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Robert Frost Trail
The Robert Frost Trail is a long footpath that passes through the eastern Connecticut River Valley of Massachusetts. The trail runs from the Connecticut River in South Hadley, Massachusetts to Ruggles Pond in Wendell State Forest, through both Hampshire and Franklin County and includes a number of scenic features such as the Holyoke Range, Mount Orient, Puffer's Pond, and Mount Toby.''A Guide to the Robert Frost Trail'' (2004). Amherst, Massachusetts: Amherst Conservation Department. The trail is named after the poet Robert Frost, who lived and taught in the area from 1916 to 1938. Trail description Although only 47 miles long, the Robert Frost Trail takes in a diverse patchwork of habitats, terrain, and scenery. The trail traverses trap rock Metacomet Ridge with its microclimate ecosystems; wetland habitat; ponds; farmland; deep ravines; wooded ledges; river banks; reservoirs; historic mill ponds; and dense forests. One segment of the trail follows a narrow greenway that succes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hampshire County, Massachusetts
Hampshire County is a historical and judicial county located in the U.S. state of Massachusetts. Following the dissolution of the county government in 1999, county affairs were managed by the Hampshire Council of Governments, which itself ceased operations in 2019, due to a "fundamentally flawed, unsustainable operational model". As of the 2020 census, the population was 162,308. Its most populous municipality is Amherst, its largest town in terms of landmass is Belchertown, and its traditional county seat is Northampton. The county is named after the county Hampshire, in England. Hampshire County is part of the Springfield, MA Metropolitan Statistical Area. Together with Hampden County, Hampshire County municipalities belong to the Pioneer Valley Planning Commission. History Hampshire County was constituted in 1662 from previously unorganized territory comprising the entire western part of Massachusetts Bay Colony. It included the original towns of Springfield, Northampto ... [...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] |
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 fluv ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacial
A glacial period (alternatively glacial or glaciation) is an interval of time (thousands of years) within an ice age that is marked by colder temperatures and glacier advances. Interglacials, on the other hand, are periods of warmer climate between glacial periods. The Last Glacial Period ended about 15,000 years ago. The Holocene is the current interglacial. A time with no glaciers on Earth is considered a greenhouse climate state. Quaternary Period Within the Quaternary, which started about 2.6 million years before present, there have been a number of glacials and interglacials. At least eight glacial cycles have occurred in the last 740,000 years alone. Penultimate Glacial Period The Penultimate Glacial Period (PGP) is the glacial period that occurred before the Last Glacial Period. It began about 194,000 years ago and ended 135,000 years ago, with the beginning of the Eemian interglacial. Last Glacial Period The last glacial period was the most recent glacial period ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Conglomerate (geology)
Conglomerate () is a clastic sedimentary rock that is composed of a substantial fraction of rounded to subangular gravel-size clasts. A conglomerate typically contains a matrix of finer-grained sediments, such as sand, silt, or clay, which fills the interstices between the clasts. The clasts and matrix are typically cemented by calcium carbonate, iron oxide, silica, or hardened clay. Conglomerates form by the consolidation and lithification of gravel. They can be found in sedimentary rock sequences of all ages but probably make up less than 1 percent by weight of all sedimentary rocks. In terms of origin and depositional mechanisms, they are closely related to sandstones and exhibit many of the same types of sedimentary structures, e.g., tabular and trough cross-bedding and graded bedding.Boggs, S. (2006) ''Principles of Sedimentology and Stratigraphy.'', 2nd ed. Prentice Hall, New York. 662 pp. Friedman, G.M. (2003) ''Classification of sediments and sedimentary rocks ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Leverett, Massachusetts
Leverett is a town in Franklin County, Massachusetts, United States. The population was 1,865 as of the 2020 census. It is part of the Springfield, Massachusetts Metropolitan Statistical Area. History The Town of Leverett is located on the traditional lands of the Pennacook and the Pocomtuc Nations. Leverett is one of the southernmost towns of Franklin County, located west of Shutesbury and Wendell, east of Sunderland, south of Montague, and north of Amherst. Leverett was originally part of Sunderland (named Swampfield at that time). The first non-indigenous settlement was established in 1750, and the settlers officially petitioned Sunderland to become their own town in 1774. The town was named for John Leverett, the twentieth Governor of the Massachusetts Bay Colony. In 1985, a Buddhist monastic order called Nipponzan Myohoji erected a large monument in Leverett. This structure, known as the New England Peace Pagoda, is considered the first of its kind in North Ameri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Amherst, Massachusetts
Amherst () is a town in Hampshire County, Massachusetts, United States, in the Connecticut River valley. As of the 2020 census, the population was 39,263, making it the highest populated municipality in Hampshire County (although the county seat is Northampton). The town is home to Amherst College, Hampshire College, and the University of Massachusetts Amherst, three of the Five Colleges. The name of the town is pronounced without the ''h'' ("AM-erst") by natives and long-time residents, giving rise to the local saying, "only the 'h' is silent", in reference both to the pronunciation and to the town's politically active populace. Amherst has three census-designated places: Amherst Center, North Amherst, and South Amherst. Amherst is part of the Springfield, Massachusetts Metropolitan Statistical Area. Lying north of the city of Springfield, Amherst is considered the northernmost town in the Hartford–Springfield Metropolitan Region, "The Knowledge Corridor". Amherst is also ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shays' Rebellion
Shays Rebellion was an armed uprising in Western Massachusetts and Worcester in response to a debt crisis among the citizenry and in opposition to the state government's increased efforts to collect taxes both on individuals and their trades. The fight took place mostly in and around Springfield during 1786 and 1787. American Revolutionary War veteran Daniel Shays led four thousand rebels (called Shaysites) in a protest against economic and civil rights injustices. In 1787, Shays' rebels marched on the federal Springfield Armory in an unsuccessful attempt to seize its weaponry and overthrow the government. The confederal government found itself unable to finance troops to put down the rebellion, and it was consequently put down by the Massachusetts State militia and a privately funded local militia. The widely held view was that the Articles of Confederation needed to be reformed as the country's governing document, and the events of the rebellion served as a catalyst for the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bivouac Shelter
A bivouac shelter is any of a variety of improvised camp site, or shelter that is usually of a temporary nature, used especially by soldiers, or people engaged in backpacking, bikepacking, scouting, or mountain climbing. It may often refer to sleeping in the open with a bivouac sack, but it may also refer to a shelter constructed of natural materials like a structure of branches to form a frame, which is then covered with leaves, ferns, and similar material for waterproofing and duff (leaf litter) for insulation. Modern bivouacs often involve the use of one- or two-man tents but may also be without tents or full cover. In modern mountaineering the nature of the bivouac shelter will depend on the level of preparedness, in particular whether existing camping and outdoor gear may be incorporated into the shelter. A bivouac shelter is colloquially known as a bivvy (also spelled ''bivy'' or ''bivvi'' or ''bivi''). Etymology The word ''bivouac'' is French and ultimately derives f ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sedimentary Rock
Sedimentary rocks are types of rock that are formed by the accumulation or deposition of mineral or organic particles at Earth's surface, followed by cementation. Sedimentation is the collective name for processes that cause these particles to settle in place. The particles that form a sedimentary rock are called sediment, and may be composed of geological detritus (minerals) or biological detritus (organic matter). The geological detritus originated from weathering and erosion of existing rocks, or from the solidification of molten lava blobs erupted by volcanoes. The geological detritus is transported to the place of deposition by water, wind, ice or mass movement, which are called agents of denudation. Biological detritus was formed by bodies and parts (mainly shells) of dead aquatic organisms, as well as their fecal mass, suspended in water and slowly piling up on the floor of water bodies ( marine snow). Sedimentation may also occur as dissolved minerals precipita ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Norwottuck
Mount Norwottuck or Mount Norwottock, above sea level, is the highest peak of the Holyoke Range of traprock mountains located in the Connecticut River Valley of Massachusetts and part of the greater Metacomet Ridge which stretches from Long Island Sound to nearly the Vermont border. The peak rises steeply from the valley below and offers sweeping views of the surrounding countryside. It is located within the towns of Amherst and Granby, Massachusetts. Description and history Mount Norwottuck received its name from Edward Hitchcock, a former professor of geology at Amherst College with a colorful history. Hitchcock coined the term "Scenographical Geology" in 1841 to describe the dramatic geologic landscape of the Holyoke Range. Originally called Hilliard Knob, Hitchcock applied the Native American name ''Norwottuck'' to the mountain. Norwottuck is the Indian name of the village of Hadley. Hitchcock is also famous for suggesting that local dinosaur tracks discovered in the Triassi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bare Mountain (Massachusetts)
:''Alternate spelling: should not be confused with Bear Mountain.'' Bare Mountain, above sea level, is a prominent peak of the Holyoke Range of traprock mountains located in the Connecticut River Valley of Massachusetts, and part of the greater Metacomet Ridge that stretches from Long Island Sound to nearly the Vermont border. The peak rises steeply from the river valley below; its bald summit offers sweeping views. Bare Mountain is located within the towns of Amherst and South Hadley, Massachusetts. Part of its northeastern flanks are in Hadley and part of its southern flanks are in Granby. It is traversed by the Metacomet-Monadnock Trail. Description and history A hiking destination popular among local college students, Bare Mountain offers a 270° vista over the surrounding valleys to the north and south, and a bird's eye view across Mount Norwottuck and the eastern peaks of the Holyoke Range. Also visible from the top are the Round Mountain quarry and the campuses of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
