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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.

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Filter Total Items: 171816

Zinc-lead deposits of the Lead Hill area on Slate Creek, Metaline District, Pend Oreille County, Washington

No abstract available.
Authors
H. L. James, J. P. Albers

Zinc-lead deposits of the Lead Hill area on Slate Creek, Metaline district, Washington

No abstract available.
Authors
H. L. James, J. P. Albers

Zinc-lead mines of the Pine Creek area, Coeur d'Alene region, Shoshone County, Idaho

No abstract available.
Authors
J.D. Forrester, E.T. McKnight

Geology of the Cimarron Range, New Mexico

In north-central New Mexico the rugged Cimarron Range marks the eastern margin of the Southern Rocky Mountains, abruptly rising more than 5000 feet above the adjacent Great Plains. Structurally the range is a northward-plunging anticline with a core of pre-Cambrian crystalline rocks. Faulting along the eastern and western margins of the anticline separates the mountains from the Great Plains and t
Authors
J.F. Smith, L.L. Ray

Feed costs of producing young rabbits to weaning age

No abstract available.
Authors
Charles E. Kellogg

Inheritance of "woolly" in rabbits

No abstract available.
Authors
A.E. Bellamy

Quartz veins in the Ouachita mountains of Arkansas and Oklahoma (Their relations to structure, metamorphism, and metalliferous deposits)?

An important chapter of the total geologic history of the Ouachita Mountains is revealed by the quartz veins and crystals. These and the associated minerals are hydrothermal deposits of probable magmatic origin, formed during the closing stage of the mid-Permsylvanian orogeny. The metalliferous deposits of the Ouachita Mountains appear to have been formed at the time of the quartz vein deposition.
Authors
Hugh Dinsmore Miser

Save game meat: it is valuable

No abstract available.
Authors
D. Irvin Rasmussen, Marvin D. Wilde

A frequency‐method of evaluating ground‐water levels

Water‐levels in wells, which are utilized by the hydrologist as a measure of ground‐water storage, customarily are measured in terms of distance below a convenient measuring point and expressed with reference to a fixed datum. Datum‐planes or surfaces of several types have been used—each serving some particular purpose advantageously. These include: “Planes” of regional extent, such as mean sea‐le
Authors
Lyman C. Huff

Correlation of ground‐water levels and precipitation on Long Island, New York

Long Island simulates in a general way an aquifer in the form of an infinite strip confined between parallel boundaries at constant head (sea‐level), over which recharge precipitation is assumedly uniform. The non‐steady flow of water in this idealized system is analyzed assuming provisionally that the effective thickness of saturated beds below sea‐level is great compared to the maximum height of
Authors
C. E. Jacob

Gigantic drying cracks in Animas Valley, New Mexico

No abstract available.
Authors
Walter B. Lang

The Finley Site: Antiquity of the Finley Site

This report is based on two months reconnaissance in the summer of 1941 in the Eden Valley, Wyoming. The work is as yet far from complete and the conclusions presented here must be regarded as tentative. It is hoped that in the future more extensive geological work may be undertaken.The Finley site provides a promising opportunity for a determination of the age of the Yuma culture. The points and
Authors
John T. Hack
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