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Taconics
The Taconic Mountains or Taconic Range () are a range of the Appalachian Mountains, running along the eastern border of New York State and adjacent New England from northwest Connecticut to western Massachusetts, north to central western Vermont. A physiographic region of the larger New England province, the range includes notable summits, including its high point, Mount Equinox in Vermont, and Mount Greylock, the highest point in Massachusetts.''Day Hiker's Guide to Vermont'' 5th ed. (2006). Green Mountain Club: Waterbury Center, VermontRaymo, Chet and Raymo, Maureen E. (1989). ''Written in Stone: A Geologic History of the Northeastern United States.'' Chester, Connecticut: Globe Pequot.Doll, Charles G. Centennial Geologic Map of Vermont' (1961). United States Geological Survey: Washington The Taconics contain several hundred miles of trails, including sections of the Appalachian Trail, and over sixty designated areas of land protected by federal, state, county, and municipal ...
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Taconic Orogeny
The Taconic orogeny was a mountain building period that ended 440 million years ago and affected most of modern-day New England. A great mountain chain formed from eastern Canada down through what is now the Piedmont of the East coast of the United States. As the mountain chain eroded in the Silurian and Devonian periods, sediments from the mountain chain spread throughout the present-day Appalachians and midcontinental North America. New England and Canada Beginning in Cambrian time, about 550 million years ago, the Iapetus Ocean began to close. The weight of accumulating sediments, in addition to compressional forces in the crust, forced the eastern edge of the North American continent to fold gradually downward. In this manner, shallow-water carbonate deposition that had persisted on the continental shelf margin through Late Cambrian into Early Ordovician time, gave way to fine-grained clastic deposition and deeper water conditions during the Middle Ordovician. In this period ...
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Dutchess County, New York
Dutchess County is a county in the U.S. state of New York. As of the 2020 census, the population was 295,911. The county seat is the city of Poughkeepsie. The county was created in 1683, one of New York's first twelve counties, and later organized in 1713. It is located in the Mid-Hudson Region of the Hudson Valley, north of New York City. Dutchess County is part of the Poughkeepsie–Newburgh–Middletown Metropolitan Statistical Area, which belongs to the larger New York–Newark–Bridgeport, NY-NJ-CT-PA Combined Statistical Area. History Before Anglo-Dutch settlement, what is today Dutchess County was a leading center for the indigenous Wappinger peoples. They had their council-fire at what is now Fishkill Hook, and had settlements throughout the area. On November 1, 1683, the Province of New York established its first twelve counties, including Dutchess. Its boundaries at that time included the present Putnam County, and a small portion of the present Columbia Cou ...
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Mount Equinox
Equinox Mountain is a mountain in Bennington County, Vermont, United States, in the town of Manchester. The mountain is the highest peak of the Taconic Range, and the highest point of Bennington County. It is one of thirteen peaks in Vermont with a topographic prominence over , ranked third behind Mansfield and Killington. Equinox is the second highest peak in southern Vermont, after Stratton Mountain. Geology The Taconic Range ridgeline continues to the north from Equinox Mountain as Mother Myrick Mountain and south as Red Mountain; it is flanked to the west by Bennetts Ridge and Bear Mountain, also of the Taconic Range, and to the east by the western escarpment and plateau of the Green Mountains, across the Batten Kill valley. The southeast side of Equinox Mountain drains into the Batten Kill, thence into the Hudson River, and into New York Harbor. The northwest side of Equinox drains into the Green River, a tributary of the Batten Kill. Buildings and other developments R ...
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New England Province
The New England province is a physiographic province of the larger Appalachian division of eastern North America. The province consists of the Seaboard Lowland, New England Upland, White Mountain, Green Mountain, and Taconic sections. Geology Much of the New England province's bedrock aquifers are in consolidated rocks of sedimentary, igneous, and metamorphic origin. Some of these aquifers, mainly in the western portion of Vermont, consist of carbonate rocks (primarily limestone, dolomite, and marble). These consolidated rocks yield water primarily from bedding planes, fractures, joints, and faults, rather than from intergranular pores. Like the adjacent physiographic provinces, a large part of the New England province was peneplained during the Jurassic and Cretaceous The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it ...
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Hudson River Valley
The Hudson Valley (also known as the Hudson River Valley) comprises the valley of the Hudson River and its adjacent communities in the U.S. state of New York. The region stretches from the Capital District including Albany and Troy south to Yonkers in Westchester County, bordering New York City. History Pre-Columbian era The Hudson Valley was inhabited by indigenous peoples ages before Europeans arrived. The Lenape, Wappinger, and Mahican branches of the Algonquins lived along the river, mostly in peace with the other groups. The lower Hudson River was inhabited by the Lenape, The Lenape people waited for the explorer Giovanni da Verrazzano onshore, traded with Henry Hudson, and sold the island of Manhattan. Further north, the Wappingers lived from Manhattan Island up to Poughkeepsie. They lived a similar lifestyle to the Lenape, residing in various villages along the river. They traded with both the Lenape to the south and the Mahicans to the north. The Mahicans lived in the ...
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Hudson Highlands
The Hudson Highlands are mountains on both sides of the Hudson River in New York state lying primarily in Putnam County on its east bank and Orange County on its west. They continue somewhat to the south in Westchester County and Rockland County, respectively. 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, and from the north in the vicinity of Breakneck Ridge and Storm King Mountain near Cornwall, New York. These highlands have played a significant role in America's environmental, cultural, and military history. Geology The bedrock of the Highlands is part of the Reading Prong and more than a billion years old, formed during the Grenville Orogeny. It represents the very core of the Appalachian range, which has been formed by successive mountain-building events ( orogenies). The present mou ...
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Burlington, Vermont
Burlington is the most populous city in the U.S. state of Vermont and the seat of Chittenden County. It is located south of the Canada–United States border and south of Montreal. As of the 2020 U.S. census, the population was 44,743. It ranks as the least populous city in the United States to also be the most populous city in its state. A regional college town, Burlington is home to Champlain College and the University of Vermont (UVM). Vermont's largest hospital, the UVM Medical Center, is within the city limits. The City of Burlington owns Vermont's largest airport, the Burlington International Airport, located in neighboring South Burlington. In 2015, Burlington became the first city in the U.S. to run entirely on renewable energy. History Early history to early 20th century Two theories have been put forward regarding the origin of Burlington's name. The first is that it was named after Richard Boyle, 3rd Earl of Burlington, and the second is that the name ...
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Brandon, Vermont
Brandon is a town in Rutland County, Vermont, United States. As of the 2020 census, the population was 4,129. History On October 20, 1761, the town of Neshobe was chartered to Capt. Josiah Powers. In October 1784, the name of the town was changed to Brandon by an act of the legislature. Brandon is a study in early American architecture and Vermont history. When the first settlers came to the area in the mid-1770s, they established the village of Neshobe. The area was rich in natural resources with excellent farmland along the rivers and abundant supplies of timber and minerals. The town flourished during the 1800s with several industries relying on the key resources of waterpower, iron ore and marble. The coming of the railroad in 1849 enabled the manufacture and shipping of iron-based products such as the Howe scale, as well as Brandon paints, wood products and marble. During its century of rapid growth, Brandon Village evolved a unique village plan. The historic Crown Point ...
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Berkshire County, Massachusetts
Berkshire County (pronounced ) is a county on the western edge of the U.S. state of Massachusetts. As of the 2020 census, the population was 129,026. Its largest city and traditional county seat is Pittsfield. The county was founded in 1761. The Berkshire Hills are centered on Berkshire County. Residents are known as Berkshirites. It exists today only as a historical geographic region, and has no county government, with the exception of the retirement board for former county workers, and certain offices such as the sheriff and registry of deeds. Law and government Of the fourteen Massachusetts counties, Berkshire County is one of eight that exists today only as a historical geographic region; it has limited county government. Berkshire County government was abolished effective July 1, 2000. Most former county functions were assumed by state agencies, and there is no county council or commission.
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Taghkanic, New York
Taghkanic () is a town in Columbia County, New York, United States. The town is in the south-central part of the county. The population was 1,231, at the 2020 US census,US Census Bureau, 2020 Census Report, Taghkanic town, Columbia County, New York https://www.census.gov/search-results.html?searchType=web&cssp=SERP&q=Taghkanic%20town,%20Columbia%20County,%20New%20York Accessed December 26, 2022 down from 1,310 at the 2010 census. "Taghkanic" is an older spelling of " Taconic". History Settlement began before 1700, while the region was part of Livingston Manor. The town was formed from the town of Livingston in 1803 as the town of Granger. Geography According to the United States Census Bureau, the town has a total area of , of which is land and , or 0.41%, is water. The town shares its name with Taghkanic Creek, a tributary of Claverack Creek, which runs through the town in a U shape from the northeastern corner to the northwestern corner. The town also shares its name with ...
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Lenape
The Lenape (, , or Lenape , del, Lënapeyok) also called the Leni Lenape, Lenni Lenape and Delaware people, are an indigenous peoples of the Northeastern Woodlands, who live in the United States and Canada. Their historical territory included present-day northeastern Delaware, New Jersey and eastern Pennsylvania along the Delaware River watershed, New York City, western Long Island, and the lower Hudson Valley. Today, Lenape people belong to the Delaware Nation and Delaware Tribe of Indians in Oklahoma; the Stockbridge–Munsee Community in Wisconsin; and the Munsee-Delaware Nation, Moravian of the Thames First Nation, and Delaware of Six Nations in Ontario. The Lenape have a matrilineal clan system and historically were matrilocal. During the last decades of the 18th century, most Lenape were removed from their homeland by expanding European colonies. The divisions and troubles of the American Revolutionary War and United States' independence pushed them farther west. ...
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Indigenous Languages Of The Americas
Over a thousand indigenous languages are spoken by the Indigenous peoples of the Americas. These languages cannot all be demonstrated to be related to each other and are classified into a hundred or so language families (including a large number of language isolates), as well as a number of extinct languages that are unclassified because of a lack of data. Many proposals have been made to relate some or all of these languages to each other, with varying degrees of success. The most notorious is Joseph Greenberg's Amerind hypothesis, which however nearly all specialists reject because of severe methodological flaws; spurious data; and a failure to distinguish cognation, contact, and coincidence. Nonetheless, there are indications that some of the recognized families are related to each other, such as widespread similarities in pronouns (e.g., ''n''/''m'' is a common pattern for 'I'/'you' across western North America, and ''ch''/''k''/''t'' for 'I'/'you'/'we' is similarly found ...
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