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Publications

Browse more than 160,000 publications authored by our scientists over the past 100+ year history of the USGS.  Publications available are: USGS-authored journal articles, series reports, book chapters, other government publications, and more.

Filter Total Items: 171105

Bisbee folio, Arizona

No abstract available.
Authors
F. L. Ransome

Catalogue and index of the publications of the Hayden, King, Powell, and Wheeler surveys

No abstract available.
Authors
Laurence Frederick Schmeckebier

Contributions to economic geology, 1903

No abstract available.
Authors
Samuel Franklin Emmons, C. W. Hayes

Contributions to the hydrology of eastern United States, 1903

No abstract available.
Authors

Cottonwood Falls folio, Kansas

The Cottonwood Falls quadrangle lies between parallels 38° and 38° 30' and meridians 96° 30' and 97°, and therefore constitutes a quarter of a square degree of the earth's surface. It is 34.35 miles long and 26.75 miles wide, and contains about 938 square miles. It is located east and a little south of the central part of Kansas, on Cottonwood River, and includes large portions of Chase and Mario
Authors
Charles Smith Prosser, Joshua William Beede

De Smet folio, South Dakota

No abstract available.
Authors
James Edward Todd, Charles Monroe Hall

Economic geology of the Iola quadrangle, Kansas

No abstract available.
Authors
George Irving Adams, Erasmus Haworth, W.R. Crane

Economic resources of the northern Black Hills

The mining district of the Black Hills comprised within the Spearfish and Sturgis quadrangles was surveyed geologically in the summers of 1898 and 1899 under the direction of Mr. S. F. Emmons. The following pages present a brief summary of the geologic features, more especially with reference to ore-bearing formations. These are confined to the Algonkian and Paleozoic strata and their associated e
Authors
J.D. Irving, S. F. Emmons, T.A. Jaggar

Edgemont folio, South Dakota-Nebraska

No abstract available.
Authors
Nelson Horatio Darton, William Sidney Tangier Smith

Experiments on schistosity and slaty cleavage

Schistosity as a structure is important, and it is a part of the business of geologists to explain its origin. Slaty cleavage has further and greater importance as a possible tectonic feature. Scarcely a great mountain range exists, or has existed, along the course of which belts of slaty rock are not found, the dip of the cleavage usually approaching verticality. Are these slate belts equivalent
Authors
George Ferdinand Becker