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Resurrection Peaks
Resurrection Peaks is a mountain ridge located in the Kenai Mountains, on the Kenai Peninsula, in the U.S. state of Alaska. The peaks are situated in Chugach National Forest, north of Mount Benson, south of Mount Ascension, and north of Seward, Alaska. These peaks, marked 4712' and 4665' on the USGS map, together with their ridges and glacier form a distinct group. The peaks overlook the mouth of Resurrection River into Resurrection Bay, and take their name from the bay named since 1792, and the river since 1898. Resurrection Peaks' name was officially adopted in 1969 by the United States Geological Survey. Climate Based on the Köppen climate classification, Resurrection Peaks are 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. This climate supports a spruce and hemlock forest on the lower slopes. The months May and June offer the most favorable weather for vi ...
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Kenai Mountains
The Kenai Mountains ( Dena'ina: ''Yaghanen Dghili'') are a mountain range in the U.S. state of Alaska. They extend northeast from the southern end of the Kenai Peninsula to the Chugach Mountains, and have an average elevation of 3,000 to 5,000 feet. The Harding and Sargent Icefields, as well as the many glaciers that emanate from them, originate in the Kenai Mountains. Several prime fish-producing rivers, including the Kenai River and the Russian River, also flow from the mountains. The Dena'ina call the mountains ''Yaghanen Dghili'', meaning "good land mountains". The name "Kenai" was first published by Constantin Grewingk in 1849, who obtained his information from I. G. Wosnesenski's account of a voyage to the area in 1842. Gallery File:Turnagain Arm Carpathian Peak Alaska.jpeg, Carpathian Peak seen from Turnagain Arm File:HardingIcefield1.jpg, Skilak Glacier in the Kenai Mountains File:Mount Alice seen from Mount Marathon.jpg, Mount Alice seen from Mount Marathon ...
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Resurrection River
The Resurrection River is a large river on the Kenai Peninsula in Alaska. It rises near Upper Russian Lake in the Kenai Mountains and flows to empty into Resurrection Bay near Seward. Part of the river passes through Kenai Fjords National Park. There has been small-scale placer mining for gold at the confluence of the river and Placer Creek. Fishing Fishing for salmon is permitted in the lower Resurrection River. The river and bay it drains into have a very productive silver salmon fishery which peaks in August. Other notable fisheries in the river include minor runs of Chinook salmon and Sockeye salmon The sockeye salmon (''Oncorhynchus nerka''), also called red salmon, kokanee salmon, blueback salmon, or simply sockeye, is an anadromous species of salmon found in the Northern Pacific Ocean and rivers discharging into it. This species is a .... References Rivers of Kenai Peninsula Borough, Alaska Rivers of Alaska {{Alaska-river-stub ...
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Mountains Of Kenai Peninsula 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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Geology Of Alaska
The geology of Alaska includes Precambrian igneous and metamorphic rocks formed in offshore terranes and added to the western margin of North America from the Paleozoic through modern times. The region was submerged for much of the Paleozoic and Mesozoic and formed extensive oil and gas reserves due to tectonic activity in the Arctic Ocean. Alaska was largely ice free during the Pleistocene, allowing humans to migrate into the Americas. Geologic History, Stratigraphy & Tectonics Compared with other areas of the North American continent, Alaska formed in the recent geologic past. Until 200 million years ago, western North America terminated at the Rocky Mountains, 120 miles further inland than the current shoreline, until the addition of the Yukon-Tanana Terrane. The Birch Creek Schist is the oldest rock in Alaska's interior and forms the core of the Yukon-Tanana Terrane with muscovite-quartz schist, mica quartzite and graphite schist. This intensely folded and rock unit extends f ...
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List Of Mountain Peaks Of Alaska
This article comprises three sortable tables of major mountain peaks of the U.S. State of Alaska. The summit of a mountain or hill may be measured in three principal ways: #The topographic elevation of a summit measures the height of the summit above a geodetic sea level. The first table below ranks the 100 highest major summits of Alaska by elevation. #The topographic prominence of a summit is a measure of how high the summit rises above its surroundings. The second table below ranks the 100 most prominent summits of Alaska. #The topographic isolation (or radius of dominance) of a summit measures how far the summit lies from its nearest point of equal elevation. The third table below ranks the 50 most isolated major summits of Alaska. __TOC__ Highest major summits Of the 100 highest major summits of Alaska, only Denali exceeds elevation, four peaks exceed , 23 peaks exceed , 61 peaks exceed , and 92 peaks exceed elevation. Five of these peaks lie on the internation ...
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Subarctic Climate
The subarctic climate (also called subpolar climate, or boreal climate) is a continental 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°N to 70°N, poleward of the humid continental climates. Like other Class D climates, they are rare in the Southern Hemisphere, only found at some isolated highland elevations. 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 on ...
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Köppen Climate Classification
The Köppen climate classification divides Earth climates into five main climate groups, with each group being divided based on patterns of seasonal precipitation and temperature. 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'' indicates a tropical rainforest climate. The system assigns a temperature subgroup for all groups other than those in the ''A'' group, indicated by the third letter for climates in ''B'', ''C'', ''D'', and the second letter for climates in ''E''. Other examples include: ''Cfb'' indicating an oceanic climate with warm summers as indicated by the ending ''b.'', while ''Dwb'' indicates a semi-Monsoon continental climate, monsoonal continental climate ...
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Resurrection Bay
Resurrection Bay, also known as Blying Sound, and Harding Gateway in its outer reaches, is a fjord on the Kenai Peninsula of Alaska, United States. Its main settlement is Seward, Alaska, Seward, located at the head of the bay. The bay received its name from Alexandr Baranov, who was forced to retreat into the bay during a bad storm in the Gulf of Alaska. When the storm settled it was Easter, Easter Sunday, so the bay and nearby Resurrection River were named in honor of it. Harding Gateway refers to the passage between Rugged and Cheval Islands. Resurrection Bay is the location of Caines Head, at the summit of which Fort McGilvray is situated above sea level. This fortification was constructed by the United States Armed Forces to defend against a possible invasion by the Imperial Japanese Army during World War II. The bay remains ice-free even in winter, making it easily navigable. It is called the "gateway to the Kenai Fjords" as many water taxis, kayak tours, anglers, and rec ...
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Seward, Alaska
Seward (Alutiiq language, Alutiiq: ; Denaʼina language, Dena'ina: ''Tl'ubugh'') is an incorporated home rule city in Alaska, United States. Located on Resurrection Bay, a fjord of the Gulf of Alaska on the Kenai Peninsula, Seward is situated on Alaska's southern coast, approximately by road from Alaska's largest city, Anchorage, Alaska, Anchorage. With a population of 2,717 people as of the 2020 United States census, 2020 census, Seward is the fourth-largest city in the Kenai Peninsula Borough, Alaska, Kenai Peninsula Borough, behind Kenai, Alaska, Kenai, Homer, Alaska, Homer, and the borough seat of Soldotna, Alaska, Soldotna. The city is named for former United States Secretary of State William H. Seward, who orchestrated the United States' Alaska Purchase, purchase of Alaska from the Russian Empire in 1867 while serving in this position as part of President Andrew Johnson's administration. Seward is the southern terminus of the Alaska Railroad and the historic starting p ...
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Mount Ascension
Mount Ascension is a prominent mountain summit located in the Kenai Mountains, on the Kenai Peninsula, in the U.S. state of Alaska. The mountain is situated in Chugach National Forest, south of Mount Adair, north of Resurrection Peaks, and north of Seward, Alaska. The peak is near the mouth of Resurrection River into Resurrection Bay. The name ''Resurrection'', referring to the Resurrection of Jesus, is overused for nearby landforms on the Kenai peninsula, as the mountain to the immediate south is Resurrection Peaks. This Ascension name is a variation of the theme. Mount Ascension's name was proposed in 1968 by the Mountaineering Club of Alaska, and officially adopted in 1969 by the United States Geological Survey. Access to the peak is via the Lost Lake Trail, and mountaineering skills are needed to reach the summit. In clear weather the immense Harding Icefield can be seen from the top. The first ascent of this peak was made October 6, 1968, by John Vincent Hoeman and his w ...
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Mount Benson (Alaska)
Mount Benson is a mountain summit located in the Kenai Mountains, on the Kenai Peninsula, in the U.S. state of Alaska. The peak is situated in Chugach National Forest, rising above the Resurrection River and Resurrection Bay, south of Resurrection Peaks, north of Marathon Mountain, and northwest of Seward, Alaska. Originally named Iron Mountain, the mountain's name was officially changed in 1974 by the United States Geological Survey to honor Benny Benson (1913-1972), who at age 13 designed Alaska's flag in 1927, as a student in Seward. Climate Based on the Köppen climate classification, Mount Benson 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. This climate supports a spruce and hemlock forest on the lower slopes. The months May and June offer the most favorable weather for viewing. Gallery File:Mount Benson, Alaska.jpg, Mount Benson from Mar ...
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Kenai Peninsula
The Kenai Peninsula ( Dena'ina: ''Yaghenen'') is a large peninsula jutting from the coast of Southcentral Alaska. The name Kenai (, ) is derived from the word "Kenaitze" or "Kenaitze Indian Tribe", the name of the Native Athabascan Alaskan tribe, the Kahtnuht’ana Dena’ina ("People along the Kahtnu (Kenai River)"), who historically inhabited the area. They called the Kenai Peninsula ''Yaghanen'' ("the good land"). Geography The peninsula extends about southwest from the Chugach Mountains, south of Anchorage. It is separated from the mainland on the west by Cook Inlet and on the east by Prince William Sound. Most of the peninsula is part of the Kenai Peninsula Borough. Athabaskan and Alutiiq Native groups lived on the peninsula for thousands of years prior to colonization during the Russian America era. The glacier-covered Kenai Mountains run along the southeast spine of the peninsula along the coast of the Gulf of Alaska. Much of the range is within Kenai Fjords Natio ...
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