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Trimountain
Trimountain or Tri-mountain, est. , is a traprock mountain located southeast of Meriden, 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. Trimountain is known for its scenic cliff faces, unique microclimate ecosystems, and rare plant communities. The mountain is traversed by the Mattabesett Trail. Geography Trimountain is located in Durham and Wallingford, Connecticut. It takes its name from its overall triangular shape, its three southern pinnacles, and the three notches between the pinnacles. A prominent landscape feature that rises above the surrounding valleys, Trimountain is roughly long by wide, although the steepness of the terrain makes the actual square mileage much larger. Although Trimountain has been subject to intensive quarrying, which has obliterated much of the northwestern face of the mountain, the Ma ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fowler Mountain
Fowler Mountain, est. , is a traprock mountain located southeast of the center of Meriden, 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. Fowler Mountain is known for its rugged topography, unique microclimate ecosystems, and rare plant communities. It rises steeply above the Ulbrich Reservoir and the Quinnipiac River valley to the west. The mountain is traversed by the Mattabesett Trail. Geography Located within the towns of Durham and Wallingford, Connecticut, Fowler Mountain is long by wide, although rugged topography makes the actual square mileage much larger. Fowler Mountain is an important aquifer; two reservoirs lie at the base of it: Ulbrich Reservoir to the west, in the town of Wallingford and Pistapaug Pond to the south, between Fowler Mountain and Pistapaug Mountain. The mountain is largely wooded with ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Besek Mountain
Besek Mountain (Alternate spelling: Bessic Mountain) also known as Black Mountain, est. , is a traprock mountain ridge located southeast of Meriden, 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. Besek Mountain is known for its long line of open cliffs, unique microclimate ecosystems, and rare plant communities. The mountain is traversed by the Mattabesett Trail, and is home to the Powder Ridge Ski Area.Farnsworth, Elizabeth J. (2004).Metacomet-Mattabesett Trail Natural Resource Assessment." United States National Park Service. Retrieved November 20, 2007''Connecticut Walk Book East: The Trail Guide to the Blue Blazed Hiking Trails of Eastern Connecticut'' (2005) 19th edition. Rockfall, Connecticut: Connecticut Forest and Park Association. Geography According to the Connecticut Forest and Park Association, the word ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mattabesett Trail
The Mattabesett Trail is a long, hook-shaped Blue-Blazed Trails, blue-blazed hiking trail in central Connecticut and a part of the New England National Scenic Trail. One half of the trail follows the high traprock ridges of the Metacomet Ridge, from Totoket Mountain in Guilford, Connecticut to Lamentation Mountain in Meriden, Connecticut from south to north. This ridge is known for its biodiversity, miles of scenic cliffs, and rugged hiking. The second half of the trail extends north from Guilford to Middletown, Connecticut and ends at the Connecticut River. Here, the trail follows an upland of metamorphic rock with occasional views and dense forests. Important features along the trail include Lamentation Mountain, Chauncey Peak, Higby Mountain, Besek Mountain, Fowler Mountain, Trimountain, Pistapaug Mountain, Totoket Mountain, the Broomstick Ledges, Seven Falls, and Coginchaug Cave. The Metacomet Trail continues north from Lamentation Mountain where the Mattabesett Trail leaves ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Durham, Connecticut
Durham is a New England town, town in Middlesex County, Connecticut, Middlesex County, Connecticut, United States. Durham is a former farming village on the Coginchaug River in central Connecticut. The population was 7,152 at the 2020 United States Census, 2020 census. Every autumn, the town hosts the Durham Fair, the largest volunteer fair, agricultural fair in New England. The Durham (CDP), Connecticut, Durham town center is listed by the U.S. Census Bureau as a census-designated place. The core of the town center has also been listed as a Main Street Historic District (Durham, Connecticut), historic district on the National Register of Historic Places. Geography According to the United States Census Bureau, the town has a total area of , of which, is land and 0.2 square miles (40 hectare, ha or 0.67%) is water. The town center CDP has a total area of . of it is land and 0.16% is water. The west side of Durham is flanked by the Metacomet Ridge, a mountainous ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Metacomet Ridge
The Metacomet Ridge, Metacomet Ridge Mountains, or Metacomet Range of southern New England is a narrow and steep fault-block mountain ridge known for its extensive cliff faces, scenic vistas, microclimate ecosystems, and rare or endangered plants. The ridge is an important recreation resource located within of more than 1.5 million people, offering four long-distance hiking trails and over a dozen parks and recreation areas, including several historic sites. It has been the focus of ongoing conservation efforts because of its natural, historic, and recreational value, involving municipal, state, and national agencies and nearly two dozen non-profit organizations.United States Census Bureau Data retrieved December 20, 2007. The Metacomet Ridge extends from |
Igneous
Igneous rock (derived from the Latin word ''ignis'' meaning fire), or magmatic rock, is one of the three main rock types, the others being sedimentary and metamorphic. Igneous rock is formed through the cooling and solidification of magma or lava. The magma can be derived from partial melts of existing rocks in either a planet's mantle or crust. Typically, the melting is caused by one or more of three processes: an increase in temperature, a decrease in pressure, or a change in composition. Solidification into rock occurs either below the surface as intrusive rocks or on the surface as extrusive rocks. Igneous rock may form with crystallization to form granular, crystalline rocks, or without crystallization to form natural glasses. Igneous rocks occur in a wide range of geological settings: shields, platforms, orogens, basins, large igneous provinces, extended crust and oceanic crust. Geological significance Igneous and metamorphic rocks make up 90–95% of the top ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quinnipiac River
The Quinnipiac River is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map, accessed April 1, 2011 long river in the New England region of the United States, located entirely in the state of Connecticut. The river rises in West Central Connecticut from Dead Wood Swamp near the city of New Britain. It flows roughly southward to Plainville, Southington, and Cheshire, west of the city of Meriden, through Wallingford and Yalesville, North Haven, and flows into New Haven Harbor, an inlet of Long Island Sound, east of downtown New Haven. History The name "Quinnipiac" comes from an Algonquian phrase meaning "long water land", and historically referred both to the river and the area around its mouth at Long Island Sound. Europeans found the river in 1614. By the early 18th century, early settlers called the Quinnipiac River the Dragon River after the seals, then referred to as “sea dragons,” that were once abundant there. Alt ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scree
Scree is a collection of broken rock fragments at the base of a cliff or other steep rocky mass that has accumulated through periodic rockfall. Landforms associated with these materials are often called talus deposits. Talus deposits typically have a concave upwards form, where the maximum inclination corresponds to the angle of repose of the mean debris particle size. The exact definition of scree in the primary literature is somewhat relaxed, and it often overlaps with both ''talus'' and ''colluvium''. The term ''scree'' comes from the Old Norse term for landslide, ''skriða'', while the term ''talus'' is a French word meaning a slope or embankment. In high-altitude arctic and subarctic regions, scree slopes and talus deposits are typically adjacent to hills and river valleys. These steep slopes usually originate from late-Pleistocene periglacial processes. Notable scree sites in Eastern North America include the Ice Caves at White Rocks National Recreation Area in southern Ve ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Earthquake
An earthquake (also known as a quake, tremor or temblor) is the shaking of the surface of the Earth resulting from a sudden release of energy in the Earth's lithosphere that creates seismic waves. Earthquakes can range in intensity, from those that are so weak that they cannot be felt, to those violent enough to propel objects and people into the air, damage critical infrastructure, and wreak destruction across entire cities. The seismic activity of an area is the frequency, type, and size of earthquakes experienced over a particular time period. The seismicity at a particular location in the Earth is the average rate of seismic energy release per unit volume. The word ''tremor'' is also used for Episodic tremor and slip, non-earthquake seismic rumbling. At the Earth's surface, earthquakes manifest themselves by shaking and displacing or disrupting the ground. When the epicenter of a large earthquake is located offshore, the seabed may be displaced sufficiently to cause ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fault (geology)
In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements. Large faults within Earth's crust result from the action of plate tectonic forces, with the largest forming the boundaries between the plates, such as the megathrust faults of subduction zones or transform faults. Energy release associated with rapid movement on active faults is the cause of most earthquakes. Faults may also displace slowly, by aseismic creep. A ''fault plane'' is the plane that represents the fracture surface of a fault. A ''fault trace'' or ''fault line'' is a place where the fault can be seen or mapped on the surface. A fault trace is also the line commonly plotted on geologic maps to represent a fault. A ''fault zone'' is a cluster of parallel faults. However, the term is also used for the zone of crushed rock along a single fault. Prolonged motion along closely spaced faults can blur the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lava
Lava is molten or partially molten rock (magma) that has been expelled from the interior of a terrestrial planet (such as Earth) or a moon onto its surface. Lava may be erupted at a volcano or through a fracture in the crust, on land or underwater, usually at temperatures from . The volcanic rock resulting from subsequent cooling is also often called ''lava''. A lava flow is an outpouring of lava during an effusive eruption. (An explosive eruption, by contrast, produces a mixture of volcanic ash and other fragments called tephra, not lava flows.) The viscosity of most lava is about that of ketchup, roughly 10,000 to 100,000 times that of water. Even so, lava can flow great distances before cooling causes it to solidify, because lava exposed to air quickly develops a solid crust that insulates the remaining liquid lava, helping to keep it hot and inviscid enough to continue flowing. The word ''lava'' comes from Italian and is probably derived from the Latin word ''labes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eurasia
Eurasia (, ) is the largest continental area on Earth, comprising all of Europe and Asia. Primarily in the Northern and Eastern Hemispheres, it spans from the British Isles and the Iberian Peninsula in the west to the Japanese archipelago and the Russian Far East to the east. The continental landmass is bordered by the Atlantic Ocean and Africa to the west, the Pacific Ocean to the east, the Arctic Ocean to the north, and by Africa, the Mediterranean Sea, and the Indian Ocean to the south. The division between Europe and Asia as two continents is a historical social construct, as many of their borders are over land; thus, in some parts of the world, Eurasia is recognized as the largest of the six, five, or four continents on Earth. In geology, Eurasia is often considered as a single rigid megablock. However, the rigidity of Eurasia is debated based on paleomagnetic data. Eurasia covers around , or around 36.2% of the Earth's total land area. It is also home to the largest ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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