All Publications
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Determination of stream flow during the frozen season
No abstract available.
Authors
Harold Kilbrith Barrows, Robert E. Horton
Economic geology of the Amity quadrangle, eastern Washington County, Pennsylvania
No abstract available.
Authors
Frederick Gardner Clapp
Experimental work conducted in the chemical laboratory of the United States fuel-testing plant at St. Louis, Missouri, January 1, 1905, to July 31, 1906
No abstract available.
Authors
Nathaniel Wright Lord
Flowing wells and municipal water supplies in the middle and northern portions of the southern peninsula of Michigan
A large amount of data on water supplies was collected by the writer in the course of glacial investigations made under the direction of Prof. T. C. Chamberlin in the last five years in the Southern Peninsula of Michigan. These investigations resulted in a partial acquaintance with conditions in about 200 separate flowing-well districts and brought out matters of such exceptional importance that a
Authors
Frank Leverett
Geography and geology of a portion of southwestern Wyoming with special reference to coal and oil
No abstract available.
Authors
A. C. Veatch
Geologic reconnaissance in the Matanuska and Talkeetna basins, Alaska
No abstract available.
Authors
Sidney Paige, Adolph Knopf
Geology and oil resources of the Santa Maria oil district, Santa Barbara County, California
No abstract available.
Authors
Ralph Arnold, Robert van Vleck Anderson
Geology and oil resources of the Summerland district, Santa Barbara County, California
No abstract available.
Authors
Ralph Arnold
Geology and water resources of the Republican River Valley and adjacent areas, Nebraska
No abstract available.
Authors
George E. Condra
Geology of oil and gas fields in Steubenville, Burgettstown, and Claysville quadrangles, Ohio, West Virginia, and Pennsylvania
No abstract available.
Authors
William Tudor Griswold, Malcolm John Munn
Geology of the Marysville mining district, Montana: A study of igneous intrusion and contact metamorphism
The Marysville mining district had been for many years previous to 1899 one of the noted gold-producing centers of Montana. The mines are situated around the margins of in irregular batholith of quartz diorite, whose surface exposure is from half a mile to 1 1/2 miles broad and 2 1/2 miles long. This invasion of igneous rock, which as shown on later pages of this report was primarily the cause of
Authors
Joseph Barrell