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Mount Cardigan
Mount Cardigan is a prominent bare-rock summit in the towns of Orange and Alexandria in western New Hampshire, USA. While its peak is only above sea level, it has extensive areas of bare granite ledges and alpine scrub, giving it the feel to hikers of a much higher mountain. Most of the summit area was denuded by devastating forest fires in 1855. The Civilian Conservation Corps helped to develop the alpine ski trail network still in use today on the east side of the mountain. The mountain is set in the Cardigan Mountain State Park. The Cardigan Lodge, operated by the Appalachian Mountain Club since 1934, is located to the east at the foot of the mountain, and is often used as a base for day hikes in and around the mountain. Many schools from around New England have overnight field trips to the mountain during the autumn and spring months.. The mountain is also a popular destination for Boy Scout troops. Geology The bedrock of Mount Cardigan is the upper member of the Lower ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Orange, New Hampshire
Orange is a town in Grafton County, New Hampshire, United States. The population was 277 at the 2020 census, down from 331 at the 2010 census.United States Census BureauAmerican FactFinder 2010 Census figures. Retrieved March 23, 2011. History Orange was granted in 1769 and incorporated in 1790. It was originally named "Cardigan", after George Brudenell, fourth Earl of Cardigan. The Cardigan name lives on with Mount Cardigan and Cardigan Mountain State Park. After the American Revolution, voters attempted to rename the town "Bradford", "Middletown", "Liscomb", and finally "Orange". The large quantities of yellow-orange ochre found in Mount Cardigan may have been the source of the name Orange. Geography According to the United States Census Bureau, the town has a total area of , of which are land and are water, comprising 0.25% of the town. The highest point in Orange is the summit of Mount Cardigan, at above sea level, near the eastern edge of the town. The west side ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bronson Hill Island Arc
The Bronson Hill Arc is a bimodal volcanic arc and associated sediments that formed over a west (?) dipping subduction zone during the Ordovician period (c. 475 - 450 million years ago (Ma)) as part of the Taconic Orogeny. These rocks are presently well exposed along the Connecticut River Valley of Vermont and New Hampshire. The arc is evidenced by plutonism and extrusive volcanicsm, including the Ammonoosuc Volcanics (c. 461 Ma from U/Pb zircon dates) and the overlying Partridge Formation (c. 457 Ma from graptolites in the formation). It is related to the slightly older Shelburne Falls arc that sits to the west. These rocks were metamorphosed and deformed during the Acadian Orogeny and the Alleghenian Orogeny The Alleghanian orogeny or Appalachian orogeny is one of the geological mountain-forming events that formed the Appalachian Mountains and Allegheny Mountains. The term and spelling Alleghany orogeny was originally proposed by H.P. Woodward in 195 .... References *Rob ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Newfound Lake
Newfound Lake is located in Grafton County, New Hampshire, United States. It is situated in the Lakes Region of central New Hampshire, in the towns of Alexandria, Bridgewater, Bristol, and Hebron. Its area of places it behind only Lake Winnipesaukee and Squam Lake among lakes located entirely within New Hampshire, and fourth in the state overall, when Umbagog Lake on the Maine border is included. Geography Newfound Lake has of shoreline. The lake is about wide and long. The deepest point is . Major tributaries include the Fowler River and the Cockermouth River. Its outlet is the Newfound River, flowing through Bristol village into the Pemigewasset River. The lake volume is 98 billion gallons of water. Wellington State Park, containing the largest freshwater swimming beach in the New Hampshire state park system, is a property located on the lake's west shore in the town of Bristol. Belle Island is a small island near the southern end of the lake. It was given to the state ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fowler River
The Fowler River is a river located in central New Hampshire in the United States. It is an inflow to Newfound Lake, part of the Pemigewasset and Merrimack River watersheds. Below Bog Brook, the Fowler River is subject to the New Hampshire Comprehensive Shoreland Protection Act. The primary tributary of the river is Clark Brook, which rises south of Mount Cardigan in the town of Alexandria and drops over Welton Falls. Chesley Brook joins from the north, at which point the stream valley widens and begins to support small agricultural operations. The brook's name changes to "Fowler River" when Brock Brook joins from the right at the first crossing of Fowler River Road. The river flows southeast to a junction with Bog Brook, where it turns north and flows one mile to Newfound Lake. See also *List of rivers of New Hampshire This is a list of rivers and significant streams in the U.S. state of New Hampshire. All watercourses named "River" (freshwater or tidal) are listed here, as ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gulf Of Maine
The Gulf of Maine is a large gulf of the Atlantic Ocean on the east coast of North America. It is bounded by Cape Cod at the eastern tip of Massachusetts in the southwest and by Cape Sable Island at the southern tip of Nova Scotia in the northeast. The gulf includes the entire coastlines of the U.S. states of New Hampshire and Maine, as well as Massachusetts north of Cape Cod, and the southern and western coastlines of the provinces and territories of Canada, Canadian provinces of New Brunswick and Nova Scotia, respectively. The gulf was named for the adjoining English colonial Province of Maine, which was in turn likely named by early explorers after the Maine (province), province of Maine in France. Massachusetts Bay, Penobscot Bay, Passamaquoddy Bay, and the Bay of Fundy are all arms of the Gulf of Maine. Geography and hydrography The Gulf of Maine is a roughly rectangular depression with a surface area of around , enclosed to the west and north by the North American mainland ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pemigewasset River
The Pemigewasset River , known locally as "The Pemi", is a river in the state of New Hampshire, the United States. It is in length and (with its tributaries) drains approximately . The name "Pemigewasset" comes from the Abenaki word ''bemijijoasek'' əmidzidzoasək meaning "where side (entering) current is". Geography The Pemigewasset originates at Profile Lake in Franconia Notch State Park, in the town of Franconia. It flows south through the White Mountains and merges with the Winnipesaukee River to form the Merrimack River at Franklin. The Merrimack then flows through southern New Hampshire, northeastern Massachusetts and into the Atlantic Ocean. The Interstate 93 highway runs parallel with the river between Franconia Notch and New Hampton. The river passes through the communities of Lincoln, North Woodstock, Woodstock, Thornton, Campton, Plymouth, Holderness, Ashland, Bridgewater, Bristol, New Hampton, Hill, Sanbornton, and Franklin. The river descends over water ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Smith River (Pemigewasset River)
The Smith River is a river located in central New Hampshire in the United States. It is a tributary of the Pemigewasset River, part of the Merrimack River drainage basin, watershed. The Smith River begins at the outlet of Tewksbury Pond in Grafton, New Hampshire. The river flows southwest and then southeast through Grafton, passing through Kilton Pond. Continuing through Danbury, New Hampshire, Danbury, the river remains generally flat until shortly before reaching the Alexandria, New Hampshire, Alexandria-Hill, New Hampshire, Hill town line, where it enters a narrow valley and produces several miles of whitewater. Passing under the New Hampshire Route 3A bridge at the Bristol, New Hampshire, Bristol-Hill town line, the Smith River drops over Profile Falls and arrives at the Pemigewasset River. U.S. Route 4 follows the Smith River from its source to Danbury. New Hampshire Route 104, NH-104 follows the river from Danbury to the east side of Alexandria. See also *List of rivers of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Long Island Sound
Long Island Sound is a marine sound and tidal estuary of the Atlantic Ocean. It lies predominantly between the U.S. state of Connecticut to the north and Long Island in New York to the south. From west to east, the sound stretches from the East River in New York City, along the North Shore of Long Island, to Block Island Sound. A mix of freshwater from tributaries and saltwater from the ocean, Long Island Sound is at its widest point and varies in depth from . Shoreline Major Connecticut cities on the Sound include Stamford, Norwalk, Bridgeport, New Haven, and New London. Cities on the New York side of the Sound include Rye, Glen Cove, New Rochelle, Larchmont and portions of Queens and the Bronx in New York City. Climate and geography The climate of Long Island Sound is warm temperate or Cfa in the Köppen climate classification. Summers are hot and humid often with convective showers and strong sunshine, while the cooler months feature cold temperatures and a mix o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mascoma River
The Mascoma River is a river in western New Hampshire in the United States. It is a tributary of the Connecticut River, which flows to Long Island Sound. The Mascoma comprises two sections which are split by Mascoma Lake in the communities of Enfield and Lebanon. Counting the lake would add to the river's length. The Mascoma River begins at Cummins Pond in a heavily forested part of the town of Dorchester and flows south into the town of Canaan, collecting water flowing from Reservoir Pond, Clark Pond, and Canaan Street Lake before reaching the Indian River. Here it turns west, collecting tributaries arriving from Goose Pond and Crystal Lake, before it passes through the mill town of Enfield and arrives at Mascoma Lake. At the western end of Mascoma Lake, the Mascoma River, now in Lebanon, drops quickly over rapids, passing numerous small hydroelectric dams in the center of Lebanon and on its way to West Lebanon, where it reaches the Connecticut River. The section of the ri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Indian River (New Hampshire)
The Indian River is a river in western New Hampshire in the United States. It is a tributary of the Mascoma River, which in turn flows to the Connecticut River and ultimately Long Island Sound. The Indian River rises in the southern corner of the town of Dorchester and flows south in a broad valley to the west of Mount Cardigan. At the town center of Canaan, the river turns west and shortly ends at the Mascoma River. For its south-flowing portion, the Indian River is followed by New Hampshire Route 118. From Canaan to the Mascoma River, U.S. Route 4 is close by. See also *List of rivers of New Hampshire This is a list of rivers and significant streams in the U.S. state of New Hampshire. All watercourses named "River" (freshwater or tidal) are listed here, as well as other streams which are either subject to thNew Hampshire Comprehensive Shoreland ... References Rivers of New Hampshire Tributaries of the Connecticut River Rivers of Grafton County, New Hampshire ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canaan, New Hampshire
Canaan is a town in Grafton County, New Hampshire, United States. The population was 3,794 at the 2020 census. It is the location of Mascoma State Forest. Canaan is home to the Cardigan Mountain School, the town's largest employer. The main village of the town, where 442 people resided at the 2020 census, is defined as the Canaan census-designated place (CDP), and is located at the junction of U.S. Route 4 with New Hampshire Route 118. History Chartered in 1761 by Governor Benning Wentworth, the town was named after the hometown of many early settlers, Canaan, Connecticut, which had been named by Puritans for the biblical land of Canaan. It was settled in the winter of 1766–1767 by John Scofield, who arrived with all his belongings on a hand sled. The land was filled with rocks, making agriculture difficult. The town constructed a broad road for its main street on a stretch of level land. In 1828 attorney George Kimball helped organize building the town's Congregational ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
