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Ford, Wisconsin
Ford is a town in Taylor County, Wisconsin, Taylor County, Wisconsin, United States. The population was 276 at the 2000 census. The unincorporated community of Polley is located in the town. Geography According to the United States Census Bureau, the town has a total area of 35.1 square miles (90.8 km2), of which, 32.8 square miles (84.8 km2) of it is land and 2.3 square miles (6.0 km2) of it (6.59%) is water. Chequamegon Waters, also known as Miller Dam, is a man-made lake that covers the northeast corner of Ford. Most of Ford's soil is silt loam with a heavy subsoil. The southeast corner of the town lies in the hilly terminal moraine that runs from Westboro, Wisconsin, Westboro through Perkinstown, Wisconsin, Perkinstown and Lublin, Wisconsin, Lublin - dumped by the Wisconsin glaciation, last glacier. The rest of Ford is the flatter till plain left by the same glacier. The Yellow River (Chippewa River), Yellow River and Hay Creek have cut channels ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Town
A town is a type of a human settlement, generally larger than a village but smaller than a city. The criteria for distinguishing a town vary globally, often depending on factors such as population size, economic character, administrative status, or historical significance. In some regions, towns are formally defined by legal charters or government designations, while in others, the term is used informally. Towns typically feature centralized services, infrastructure, and governance, such as municipal authorities, and serve as hubs for commerce, education, and cultural activities within their regions. The concept of a town varies culturally and legally. For example, in the United Kingdom, a town may historically derive its status from a market town designation or City status in the United Kingdom, royal charter, while in the United States, the term is often loosely applied to incorporated municipality, municipalities. In some countries, such as Australia and Canada, distinction ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Westboro, Wisconsin
Westboro is a town in Taylor County, Wisconsin, United States. The population was 660 at the 2000 census. The census-designated place of Westboro is located in the town. The unincorporated community of Queenstown is also located in the town. Geography Westboro is the largest town in Taylor County. Instead of the typical six miles by six, it is six by twenty miles. According to the United States Census Bureau, the town has a total area of 125.4 square miles (324.9 km2), of which, 124.1 square miles (321.4 km2) is land and 1.3 square miles (3.5 km2) (1.07%) is water. Westboro contains three of Taylor County's twelve Wisconsin State Natural Areas: Kidrick Swamp SNA, Silver Creek & Mondeaux River SNA, and part of Mondeaux Hardwoods SNA. History In 1847, surveyors working for the U.S. government walked the six mile squares that would become the town of Westboro. They marked off the outlines of those squares on foot using compass and chain. A crew ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gunter's Chain
Gunter's chain (also known as Gunter's measurement) is a distance-measuring device used for surveying. It was designed and introduced in 1620 by English clergyman and mathematician Edmund Gunter (1581–1626). It enabled plots of land to be accurately surveyed and plotted, for legal and commercial purposes. Gunter developed an actual measuring chain of 100 links. These, the chain and the link, became statutory measures in England and subsequently the British Empire. Description The chain is divided into 100 links, usually marked off into groups of 10 by brass rings or tags which simplify intermediate measurement. Each link is thus long. A quarter chain, or 25 links, measures and thus measures a rod (or pole). Ten chains measure a furlong and 80 chains measure a statute mile. Gunter's chain reconciled two seemingly incompatible systems: the traditional English land measurements, based on the number four, and decimals based on the number 10. Since an acre measured 10 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Survey Township
A survey township, sometimes called a Congressional township or just township, as used by the United States Public Land Survey System and by Canada's Dominion Land Survey is a nominally-square area of land that is nominally six survey miles (about 9.66 km) on a side. Each 36-square-mile (about 93.2 km2) township is divided into 36 section (land), sections of one square mile (640 acres, roughly 2.6 km2) each. The sections can be further subdivided for sale. The townships are referenced by a numbering system that locates the township in relation to a principal meridian (north-south) and a Baseline (surveying), base line (east-west). For example, Township 2 North, Range 4 East is the 4th township east of the principal meridian and the 2nd township north of the base line. History in the US Township (exterior) lines were originally surveyed and platted by the United States General Land Office using contracted private survey crews. Later survey crews subdivided the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Section (United States Land Surveying)
In U.S. land surveying under the Public Land Survey System (PLSS), a section is an area nominally , containing , with 36 sections making up one survey township on a rectangular grid. The legal description of a tract of land under the PLSS includes the name of the U.S. state, state, name of the County (United States), county, township number, range number, section number, and portion of a section. Sections are customarily Surveying, surveyed into smaller squares by repeated halving and quartering. A quarter section is and a "quarter-quarter section" is . In 1832 the smallest area of land that could be acquired was reduced to the quarter-quarter section, and this size parcel became entrenched in American mythology. After the American Civil War, Civil War, freedman, freedmen (freed slaves) were reckoned to be self-sufficient with "40 acres and a mule," though they never received it. In the 20th century real estate developers preferred working with parcels. The phrases "front 40" ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Surveying
Surveying or land surveying is the technique, profession, art, and science of determining the land, terrestrial Plane (mathematics), two-dimensional or Three-dimensional space#In Euclidean geometry, three-dimensional positions of Point (geometry), points and the Euclidean distance, distances and angles between them. These points are usually on the surface of the Earth, and they are often used to establish maps and boundaries for ownership, locations, such as the designated positions of structural components for construction or the surface location of subsurface features, or other purposes required by government or civil law, such as property sales. A professional in land surveying is called a land surveyor. Surveyors work with elements of geodesy, geometry, trigonometry, regression analysis, physics, engineering, metrology, programming languages, and the law. They use equipment, such as total stations, robotic total stations, theodolites, Satellite navigation, GNSS receivers, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a Clastic rock#Sedimentary clastic rocks, clastic sedimentary rock composed mainly of grain size, sand-sized (0.0625 to 2 mm) silicate mineral, silicate grains, Cementation (geology), cemented together by another mineral. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar, because they are the most resistant minerals to the weathering processes at the Earth's surface. Like uncemented sand, sandstone may be imparted any color by impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Because sandstone beds can form highly visible cliffs and other topography, topographic features, certain colors of sandstone have become strongly identified with certain regions, such as the red rock deserts of Arches National Park and other areas of the Southwestern United States, American Southwest. Rock formations composed of sandstone usually allow the p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Amphibolite
Amphibolite () is a metamorphic rock that contains amphibole, especially hornblende and actinolite, as well as plagioclase feldspar, but with little or no quartz. It is typically dark-colored and dense, with a weakly foliated or schistose (flaky) structure. The small flakes of black and white in the rock often give it a salt-and-pepper appearance. Amphibolite frequently forms by metamorphism of mafic igneous rocks, such as basalt. However, because metamorphism creates minerals entirely based upon the chemistry of the protolith, certain 'dirty marls' and volcanic sediments may also metamorphose to an amphibolite assemblage. Deposits containing dolomite and siderite also readily yield amphibolite ( tremolite-schist, grunerite-schist, and others) especially where there has been a certain amount of contact metamorphism by adjacent granitic masses. Metamorphosed basalt (metabasalt) creates ''ortho-amphibolite'' and other chemically appropriate lithologies create ''par ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Metasedimentary Rock
In geology, metasedimentary rock is a type of metamorphic rock. Such a rock was first formed through the deposition and solidification of sediment Sediment is a solid material that is transported to a new location where it is deposited. It occurs naturally and, through the processes of weathering and erosion, is broken down and subsequently sediment transport, transported by the action of .... Then, the rock was buried underneath subsequent rock and was subjected to high pressures and temperatures, causing the rock to recrystallize. The overall composition of a metasedimentary rock can be used to identify the original sedimentary rock, even where they have been subject to high-grade metamorphism and intense deformation. Types of metasedimentary rocks See also * References Metamorphic petrology {{Rock-stub ... [...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] |
Yellow River (Chippewa River)
The Yellow River in north central Wisconsin is a tributary of the Chippewa River. For the most part it is a mud and rock-bottomed river flowing through forest and farmland. It is one of four distinct rivers in the state bearing the name ''Yellow River''. Geography This Yellow River begins at Matt Ochs Lake and Perch Lake in the township of Molitor near Perkinstown in the Chequamegon National Forest. This area of small lakes and swamps is the terminal moraine left by the last glacier, which reached this far about 18,000 years ago. The river runs a short way before it forms Chequamegon Waters Flowage, locally known as Miller Dam. Below Miller Dam, there is one more dam, at Cadott, forming another small reservoir, before the river joins the Chippewa River when it flows into Lake Wissota at Moon Bay. Much of the Yellow is undeveloped - in particular the upper stretches through the Chequamegon Forest. In very few places will you see any sign of man. The only settlements ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Till
image:Geschiebemergel.JPG, Closeup of glacial till. Note that the larger grains (pebbles and gravel) in the till are completely surrounded by the matrix of finer material (silt and sand), and this characteristic, known as ''matrix support'', is diagnostic of till. image:Glacial till exposed in roadcut-750px.jpg, Glacial till with tufts of grass Till or glacial till is unsorted glacier, glacial sediment. Till is derived from the erosion and entrainment of material by the moving ice of a glacier. It is deposited some distance down-ice to form terminal, lateral, medial and ground moraines. Till is classified into primary deposits, laid down directly by glaciers, and secondary deposits, reworked by fluvial transport and other processes. Description Till is a form of '' glacial drift'', which is rock material transported by a glacier and deposited directly from the ice or from running water emerging from the ice. It is distinguished from other forms of drift in that it is de ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
