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The USGS provides unbiased, objective, and impartial scientific information upon which our audiences, including resource managers, planners, and other entities, rely.

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Browse more than 82,000 reports authored by our scientists over the past 100+ year history of the USGS and refine search by topic, location, year, and advanced search.

Filter Total Items: 83895

Surface water supply of the United States, 1935, Part VI, Missouri River basin

No abstract available.
Authors

Surface water supply of the United States, 1935, Part VII, Lower Mississippi River basin

No abstract available.
Authors

The Book Cliffs coal field in Emery and Grand counties, Utah

No abstract available.
Authors
Daniel Jerome Fisher

The flora of the New Albany shale: Part 1, Diichnia kentuckiensis, a new representative of the Calamopityeae

No abstract available.
Authors
C.B. Read

The mammals and life zones of Oregon

No abstract available.
Authors
Vernon Bailey

The New York State flood of July 1935

No abstract available.
Authors
Hollister Johnson

The Richey-Lambert coal field, Richland and Dawson Counties, Montana

No abstract available.
Authors
F.S. Parker

The Rosebud coal field, Rosebud and Custer Counties, Montana

No abstract available.
Authors
W. G. Pierce

The Tertiary floras of Alaska, with a chapter on the geology of the Tertiary deposits

No abstract available.
Authors
Arthur Hollick, P. S. Smith

The thiem method for determining permeability of water-bearing materials and its application to the determination of specific yield; results of investigations in the Platte river valley, Nebraska

Abstract contains content that can not be displayed, please see the publication for abstract
Authors
Leland K. Wenzel

Water levels and artesian pressure in observation wells in the United States in 1935 : with statements concerning previous work and results

No abstract available.
Authors
Oscar Edward Meinzer, Leland K. Wenzel

Water resources of the Edwards limestone in the San Antonio area, Texas

The water discharged from the large springs of San Antonio and most of the deep wells of the San Antonio area comes from a common reservoir in fissures and solution channels in the Edwards limestone. The water enters the limestone in a zone of outcrop along the Balcones escarpment, which crosses the northern parts of Bexar and Medina Counties and extends a long distance both to the east and west o
Authors
Penn Livingston, A.N. Sayre, W. N. White
By
Water Resources Mission Area, Oklahoma-Texas Water Science Center
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