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Dewart Lake
Dewart Lake, (formerly Lake Wawasee before Turkey Lake became Lake Wawasee), is a natural lake southwest of Syracuse in Kosciusko County, Indiana, United States. It was formed during the most recent glacial retreat of the Pleistocene era. Dewart Lake is a 551-acre (223 ha) natural lake, located three miles (4.8 km) south of Syracuse and three miles (4.8 km) east of Indiana State Road 15. 41 degrees 22' 03.31" North Latitude x 85 degrees 46' 18.22" West Longitude, above Sea Level. is the maximum depth with an average depth of . It lies within the Elkhart River watershed and drains . Two small inlets enter on the east side and the outlet, Hammond Ditch, leaves the west side and flows to Waubee Lake Waubee Lake (also incorrectly Wabee) is a small freshwater lake situated 2 miles (3 km) southeast of Milford, Kosciusko County, Indiana, United States. Waubee is typical in structure of natural lakes of the glaciated portions of the upper Mid .... Large areas on t ...
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Kosciusko County, Indiana
Kosciusko County ( ) is a county in the U.S. state of Indiana. At the 2020 United States Census, its population was 80,240. The county seat (and only incorporated city) is Warsaw. The county was organized in 1836. It was named for the Polish general Tadeusz Kościuszko who served in the American Revolutionary War and then returned to Poland. The county seat is named for Warsaw, the capital of Poland. History The Indiana State Legislature passed an omnibus county bill on 7 February 1835 that authorized the creation of thirteen counties in northeast Indiana, including Kosciusko. The county government was organized beginning in 1836. The county's boundary lines have remained unchanged since 1835. Geographical features Kosciusko County terrain consists of low rolling hills dotted with bodies of water and drainages, with all available area devoted to agriculture or urban development. Its highest point (1025'/312 meters ASL) is a hill NE of Dewart Lake. The Tippecanoe River flows west ...
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Lake
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 la ...
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Syracuse, Indiana
Syracuse is a town in Turkey Creek Township, Kosciusko County, Indiana, Turkey Creek Township, Kosciusko County, Indiana, Kosciusko County, in the U.S. state of Indiana. The population was 3,079 at the 2020 census. Syracuse is the location of Syracuse Lake, Lake Syracuse and the nearby, larger Lake Wawasee, in addition to several other lakes in the region. The National Weather Service operates a Weather Forecast Office in the town. It serves Northern Indiana. History Syracuse was laid out in 1837. It was likely named after the city of Syracuse, New York. The Syracuse post office was established in 1837. Geography Syracuse is located at (41.423389, -85.749887). According to the 2010 census, Syracuse has a total area of , of which (or 83.02%) is land and (or 16.98%) is water. Demographics 2010 census At the 2010 census, there were 2,810 people, 1,158 households and 729 families living in the town. The population density was . There were 1,492 housing units at an average dens ...
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Pleistocene Era
The Pleistocene ( , often referred to as the ''Ice age'') is the geological epoch that lasted from about 2,580,000 to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed in 2009 by the International Union of Geological Sciences, the cutoff of the Pleistocene and the preceding Pliocene was regarded as being 1.806 million years Before Present (BP). Publications from earlier years may use either definition of the period. The end of the Pleistocene corresponds with the end of the last glacial period and also with the end of the Paleolithic age used in archaeology. The name is a combination of Ancient Greek grc, label=none, πλεῖστος, pleīstos, most and grc, label=none, καινός, kainós (latinized as ), 'new'. At the end of the preceding Pliocene, the previously isolated North and South American continents were joined by the Isthmus of Panama, causing a faunal interchange between the two reg ...
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Indiana State Road 15
State Road 15 (SR 15) is a north–south state road in northern part of the US state of Indiana. Its southern terminus is at U.S. Highway 35 (US 35) and SR 22 near Jonesboro and its northern terminus is the Michigan state line, north of Bristol, where the roadway continues north as M-103. It is a surface highway that mostly passes farm fields but passing through a few cities of Marion, Wabash, Warsaw, and Goshen. Running for through the state, SR 15 is maintained by the Indiana Department of Transportation (INDOT). Dating back to the before the state road system, the corridor that SR 15 takes today was part of the Hoosier Dixie Highway. The first numbered route along the modern SR 15 corridor was SR 27, while SR 15 ran from Indianapolis to near Michigan City. SR 15 was moved to its modern routing in late 1926, running from Marion to Goshen. During the late 1920s, SR 15 was moved onto its modern routing between Milford and New Paris. In 1930 the road wa ...
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Elkhart River
The Elkhart River is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map , accessed May 19, 2011 tributary of the St. Joseph River in northern Indiana in the United States. It is almost entirely contained in Elkhart County. It begins as the South Branch Elkhart River from Port Mitchell Lake and the North Branch Elkhart River from Waldron Lake and merge to form the Elkhart River west of Wawaka, Indiana. It flows generally westward through Benton and then turns northward. It then flows through Baintertown and Waterford Mills into the Goshen Dam Pond. From there it flows northwest through Goshen, Dunlap and Elkhart. It flows into the St. Joseph River at Island Park just north of downtown Elkhart."Elkhart River"
Indiana Department of Natural Resources. Retrieved 24 January 2010.
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Waubee Lake
Waubee Lake (also incorrectly Wabee) is a small freshwater lake situated 2 miles (3 km) southeast of Milford, Kosciusko County, Indiana, United States. Waubee is typical in structure of natural lakes of the glaciated portions of the upper Midwest. Like other lakes in the general area, Waubee is lined with vacation homes and year-round residences. Part of the extreme upper west shore is void of residences and borders farm land. A boat ramp can be found on the lake's upper east shore. Waubee Lake is also home to Camp Alexander Mack, a Christian Camp, Conference, and Retreat Center operated by the Church of the Brethren. The name Waubee is believed to have come from a common name, Wau-Be, of the Potawatomi people who had a camp where now stands but no authority exists for this claim. The USGS/GNIS has Waubee Lake incorrectly spelled as Wabee Lake. A name change request has been submitted to the United States Geographical Survey The United States Geological Survey (USGS), ...
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Lakes Of Kosciusko County, Indiana
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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