Runaway Pond
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Runaway Pond
Runaway Pond is a marsh at the former site of Long Pond in Glover, Vermont. The name arose from an environmental disaster in 1810, when a manual attempt to divert some of the water of Long Pond broke the bank, causing the entire lake to suddenly empty out into the Barton River, uncontrolled. The site is located south of what is today the central village of Glover. Hydrology An engineer estimated that Long Pond must have contained of water. It was about long, wide, and averaged from deep and deep in the center. With a surface area of 480 acres, Long Pond exceeded the 100-acre guideline to be considered a lake by today's standards. History On June 6, 1810 it was a dry summer and the Barton River, which supplied the power for grist mills in Glover and northward, was running very low. At the request of Arron Willson, the local Glover gristmill owner, 60 men and boys attempted to create a new north outlet from Long Pond to the Barton River, but instead, they unintentionally ...
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Glover, Vermont
Glover is a town in Orleans County, Vermont, in the United States. As of the 2020 census, the town's population was 1,114. It contains two unincorporated villages, Glover and West Glover. The town is named for Brigadier General John Glover, who served in the American Revolutionary War. He was the prime proprietor of the town. Glover is home to three museums: the Bread & Puppet Museum, the Glover Historical Society museum, and The Museum of Everyday Life. Geography According to the United States Census Bureau, the town has a total area of 38.6 square miles (100.0 km2), of which 37.9 square miles (98.1 km2) is land and 0.7 square mile (1.9 km2) (1.92%) is water. The surface of the town is uneven, with hills and valleys. The highest elevation is Black Hills, at , in the south part of town. The town drains northward via the northern branches of the Barton River, and southward via branches of the Passumpsic, Lamoille, and Black Rivers, which have their sources he ...
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Barton (village), Vermont
Barton is a village located near the center of the town of Barton, in Orleans County, Vermont, United States. The population was 690 at the 2020 census. History In the 19th century, the village was the economic center of the county. Prior to incorporation, the village had been known as "Barton Mills." Tourists from Boston and New York arrived by train and could register in one of three major hotels. The village was incorporated on November 21, 1874. Fire permanently reshaped the village, starting with the 1883 destruction of the building on the site now occupied by the Pierce Building. The hotels were destroyed, mostly by fire, in 1967 and 1971. The Pierce Block was built in 1885 and is still being used for commercial purposes, one of the few business buildings to survive the multitude of fires that the village has experienced.''Discover the Barton Area''. Barton Area Chamber of Commerce,undated, referenced February 2007 In 1889, a waterworks was constructed using May Pond. Pre ...
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Floods In The United States
Lists of floods in the United States provide overviews of major floods in the United States. They are organized by time period: before 1901, from 1901 to 2000, and from 2001 to the present. Lists * Floods in the United States before 1901 Floods in the United States before 1900 is a list of flood events that were of significant impact to the country, before 1900. Floods are generally caused by excessive rainfall, excessive snowmelt, and dam failure. Prehistoric events Kankakee Tor ... * Floods in the United States: 1901–2000 * Floods in the United States: 2001–present {{DEFAULTSORT:Floods in the United States ...
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Lakes Of Orleans County, Vermont
A lake is an area filled with water, localized in a basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the ocean, although, like the much larger oceans, they do form part of the Earth's water cycle. Lakes are distinct from lagoons, which are generally coastal parts of the ocean. Lakes are typically larger and deeper than ponds, which also lie on land, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which usually flow in a channel on land. Most lakes are fed and drained by rivers and streams. Natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, where a river channel has widened into a basin. Some parts of the world have many lakes formed by the chaotic drainage patterns left over from the last ice ...
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Former Lakes Of The United States
A former is an object, such as a template, gauge or cutting die, which is used to form something such as a boat's hull. Typically, a former gives shape to a structure that may have complex curvature. A former may become an integral part of the finished structure, as in an aircraft fuselage, or it may be removable, being using in the construction process and then discarded or re-used. Aircraft formers Formers are used in the construction of aircraft fuselage, of which a typical fuselage has a series from the nose to the empennage, typically perpendicular to the longitudinal axis of the aircraft. The primary purpose of formers is to establish the shape of the fuselage and reduce the column length of stringers to prevent instability. Formers are typically attached to longerons, which support the skin of the aircraft. The "former-and-longeron" technique (also called stations and stringers) was adopted from boat construction, and was typical of light aircraft built until the ad ...
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Environmental Disasters
An environmental disaster or ecological disaster is defined as a catastrophic event regarding the natural environment that is due to human activity.Jared M. Diamond, '' Collapse: How Societies Choose to Fail or Succeed'', 2005 This point distinguishes environmental disasters from other disturbances such as natural disasters and intentional acts of war such as nuclear bombings. Environmental disasters show how the impact of humans' alteration of the land has led to widespread and/or long-lasting consequences. These disasters have included deaths of wildlife, humans and plants, or severe disruption of human life or health, possibly requiring migration. Environmental disasters Environmental disasters historically have affected agriculture, biodiversity including wildlife, the economy and human health. The most common causes include pollution that seeps into groundwater or a body of water, emissions into the atmosphere and depletion of natural resources, industrial activity or ...
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Lakes Of Vermont
A lake is an area filled with water, localized in a basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the ocean, although, like the much larger oceans, they do form part of the Earth's water cycle. Lakes are distinct from lagoons, which are generally coastal parts of the ocean. Lakes are typically larger and deeper than ponds, which also lie on land, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which usually flow in a channel on land. Most lakes are fed and drained by rivers and streams. Natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, where a river channel has widened into a basin. Some parts of the world have many lakes formed by the chaotic drainage patterns left over from the last ice ...
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History Of Vermont
The geologic history of Vermont begins more than 450 million years ago during the Cambrian and Devonian periods. Human history of Native American settlement can be divided into the hunter-gatherer Archaic Period, from c. 7000–1000 BC, and the sedentary Woodland Period, from c. 1000 BC to AD 1600. Vermont was admitted to the United States as the fourteenth state in 1791 after a brief period of sovereignty following the American Revolutionary War. Vermont experienced rising abolitionist sentiment and subsequently fought on the Union side of the American Civil War. Geological and marine history Vermont was covered with shallow seas periodically from the Cambrian to Devonian periods. Most of the sedimentary rocks laid down in these seas were deformed by mountain-building. Fossils, however, are common in the Lake Champlain region. Lower areas of western Vermont have flooded again, as part of the St. Lawrence Valley and Champlain Valley by Lake Vermont whose northern boundary f ...
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Lake Memphremagog
Lake Memphremagog (; french: Lac Memphrémagog) is a fresh water glacial lake located between Newport, Vermont, United States and Magog, Quebec, Canada. The lake spans both Quebec and Vermont, but is mostly in Quebec. Most of the watershed that feeds the lake is located in Vermont, and is a source for accumulated phosphorus, sediments and other pollutants. Cleanup efforts since the late 1980s have improved the water quality. The lake furnishes potable water for 200,000 people. Physical characteristics The lake is long with 73 percent of the lake's surface area in Quebec, where it drains into the Magog River. However, three-quarters of its watershed, , is in Vermont. The total is , with located in Quebec. In Vermont, the lake lies in parts of the towns of Derby and Newport, in addition to the City of Newport (city), Vermont, Newport, all in Orleans County, Vermont, Orleans County. In Quebec, the lake lies in parts of Austin, Quebec, Austin, Magog, Quebec, Magog, Ogden, Quebec ...
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Orleans County, Vermont
Orleans County is a county located in the northeastern part of the U.S. state of Vermont. As of the 2020 census, the population was 27,393. Its county seat is the city of Newport. The county was created in 1792 and organized in 1799. As in the rest of New England, few governmental powers have been granted to the county. The county is an expedient way of grouping and distributing state-controlled governmental services. History The county shares the same pre-Columbian history with the Northeast Kingdom. In 1753, the Abenakis brought the ransomed John Stark down Lake Memphremagog and came ashore where Newport is now. They then traveled southeast to his home in New Hampshire. Rogers' Rangers were forced to retreat through the county following their attack on Saint-Francis, Quebec in 1759. To confound their avenging pursuers, they split up on the east shore of Lake Memphremagog. One group followed the Clyde River. Another followed the Barton River south to the falls at the outl ...
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Barton, Vermont
Barton is a town in Orleans County, Vermont, United States. The population was 2,872 at the 2020 census. The town includes two incorporated villages, Barton and Orleans. Approximately a quarter of the town's population lives in each of the villages, and approximately half lives outside the villages. Only four other towns in the state contain two incorporated villages. The Nulhegan Abenaki Tribe, a state-recognized tribe, is headquartered here. History The Abenaki and their ancestors had been in this area for 12,000 years. They were part of the large Wabanaki confederacy of related Algonguian-speaking peoples that extended into what is now Canada. In 2011 and 2012 the state of Vermont officially recognized four Abenaki tribes. The Nulhegan Abenaki Tribe has its headquarters in Barton. Early European traders and colonists were French. Anglo-Americans began to enter the area later in the 18th century. Both groups pushed the Abenaki aside when they wanted the land, and th ...
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Orleans, Vermont
Orleans is a village in the northwestern corner of Barton, Orleans County, Vermont, United States. With a population of 788 at the 2020 census, it is the largest village in the county. History Roger Enos purchased land in 1820 in the area from Ira Allen. He had been given a land grant as a veteran in lieu of pay after the Revolutionary War; he may also have purchased this parcel from Herman Allen. It was named "Barton Landing"; this was the first place where craft could be safely loaded for transportation down the Barton River to Lake Memphremagog. It was at the confluence of the Willoughby and Barton rivers, providing sufficient water for flotation. Native Americans had used this landing for years before the pioneers. Enos built the first building, a sawmill, at the confluence. Jesse Cook bought this building in 1830 to convert to a textile mill for weaving cloth, part of the northern economy using cotton from the South. In 1839 John Little converted it into a grain mill. Lo ...
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