Deputy, Indiana
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Deputy, Indiana
Deputy is a mid unincorporated community and census-designated place (CDP) in Graham Township, Jefferson County, Indiana, Graham Township, Jefferson County, Indiana, Jefferson County, Indiana, United States. By road it is approximately northwest of Madison, Indiana, Madison, the county seat. As of the 2010 United States Census, 2010 census it had a population of 86. Geography Deputy is located in western Jefferson County at , northwest of the center of Graham Township. Indiana State Road 3 forms the eastern edge of the community; the highway leads north to North Vernon, Indiana, North Vernon and south to Jeffersonville, Kentucky, Jeffersonville. According to the U.S. Census Bureau, the Deputy CDP has an area of , all of it recorded as land. Lewis Creek flows northward just east of the community, leading in to the Muscatatuck River, part of the White River (Indiana), White River watershed. Deputy is located on land that is considered to be of karst topography. The town and the ...
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Census-designated Place
A census-designated place (CDP) is a concentration of population defined by the United States Census Bureau for statistical purposes only. CDPs have been used in each decennial census since 1980 as the counterparts of incorporated places, such as self-governing cities, towns, and villages, for the purposes of gathering and correlating statistical data. CDPs are populated areas that generally include one officially designated but currently unincorporated community, for which the CDP is named, plus surrounding inhabited countryside of varying dimensions and, occasionally, other, smaller unincorporated communities as well. CDPs include small rural communities, edge cities, colonias located along the Mexico–United States border, and unincorporated resort and retirement communities and their environs. The boundaries of any CDP may change from decade to decade, and the Census Bureau may de-establish a CDP after a period of study, then re-establish it some decades later. Most unin ...
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2010 United States Census
The United States census of 2010 was the twenty-third United States national census. National Census Day, the reference day used for the census, was April 1, 2010. The census was taken via mail-in citizen self-reporting, with enumerators serving to spot-check randomly selected neighborhoods and communities. As part of a drive to increase the count's accuracy, 635,000 temporary enumerators were hired. The population of the United States was counted as 308,745,538, a 9.7% increase from the 2000 census. This was the first census in which all states recorded a population of over half a million people as well as the first in which all 100 largest cities recorded populations of over 200,000. Introduction As required by the United States Constitution, the U.S. census has been conducted every 10 years since 1790. The 2000 U.S. census was the previous census completed. Participation in the U.S. census is required by law of persons living in the United States in Title 13 of the United ...
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Wakefield, Indiana
Wakefield is an unincorporated community in Jefferson County, Indiana, in the United States The United States of America (U.S.A. or USA), commonly known as the United States (U.S. or US) or America, is a country primarily located in North America. It consists of 50 states, a federal district, five major unincorporated territorie .... History A post office was established at Wakefield in 1899, and remained in operation until it was discontinued in 1905. The community was named for Robert Wakefield. Wakefield was the home of the famous bird dog trainer Samuel M. Lewis. Sam raised his four children on his farm on Sage Lane. He was well known and liked in the area for many years (1915-2004). His daughter now lives on the farm. References Unincorporated communities in Jefferson County, Indiana Unincorporated communities in Indiana {{JeffersonCountyIN-geo-stub ...
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Indiana State Road 7
State Road 7 in the U.S. State of Indiana is located in southeast Indiana. It runs from northwest-to-southeast connecting the cities of Columbus and Madison. Route description SR 7 begins at Main Street in Madison, of which it then travels in a northward direction along Cragmont Street. Along the way, SR 7 briefly meanders through hilly terrain. After leaving the hilly terrain, SR 7 briefly turns northwest on another road before turning west near a railroad crossing. As the road approaches the east side of Clifty Falls State Park Clifty Falls State Park is an Indiana state park on in Jefferson County, Indiana in the United States. It is northeast of Louisville, Kentucky. The park attracts about 370,000 visitors annually. On October 27, 1920, citizens of Madison, Ind ..., the road curves northwest again, becoming Lanier Drive. After that, the route intersects with SR 56/SR 62 (Clifty Drive). On its way toward Vernon, SR 7 travels northwest an ...
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Treaty Of Fort Wayne (1809)
The Treaty of Fort Wayne, sometimes called the Ten O'clock Line Treaty or the Twelve Mile Line Treaty, is an 1809 treaty that obtained 29,719,530 acres of Native American land for the settlers of Illinois and Indiana. The negotiations primarily involved the Delaware tribe but included other tribes as well. However, the negotiations excluded the Shawnee, who were minor inhabitants of the area and had previously been asked to leave by Miami War Chief Little Turtle. Territorial Governor William Henry Harrison negotiated the treaty with the tribes. The treaty led to a war with the United States begun by Shawnee leader Tecumseh and other dissenting tribesmen in what came to be called "Tecumseh's War". The parcels The treaty has two nicknames in popular American culture: the "Ten O'clock Line Treaty of 1809" and the "Twelve Mile Line Treaty", both of which are associated with the disparate parcels of land defined by the treaty. The first nickname comes from tradition that says the Nat ...
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Sussex County, Delaware
Sussex County is located in the southern part of the U.S. state of Delaware, on the Delmarva Peninsula. As of the 2020 census, the population was 237,378. The county seat is Georgetown. The first European settlement in the state of Delaware was founded by the Dutch in 1631 near the present-day town of Lewes on the Atlantic Coast. However, Sussex County was not organized until 1683 under English colonial rule. Sussex County is included in the Salisbury, MD-DE Metropolitan Statistical Area which encompasses much of central Delmarva. History Beginnings Archaeologists estimate that the first inhabitants of Sussex County, the southernmost county in Delaware, arrived between 10,000 and 14,000 years ago. Various indigenous cultures occupied the area, especially along the river and the coast, often having seasonal fishing villages. Historic Native Americans in Sussex County were members of Algonquian-speaking tribes, as were most coastal peoples along the Atlantic Coast. By the ...
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Clark County, Indiana
Clark County is a county in the U.S. state of Indiana, located directly across the Ohio River from Louisville, Kentucky. At the 2020 census, the population was 121,093. The county seat is Jeffersonville. Clark County is part of the Louisville/Jefferson County, KY–IN Metropolitan Statistical Area. History Clark County lies on the north bank of the Ohio River. A significant gateway to the state of Indiana, Clark County's settlement began in 1783. The state of Virginia rewarded General George Rogers Clark and his regiment for their victorious capture of Forts Kaskaskia, Cahokia, and Vincennes from the British, by granting them of land. A small portion of this land, , became known as Clarksville, the first authorized American settlement in the Northwest Territory, founded the next year in 1784.
Clark County Genealogical Records (accessed 21 January ...
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Humid Subtropical Climate
A humid subtropical climate is a zone of climate characterized by hot and humid summers, and cool to mild winters. These climates normally lie on the southeast side of all continents (except Antarctica), generally between latitudes 25° and 40° and are located poleward from adjacent tropical climates. It is also known as warm temperate climate in some climate classifications. Under the Köppen climate classification, ''Cfa'' and ''Cwa'' climates are either described as humid subtropical climates or warm temperate climates. This climate features mean temperature in the coldest month between (or ) and and mean temperature in the warmest month or higher. However, while some climatologists have opted to describe this climate type as a "humid subtropical climate", Köppen himself never used this term. The humid subtropical climate classification was officially created under the Trewartha climate classification. In this classification, climates are termed humid subtropical when the ...
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Köppen Climate Classification
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notably in 1918 and 1936. Later, the climatologist Rudolf Geiger (1894–1981) introduced some changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification system. The Köppen climate classification divides climates into five main climate groups, with each group being divided based on seasonal precipitation and temperature patterns. 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'' indi ...
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Karst
Karst is a topography formed from the dissolution of soluble rocks such as limestone, dolomite, and gypsum. It is characterized by underground drainage systems with sinkholes and caves. It has also been documented for more weathering-resistant rocks, such as quartzite, given the right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes. However, in regions where the dissolved bedrock is covered (perhaps by debris) or confined by one or more superimposed non-soluble rock strata, distinctive karst features may occur only at subsurface levels and can be totally missing above ground. The study of ''paleokarst'' (buried karst in the stratigraphic column) is important in petroleum geology because as much as 50% of the world's hydrocarbon reserves are hosted in carbonate rock, and much of this is found in porous karst systems. Etymology The English word ''karst'' was borrowed from German in the late 19th century, which entered German much earlier ...
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White River (Indiana)
The White River is an American two-forked river that flows through central and southern Indiana and is the main tributary to the Wabash River. Via the west fork, considered to be the main stem of the river by the U.S. Board on Geographic Names, the White River is long.U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map accessed May 19, 2011 Indiana's capital, Indianapolis, is located on the river. The two forks meet just north of Petersburg and empty into the Wabash River at Mount Carmel, Illinois. West Fork The West Fork, long, is the main fork of the river. Federal maps refer to it simply as the White River, per a 1950 Board on Geographic Names decision. It starts south of Winchester in Randolph County at 40° 04' 46" N, 84° 55' 58" W in Washington Township. The river winds through Muncie, Anderson, Noblesville, and Indianapolis before being joined by the east fork in the triad of Daviess, Knox, and Pike counties. Alon ...
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Muscatatuck River
The Muscatatuck River is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map accessed May 19, 2011 river in south-central Indiana, United States. It is a major tributary of the East Fork of the White River, and drains . In one area it serves as the southern boundary of the main unit of the Muscatatuck National Wildlife Refuge. It also goes across the Crosley Fish and Wildlife Area and by Muscatatuck County Park. Below the mouth of the Vernon Fork, the Muscatatuck measures approximately 585 cubic feet per second. This figure is arrived at by combining the approximate discharge of the Muscatatuck at Deputy, Indiana & the approximate discharge of the Vernon Fork Muscatatuck River at Vernon, Indiana. The path of the Muscatatuck was formed by valley beds created during an ice age. It is believed that the first people arrived and lived by the Muscatatuck around 8000 BC, maintaining permanent structures between 1000 BC to 1000 AD. The ...
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