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Talcott Mountain
Talcott Mountain of central Connecticut, with a high point of , is a long trap rock mountain ridge located west of the city of Hartford. The ridge, a prominent landscape feature, forms a continuous line of exposed western cliffs visible across the Farmington River valley from Farmington to Simsbury. Talcott Mountain is part of the narrow, linear Metacomet Ridge that extends from Long Island Sound near New Haven, Connecticut, north through the Connecticut River Valley of Massachusetts to the Vermont border.Farnsworth, Elizabeth J"Metacomet-Mattabesett Trail Natural Resource Assessment.", 2004. PDF file. Cited Nov. 20, 2007. A popular outdoor recreation resource, Talcott Mountain is known for its microclimate ecosystems, rare plant communities, and expansive views from cliffs that tower up to above the surrounding landscape.DeLorme Topo 6.0. Mapping Software. DeLorme, Yarmouth, Maine Talcott Mountain encompasses two state parks, several municipal recreation areas and reservoi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Floodplain
A floodplain or flood plain or bottomlands is an area of land adjacent to a river which stretches from the banks of its channel to the base of the enclosing valley walls, and which experiences flooding during periods of high discharge.Goudie, A. S., 2004, ''Encyclopedia of Geomorphology'', vol. 1. Routledge, New York. The soils usually consist of clays, silts, sands, and gravels deposited during floods. Because the regular flooding of floodplains can deposit nutrients and water, floodplains frequently have high soil fertility; some important agricultural regions, such as the Mississippi river basin and the Nile, rely heavily on the flood plains. Agricultural regions as well as urban areas have developed near or on floodplains to take advantage of the rich soil and fresh water. However, the risk of flooding has led to increasing efforts to control flooding. Formation Most floodplains are formed by deposition on the inside of river meanders and by overbank flow. Wherev ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Connecticut River Valley
The Connecticut River is the longest river in the New England region of the United States, flowing roughly southward for through four states. It rises 300 yards (270 m) south of the U.S. border with Quebec, Canada, and discharges at Long Island Sound. Its watershed encompasses , covering parts of five U.S. states and one Canadian province, via 148 tributaries, 38 of which are major rivers. It produces 70% of Long Island Sound's fresh water, discharging at per second. The Connecticut River Valley is home to some of the northeastern United States' most productive farmland, as well as the Hartford–Springfield Knowledge Corridor, a metropolitan region of approximately two million people surrounding Springfield, Massachusetts, and Hartford, Connecticut. History The word "Connecticut" is a corruption of the Mohegan word ''quinetucket'', which means "beside the long, tidal river". The word came into English during the early 1600s to name the river, which was also called simply "T ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Connecticut River
The Connecticut River is the longest river in the New England region of the United States, flowing roughly southward for through four states. It rises 300 yards (270 m) south of the U.S. border with Quebec, Canada, and discharges at Long Island Sound. Its watershed encompasses , covering parts of five U.S. states and one Canadian province, via 148 tributaries, 38 of which are major rivers. It produces 70% of Long Island Sound's fresh water, discharging at per second. The Connecticut River Valley is home to some of the northeastern United States' most productive farmland, as well as the Hartford–Springfield Knowledge Corridor, a metropolitan region of approximately two million people surrounding Springfield, Massachusetts, and Hartford, Connecticut. History The word "Connecticut" is a corruption of the Mohegan word ''quinetucket'', which means "beside the long, tidal river". The word came into English during the early 1600s to name the river, which was also called simply " ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Farmington Mountain
Farmington Mountain, , is a traprock ridge located southwest of Hartford, Connecticut, in the town of Farmington. It is part of the narrow, linear Metacomet Ridge that extends from Long Island Sound near New Haven, Connecticut, north through the Connecticut River Valley of Massachusetts to the Vermont border. Farmington Mountain is known for its microclimate ecosystems, rare plant communities, and for the historic Hill-Stead Museum. Farmington Mountain is traversed by the Metacomet Trail.Farnsworth, Elizabeth J.Metacomet-Mattabesett Trail Natural Resource Assessment." 2004. PDF wefile cited November 1, 2007.DeLorme Topo 6.0. Mapping software. DeLorme, Yarmouth, Maine. Geography Roughly long by wide, Farmington Mountain rises steeply above the town of Farmington to the west. The mountain consists of an upper summit ridge with two distinct peaks and a lower plateau and ledge that hangs just above the center of Farmington. This ledge is contiguous with the lower ridges of Ta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hatchet Hill
Hatchett Hill, est. , is a trap rock ridge located in East Granby, Connecticut, northeast of Hartford, Connecticut. It is part of the narrow, linear Metacomet Ridge that extends from Long Island Sound near New Haven, Connecticut, north through the Connecticut River Valley of Massachusetts to the Vermont border. The southern edge of the ridge plunges nearly 200 vertical feet (61 m) into the Tariffville Gorge. The ridge is known for its rugged topography, unique microclimate ecosystems, rare plant communities, and as a seasonal raptor migration path. It is traversed by the Metacomet Trail. Geography Roughly long by wide, Hatchett Hill is a collection of closely set tiered ridges and abrupt cliff faces with a high point of . Its southern end is cut with steep cliffs at the Tariffville Gorge where the Farmington River gouges out a chasm between it and Talcott Mountain to the south. Also notable is ''Marsh Pond'', a glacial kettle pond nestled in the center of the ridge. From H ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Connecticut Route 185
Route 185 is a Connecticut state highway in the western Hartford suburbs, running from Simsbury to West Hartford. Route description Route 185 begins as Hartford Road at an intersection with US 202 and Route 10 in the Weatogue section of Simsbury. The road heads east across the Farmington River and turns southeast, passing by Talcott Mountain State Park then heading into the town of Bloomfield, where it becomes Simsbury Road. In Bloomfield, it passes the western end of Route 178 and continues generally southeast across the southwestern part of town into West Hartford. At the Bloomfield-West Hartford line, the road becomes four lanes wide as it intersects with Route 218. The road runs for another in West Hartford as it continues southeast to end at an intersection with Route 189 near the University of Hartford. History In the 1920s, the Weatogue-Hartford route was a primary state highway known as Highway 115. It ran along modern Route 185 to Route 218 then used modern Rou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Connecticut Route 4
Route 4 is an east–west primary state highway connecting rural Litchfield County to the Greater Hartford area of the U.S. state of Connecticut. It runs from the town of Sharon to the town of West Hartford. Route description Route 4 begins at the junction of Route 41 and Route 343 in Sharon as a rural, minor arterial road. In Cornwall, it briefly overlaps with US 7 to cross the Housatonic River on the Cornwall Bridge. Farther east in Cornwall, it intersects with Routes 125, 43, and 128 before crossing into Goshen. In Goshen, it meets Route 63 at a roundabout in the center of town. After entering Torrington, the road becomes more of a principal arterial road upon meeting the southern end of Route 272. After skirting the northern edge of downtown, it meets the Route 8 freeway at exit 44 and briefly overlaps with US 202 just east of the interchange. The road turns southeast and returns to more of a rural character, meeting the south ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kettle Pond
A kettle (also known as a kettle lake, kettle hole, or pothole) is a depression/hole in an outwash plain formed by retreating glaciers or draining floodwaters. The kettles are formed as a result of blocks of dead ice left behind by retreating glaciers, which become surrounded by sediment deposited by meltwater streams as there is increased friction. The ice becomes buried in the sediment and when the ice melts, a depression is left called a kettle hole, creating a dimpled appearance on the outwash plain. Lakes often fill these kettles; these are called kettle hole lakes. Another source is the sudden drainage of an ice-dammed lake. When the block melts, the hole it leaves behind is a kettle. As the ice melts, ramparts can form around the edge of the kettle hole. The lakes that fill these holes are seldom more than deep and eventually fill with sediment. In acid conditions, a kettle bog may form but in alkaline conditions, it will be kettle peatland. Overview Kettles are fluviog ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Reservoir
A reservoir (; from French ''réservoir'' ) is an enlarged lake behind a dam. Such a dam may be either artificial, built to store fresh water or it may be a natural formation. Reservoirs can be created in a number of ways, including controlling a watercourse that drains an existing body of water, interrupting a watercourse to form an embayment within it, through excavation, or building any number of retaining walls or levees. In other contexts, "reservoirs" may refer to storage spaces for various fluids; they may hold liquids or gasses, including hydrocarbons. ''Tank reservoirs'' store these in ground-level, elevated, or buried tanks. Tank reservoirs for water are also called cisterns. Most underground reservoirs are used to store liquids, principally either water or petroleum. Types Dammed valleys Dammed reservoirs are artificial lakes created and controlled by a dam constructed across a valley, and rely on the natural topography to provide most of the basin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Penwood State Park
Penwood State Park is a public recreation area located on Talcott Mountain in the town of Bloomfield, Connecticut. The state park's are contiguous with the north end of Talcott Mountain State Park. Both parks are managed by the Connecticut Department of Energy and Environmental Protection. History Penwood State Park was donated to the state in 1944 by Curtis H. Veeder, an industrialist (founder of Gilbarco Veeder-Root Gilbarco Inc., doing business as Gilbarco Veeder-Root, is a supplier of fuel dispensers, point of sales systems, payment systems, forecourt merchandising and support services. The company operates as a subsidiary of Vontier and its headquarters ...), inventor, and outdoorsperson. Veeder wished the property to "be kept in a natural state so that those who love nature may enjoy this property as I have enjoyed it." He blazed many of the original trails in the park; Lake Louise, a scenic kettle bog atop the ridge, was named after his wife. Activities and amen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pinnacle Rock (Connecticut)
Pinnacle Rock, , is a traprock mountain peak located southwest of Hartford, Connecticut, in the towns of Farmington and Plainville. It is part of the narrow, linear Metacomet Ridge that extends from Long Island Sound near New Haven, Connecticut, north through the Connecticut River Valley of Massachusetts to the Vermont border. Pinnacle Rock, popular as an outdoor recreation destination in the metropolitan Hartford area, is known for its clifftop scenic vistas, unique microclimate ecosystems, rare plant communities, and as a seasonal raptor migration path. Pinnacle Rock is traversed by the Metacomet Trail. Pinnacle Rock should not be confused with ''The Pinnacle'', a name used for two other peaks also on the Metacomet Ridge in Connecticut (on Talcott Mountain and Higby Mountain). Geography Pinnacle Rock occupies the high point of a long mountain ridge which rises steeply above the upper Quinnipiac River valley to the southwest and the Farmington River valley to the nort ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Penwood State Park
Penwood State Park is a public recreation area located on Talcott Mountain in the town of Bloomfield, Connecticut. The state park's are contiguous with the north end of Talcott Mountain State Park. Both parks are managed by the Connecticut Department of Energy and Environmental Protection. History Penwood State Park was donated to the state in 1944 by Curtis H. Veeder, an industrialist (founder of Gilbarco Veeder-Root Gilbarco Inc., doing business as Gilbarco Veeder-Root, is a supplier of fuel dispensers, point of sales systems, payment systems, forecourt merchandising and support services. The company operates as a subsidiary of Vontier and its headquarters ...), inventor, and outdoorsperson. Veeder wished the property to "be kept in a natural state so that those who love nature may enjoy this property as I have enjoyed it." He blazed many of the original trails in the park; Lake Louise, a scenic kettle bog atop the ridge, was named after his wife. Activities and amen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
