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The Berkshires
The Berkshires () are highlands located in western Massachusetts and northwestern Connecticut in the United States. Generally, "Berkshires" may refer to the range of hills in Massachusetts that lie between the Housatonic and Connecticut Rivers. Highlands of northwest Connecticut may be seen as part of the Berkshires and sometimes called the Northwest Hills or Litchfield Hills. The segment of the Taconic Mountains in Massachusetts is often considered a part of the Berkshires, although they are geologically separate and are a comparatively narrow range along New York's eastern border. 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 subrange of the Appalachian Mountains. The Berkshires were named among the 12 Last Great Places by The Nature Conservancy. Definition The term "The Berkshires" has overlappi ... [...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 dist ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Colonial Governors Of Massachusetts
The territory of the Massachusetts, Commonwealth of Massachusetts, one of the fifty United States, was settled in the 17th century by several different English colonies. The territories claimed or administered by these colonies encompassed a much larger area than that of the modern state, and at times included areas that are now within the jurisdiction of other New England states or of the Canadian provinces of New Brunswick and Nova Scotia. Some colonial land claims extended all the way to the Pacific Ocean. The first permanent settlement was the Plymouth Colony (1620), and the second major settlement was the Massachusetts Bay Colony at Salem, Massachusetts, Salem in 1629. Settlements that failed or were merged into other colonies included the failed Popham Colony (1607) on the coast of Maine, and the Wessagusset Colony (1622–23) in Weymouth, Massachusetts, whose remnants were folded into the Plymouth Colony. The Plymouth and Massachusetts Bay colonies coexisted until 1686, ea ... [...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 from 1983 to 2003, now collected and extended with his further writings on his personal website. 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 alon ... [...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 subsur ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North America
North America is a continent in the Northern Hemisphere, Northern and Western Hemisphere, Western hemispheres. North America 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 south and west by the Pacific Ocean. The region includes Middle America (Americas), Middle America (comprising the Caribbean, Central America, and Mexico) and Northern America. North America covers an area of about , representing approximately 16.5% of Earth's land area and 4.8% of its total surface area. It is the third-largest continent by size after Asia and Africa, and the list of continents and continental subregions by population, fourth-largest continent by population after Asia, Africa, and Europe. , North America's population was estimated as over 592 million people in list of sovereign states and dependent territories in North America, 23 independent states, or about 7.5% of the world's popula ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Africa
Africa is the world's second-largest and second-most populous continent after Asia. At about 30.3 million km2 (11.7 million square miles) including adjacent islands, it covers 20% of Earth's land area and 6% of its total surface area.Sayre, April Pulley (1999), ''Africa'', Twenty-First Century Books. . With nearly billion people as of , it accounts for about of the world's human population. Demographics of Africa, Africa's population is the youngest among all the continents; the median age in 2012 was 19.7, when the worldwide median age was 30.4. Based on 2024 projections, Africa's population will exceed 3.8 billion people by 2100. Africa is the least wealthy inhabited continent per capita and second-least wealthy by total wealth, ahead of Oceania. Scholars have attributed this to different factors including Geography of Africa, geography, Climate of Africa, climate, corruption, Scramble for Africa, colonialism, the Cold War, and neocolonialism. Despite this lo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dissected Plateau
A dissected plateau is a plateau area that has been severely eroded, and 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 fold (geology), folding, Metamorphic rock, metamorphism, extensive Geological fault, faulting, or magmatic activity accompanying orogeny. Formation A dissected plateau may also be formed, 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 Glaciation, glacial period, the margins of the Till, 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 United Kingdom, Britain by the older name of boulder clay. Dissected volcanic plateaus includ ... [...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 |
Hudson Highlands
The Hudson Highlands are mountains on both sides of the Hudson River in New York (state), New York state lying primarily in Putnam County, New York, Putnam County on its east bank and Orange County, New York, Orange County on its west. They continue somewhat to the south in Westchester County, New York, Westchester County and Rockland County, New York, Rockland County, respectively. The highlands are a List of subranges of the Appalachian Mountains, subrange of the Appalachian Mountains. North to south they fall between Newburgh Bay and Haverstraw Bay, the latter forming the northern region of the New York - New Jersey Highlands. The Hudson River enters this region in the south at Dunderberg Mountain near Stony Point, New York, Stony Point, and from the north in the vicinity of Breakneck Ridge and Storm King Mountain (New York), Storm King Mountain near Cornwall, New York. These highlands have played a significant role in America's environmental, cultural, and military history. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vermont
Vermont () is a U.S. state, state in the New England region of the Northeastern United States. It borders Massachusetts to the south, New Hampshire to the east, New York (state), New York to the west, and the Provinces and territories of Canada, Canadian province of Quebec to the north. According to the most recent U.S. Census estimates, the state has an estimated population of 648,493, making it the List of U.S. states and territories by population, second-least populated of all U.S. states. It is the nation's List of U.S. states and territories by area, sixth smallest state in area. The state's capital of Montpelier, Vermont, Montpelier is the least populous List of capitals in the United States, U.S. state capital. No other U.S. state has a List of largest cities of U.S. states and territories by population, most populous city with fewer residents than Burlington, Vermont, Burlington. Native Americans in the United States, Native Americans have inhabited the area for abou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Green Mountains
The Green Mountains are a mountain range in the U.S. state of Vermont and are a subrange of the Appalachian Mountains. The range runs primarily south to north and extends approximately from the border with Massachusetts to the border with Quebec, Canada. The part of the same range that is in Massachusetts and Connecticut is known as The Berkshires or the Berkshire Hills (with the Connecticut portion, mostly in Litchfield County, locally called the Northwest Hills or Litchfield Hills) and the Quebec portion is called the Sutton Mountains, or ' in French. All mountains in Vermont are often referred to as the "Green Mountains". However, other ranges within Vermont, including the Taconic Mountains in southwestern Vermont and the Northeastern Highlands, are not geologically part of the Green Mountains. Peaks The best-known mountains—for reasons such as high elevation, ease of public access by road or trail (especially the Long Trail and Appalachian Trail), or with ski re ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
