Johnson Lake State Recreation Area
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Johnson Lake State Recreation Area
The Kasilof River ( ) or ''Ggasilatnu'' in the Dena'ina language is a river on the western Kenai Peninsula in southern Alaska. The name is an anglicization of ''Reka Kasilova'', the name given to the river by early Russian settlers in the area. It begins at Tustumena Lake and flows northwest to Cook Inlet near Kasilof. The upper section of the river is very swift, with several sections considered Class II whitewater, and underwater hazards are difficult to detect, due to the silty nature of the glacial runoff that comprises most of the river. The entire river has powerful currents and is very cold. There is public access to the lower section from the Sterling Highway. Drift and bank fishing for salmon is popular on the lower Kasilof. Parks Three Alaska State Parks units are on or near the Kasilof River. At mile 109 of the Sterling Highway, adjacent to the bridge where the highway crosses the river is the Kasilof River State Recreation Site, a day-use only park with picnic areas a ...
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Tustumena Lake
Tustumena Lake ( Dena'ina: ''Dusdu Bena'') is a lake on the west side of the Kenai Peninsula in southcentral Alaska, within Kenai National Wildlife Refuge and near the town of Kasilof. Access is only via the Kasilof River, as there are no roads that lead directly to the lake. Overview At 73,437 acres Tustumena Lake is Alaska's eighth largest lake and the largest lake on the Kenai Peninsula. With a maximum depth of 950 feet, Tustumena Lake is exceptionally deep; it is deeper than Cook Inlet. The lake is long and up to wide and receives drainage from Tustumena Glacier, and several creeks., The outlet forms the headwaters of the Kasilof River. The lake and the area around it are known for game hunting, and for the Tustumena 200 Sled Dog Race. Most of the land surrounding the lake is in the Kenai National Wildlife Refuge. This lake has a reputation for being very dangerous to small boats due to the high winds that regularly blow off of Tustumena Glacier. History Early R ...
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Sterling Highway
The Sterling Highway is a state highway in the south-central region of the U.S. state of Alaska, leading from the Seward Highway at Tern Lake Junction, south of Anchorage, to Homer. Route description Construction of the highway began in 1947 and was completed in 1950. The Sterling Highway is part of Alaska Route 1. It leads mainly west from Tern Lake to Soldotna, paralleling the Kenai River, at which point it turns south to follow the eastern shore of Cook Inlet. It is the only highway in the western and central Kenai Peninsula, and most of the population of the Kenai Peninsula Borough lives near it. The highway also gives access to many extremely popular fishing and recreation areas, including the Chugach National Forest, Kenai National Wildlife Refuge, and the Kenai, Funny, and Russian rivers. The southern end of the highway is at the tip of the Homer Spit, a landspit extending into Kachemak Bay. A ferry terminal here connects the road to the Alaska Marine Highwa ...
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Rivers Of Kenai Peninsula Borough, Alaska
A river is a natural flowing watercourse, usually freshwater, flowing towards an ocean, sea, lake or another river. In some cases, a river flows into the ground and becomes dry at the end of its course without reaching another body of water. Small rivers can be referred to using names such as creek, brook, rivulet, and rill. There are no official definitions for the generic term river as applied to geographic features, although in some countries or communities a stream is defined by its size. Many names for small rivers are specific to geographic location; examples are "run" in some parts of the United States, "burn" in Scotland and northeast England, and "beck" in northern England. Sometimes a river is defined as being larger than a creek, but not always: the language is vague. Rivers are part of the water cycle. Water generally collects in a river from precipitation through a drainage basin from surface runoff and other sources such as groundwater recharge, springs, a ...
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List Of Alaska Rivers
This is a List of rivers in Alaska, which are at least fifth-order according to the Strahler method of stream classification, and an incomplete list of otherwise-notable rivers and streams. Alaska has more than 12,000 rivers, and thousands more streams and creeks. According to United States Geological Survey Geographic Names Information System, Alaska has about 9,728 officially named rivers, creeks, and streams. The length of the river is given if it is available from the United States Geological Survey Geographic Names Information System (GNIS). By drainage basin This list is arranged by drainage basin, with respective tributaries ordered from mouth to source, and indented under their downstream parent's name. Arctic Ocean *Firth River – * Kongakut River – * Aichilik River – * Jago River – * Okpilak River – * Hulahula River – * Sadlerochit River – *Canning River – ** Marsh Fork Canning River – * Shaviovik River – ** Kavik River – * Kadleroshili ...
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Johnson Lake (Kenai Peninsula Borough, Alaska)
Johnson Lake is a small lake on the Kenai Peninsula in the state of Alaska. It covers about 84 acres and is stocked with Pacific salmon, coho salmon, steelhead, and rainbow trout. The lake is surrounded by Johnson Lake State Recreation Area, which consists of 332 wooded acres (134 ha) with a large campground, picnic areas, and access to the Tustumena Lake road, which ends at the Slackwater boat launch on the river with a small, free campground. Camping, fishing, canoeing and walking are popular activities in the recreation area. There are 48 campsites, 16 day use parking sites, and a group picnic area. Moose, black and brown bear, lynx, squirrels, and hares are plentiful. See also *List of lakes of Alaska Alaska has about 3,197 officially named natural lakes, out of over 3,000,000 unnamed natural lakes, approximately 67 named artificial reservoirs, and 167 named dams. For named artificial reservoirs and dams, see the List of dams and reservoirs in ... References Rivers of K ...
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Alaska Department Of Natural Resources
The Alaska Department of Natural Resources is a department within the government of Alaska in the United States of America. The department has the mission of responsibly developing Alaska's resources by making them available for maximum use and benefit consistent with the public interest. The department comprises seven divisions: * Division of Agriculture * Division of Forestry * Division of Geological and Geophysical Surveys * Division of Mining, Land and Water * Division of Oil and Gas (including the Petroleum Systems Integrity Office) * Division of Parks and Outdoor Recreation * Support Services Division Official mission The official mission of the Alaska Department of Natural Resources is "to develop, conserve and maximize the use of Alaska's natural resources consistent with the public interest". The Department of Natural Resources articulates its activities on its official website stating: "The Department of Natural Resources manages all state-owned land, water and n ...
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Alaska State Parks
Alaska’s state park system is managed by the Alaska Department of Natural Resources division of Parks and Outdoor Recreation. The system contains over 120 units spanning 3,427,895 acres, making it far larger than any other state park system in the United States. The State Park system began in 1970 with the creation of Denali State Park, Chugach State Park and Kachemak Bay State Park, three of the largest and still most popular parks in the state system. Wood-Tikchik State Park is the largest state park in the United States, comprising some 15% of total state park land in the nation. The division manages full state parks, state recreation areas, state recreation sites, and state historic sites.DeVaugh, MelissaHistory of Alaska State Parks/ref> Anchorage area park * Chugach State Park Copper River Basin area parks * Dry Creek State Recreation Site * Lake Louise State Recreation Area * Liberty Falls State Recreation Site * Porcupine Creek State Recreation Site * Squirr ...
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The Milepost
''The'' () is a grammatical article in English, denoting persons or things already mentioned, under discussion, implied or otherwise presumed familiar to listeners, readers, or speakers. It is the definite article in English. ''The'' is the most frequently used word in the English language; studies and analyses of texts have found it to account for seven percent of all printed English-language words. It is derived from gendered articles in Old English which combined in Middle English and now has a single form used with pronouns of any gender. The word can be used with both singular and plural nouns, and with a noun that starts with any letter. This is different from many other languages, which have different forms of the definite article for different genders or numbers. Pronunciation In most dialects, "the" is pronounced as (with the voiced dental fricative followed by a schwa) when followed by a consonant sound, and as (homophone of pronoun ''thee'') when followed by a v ...
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Salmon
Salmon () is the common name for several list of commercially important fish species, commercially important species of euryhaline ray-finned fish from the family (biology), family Salmonidae, which are native to tributary, tributaries of the North Atlantic (genus ''Salmo'') and North Pacific (genus ''Oncorhynchus'') basin. Other closely related fish in the same family include trout, Salvelinus, char, Thymallus, grayling, Freshwater whitefish, whitefish, lenok and Hucho, taimen. Salmon are typically fish migration, anadromous: they hatch in the gravel stream bed, beds of shallow fresh water streams, migrate to the ocean as adults and live like sea fish, then return to fresh water to reproduce. However, populations of several species are restricted to fresh water throughout their lives. Folklore has it that the fish return to the exact spot where they hatched to spawn (biology), spawn, and tracking studies have shown this to be mostly true. A portion of a returning salmon run ma ...
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Glacial
A glacial period (alternatively glacial or glaciation) is an interval of time (thousands of years) within an ice age that is marked by colder temperatures and glacier advances. Interglacials, on the other hand, are periods of warmer climate between glacial periods. The Last Glacial Period ended about 15,000 years ago. The Holocene is the current interglacial. A time with no glaciers on Earth is considered a greenhouse climate state. Quaternary Period Within the Quaternary, which started about 2.6 million years before present, there have been a number of glacials and interglacials. At least eight glacial cycles have occurred in the last 740,000 years alone. Penultimate Glacial Period The Penultimate Glacial Period (PGP) is the glacial period that occurred before the Last Glacial Period. It began about 194,000 years ago and ended 135,000 years ago, with the beginning of the Eemian interglacial. Last Glacial Period The last glacial period was the most recent glacial period ...
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Cook Inlet
Cook Inlet ( tfn, Tikahtnu; Sugpiaq: ''Cungaaciq'') stretches from the Gulf of Alaska to Anchorage in south-central Alaska. Cook Inlet branches into the Knik Arm and Turnagain Arm at its northern end, almost surrounding Anchorage. On its southern end, it merges with Shelikof Strait, Stevenson Entrance, Kennedy Entrance and Chugach Passage. The Cook Inlet watershed is the most populated watershed in Alaska. The watershed covers about of southern Alaska, east of the Aleutian Range, south and east of the Alaska Range, receiving water from its tributaries, the Knik River, the Little Susitna River, and the Susitna and Matanuska rivers. The watershed includes the drainage areas of Denali (formerly named Mount McKinley). Within the watershed there are several national parks and the active volcano Mount Redoubt, along with three other historically active volcanoes. Cook Inlet provides navigable access to the port of Anchorage at the northern end, and to the smaller Homer port fu ...
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Silt
Silt is granular material of a size between sand and clay and composed mostly of broken grains of quartz. Silt may occur as a soil (often mixed with sand or clay) or as sediment mixed in suspension with water. Silt usually has a floury feel when dry, and lacks plasticity when wet. Silt also can be felt by the tongue as granular when placed on the front teeth (even when mixed with clay particles). Silt is a common material, making up 45% of average modern mud. It is found in many river deltas and as wind-deposited accumulations, particularly in central Asia, north China, and North America. It is produced in both very hot climates (through such processes as collisions of quartz grains in dust storms) and very cold climates (through such processes as glacial grinding of quartz grains.) Loess is soil rich in silt which makes up some of the most fertile agricultural land on Earth. However, silt is very vulnerable to erosion, and it has poor mechanical properties, making construction ...
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