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Andy Simons Mountain
Andy Simons Mountain is a prominent double summit mountain located in the Kenai Mountains, and the fourth-highest peak on the Kenai Peninsula in the state of Alaska. The true summit is 1.3 mile west of the 5,300+ foot subsidiary east peak on this five-mile-long northwest-to-southeast trending mountain. The mountain is situated in Chugach National Forest, east of Mount Adair, and north of Seward, Alaska. The Seward Highway and Alaska Railroad traverse its western foot. Precipitation runoff from the mountain drains into Kenai Lake. History The first ascent of this mountain was made May 18, 1963, by a Mountaineerng Club of Alaska party led by Dave Johnston. This group left a summit register with the name "Big Bad Wolf Peak" as the intended name, in keeping with a theme of the already named Mother Goose Glacier at the south end of this mountain. However, that same year the Seward Chamber of Commerce submitted a request that the mountain be named after Andrew Adrian Simons (1882â ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kenai Mountains
The Kenai Mountains ( Dena'ina: ''Yaghanen Dghili'') are a mountain range in the U.S. state of Alaska. They extend 192 km (120 mi) 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 Image:HardingIcefield1.jpg, Skilak Glacier in the Kenai Mountains File:Mount Alice seen from Mount Marathon.jpg, Mount Alice seen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Prospecting
Prospecting is the first stage of the geological analysis (followed by exploration) of a territory. It is the search for minerals, fossils, precious metals, or mineral specimens. It is also known as fossicking. Traditionally prospecting relied on direct observation of mineralization in rock outcrops or in sediments. Modern prospecting also includes the use of geologic, geophysical, and geochemical tools to search for anomalies which can narrow the search area. Once an anomaly has been identified and interpreted to be a potential prospect direct observation can then be focused on this area. In some areas a prospector must also make claims, meaning they must erect posts with the appropriate placards on all four corners of a desired land they wish to prospect and register this claim before they may take samples. In other areas publicly held lands are open to prospecting without staking a mining claim. Historical methods The traditional methods of prospecting involved combi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paradise Peak (Kenai Mountains)
Paradise Peak is a mountain summit in Alaska, United States. Description Paradise Peak is located northeast of Seward in the Kenai Mountains, on land managed by Chugach National Forest. Precipitation runoff and glacial meltwater from the mountain's slopes drains to Kenai Lake via the Snow River. Although modest in elevation, topographic relief is significant as the summit rises over 4,800 feet (1,463 m) above Paradise Valley in . The mountain is named in association with Paradise Valley which it borders, and the toponym was officially adopted in 1971 by the United States Board on Geographic Names. The first ascent of the summit was made on June 29, 1969, by Grace Hoeman via the West Ridge.''World Climbing: Based on Mountain Magazine'', Dark Peak, 1980, , p. 46. Climate Based on the Köppen climate classification, Paradise Peak is located in a tundra climate zone with long, cold, snowy winters, and mild summers. Weather systems coming off the Gulf of Alaska are force ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Snow River
The Snow River is a tributary of Kenai Lake in the U.S. state of Alaska. Beginning in the Kenai Mountains of the Kenai Peninsula, it flows southwest through Chugach National Forest where its main and south forks join to near Primrose at the southern inlet of the lake. The river mouth is about northeast of Seward. Along its final reaches, the river intersects the Iditarod Trail and passes under the Seward Highway. The glacier from which it flows has an associated glacial dammed lake that releases every few years, often causing flooding in Primrose and Kenai Lake. See also * |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Mountain Peaks Of Alaska
This article comprises three sortable tables of major mountain peaksThis article defines a significant summit as a summit with at least of topographic prominence, and a major summit as a susexxleast of topographic prominence. All summits in this article have at least 500 meters of topographic prominence. An ultra-prominent summit is a summit with at least of topographic prominence. 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.If the elevation or prominence of a summit is calculated as a range of values, the arithmetic mean is shown. 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 topographic prominence of a summit is the topographic elevation difference between the s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Orographic Lift
Orographic lift occurs when an air mass is forced from a low elevation to a higher elevation as it moves over rising terrain. As the air mass gains altitude it quickly cools down adiabatically, which can raise the relative humidity to 100% and create clouds and, under the right conditions, precipitation. Orographic lifting can have a number of effects, including precipitation, rain shadowing, leeward winds, and associated clouds. Precipitation Precipitation induced by orographic lift occurs in many places throughout the world. Examples include: * The Mogollon Rim in central Arizona * The western slope of the Sierra Nevada range in California * The mountains near Baja California North – specifically La Bocana to Laguna Hanson. * The windward slopes of Khasi and Jayantia Hills (see Mawsynram) in the state of Meghalaya in India. * The Western Highlands of Yemen, which receive by far the most rain in Arabia. * The Western Ghats that run along India's western coast. * The Grea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gulf Of Alaska
The Gulf of Alaska (Tlingit: ''Yéil T'ooch’'') is an arm of the Pacific Ocean defined by the curve of the southern coast of Alaska, stretching from the Alaska Peninsula and Kodiak Island in the west to the Alexander Archipelago in the east, where Glacier Bay and the Inside Passage are found. The Gulf shoreline is a combination of forest, mountain and a number of tidewater glaciers. Alaska's largest glaciers, the Malaspina Glacier and Bering Glacier, spill out onto the coastal line along the Gulf of Alaska. The coast is heavily indented with Cook Inlet and Prince William Sound, the two largest connected bodies of water. It includes Yakutat Bay and Cross Sound. Lituya Bay (a fjord north of Cross Sound, and south of Mount Fairweather) is the site of the largest recorded tsunami in history. It serves as a sheltered anchorage for fishing boats. Ecology The Gulf of Alaska is considered a Class I, productive ecosystem with more than 300 grams of carbon per square meter per year ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Holiday (magazine)
''Holiday'' was an American travel magazine published from 1946 to 1977, whose circulation grew to more than one million subscribers at its height. The magazine employed writers such as Truman Capote, Joan Didion, Lawrence Durell, James Michener, and E. B. White. In 2014, the magazine was relaunched as a bi-annual magazine based in Paris, but written in English. History Launched by the Curtis Publishing Company, the first issue of ''Holiday'' appeared in March 1946. The magazine was headquartered in Philadelphia, Pennsylvania in the Curtis Center near Independence Hall. After a lackluster start, with the fifth issue Ted Patrick became editor, a position he held until his sudden death in 1964. By the end of the first year the circulation topped 425,000. The magazine was known as a cosmopolitan travel wishbook with photo essays in full-color oversize 11 X 13.5 package along with articles by famous authors. John Lewis Stage, a photographer for Holiday described they way that Pat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
