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Sutton, Vermont
Sutton is a town in Caledonia County, Vermont, United States. The population was 913 at the 2020 census. History Sutton was chartered on February 26, 1782, by the Vermont Legislature. Chartered as Billymead to Dr. Jonathan Arnold of Rhode Island and associates, and named for Arnold's younger son, William. By 1810, townsfolk had had enough of Billy and his name due to his bullying and drunken behavior, and at a town meeting they voted overwhelmingly to change the name to Sutton. Villages and hamlets in Sutton include Sutton, Sutton Depot, and Summit Siding. The population at the 2010 US Census was 1,029. Geography Sutton is located in northern Caledonia County. It is bordered by the town of Lyndon to the south, Wheelock to the southwest, Sheffield to the west, Barton to the northwest, Westmore to the north, Newark to the northeast, and Burke to the east. According to the United States Census Bureau, the town has a total area of , of which is land and , or 0.51%, is water. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
New England Town
The town is the basic unit of Local government in the United States, local government and local division of state authority in the six New England states. Most other U.S. states lack a direct counterpart to the New England town. New England towns overlie the entire area of a state, similar to civil townships in other states where they exist, but they are fully functioning Incorporation (municipal government), municipal corporations, possessing powers similar to city, cities and county, counties in other states. Local government in New Jersey, New Jersey's system of equally powerful townships, boroughs, towns, and cities is the system which is most similar to that of New England. New England towns are often governed by a town meeting, an assembly of eligible town residents. The great majority of municipal corporations in New England are based on the town model; there, statutory forms based on the concept of a Place (United States Census Bureau), compact populated place are uncommon ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wheelock, Vermont
Wheelock is a town in Caledonia County, Vermont, United States. The population was 759 at the 2020 census. History The town was named after Eleazar Wheelock, the founder of Dartmouth College. Through a provision of the college dating to , any full-time resident of Wheelock who is accepted as an undergraduate at Dartmouth College may attend the school entirely free of tuition. Between the 1890s and 2025, ten Wheelock Scholars attended Dartmouth College. Standing in the center of the village for many years was the old brick hotel, known as the Caledonia Spring House. In 1893, Myron D. Park, who served four years as a Wheelock selectman, sold the Caledonia Spring House to Marshall Way. The hotel was the site of a notorious murder on May 20, 1896, when owner Marshall Way killed his 44-year-old wife, Ellen Sheldon Way, in the dooryard. According to the St. Johnsbury ''Caledonian'' of May 22, 1896, "The little town of Wheelock was thrown into a state of wild excitement last Wednesday ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Population Density
Population density (in agriculture: Standing stock (other), standing stock or plant density) is a measurement of population per unit land area. It is mostly applied to humans, but sometimes to other living organisms too. It is a key geographical term.Matt RosenberPopulation Density Geography.about.com. March 2, 2011. Retrieved on December 10, 2011. Biological population densities Population density is population divided by total land area, sometimes including seas and oceans, as appropriate. Low densities may cause an extinction vortex and further reduce fertility. This is called the Allee effect after the scientist who identified it. Examples of the causes of reduced fertility in low population densities are: * Increased problems with locating sexual mates * Increased inbreeding Human densities Population density is the number of people per unit of area, usually transcribed as "per square kilometre" or square mile, and which may include or exclude, for example, ar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Census
A census (from Latin ''censere'', 'to assess') is the procedure of systematically acquiring, recording, and calculating population information about the members of a given Statistical population, population, usually displayed in the form of statistics. This term is used mostly in connection with Population and housing censuses by country, national population and housing censuses; other common censuses include Census of agriculture, censuses of agriculture, traditional culture, business, supplies, and traffic censuses. The United Nations (UN) defines the essential features of population and housing censuses as "individual enumeration, universality within a defined territory, simultaneity and defined periodicity", and recommends that population censuses be taken at least every ten years. UN recommendations also cover census topics to be collected, official definitions, classifications, and other useful information to coordinate international practices. The United Nations, UN's Food ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Microclimate
A microclimate (or micro-climate) is a local set of atmosphere of Earth, atmospheric conditions that differ from those in the surrounding areas, often slightly but sometimes substantially. The term may refer to areas as small as a few square meters or smaller (for example a raised-bed gardening, garden bed, underneath a rock, or a cave) or as large as many square kilometers. Because climate is statistics, statistical, which implies Spatial analysis, spatial and temporal variation of the mean values of the describing parameters, microclimates are identified as statistically distinct conditions which occur and/or persist within a region. Microclimates can be found in most places but are most pronounced in topographically dynamic zones such as mountainous areas, islands, and coastal areas. Microclimates exist, for example, near bodies of water which may cool the local atmosphere, or in heavy urban areas where brick, concrete, and Asphalt concrete, asphalt absorb the sun's energy, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Frost Hollow
In meteorology, an inversion (or temperature inversion) is a phenomenon in which a layer of warmer air overlies cooler air. Normally, air temperature gradually decreases as altitude increases, but this relationship is reversed in an inversion. An inversion traps air pollution, such as smog, near the ground. An inversion can also suppress convection by acting as a "cap". If this cap is broken for any of several reasons, convection of any humidity can then erupt into violent thunderstorms. Temperature inversion can cause freezing rain in cold climates. Normal atmospheric conditions Usually, within the lower atmosphere (the troposphere) the air near the surface of the Earth is warmer than the air above it, largely because the atmosphere is heated from below as solar radiation warms the Earth's surface, which in turn then warms the layer of the atmosphere directly above it, e.g., by thermals (convective heat transfer). Air temperature also decreases with an increase in altitu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
National Weather Service
The National Weather Service (NWS) is an Government agency, agency of the Federal government of the United States, United States federal government that is tasked with providing weather forecasts, warnings of hazardous weather, and other weather-related products to organizations and the public for the purposes of protection, safety, and general information. It is a part of the National Oceanic and Atmospheric Administration (NOAA) branch of the United States Department of Commerce, Department of Commerce, and is headquartered in Silver Spring, Maryland, within the Washington metropolitan area. The agency was known as the United States Weather Bureau from 1891 until it adopted its current name in 1970. The NWS performs its primary task through a collection of national and regional centers, and 122 local List of National Weather Service Weather Forecast Offices, Weather Forecast Offices (WFOs). As the NWS is an agency of the U.S. federal government, most of its products are in the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Köppen Climate Classification
The Köppen climate classification divides Earth climates into five main climate groups, with each group being divided based on patterns of seasonal precipitation and temperature. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' indicates a tropical rainforest climate. The system assigns a temperature subgroup for all groups other than those in the ''A'' group, indicated by the third letter for climates in ''B'', ''C'', ''D'', and the second letter for climates in ''E''. Other examples include: ''Cfb'' indicating an oceanic climate with warm summers as indicated by the ending ''b.'', while ''Dwb'' indicates a semi-Monsoon continental climate, monsoonal continental climate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Humid Continental Climate
A humid continental climate is a climatic region defined by Russo-German climatologist Wladimir Köppen in 1900, typified by four distinct seasons and large seasonal temperature differences, with warm to hot (and often humid) summers, and cold (sometimes severely cold in the northern areas) and snowy winters. Precipitation is usually distributed throughout the year, but often these regions do have dry seasons. The definition of this climate in terms of temperature is as follows: the mean temperature of the coldest month must be below or depending on the isotherm, and there must be at least four months whose mean temperatures are at or above . In addition, the location in question must not be semi-arid or arid. The cooler ''Dfb'', ''Dwb'', and ''Dsb'' subtypes are also known as hemiboreal climates. Although amount of snowfall is not a factor used in defining the humid continental climate, snow during the winter in this type of climate is almost a guarantee, either intermitte ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Hor (Vermont)
Mount Hor is a mountain in Sutton, Vermont, Sutton, Vermont. It is part of the Northeastern Highlands of Vermont. It is located on the west side of Lake Willoughby and constitutes the west side of "Willoughby Notch" ("Willoughby Gap"). There are hiking trails in Willoughby State Forest. Mount Hor is the subject of a poem by Robert Frost. "The Mountain" appears in Frost's second book of poetry, ''North of Boston'' (1914). See also *Mount Pisgah (Vermont) References Mountains of Vermont, Hor Sutton, Vermont Landforms of Caledonia County, Vermont {{Vermont-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Burke, Vermont
Burke is a New England town, town in Caledonia County, Vermont, Caledonia County, Vermont, United States. The population was 1,651 at the 2020 United States Census, 2020 census. The town contains the villages of East Burke, Vermont, East Burke, West Burke, Vermont, West Burke and Burke Hollow. The town is home to Burke Mountain (Vermont), Burke Mountain and Burke Mountain Academy. Etymology The town was named for Sir Edmund Burke, a member of the English Parliament. Geography According to the United States Census Bureau, the town has a total area of , of which is land and , or 0.40%, is water. Burke is bordered by the towns of Lyndon, Vermont, Lyndon and Kirby, Vermont, Kirby to the south, Victory, Vermont, Victory to the southeast, East Haven, Vermont, East Haven to the northeast, Newark, Vermont, Newark to the north, and Sutton, Vermont, Sutton to the west. U.S. Route 5 runs through the western part of the town, connecting Lyndonville, Vermont, Lyndonville to the south with B ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Newark, Vermont
Newark is a town in Caledonia County, Vermont, United States. The population was 584 at the 2020 census. Geography Newark is located at the northern tip of Caledonia County, Vermont. It is bordered by the town of Burke to the south, Sutton to the west, Westmore to the northwest, Brighton to the north, Ferdinand to the northeast, and East Haven to the southeast. According to the United States Census Bureau, the town has a total area of , of which is land and , or 1.25%, is water. Vermont Route 114 passes through the town, leading north to Island Pond in the town of Brighton and south to Lyndonville. Vermont Route 5A crosses the western corner of Newark, leading north past Lake Willoughby to Derby and south to U.S. Route 5 in West Burke. The highest point in Newark is an unnamed summit near the northwest border with Westmore, west of Abbott Hill Road. Demographics As of the census of 2000, there were 470 people, 19 households, and 12 families residing in the town. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
