographic Names to commemorate Harvey Golub (1930–1971), member of the 1968 first ascent party. Other members of the party were Richard Folta, Delbert Carnes, and Keith Hart. Hart submitted the name for consideration following the September 4, 1971, untimely death of Harvey Golub who perished in the Alaska Airlines Flight 1866 disaster. That flight, which took all 111 lives aboard, crashed in a canyon approximately seven miles south of his namesake mountain. Climate Based on the Köppen climate classification, Mount Golub has a subarctic climate wi ...
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Tlingit People
The Tlingit ( or ; also spelled Tlinkit) are indigenous peoples of the Pacific Northwest Coast of North America. Their language is the Tlingit language (natively , pronounced ),"Lingít Yoo X'atángi: The Tlingit Language."
''Sealaska Heritage Institute.'' (retrieved 3 December 2009)
in which the name means 'People of the Tides'.Pritzker, 208 The Russian name ' (, from a Sugpiaq-Alutiiq term ' for the worn by women) or the related German name ' may be encountered referring to the people in older historical literature, such as

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United States Geological Survey
The United States Geological Survey (USGS), formerly simply known as the Geological Survey, is a scientific agency of the United States government. The scientists of the USGS study the landscape of the United States, its natural resources, and the natural hazards that threaten it. The organization's work spans the disciplines of biology, geography, geology, and hydrology. The USGS is a fact-finding research organization with no regulatory responsibility. The agency was founded on March 3, 1879. The USGS is a bureau of the United States Department of the Interior; it is that department's sole scientific agency. The USGS employs approximately 8,670 people and is headquartered in Reston, Virginia. The USGS also has major offices near Lakewood, Colorado, at the Denver Federal Center, and Menlo Park, California. The current motto of the USGS, in use since August 1997, is "science for a changing world". The agency's previous slogan, adopted on the occasion of its hundredt ...
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Davidson Glacier
The Davidson Glacier is a large glacier, valley glacier near Haines, Alaska, Haines, Alaska that finds its source in the Chilkat Range. History The Davidson Glacier was named in 1867 for George Davidson (geographer), George Davidson. Its Indian name is Ssitkaje. It was recounted by John Muir in his famous travels in and around Glacier Bay in 1879. The glacier was, at that time, a glacier that nearly reached tidewater.(Wilderness Essays, The Alaska Trip (pg 60) John Muir). It has since receded into the mountains, becoming a valley glacier, and created its very own glacial lake in the glacier's moraine (similar to the Mendenhall Glacier and Mendenhall Lake, lake) about one mile inland from the Chilkat Inlet. Current status Currently, the Davidson Glacier serves as a tourist attraction for Haines and Skagway. See also *List of glaciers *Mount Rifenburgh References External links

* Glaciers of Alaska Glaciers of Haines Borough, Alaska Tourist attractions in Haines Borough, ...
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Ice Field
An ice field (also spelled icefield) is a mass of interconnected valley glaciers (also called mountain glaciers or alpine glaciers) on a mountain mass with protruding rock ridges or summits. They are often found in the colder climates and higher altitudes of the world where there is sufficient precipitation for them to form. The higher peaks of the underlying mountain rock that protrude through the icefields are known as nunataks. Ice fields are larger than alpine glaciers, but smaller than ice caps and ice sheets. The topography of ice fields is determined by the shape of the surrounding landforms, while ice caps have their own forms overriding underlying shapes. Formation Ice fields are formed by a large accumulation of snow which, through years of compression and freezing, turns into ice. Due to ice's susceptibility to gravity, ice fields usually form over large areas that are basins or atop plateaus, thus allowing a continuum of ice to form over the landscape uninterrupted b ...
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Glacier Bay
Glacier Bay Basin in southeastern Alaska, in the United States, encompasses the Glacier Bay and surrounding mountains and glaciers, which was first proclaimed a U.S. National Monument on February 25, 1925, and which was later, on December 2, 1980, enlarged and designated as the Glacier Bay National Park and Preserve under the Alaska National Interest Lands Conservation Act, covering an area of 3,283,000 acres (1,329,000 ha). In 1986, UNESCO declared an area of 57,000 acres (23,000 ha) within a World Biosphere Reserve. This is the largest UNESCO protected biosphere in the world. In 1992, UNESCO included this area as a part of a World Heritage site, extending over an area of 24,300,000-acre (98,000 km2) which also included the Wrangell-St. Elias National Park, Kluane National Park (Canada) and Tatshenshini-Alsek Park (Canada). Part of the National Park is also designated a Wilderness area covering 2,658,000 acres (1,076,000 ha). Current glaciers cover an area 1,375 square miles ...
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Mountain Range
A mountain range or hill range is a series of mountains or hills arranged in a line and connected by high ground. A mountain system or mountain belt is a group of mountain ranges with similarity in form, structure, and alignment that have arisen from the same cause, usually an orogeny. Mountain ranges are formed by a variety of geological processes, but most of the significant ones on Earth are the result of plate tectonics. Mountain ranges are also found on many planetary mass objects in the Solar System and are likely a feature of most terrestrial planets. Mountain ranges are usually segmented by highlands or mountain passes and valleys. Individual mountains within the same mountain range do not necessarily have the same geologic structure or petrology. They may be a mix of different orogenic expressions and terranes, for example thrust sheets, uplifted blocks, fold mountains, and volcanic landforms resulting in a variety of rock types. Major ranges Most geolo ...
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Muir Inlet
Muir Inlet is an inlet in Glacier Bay, U.S.A. ''Muir Inlet'' heads in Muir Glacier, and extends for south to Glacier Bay, NW of Hoonah, Alaska ''Muir Inlet'' is separated from Chilkat Inlet and Lynn Canal by Chilkat Range. ''Muir Inlet'' has several glacier's terminuses besides Muir Glacier, most prominent are Casement Glacier, McBride Glacier and Riggs Glacier. In the west lies the Wachusett Inlet and in the east the Adam's Inlet. ''Muir Inlet'' was named in 1883 by U.S. Coast and Geodetic Survey (USC&GS) for John Muir, (1838–1914), who visited this area in 1890. ''Muir Inlet'' is popular kayaking Kayaking is the use of a kayak for moving over water. It is distinguished from canoeing by the sitting position of the paddler and the number of blades on the paddle. A kayak is a low-to-the-water, canoe-like boat in which the paddler sits fac ... destination. References External links Marine Benthic Habitat Mapping of Muir Inlet, Glacier Bay National Park and Prese ...
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