Burns Knoll, Utah - 7.5 Minute Series Topo Map Capitol Reef National Park Thick late Pleistocene-age Lake Bonneville

Thick late Pleistocene-age Lake Bonneville (30 to 13 ka) deltaic and lacustrine deposits are prevalent mostly west of the Wasatch fault zone

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Burns Knoll, Utah - 7.5 Minute Series Topo Map Capitol Reef National Park Thick late Pleistocene-age Lake BonnevilleThe distinctive characteristic of a topographic map is that the shape of the Earth's surface is shown by contour lines. Contours are imaginary lines that join points of equal elevation on the surface of the land above or below a reference surface, such as mean sea level. Contours make it possible to measure the height of mountains, depths of the ocean bottom, and steepness of slopes. A topographic map shows more than contours. The map also includes