Noyes Mountain (Maine)
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Noyes Mountain (Maine)
Noyes Mountain is a mountain located in Maine near the town of South Paris. It is named after George Lorenzo Noyes, who built and operated Harvard Quarry located nearby. Noyes Mountain stands within the watershed of the Little Androscoggin River, which drains into the Androscoggin River, and thence into Merrymeeting Bay in the Kennebec River The Kennebec River (Abenaki language, Abenaki: ''Kinəpékʷihtəkʷ'') is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map , accessed June 30, 2011 river within the U.S. state of Maine. It ri ... estuary. The east and south sides of Noyes Mtn. drain into Pennesseewassee Lake, and thence into Pennesseewassee Stream and the Little Androscoggin River. The northeast side of Noyes Mtn. drains into Niles Brook, and the Little Androscoggin. The west side of Noyes Mtn. drains into Mud Pond, thence into Hicks Pond and Niles Brook. Tourist attractions Noyes Mountain has many tourist at ...
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Key Col
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'', or ''linking col'', or ''link'') is defined as the highest of these points, along all connecting paths; the prom ...
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Oxford County, Maine
Oxford County is a county in the state of Maine, United States. As of the 2020 Census, the county had a population of 57,777. Its county seat is the town of Paris. The county was formed on March 4, 1805, by the Massachusetts General Court in the Maine District from northerly portions of York and Cumberland counties. It borders the Canadian province of Quebec. Part of Oxford County is included in the Lewiston- Auburn, Maine metropolitan New England City and Town Area while a different part of Oxford County is included in the Portland- South Portland-Biddeford, Maine metropolitan New England City and Town Area. Geography According to the U.S. Census Bureau, the county has a total area of , of which is land and (4.5%) is water. Adjacent counties and municipalities * Franklin County – northeast * Androscoggin County – east * Cumberland County – southeast * York County – south * Carroll County, New Hampshire – southwest * Coös County, New Hampshire – west * Le G ...
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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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United States Geological Survey
The United States Geological Survey (USGS), formerly simply known as the Geological Survey, is a scientific agency of the United States government. The scientists of the USGS study the landscape of the United States, its natural resources, and the natural hazards that threaten it. The organization's work spans the disciplines of biology, geography, geology, and hydrology. The USGS is a fact-finding research organization with no regulatory responsibility. The agency was founded on March 3, 1879. The USGS is a bureau of the United States Department of the Interior; it is that department's sole scientific agency. The USGS employs approximately 8,670 people and is headquartered in Reston, Virginia. The USGS also has major offices near Lakewood, Colorado, at the Denver Federal Center, and Menlo Park, California. The current motto of the USGS, in use since August 1997, is "science for a changing world". The agency's previous slogan, adopted on the occasion of its hundredt ...
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South Paris, Maine
South Paris is a census-designated place (CDP) located within the town of Paris in Oxford County, Maine, in the United States. The population was 2,237 at the 2000 census. While the CDP refers only to the densely settled area in the southern part of the town of Paris, the entire town, outside of Paris Hill, is located within the South Paris ZIP code, resulting in many residents referring to the entire town as South Paris. History During the 19th-century, the Little Androscoggin River provided water power to operate mills in South Paris, and the village grew up around them. The opening of the Atlantic and St. Lawrence Railroad on June 8, 1850 further spurred development of the small mill town. In the 1890s, the Oxford County Courthouse moved from Paris Hill to be near the Grand Trunk Railway station. Much of the manufacturing and industry faded with the Great Depression, but South Paris remains the commercial section of Paris, and retains much of its Victorian era architecture ...
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George Lorenzo Noyes
George "Shavey" Lorenzo Noyes (August 30, 1863 – 1945) was an American mineralogist, naturalist, development criticism, development critic, writer and landscape artist. Biography Noyes was born in Norway, Maine, and was the son of Amos Oscar Noyes and Anna Chase Noyes. Since A. Oscar Noyes neglected the family as he was away much of the time attending to his business interests and civic commitments, George's mother Anna had the most influence on him. As a result, young George spent extended periods with his grandfather Chase in the western mountains of Maine where he came to embrace the solitude of the Maine wilderness, rejecting formal education and organized religion. He was known as the thoreauvian of Maine. In the summer of 1890, while in Fryeburg, Maine, George went to the nearby White Mountain art, White Mountain artist colony in North Conway, New Hampshire to pursue his interest in art and talked with some of the many artists who came there every summer. It is not known h ...
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Drainage Basin
A drainage basin is an area of land where all flowing surface water converges to a single point, such as a river mouth, or flows into another body of water, such as a lake or ocean. A basin is separated from adjacent basins by a perimeter, the '' drainage divide'', made up of a succession of elevated features, such as ridges and hills. A basin may consist of smaller basins that merge at river confluences, forming a hierarchical pattern. Other terms for a drainage basin are catchment area, catchment basin, drainage area, river basin, water basin, and impluvium. In North America, they are commonly called a watershed, though in other English-speaking places, "watershed" is used only in its original sense, that of a drainage divide. In a closed drainage basin, or endorheic basin, the water converges to a single point inside the basin, known as a sink, which may be a permanent lake, a dry lake, or a point where surface water is lost underground. Drainage basins are similar ...
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Little Androscoggin River
} The Little Androscoggin River is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map, accessed June 30, 2011 river in Maine. It flows from Bryant Pond in Woodstock () to its confluence with the Androscoggin River in Auburn. The Androscoggin flows into Merrymeeting Bay in the Kennebec River estuary. The Little Androscoggin flows through the towns of Woodstock, Greenwood, West Paris, Paris (including the village of South Paris), Norway, Oxford, Mechanic Falls, Minot, and Poland, and the city of Auburn. Thompson Lake Thompson Lake is the largest lake in the Little Androscoggin watershed. The north end of the lake overflows into the Little Androscoggin River through the village of Oxford. The lake forms the boundary between Otisfield to the west and Oxford and Poland to the northeast and southeast, respectively. The southern tip of the lake is in Casco. Greeley Brook is the largest tributary to the lake, and flows from Sand Pon ...
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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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Merrymeeting Bay
Merrymeeting Bay is a large freshwater tidal bay located in the U.S. state of Maine. Merrymeeting Bay's unusual geography defies common landform terms. It is not what is usually meant by the word bay. It is somewhat like an estuary but it has fresh water with very little salt. Geologically it is described as an "inland delta" and biologically as "tidal riverine." The head of Merrymeeting Bay is generally considered to begin at the southernmost point of Swan Island. Bordering towns and cities include Bath, Brunswick, Topsham, Bowdoinham, Dresden, and Woolwich. Public access to the bay is gained mainly from public docks on one of the contributing rivers in Brunswick, Bath, Richmond, and Bowdoinham. Geology Six rivers flow into the bay, the two largest being the Kennebec River and the Androscoggin River. The four smaller rivers are the Cathance, Eastern, Abagadasset, and Muddy rivers. The bay receives water from nearly 40% of Maine's land area as well as from part of New Ha ...
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Kennebec River
The Kennebec River (Abenaki language, Abenaki: ''Kinəpékʷihtəkʷ'') is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map , accessed June 30, 2011 river within the U.S. state of Maine. It rises in Moosehead Lake in west-central Maine. The East and West Outlets join at Indian Pond and the river flows southward. Harris Station Dam, the largest hydroelectric dam in the state, was constructed near that confluence. The river is joined at The Forks, Maine, The Forks by its tributary the Dead River (Kennebec River), Dead River, also called the West Branch. It continues south past the cities of Madison, Maine, Madison, Skowhegan, Maine, Skowhegan, Waterville, Maine, Waterville, and the state capital Augusta, Maine, Augusta. At Richmond, Maine, Richmond, it flows into Merrymeeting Bay, a freshwater tidal bay into which also flow the Androscoggin River and five smaller rivers. The Kennebec runs past the shipbuilding center of Bath, ...
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Estuary
An estuary is a partially enclosed coastal body of brackish water with one or more rivers or streams flowing into it, and with a free connection to the open sea. Estuaries form a transition zone between river environments and maritime environments and are an example of an ecotone. Estuaries are subject both to marine influences such as tides, waves, and the influx of saline water, and to fluvial influences such as flows of freshwater and sediment. The mixing of seawater and freshwater provides high levels of nutrients both in the water column and in sediment, making estuaries among the most productive natural habitats in the world. Most existing estuaries formed during the Holocene epoch with the flooding of river-eroded or glacially scoured valleys when the sea level began to rise about 10,000–12,000 years ago. Estuaries are typically classified according to their geomorphological features or to water-circulation patterns. They can have many different names, such as bays, ...
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