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Whiteface Mountain (Simi Valley)
Whiteface Mountain is the fifth-highest mountain in the U.S. state of New York (state), New York, and one of the Adirondack High Peaks, High Peaks of the Adirondack Mountains, located in the town of Wilmington, New York, Wilmington in Essex County, New York, Essex County. Set apart from most of the other High Peaks, the summit offers a 360-degree view of the Adirondacks and clear-day glimpses of Vermont and Canada, where Montreal can be seen on a very clear day. Because of its relative isolation, the mountain is exposed to Prevailing winds, prevailing winds from the west and frequently capped with snow and ice, making it an area of interest to meteorologists. Weather data has been collected on the summit since 1937. The mountain's east slope is home to a major ski area which boasts the greatest vertical drop east of the Rockies, and which hosted the Alpine skiing at the 1980 Winter Olympics, alpine skiing competitions of the 1980 Winter Olympics. Unique among the High Peaks, Whit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Adirondack High Peaks
The Adirondack High Peaks are a set of 46 mountain peaks in the Adirondack Mountains of New York (state), New York state. They have been popular hiking destinations since the late 1920s, when the list of peaks was published in Russell Carson's book ''Peaks and Peoples of the Adirondacks''. Those who have climbed all 46 High Peaks are eligible to join the Adirondack Forty-Sixers club. Origin The list of peaks was originally compiled by the mountaineers Herbert Clark, Bob Marshall (wilderness activist), Bob Marshall, and George Marshall (conservationist), George Marshall, with input from Russell Carson. The Marshall brothers wished to climb every notable peak in the Adirondacks, which they accomplished with Clark between 1918 and 1925. The criteria used were that all peaks should be at least in elevation and either have of Topographic prominence, prominence or of distance from another peak. Several exceptions to these rules were made to include or exclude peaks based on their pref ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alpine Skiing At The 1980 Winter Olympics
Alpine Skiing at the 1980 Winter Olympics consisted of six alpine skiing events. The races were held February 14–23 at Whiteface Mountain in Wilmington, New York, northeast of host This was the first Olympics in which the women's giant slalom consisted of two runs, rather than one, and both GS events ran only one run per day. This was the last Olympics which also served as World Championships for alpine skiing. Medal summary Eight nations won medals in Alpine skiing, with Liechtenstein leading the medal table, winning two gold, and two silver. Hanni Wenzel led the individual medal table, finishing on the podium in all three women's events, with two gold and one silver. Ingemar Stenmark was the leading male medalist, with two golds. Wenzel's two gold medals were the first, and to date , only, won by Liechtenstein at the Olympics. Medal table Source: Men's events Source: Women's events Source: Course information : Participating nations Thirty nations sent alpine ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mohawk Language
Mohawk (; ''Kanienʼkéha'', " anguageof the Flint Place") is an Iroquoian language currently spoken by around 3,500 people of the Mohawk nation, located primarily in current or former Haudenosaunee territories, predominately Canada (southern Ontario and Quebec), and to a lesser extent in the United States (western and northern New York). The word "Mohawk" is an exonym. In the Mohawk language, the people say that they are from ''Kanien:ke'' ('Mohawk Country' or "Flint Stone Place") and that they are ''Kanienʼkehá꞉ka'' "People of the Flint Stone Place" or "People of the Flint Nation". The Mohawks were extremely wealthy traders, as other nations in their confederacy needed their flint for tool-making. Their Algonquian-speaking neighbors (and competitors), the People of ''Muh-heck Heek Ing'' ("food-area place"), a people called by the Dutch "Mohicans" or "Mahicans", called the People of Ka-nee-en Ka "Maw Unk Lin" or ''Bear People''. The Dutch heard and wrote that as "Mohawks" ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Algonquin Language
Algonquin (also spelled Algonkin; in Algonquin: or ) is either a distinct Algonquian language closely related to the Ojibwe language or a particularly divergent Ojibwe dialect. It is spoken, alongside French and to some extent English, by the Algonquin First Nations of Quebec and Ontario. As of 2006, there were 2,680 Algonquin speakers,. less than 10% of whom were monolingual. Algonquin is the language for which the entire Algonquian language subgroup is named; the similarity among the names often causes considerable confusion. Like many Native American languages, it is strongly verb-based, with most meaning being incorporated into verbs instead of using separate words for prepositions, tense, etc. Classification Omà mìwininìmowin (Algonquin) is an Algonquian language, of the Algic family of languages, and is descended from Proto-Algonquian. It is considered a particularly divergent dialect of Ojibwe by many. But, although the speakers call themselves '' Omà mìwininà ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rime Ice
Rime ice forms when supercooled water liquid droplets freeze onto surfaces. Meteorologists distinguish between three basic types of ice forming on vertical and horizontal surfaces by deposition of supercooled water droplets. There are also intermediate formations. *Soft rime is less dense than hard rime and is milky and crystalline, like sugar. Soft rime appears similar to hoar frost. *Hard rime is somewhat less milky, especially if it is not heavy. *Clear ice is transparent and homogeneous and resembles ice-cube ice in appearance. Its amorphousWikipedia:_Citing_sources.html" "title="nowiki/>Wikipedia: Citing sources">citation needed], dense structure helps it cling tenaciously to any surface on which it forms. Both rime types are less dense than clear ice and cling less tenaciously, therefore damage due to rime is generally minor compared to clear ice. Glaze ice is similar in appearance to clear ice but it is the result of a completely different process, occurring during freezi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landslide
Landslides, also known as landslips, are several forms of mass wasting that may include a wide range of ground movements, such as rockfalls, deep-seated grade (slope), slope failures, mudflows, and debris flows. Landslides occur in a variety of environments, characterized by either steep or gentle slope gradients, from mountain ranges to coastal cliffs or even underwater, in which case they are called submarine landslides. Gravity is the primary driving force for a landslide to occur, but there are other factors affecting slope stability that produce specific conditions that make a slope prone to failure. In many cases, the landslide is triggered by a specific event (such as a heavy rainfall, an earthquake, a slope cut to build a road, and many others), although this is not always identifiable. Causes Landslides occur when the slope (or a portion of it) undergoes some processes that change its condition from stable to unstable. This is essentially due to a decrease in the She ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Igneous Rock
Igneous rock (derived from the Latin word ''ignis'' meaning fire), or magmatic rock, is one of the three main The three types of rocks, rock types, the others being Sedimentary rock, sedimentary and metamorphic rock, metamorphic. Igneous rock is formed through the cooling and solidification of magma or lava. The magma can be derived from Partial melting, partial melts of existing rocks in either a Terrestrial planet, planet's mantle (geology), mantle or crust (geology), crust. Typically, the melting is caused by one or more of three processes: an increase in temperature, a decrease in pressure, or a change in composition. Solidification into rock occurs either below the surface as intrusive rocks or on the surface as extrusive (geology), extrusive rocks. Igneous rock may form with crystallization to form granular, crystalline rocks, or without crystallization to form Volcanic glass, natural glasses. Igneous rocks occur in a wide range of geological settings: shields, platforms ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anorthosite
Anorthosite () is a phaneritic, intrusive igneous rock characterized by its composition: mostly plagioclase feldspar (90–100%), with a minimal mafic component (0–10%). Pyroxene, ilmenite, magnetite, and olivine are the mafic minerals most commonly present. Anorthosites are of enormous geologic interest, because it is still not fully understood how they form. Most models involve separating plagioclase crystals based on their density. Plagioclase crystals are usually less dense than magma; so, as plagioclase crystallizes in a magma chamber, the plagioclase crystals float to the top, concentrating there. Anorthosite on Earth can be divided into five types: # Archean-age anorthosites # Proterozoic anorthosite (also known as massif or massif-type anorthosite) – the most abundant type of anorthosite on Earth # Layers within Layered Intrusions (e.g., Bushveld and Stillwater intrusions) # Mid-ocean ridge and transform fault anorthosites # Anorthosite xenoliths in other rocks ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Champlain
, native_name_lang = , image = Champlainmap.svg , caption = Lake Champlain-River Richelieu watershed , image_bathymetry = , caption_bathymetry = , location = New York/Vermont in the United States; and Quebec in Canada , coords = , type = , inflow = Otter Creek, Winooski River, Missisquoi River, Poultney River, Lamoille River, Ausable River, Chazy River, Boquet River, Saranac River, La Chute River , outflow = Richelieu River , catchment = , basin_countries = Canada, United States , length = , width = , area = , depth = , max-depth = , volume = , residence_time = 3.3 years , shore = , elevation = , islands = 80 ( Grand Isle, North Hero, Isle La Motte, '' see list'') , cities = Burlington, Vermont; Plattsburgh, New York Lake Champlain ( ; french: Lac Champlain) is a natural freshwater lake in North America. It mostly lies between the US states of New York and Vermont, but also extends north into the Canadian province of Quebec. The New York portion of the Ch ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Esther Mountain
Esther Mountain is a mountain located in Essex County, New York. The mountain is the northernmost of the High Peaks of the Adirondack Mountains and its 28th highest peak. It was the only High Peak named for a woman until 2014, having been named in honor of Esther McComb, who made the first recorded climb to the summit in 1839, at age 15; at the time she was attempting to climb Whiteface Mountain from the north (Whiteface is a higher mountain which flanks Esther to the south).Goodwin, Tony, ed., ''Adirondack Trails, High Peaks Region'', Lake George, New York: Adirondack Mountain Club, 2004, p. 155. Esther Mountain stands within the watershed of Lake Champlain, which drains into Canada's Richelieu River, the Saint Lawrence River, and into the Gulf of Saint Lawrence. The southeast side of Esther Mtn. drains into White Brook, thence into the West Branch of the Ausable River, which drains into Lake Champlain. The southwest and north sides of Esther Mountain drain into F ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Clean Prominence
In topography, prominence (also referred to as autonomous height, relative height, and shoulder drop in US English, and drop or relative height in British English) measures the height of a mountain or hill's summit relative to the lowest contour line encircling it but containing no higher summit within it. It is a measure of the independence of a summit. A peak's ''key col'' (the highest col surrounding the peak) is a unique point on this contour line and the ''parent peak'' is some higher mountain, selected according to various criteria. Definitions The prominence of a peak may be defined as the least drop in height necessary in order to get from the summit to any higher terrain. This can be calculated for a given peak in the following way: for every path connecting the peak to higher terrain, find the lowest point on the path; the ''key col'' (or ''key Saddle point, saddle'', or ''linking col'', or ''link'') is defined as the highest of these points, along all connecting pat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Elevator
An elevator or lift is a wire rope, cable-assisted, hydraulic cylinder-assisted, or roller-track assisted machine that vertically transports people or freight between floors, levels, or deck (building), decks of a building, watercraft, vessel, or other structure. They are typically powered by electric motors that drive traction cables and counterweight systems such as a hoist (device), hoist, although some pump hydraulic fluid to raise a cylindrical piston like a hydraulic jack, jack. In agriculture and manufacturing, an elevator is any type of conveyor device used to lift materials in a continuous stream into bins or silos. Several types exist, such as the chain and bucket elevator, grain auger screw conveyor using the principle of Archimedes' screw, or the chain and paddles or forks of hay elevators. Languages other than English, such as Japanese, may refer to elevators by loanwords based on either ''elevator'' or ''lift''. Due to wheelchair access laws, elevators are ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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