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Berkshire Hills
The Berkshires () are a highland geologic region located in the western parts of Massachusetts and northwest Connecticut Connecticut () is the southernmost state in the New England region of the Northeastern United States. It is bordered by Rhode Island to the east, Massachusetts to the north, New York to the west, and Long Island Sound to the south. Its cap .... The term "Berkshires" is normally used by locals in reference to the portion of the Vermont-based Green Mountains that extend south into western Massachusetts; the portion extending further south into northwestern Connecticut is grouped with the Connecticut portion of the Taconic Mountains and referred to as either the Northwest Hills or Litchfield Hills. Also referred to as the Berkshire Highlands, Berkshire Hills, Berkshire Mountains, and Berkshire Plateau, the region enjoys a vibrant tourism industry based on music, arts, and recreation. Geologically, the mountains are a range of the Appalachian Mountains. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Metamorphic Rock
Metamorphic rocks arise from the transformation of existing rock to new types of rock in a process called metamorphism. The original rock ( protolith) is subjected to temperatures greater than and, often, elevated pressure of or more, causing profound physical or chemical changes. During this process, the rock remains mostly in the solid state, but gradually recrystallizes to a new texture or mineral composition. The protolith may be an igneous, sedimentary, or existing metamorphic rock. Metamorphic rocks make up a large part of the Earth's crust and form 12% of the Earth's land surface. They are classified by their protolith, their chemical and mineral makeup, and their texture. They may be formed simply by being deeply buried beneath the Earth's surface, where they are subject to high temperatures and the great pressure of the rock layers above. They can also form from tectonic processes such as continental collisions, which cause horizontal pressure, friction, and di ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Berkshire
Berkshire ( ; in the 17th century sometimes spelt phonetically as Barkeshire; abbreviated Berks.) is a historic county in South East England. One of the home counties, Berkshire was recognised by Queen Elizabeth II as the Royal County of Berkshire in 1957 because of the presence of Windsor Castle, and letters patent were issued in 1974. Berkshire is a county of historic origin, a ceremonial county and a non-metropolitan county without a county council. The county town is Reading. The River Thames formed the historic northern boundary, from Buscot in the west to Old Windsor in the east. The historic county, therefore, includes territory that is now administered by the Vale of White Horse and parts of South Oxfordshire in Oxfordshire, but excludes Caversham, Slough and five less populous settlements in the east of the Royal Borough of Windsor and Maidenhead. All the changes mentioned, apart from the change to Caversham, took place in 1974. The towns of Abingdon, D ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Deerfield River
Deerfield River is a river that runs for from southern Vermont through northwestern Massachusetts to the Connecticut River. The Deerfield River was historically influential in the settlement of western Franklin County, Massachusetts, and its namesake town. It is the Connecticut River's second-longest tributary in Massachusetts, shorter than Metropolitan Springfield's Westfield River. The river's confluence with the Connecticut is in Greenfield, Massachusetts, downstream of Turners Falls (). The Deerfield is one of the most heavily dammed rivers in the country with, on average, a dam almost every for its entire length. In Shelburne Falls, the glacial potholes and the Bridge of Flowers are popular tourist attractions around the river. Geography The great descent of the river of nearly 1,100 feet over 50 miles furnished water power at many places. Several streams nearly as large as the main river enter the Deerfield River from the north. Among its tributaries is the Green ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Monroe, Massachusetts
Monroe is a town in Franklin County, Massachusetts, United States. The population was 118 at the 2020 census. By area, population, and population density, it is the smallest town in the county; and is the second-smallest town by population in the Commonwealth, with only Gosnold having fewer residents. Monroe is part of the Springfield, Massachusetts Metropolitan Statistical Area. History Monroe was first settled in 1800 and was officially incorporated in 1822. The town was named for President James Monroe, who was in office at the time of incorporation. The town was mostly rural, with dairy farming taking up much of the town's economic activity. During the mid-19th century, the town did get some business from the building of the Hoosac Tunnel, just south of town in Florida. In 1885, however, a railroad line was built between neighboring Readsboro, Vermont, and Holyoke to haul wood pulp to a paper factory. This, in turn, enticed the Ramage family to establish the James Ramage P ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Crum Hill
Crum Hill, , located in northwest Massachusetts, United States, in the towns of Monroe and Florida, is the highest point in Franklin County. The mountain, part of the Hoosac Range (a west facing escarpment rising from the Hoosic River Valley directly east of North Adams, Massachusetts), is crossed by a trail system maintained by a local snowmobile club, the Florida Mountaineers. They maintain a trail map on their website. Although Crum Hill is the highest geologic point of the Berkshires, Mount Greylock, , part of the Taconic Mountains and unrelated to the Berkshires geology, is often misattributed with the high point.Raymo, Chet and Raymo, Maureen E. (1989). ''Written in Stone: A Geologic History of the Northeastern United States.'' Chester, Connecticut: Globe Pequot. The summit of Crum Hill is located in the town of Monroe, Franklin County; the west side of the mountain is located in the town of Florida, part of Berkshire County. The north and east sides of Crum Hill drain i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Globe Pequot
Globe Pequot is a book publisher and distributor of outdoor recreation and leisure titles that publishes 500 new titles. Globe Pequot was acquired by Morris Communications in 1997. Lyons Press was acquired in 2001. It was sold to Rowman & Littlefield Rowman & Littlefield Publishing Group is an independent publishing house founded in 1949. Under several imprints, the company offers scholarly books for the academic market, as well as trade books. The company also owns the book distributing compa ... in 2014. Imprints Globe Pequot publishes several imprints, including '' Prometheus Books'' ''Lyons Press'', ''FalconGuides'', ''Knack'', and ''Insiders' Guide''. References External links *{{Official website, http://globepequot.com Companies based in New Haven County, Connecticut Morris Communications Publishing companies of the United States ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Raymo, Chet
Chet Raymo (born September 17, 1936 in Chattanooga, Tennessee) is a noted writer, educator and naturalist. He is Professor Emeritus of Physics at Stonehill College, in Easton, Massachusetts. His weekly newspaper column ''Science Musings'' appeared in the Boston Globe for twenty years. This is now a daily blog by him. Raymo espouses his Religious Naturalism in ''When God is Gone Everything is Holy – The Making of a Religious Naturalist'' and frequently in his blog. As Raymo says – "I attend to this infinitely mysterious world with reverence, awe, thanksgiving, praise. All religious qualities." Raymo has been a contributor to ''The Notre Dame Magazine'' and ''Scientific American''. His most famous book is the novel entitled ''The Dork of Cork'', which was made into the feature-length film '' Frankie Starlight''. Raymo is also the author of ''Walking Zero'', a scientific and historical account of his wanderings along the Prime Meridian in Great Britain. Raymo was the recipie ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bedrock
In geology, bedrock is solid rock that lies under loose material ( regolith) within the crust of Earth or another terrestrial planet. Definition Bedrock is the solid rock that underlies looser surface material. An exposed portion of bedrock is often called an outcrop. The various kinds of broken and weathered rock material, such as soil and subsoil, that may overlie the bedrock are known as regolith. Engineering geology The surface of the bedrock beneath the soil cover (regolith) is also known as ''rockhead'' in engineering geology, and its identification by digging, drilling or geophysical methods is an important task in most civil engineering projects. Superficial deposits can be very thick, such that the bedrock lies hundreds of meters below the surface. Weathering of bedrock Exposed bedrock experiences weathering, which may be physical or chemical, and which alters the structure of the rock to leave it susceptible to erosion. Bedrock may also experience ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North America
North America is a continent in the Northern Hemisphere and almost entirely within the Western Hemisphere. It is bordered to the north by the Arctic Ocean, to the east by the Atlantic Ocean, to the southeast by South America and the Caribbean Sea, and to the west and south by the Pacific Ocean. Because it is on the North American Plate, North American Tectonic Plate, Greenland is included as a part of North America geographically. North America covers an area of about , about 16.5% of Earth's land area and about 4.8% of its total surface. North America is the third-largest continent by area, following Asia and Africa, and the list of continents and continental subregions by population, fourth by population after Asia, Africa, and Europe. In 2013, its population was estimated at nearly 579 million people in List of sovereign states and dependent territories in North America, 23 independent states, or about 7.5% of the world's population. In Americas (terminology)#Human ge ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Africa
Africa is the world's second-largest and second-most populous continent, after Asia in both cases. At about 30.3 million km2 (11.7 million square miles) including adjacent islands, it covers 6% of Earth's total surface area and 20% of its land area.Sayre, April Pulley (1999), ''Africa'', Twenty-First Century Books. . With billion people as of , it accounts for about of the world's human population. Africa's population is the youngest amongst all the continents; the median age in 2012 was 19.7, when the worldwide median age was 30.4. Despite a wide range of natural resources, Africa is the least wealthy continent per capita and second-least wealthy by total wealth, behind Oceania. Scholars have attributed this to different factors including geography, climate, tribalism, Scramble for Africa, colonialism, the Cold War, neocolonialism, lack of democracy, and corruption. Despite this low concentration of wealth, recent economic expansion and the large and young ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dissected Plateau
A dissected plateau is a plateau area that has been severely eroded such that the relief is sharp. Such an area may be referred to as mountainous, but dissected plateaus are distinguishable from orogenic mountain belts by the lack of folding, metamorphism, extensive faulting, or magmatic activity that accompanies orogeny. Formation A dissected plateau may also be formed, or created, usually on a comparatively small scale, by the levelling of terrain by planing and deposition beneath an ice sheet or perhaps, an ice cap. Subsequently, during the same or a later glacial, the margins of the glacial till plain are removed by glaciers, leaving the plateau into which erosion by water incises valleys. Such a plateau may be level or gently sloping but may be distinguished by the till caps on its hills. Glacial till is still widely known in Britain by the older name of boulder clay. Dissected volcanic plateaus include the Pajarito Plateau in New Mexico, on the skirt of the enormou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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