Wildcat Hollow, Connecticut
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Wildcat Hollow, Connecticut
Wildcat Hollow is a valley in the Appalachian Mountains in rural Litchfield County, Connecticut located on a riverbend of the Housatonic River. It is located about 3 miles west of Salisbury Salisbury ( ) is a cathedral city in Wiltshire, England with a population of 41,820, at the confluence of the rivers Avon, Nadder and Bourne. The city is approximately from Southampton and from Bath. Salisbury is in the southeast of Wil ..., miles north of Falls Village, 2 miles south of Twin Lakes, and a mile north west of the peak of Mount Prospect. It also has two roads, Wildcat Hollow Road that heads North West up Flink Hill and Housatonic River Road that runs north from Amesville and Falls Village to the south up north to Smith Hill. References External linksWildcat Hollow on google maps {{coord, 41.9885, -73.3709, type:landmark_source:enwiki-googlemaplink, display=title Valleys of Connecticut Landforms of Litchfield County, Connecticut ...
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Valley
A valley is an elongated low area often running between Hill, hills or Mountain, mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacier, glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glaciation, glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In karst, areas of limestone bedrock, dry valleys may also result from drainage now taking place cave, underground rather than at the surface. Rift valleys arise principally from tectonics, earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms th ...
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Appalachian Mountains
The Appalachian Mountains, often called the Appalachians, (french: Appalaches), are a system of mountains in eastern to northeastern North America. The Appalachians first formed roughly 480 million years ago during the Ordovician Period. They once reached elevations similar to those of the Alps and the Rocky Mountains before experiencing natural erosion. The Appalachian chain is a barrier to east–west travel, as it forms a series of alternating ridgelines and valleys oriented in opposition to most highways and railroads running east–west. Definitions vary on the precise boundaries of the Appalachians. The United States Geological Survey (USGS) defines the ''Appalachian Highlands'' physiographic division as consisting of 13 provinces: the Atlantic Coast Uplands, Eastern Newfoundland Atlantic, Maritime Acadian Highlands, Maritime Plain, Notre Dame and Mégantic Mountains, Western Newfoundland Mountains, Piedmont, Blue Ridge, Valley and Ridge, St. Lawrence Valley, Appalac ...
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Litchfield County, Connecticut
Litchfield County is in northwestern Connecticut. As of the 2020 census, the population was 185,186. The county was named after Lichfield, in England. Litchfield County has the lowest population density of any county in Connecticut and is the state's largest county by area. Litchfield County comprises the Torrington, CT Micropolitan Statistical Area, which is included in the New York–Newark, NY– NJ–CT– PA Combined Statistical Area. As is the case with the other seven Connecticut counties, there is no county government and no county seat. Each town is responsible for all local services such as schools, snow removal, sewers, and fire and police departments. However, in some cases in rural areas, adjoining towns may agree to jointly provide services or even establish a regional school system. History Litchfield County was created on October 9, 1751, by an act of the Connecticut General Court from land belonging to Fairfield, New Haven, and Hartford counties. The ac ...
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Connecticut
Connecticut () is the southernmost state in the New England region of the Northeastern United States. It is bordered by Rhode Island to the east, Massachusetts to the north, New York to the west, and Long Island Sound to the south. Its capital is Hartford and its most populous city is Bridgeport. Historically the state is part of New England as well as the tri-state area with New York and New Jersey. The state is named for the Connecticut River which approximately bisects the state. The word "Connecticut" is derived from various anglicized spellings of "Quinnetuket”, a Mohegan-Pequot word for "long tidal river". Connecticut's first European settlers were Dutchmen who established a small, short-lived settlement called House of Hope in Hartford at the confluence of the Park and Connecticut Rivers. Half of Connecticut was initially claimed by the Dutch colony New Netherland, which included much of the land between the Connecticut and Delaware Rivers, although the firs ...
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Housatonic River
The Housatonic River ( ) is a river, approximately long,U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map , accessed April 1, 2011 in western Massachusetts and western Connecticut in the United States. It flows south to southeast, and drains about of southwestern Connecticut into Long Island Sound. Its Drainage basin, watershed is just to the west of the watershed of the lower Connecticut River. History Indigenous history Indigenous people began using the river area for fishing and hunting at least 6,000 years ago. By 1600, the inhabitants were mostly Mohicans and may have numbered 30,000. The river's name is derived from the Mohican phrase ''"usi-a-di-en-uk"'', translated as "beyond the mountain place" or "river of the mountain place".Housatonic Valley Association. Cornwall Bridge, CT"History of the Housatonic Valley." Accessed 2015-10-1. It is referred to in the deed by which a group of twelve colonists called "The Proprietor ...
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Salisbury, Connecticut
Salisbury () is a town situated in Litchfield County, Connecticut, United States. The town is the northwesternmost in the state of Connecticut; the Massachusetts-New York-Connecticut tri-state marker is located at the northwest corner of the town. The population was 4,194 at the 2020 census. History Salisbury was established and incorporated in 1741, and contains several historic homes, though some were replaced by larger modern structures in the late 20th century. Salisbury was named for Salisbury, a city in England. Historian Ed Kirby tells that traces of iron were discovered in what was to become Salisbury in 1728, with the discovery of the large deposit at Old Hill (later Ore Hill) in 1731 by John Pell and Ezekiel Ashley. From before the American Revolution, through the Federal Period of the nation, and until around 1920, Salisbury was the seat of an important iron industry. Additional iron mines were opened, mostly in the western end of the town, although historian Diana ...
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Falls Village, Connecticut
Falls Village is a village and census-designated place in the town of Canaan in Litchfield County, Connecticut, United States. As of the 2010 census it had a population of 538, out of 1,234 in the entire town of Canaan. Because Falls Village is the town center and principal constituent village in Canaan, the entire town is often referred to as "Falls Village". That usage also avoids confusion of the town with Canaan Village in the town of North Canaan, Connecticut, just to the north. Falls Village derives its name from a waterfall, known as Great Falls, on the Housatonic River within the village. The Falls Village post office is assigned ZIP code 06031, which encompasses the entire town of Canaan. Geography Falls Village is on the western side of the town of Canaan in northwestern Connecticut. The western edge of the census-designated place is the Canaan–Salisbury town line following the Housatonic River, it extends north of the village as far as Page Road, and south to a pow ...
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Twin Lakes, Connecticut
The Twin Lakes are adjacent Lakes Washining and Washinee, commonly referred to as East Twin Lake and West Twin Lake, in Salisbury amidst Connecticut's Northwest Hills. Geography Lake Washinee is about 1.6 miles (2.6 km) long, and under a quarter mile (0.4 km) wide of except for its squarish roughly 0.5 by 0.6 mile (0.8 by 1.0 km) southernmost section. Its deepest part is around . Lake Washining is much rounder, and roughly 0.9 by 1.3 miles (1.5 by 2 km). It has a maximum depth of . Much of the shore is wetland, but there are some private residences. There is a thermocline that forms around . The Twin Lakes are located in Salisbury, Connecticut, roughly five miles away from both the Massachusetts and New York borders. The two lakes are separated by an isthmus under 300 feet (100 m) wide, and they maintain the same water level. They are located in the Housatonic Valley in northwestern Connecticut. Near the 'Between the Lakes Road' is located a series of lime ...
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Mount Prospect (Connecticut)
Mount Prospect may refer to: * Mount Prospect, Illinois, an incorporated village in Cook County, Illinois ** Mount Prospect Public Library ** Mount Prospect School District 57 ** Mount Prospect station, a railroad station * Mount Prospect (Leggett, North Carolina), a historic house * Mount Prospect, a subordinate summit of Mount Greylock, located in Massachusetts * Mount Prospect Baptist Church, Rock Hill, South Carolina * Mount Prospect Methodist Church The Mt. Prospect Methodist Church was designed by John Pickering in a Greek Revival style and was built in 1886. It was listed on the National Register of Historic Places The National Register of Historic Places (NRHP) is the United State ..., Richland, Arkansas * Mount Prospect Park, in Brooklyn, New York {{Disambig ...
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Valleys Of Connecticut
A valley is an elongated low area often running between hills or mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In areas of limestone bedrock, dry valleys may also result from drainage now taking place underground rather than at the surface. Rift valleys arise principally from earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms that may be global in use or else applied only locally. For ...
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