Rasmussen Lakes, Utah - 7.5 Minute Series Topo Map Wasatch Back Aerial Spontaneous potential and resistivity surveys

Spontaneous potential and resistivity surveys sharply define the geometry of the dominant upflow zone (not yet explored)

A small area of Tertiary volcanic rocks is exposed in the northwestern comer of the quadrangle

geologists

Added fish habitat to all four lakes: Rock rubble reefs

Characterization of Fluvial Sand Bodies in the Neslen and Lower Farrer Formations (Upper Cretaceous)

Rasmussen Lakes, Utah - 7.5 Minute Series Topo Map Wasatch Back Aerial Spontaneous potential and resistivity surveysThe 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