Avalanche Lake (New York)
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Avalanche Lake (New York)
Avalanche Lake is a mountain lake located in the Adirondack High Peaks in New York. Avalanche Lake sits at between Mount Colden and Avalanche Mountain. The two mountains rise in vertical cliffs from the surface of the lake. Immediately west of Avalanche Mountain (formerly known as Caribou Mountain) lies the MacIntyre Range: Algonquin Peak (the second highest mountain in the state), Boundary Peak, Iroquois Peak and Mount Marshall. Mount Marcy is to the east. Avalanche Lake feeds Lake Colden to the south, in the Hudson River watershed. To the north, the trail to the lake from the Adirondak Loj surmounts Avalanche Pass, which is only slightly above lake level but separates it from the Lake Champlain (St. Lawrence River) watershed. Following the lake toward Lake Colden, the trail is choked with large boulders, and a number of wooden ladders have been built to make passage possible. There are also three places where the trail takes to wooden catwalks, first built in the 1920s, ...
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Mount Colden
Mount Colden is the eleventh-highest peak in the Adirondack High Peaks, High Peaks of the Adirondack Mountains, New York (state), New York, United States. The peak was named after David S. Colden, an investor in the McIntyre Iron Works, in 1836. The peak was briefly renamed "Mount McMartin" the next year, but the older name persisted. The mountain is known for its distinctive Trap Dike, a large crevice running up the center of the mountain, which can clearly be seen from Avalanche Lake (New York), Avalanche Lake. There are two maintained trails up Mount Colden. The first, which approaches from the northeast, passes by Lake Arnold before ascending the summit after crossing over several false summits. This trail was laid out in 1966 to replace a steeper trail which ascended the southeast face of the mountain and which was abandoned by 1975.''Guide to Adirondack Trails'', eighth edition, Adirondack Mountain Club, 1975, p. B6-17. The second trail, which is steeper, approaches fro ...
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Mount Marcy
Mount Marcy (Mohawk: ''Tewawe’éstha'') is the highest point in New York, with an elevation of . It is located in the Town of Keene in Essex County. The mountain is in the heart of the Adirondack High Peaks region of the High Peaks Wilderness Area. Its stature and expansive views make it a popular destination for hikers, who crowd its summit in the summer months. Lake Tear of the Clouds, at the col between Mounts Marcy and Skylight, is often cited as the highest source of the Hudson River, via Feldspar Brook and the Opalescent River, even though the main stem of the Opalescent River has as its source a higher point two miles north of Lake of the Clouds, and that stem is a mile longer than Feldspar Brook. History The mountain is known as ''Tewawe'éstha'' ("it pierces") in Mohawk and ''Tahawus'' ("cloud-splitter") in Algonquin. The mountain was named after Gov. William L. Marcy, the 19th-century Governor of New York, who authorized the environmental survey that explore ...
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Lakes Of New York (state)
This is a list of lakes in the state of New York in the United States. The list is not exhaustive. * Adirondack Lake * Ampersand Lake * Atwood Lake * Avalanche Lake * Augur Lake * Bailey Pond * Ballston Lake * Basket Pond * Bass Lake * Bear Cub Pond * Beaverdam Lake * Big Diamond Pond * Big Moose Lake * Blackfoot Pond * Black Lake * Blue Mountain Lake * Brantingham Lake * Brydon Lake * Buck Horn Lake * Busfield Pond * Cables Lake * East Canada Lake * West Canada Lake * Canadice Lake * Canaan Lake * Canadarago Lake * Canandaigua Lake * Caroga Lake * Catlin Lake * Cayuga Lake * Cayuta Lake * Cazenovia Lake * Chadwick Lake * Chateaugay Lake * Chautauqua Lake * Chazy Lake * Chisholm Pond * Clapper Lake * Columbia Lake * Combs Lake * Conesus Lake * Cossayuna Lake * Cranberry Lake * Cross Lake * Dart Lake * Lake Delaware * Delta Lake * Duck Lake * Dwight Pond * Eagle Lake, Essex County * Eagle Lake, Hamilton County * Eagle Lake, Orange County * E ...
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Avalanche Lake, Looking South
An avalanche is a rapid flow of snow down a slope, such as a hill or mountain. Avalanches can be set off spontaneously, by such factors as increased precipitation or snowpack weakening, or by external means such as humans, animals, and earthquakes. Primarily composed of flowing snow and air, large avalanches have the capability to capture and move ice, rocks, and trees. Avalanches occur in two general forms, or combinations thereof: slab avalanches made of tightly packed snow, triggered by a collapse of an underlying weak snow layer, and loose snow avalanches made of looser snow. After being set off, avalanches usually accelerate rapidly and grow in mass and volume as they capture more snow. If an avalanche moves fast enough, some of the snow may mix with the air, forming a powder snow avalanche. Though they appear to share similarities, avalanches are distinct from slush flows, mudslides, rock slides, and serac collapses. They are also different from large scale movemen ...
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Landslides
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 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 shear strength of ...
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Avalanche
An avalanche is a rapid flow of snow down a slope, such as a hill or mountain. Avalanches can be set off spontaneously, by such factors as increased precipitation or snowpack weakening, or by external means such as humans, animals, and earthquakes. Primarily composed of flowing snow and air, large avalanches have the capability to capture and move ice, rocks, and trees. Avalanches occur in two general forms, or combinations thereof: slab avalanches made of tightly packed snow, triggered by a collapse of an underlying weak snow layer, and loose snow avalanches made of looser snow. After being set off, avalanches usually accelerate rapidly and grow in mass and volume as they capture more snow. If an avalanche moves fast enough, some of the snow may mix with the air, forming a powder snow avalanche. Though they appear to share similarities, avalanches are distinct from slush flows, mudslides, rock slides, and serac collapses. They are also different from large scale movement ...
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William C
William is a male given name of Germanic origin.Hanks, Hardcastle and Hodges, ''Oxford Dictionary of First Names'', Oxford University Press, 2nd edition, , p. 276. It became very popular in the English language after the Norman conquest of England in 1066,All Things William"Meaning & Origin of the Name"/ref> and remained so throughout the Middle Ages and into the modern era. It is sometimes abbreviated "Wm." Shortened familiar versions in English include Will, Wills, Willy, Willie, Bill, and Billy. A common Irish form is Liam. Scottish diminutives include Wull, Willie or Wullie (as in Oor Wullie or the play ''Douglas''). Female forms are Willa, Willemina, Wilma and Wilhelmina. Etymology William is related to the given name ''Wilhelm'' (cf. Proto-Germanic ᚹᛁᛚᛃᚨᚺᛖᛚᛗᚨᛉ, ''*Wiljahelmaz'' > German ''Wilhelm'' and Old Norse ᚢᛁᛚᛋᛅᚼᛅᛚᛘᛅᛋ, ''Vilhjálmr''). By regular sound changes, the native, inherited English form of th ...
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Albany, New York
Albany ( ) is the capital of the U.S. state of New York, also the seat and largest city of Albany County. Albany is on the west bank of the Hudson River, about south of its confluence with the Mohawk River, and about north of New York City. The city is known for its architecture, commerce, culture, institutions of higher education, and rich history. It is the economic and cultural core of the Capital District of the State of New York, which comprises the Albany–Schenectady–Troy Metropolitan Statistical Area, including the nearby cities and suburbs of Troy, Schenectady, and Saratoga Springs. With an estimated population of 1.1 million in 2013, the Capital District is the third most populous metropolitan region in the state. As of 2020, Albany's population was 99,224. The Hudson River area was originally inhabited by Algonquian-speaking Mohican (Mahican), who called it ''Pempotowwuthut-Muhhcanneuw''. The area was settled by Dutch colonists who, in 1614, built Fort ...
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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 ...
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Adirondak Loj
The Adirondak Loj (pronounced "Adirondack Lodge") is a historic lodge in North Elba, Essex County, New York. It is near Lake Placid in the Adirondack Mountains. The current facility, located on the shore of Heart Lake, was built in 1927 and is owned and operated by ADK ( Adirondack Mountain Club). The Loj property hosts the trailhead of the popular Van Hoevenberg Trail, which leads to Mount Marcy and Algonquin Peak, the two highest points in the state. Accommodations include private rooms and hostel-style bunkrooms, with a buffet breakfast included and dinner available by reservation. There are also campsites, lean-tos, and canvas tents available on the property at the Wilderness Campground, which is also managed by ADK. The Loj sits on a private protected area of 706 acres that includes Heart Lake and Mount Jo; the preserve is owned and managed by ADK. History Currently in its second iteration, the original Adirondack Lodge was designed by Henry Van Hoevenberg, one of the ...
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Hudson River
The Hudson River is a river that flows from north to south primarily through eastern New York. It originates in the Adirondack Mountains of Upstate New York and flows southward through the Hudson Valley to the New York Harbor between New York City and Jersey City, eventually draining into the Atlantic Ocean at Lower New York Bay. The river serves as a political boundary between the states of New Jersey and New York at its southern end. Farther north, it marks local boundaries between several New York counties. The lower half of the river is a tidal estuary, deeper than the body of water into which it flows, occupying the Hudson Fjord, an inlet which formed during the most recent period of North American glaciation, estimated at 26,000 to 13,300 years ago. Even as far north as the city of Troy, the flow of the river changes direction with the tides. The Hudson River runs through the Munsee, Lenape, Mohican, Mohawk, and Haudenosaunee homelands. Prior to European ...
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Mount Marshall (New York)
Mount Marshall is a mountain located in Essex County, New York, Essex County, New York (state), New York. Originally named for Governor DeWitt Clinton, and then for Herbert Clark, it was renamed for wilderness activist Bob Marshall (wilderness activist), Bob Marshall (1901–1939) after his death. Marshall is part of the MacIntyre Mountains. Mount Marshall is flanked to the northeast by Iroquois Peak, and faces Wallface Mountain to the northwest across Indian Pass. The northeast end of Mount Marshall drains into Cold Brook, thence into Lake Colden, the Flowed Lands, the Opalescent River, the Hudson River, and into New York Bay. The east side of Mt. Marshall drains into Herbert Brook, thence into the Flowed Lands. The southwest end of Mt. Marshall drains into Calamity Brook, thence into the Hudson River. The west side of Marshall drains into the southern Indian Pass Brook, thence into Henderson Lake (New York), Henderson Lake, the source of the Hudson River. The north side of Ma ...
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