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Atkinson And Gilmanton Academy Grant, New Hampshire
Atkinson and Gilmanton Academy Grant is a township in Coös County, New Hampshire, United States. It was granted by the state legislature to Gilmanton Academy and Atkinson Academy in equal shares in 1809 and contained about . It was later expanded by annexation of previously ungranted land to the west. The population was zero as of the 2020 census. It is part of the Berlin, NH– VT Micropolitan Statistical Area. In New Hampshire, locations, grants, townships (which are different from towns), and purchases are unincorporated portions of a county which are not part of any town and have limited self-government (if any, as many are uninhabited). Atkinson and Gilmanton Academy Grant will fall within the path of totality during the solar eclipse of April 8, 2024. Geography According to the United States Census Bureau, the grant has a total area of , of which are land and or 0.57%, is covered by water. The township is drained by the Dead Diamond River and its branches, exce ...
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Coös County, New Hampshire
Coös County (, with two syllables), frequently spelled Coos County, is a county in the U.S. state of New Hampshire. As of the 2020 census, the population was 31,268, making it the least-populated county in the state. The county seat is Lancaster. The two-syllable pronunciation is sometimes indicated with a diaeresis, notably in the Lancaster-based weekly newspaper ''The Coös County Democrat'' and on some county-owned vehicles. The county government uses both spellings interchangeably. Coös County is part of the Berlin, NH– VT Micropolitan Statistical Area. It is the only New Hampshire county on the Canada–United States border, south of the province of Quebec, and thus is home to New Hampshire's only international port of entry, the Pittsburg–Chartierville Border Crossing. The only city in Coös County is Berlin, with the rest of the communities being towns, or unincorporated townships, gores and grants. Coös County includes the northernmost part of the state. M ...
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Berlin Micropolitan Area
The Berlin Micropolitan Statistical Area is the core-based statistical area centered on the urban cluster associated with the city Berlin, New Hampshire, in the United States. As defined by the Office of Management and Budget using counties as building blocks, the area consists of two counties – Coos County in New Hampshire, which contains the city of Berlin, and the adjacent Essex County in Vermont. An alternative definition using towns as building blocks is the Berlin Micropolitan NECTA. In addition to the city of Berlin, the NECTA consists of the towns of Dummer, Gorham, Milan, Randolph, Shelburne, Stark, and Success. As of the 2000 census, the micropolitan area had a population of 39,570 (though a July 1, 2009 estimate placed the population at 37,881). As of the 2000 census, the NECTA had a population of 16,102. Counties *Coos County, New Hampshire *Essex County, Vermont Communities Coos County *Cities **Berlin (Principal city) *Towns ** Carroll ** Clarksv ...
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Lincoln Plantation, Maine
Lincoln Plantation is a plantation in Oxford County, Maine, United States. It contains the village of Wilson's Mills. The population was 41 at the 2020 census. Geography According to the United States Census Bureau, the plantation has a total area of 36.8 square miles (95.4 km²), of which, 32.5 square miles (84.1 km²) of it is land and 4.4 square miles (11.3 km²) of it (11.83%) is water. The southern portion of the Aziscohos Lake reservoir is located in the plantation, along with the Aziscohos Dam on the Magalloway River that impounds the reservoir. Lincoln Plantation is also home to Aziscohos Mountain, whose summit sits at an elevation of . Demographics As of the census of 2000, there were 46 people, 24 households, and 19 families residing in the plantation. The population density was 1.4 people per square mile (0.5/km²). There were 119 housing units at an average density of 3.7 per square mile (1.4/km²). The racial makeup of the plantatio ...
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North Oxford, Maine
North Oxford is an unorganized territory in Oxford County, Maine, United States. The population was 16 at the 2020 census. Geography According to the United States Census Bureau, the unorganized territory has a total area of 546.2 square miles (1,414.7 km2), of which, 509.6 square miles (1,319.9 km2) of it is land and 36.6 square miles (94.8 km2) of it (6.70%) is water. The territory consists of fifteen townships, which are Riley, Grafton, Andover North Surplus, Andover West Surplus, Township C, C Surplus, Richardsontown, Adamstown, Lower Cupsuptic, Parkertown, Upper Cupsuptic, Lynchtown, Oxbow, Parmachenee, and Bowmantown. The terrain is mountainous with little level ground suitable for raising crops; and the elevation causes frost in June and August leaving a growing season of about 60 days. History of Grafton Grafton, the southernmost township, was the only township to achieve incorporation. The first European settler was James Brown in 1834. ...
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Pittsburg, New Hampshire
Pittsburg is a town in Coös County, New Hampshire, United States. The population was 800 at the 2020 census. It is the northernmost town in New Hampshire and the largest town by area in New England. U.S. Route 3 is the only major highway in the town, although the northern terminus of New Hampshire Route 145 also lies within Pittsburg. Pittsburg is part of the Berlin, New Hampshire–Vermont Micropolitan Statistical Area. History Pittsburg derives its name from William Pitt, Prime Minister of Great Britain. Prior to its incorporation in 1840, the area was settled and known as the Territory of Indian Stream. It had the unique distinction of having been its own microstate briefly during the 1830s, called the Republic of Indian Stream, due to an ambiguous boundary between the United States and Canada. The Indian Stream Schoolhouse on Tabor Road, which dates to 1897, is listed in both the National Register of Historic Places and the New Hampshire State Register of Historic P ...
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Clarksville, New Hampshire
Clarksville is a town in northern Coös County, New Hampshire, United States. The population was 294 at the 2020 census. It is part of the Berlin, NH– VT Micropolitan Statistical Area. History The first census taken was in 1830; there were 88 residents. Clarksville was incorporated in 1853, but known as "Dartmouth College Grant" until 1872. Clarksville derives its name from the Clark family, who cleared the land for settlement. The area was originally part of a tract granted to Dartmouth College; sections were sold off by the college to raise money. It was purchased by Benjamin Clark of Boston and Joseph Murdock of Norwich, Vermont. In the late 19th century, major industries included starch and maple sugar.1874 ''NH Gazetteer'' For many years the largest employers in town have been logging companies. Geography Clarksville is bordered to the north and west by Pittsburg, and to the west by one mile of waterfront on the Connecticut River (across from the village of Bee ...
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Second College Grant, New Hampshire
Second College Grant (also known as the Dartmouth College Grant) is a township in Coös County, New Hampshire, United States. The area of this township is owned and controlled by Dartmouth College. As of the 2020 census, the grant had a population of one. In New Hampshire, locations, grants, purchases, and townships (which are different from towns) are unincorporated portions of a county which are not part of any town and have limited self-government (if any, as many are uninhabited). Trails and cabins are available for use by the Dartmouth community, and are maintained by the Dartmouth Outing Club and Dartmouth's Outdoor Programs Office. The DOC maintains three cabins available for rent by DOC members (Peaks, Alder Brook, and Stoddard), and the OPO maintains seven cabins for use by Dartmouth-affiliated individuals and their guests. Many freshmen spend a few days in the grant as part of their freshmen trips just before freshman orientation. The grant is also used for timber prod ...
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Dix's Grant, New Hampshire
Dix's Grant is a township in Coös County, New Hampshire, United States. As of the 2020 census, the grant had a population of zero. In New Hampshire, locations, grants, townships (which are different from towns), and purchases are unincorporated portions of a county which are not part of any town and have limited self-government (if any, as many are uninhabited). Dix's Grant will fall within the path of totality during the solar eclipse of April 8, 2024. History Dix's Grant was originally part of adjacent Dixville, which was granted by the legislature to Timothy Dix Jr. in 1805 and contained about ; the price was $4,500. The eastern portion of the original grant (north of Wentworth Location) became present-day Dix's Grant. Geography According to the United States Census Bureau, the grant has a total area of , of which is covered by water. The township is drained by the Swift Diamond River and its tributary, Fourmile Brook. The Swift Diamond is an east-flowing tributary o ...
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Maine
Maine () is a state in the New England and Northeastern regions of the United States. It borders New Hampshire to the west, the Gulf of Maine to the southeast, and the Canadian provinces of New Brunswick and Quebec to the northeast and northwest, respectively. The largest state by total area in New England, Maine is the 12th-smallest by area, the 9th-least populous, the 13th-least densely populated, and the most rural of the 50 U.S. states. It is also the northeasternmost among the contiguous United States, the northernmost state east of the Great Lakes, the only state whose name consists of a single syllable, and the only state to border exactly one other U.S. state. Approximately half the area of Maine lies on each side of the 45th parallel north in latitude. The most populous city in Maine is Portland, while its capital is Augusta. Maine has traditionally been known for its jagged, rocky Atlantic Ocean and bayshore coastlines; smoothly contoured mountains; heavily f ...
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Sea Level
Mean sea level (MSL, often shortened to sea level) is an average surface level of one or more among Earth's coastal bodies of water from which heights such as elevation may be measured. The global MSL is a type of vertical datuma standardised geodetic datumthat is used, for example, as a chart datum in cartography and marine navigation, or, in aviation, as the standard sea level at which atmospheric pressure is measured to calibrate altitude and, consequently, aircraft flight levels. A common and relatively straightforward mean sea-level standard is instead the midpoint between a mean low and mean high tide at a particular location. Sea levels can be affected by many factors and are known to have varied greatly over geological time scales. Current sea level rise is mainly caused by human-induced climate change. When temperatures rise, Glacier, mountain glaciers and the Ice sheet, polar ice caps melt, increasing the amount of water in water bodies. Because most of human settlem ...
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Androscoggin River
The Androscoggin River (Abenaki: ''Aləssíkαntekʷ'') is a river in the U.S. states of Maine and New Hampshire, in northern New England. It is U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map, accessed June 30, 2011 long and joins the Kennebec River at Merrymeeting Bay in Maine before its water empties into the Gulf of Maine on the Atlantic Ocean. Its drainage basin is in area. The name "Androscoggin" comes from the Eastern Abenaki term ''/aləssíkɑntəkw/'' or ''/alsíkɑntəkw/'', meaning "river of cliff rock shelters" (literally "thus-deep-dwelling-river"); or perhaps from Penobscot ''/aləsstkɑtəkʷ/'', meaning "river of rock shelters". The Anglicization of the Abenaki term is likely an analogical contamination with the colonial governor Edmund Andros. Course The Androscoggin begins in Errol, New Hampshire, where the Magalloway River joins the outlet of Umbagog Lake. The river flows generally south but with numerous b ...
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Magalloway River
The Magalloway River is a river in northwestern Maine and northern New Hampshire in the United States. It is a tributary of the Androscoggin River, which flows to the Kennebec River at Merrymeeting Bay in Maine, near the Atlantic Ocean. The total length of the river is , or if the distances across intervening lakes are included. The Magalloway River rises near the extreme northwestern corner of Maine, at the juncture of the West Branch and the Third East Branch of the Magalloway. The river flows south through logging country to Parmachenee Lake, then descends for another to the Aziscohos Lake. Below the lake dam, the Magalloway turns west and descends in to the village of Wilsons Mills, Maine, before once again turning south, now along the New Hampshire–Maine border. The river ends where it joins the outlet of Umbagog Lake, forming the Androscoggin River. Tributaries of the Magalloway include the West Branch, the First, Second, and Third East Branches, the Little Magallowa ...
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