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United States of America topographic maps
Click on a map to view its topography, its elevation and its terrain.
Ketchikan
United States of America > Alaska > Ketchikan
Due to its steep and forested terrain, Ketchikan is long and narrow with much of the built-up area being located along, or no more than a few city blocks from, the waterfront. Elevations of inhabited areas range from just above sea level to about 300 feet (91 m). Deer Mountain, a 3,001-foot (915 m) peak, rises…
Average elevation: 150 m
Bowens Addition
United States of America > Wisconsin > Madison > Bowens Addition
Average elevation: 266 m
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Lawrence
United States of America > Kansas > Lawrence
Downtown Lawrence is located at 38°58′18″N 95°14′7″W / 38.97167°N 95.23528°W / 38.97167; -95.23528 (38.959902, −95.253199), approximately 25 miles (40 kilometers) east of Topeka, and 35 mi (56 km) west of Kansas City, Kansas. Though Lawrence has a designated elevation of 866 feet (264…
Average elevation: 265 m
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Lander County
United States of America > Nevada
The 11,477 ft (3498 m) summit of Bunker Hill, located in the Toiyabe Range near the Nye County border, is the highest point in the county while the county's most topographically prominent peak is Mount Lewis.
Average elevation: 1,768 m
Hillsboro
United States of America > Oregon > Hillsboro
Hillsboro is located at 45°31′N 122°59′W / 45.517°N 122.983°W / 45.517; -122.983 (Hillsboro, Oregon). The United States Census Bureau reports the city has a total area of 21.6 square miles (55.9 km2), all of which is land. In 2013, Hillsboro itself reported an area of 23.88 square miles…
Average elevation: 53 m
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Highland County
United States of America > Ohio
Highland County is a county located in the U.S. state of Ohio. As of the 2010 census, the population was 43,589. Its county seat is Hillsboro. The county is named for the topography which is hilly and divides the watersheds of the Little Miami and Scioto Rivers.
Average elevation: 305 m
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Champaign County
United States of America > Illinois
The topography of Champaign County was formed by the Wisconsin Glacier about 20,000 years before the present. Lobes of ice from what is now Lake Michigan crossed the county, creating a deep pile of glacial soil, up to 300 feet thick, topped by numerous moraines forming small, flat watersheds with no outlets.
Average elevation: 217 m
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