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Our programs produce accurate geologic maps and 3-D geologic frameworks that provide critical data for sustaining and improving the quality of life and economic vitality of the Nation. 

Filter Total Items: 9000

Structure contour map on top of the Canyon Coal Bed, Birney 30' x 60' Quadrangle, Big Horn, Rosebud, and Powder River counties, Montana

No abstract available.

Submarine topography, surficial geology, and fauna of Oceanographer Canyon, northern part

No abstract available.

Summary geochemical maps, Hoover Wilderness and adjacent study area, Mono and Tuolumne counties, California

The Hoover Wilderness and the adjacent Hoover Extension (East), Hoover Extension (West), and Cherry Creek A Roadless Areas (the adjacent study area) encompass approximately 153,900 acres (241 mi2; 623 km2) in the Inyo, Stanislaus, and Toiyabe Naitonal Forests, Mono and Tuolumne Counties, Calif. These two areas lie along and mostly east of the crest of the Sierra Nevada, along the north and east si

Surficial geologic map of the Ambler River Quadrangle, Alaska

No abstract available.

Surficial geologic map of the Bethel Quadrangle, Connecticut

No abstract available.

Surficial geologic map of the Howard Pass Quadrangle, Alaska

No abstract available.

Surficial geologic map of the Iron River 1 degree by 2 degrees Quadrangle, Michigan and Wisconsin

No abstract available.

Surficial geologic map of the Norwalk North Quadrangle, Connnecticut

No abstract available.

Surficial geologic map of the Recluse 30' x 60' Quadrangle, Wyoming and Montana

No abstract available.

Surficial geologic map of the Sheridan 30' by 60' Quadrangle, Wyoming and Montana

No abstract available.

Topographic map of Venus (sheet 1); shaded relief map of Venus (sheet 2)

No abstract available.

Types of damage that could result from a great earthquake in the New Madrid, Missouri, seismic zone

In the winter of 1811–1812 a series of three great earthquakes occurred in the New Madrid seismic zone. In addition to the three principal shocks, at least 15 other earthquakes, Io ≥ VIII, occurred within a year of the first large earthquake on December 16, 1811. The three main shocks were felt over the entire eastern United States. They were strong enough to cause minor damage as far away as Indi