Publications
Publications from the staff of the Geology, Minerals, Energy, and Geophysics Science Center
Filter Total Items: 2350
Cenozoic plate motions and the volcano-tectonic evolution of western Oregon and Washington
A refined northeast Pacific plate-motion model provides a framework for analysis of the Tertiary volcanic and tectonic history of western Oregon and Washington. We examine three possible models for the origin of the allochthonous Paleocene and Eocene oceanic basalt basement of the Coast Range: (1) accretion to the continent of hot spot generated linear seamount chains; (2) accretion of thick ocean
Authors
Ray Wells, David C. Engebretson, P. D. Snavely, R. S. Coe
Shimada Seamount: An example of recent mid-plate volcanism
Shimada Seamount is an isolated volcanic feature located between the Clipperton and Clarion Fracture Zones ∼1,150 km west of the East Pacific Rise and ∼600 km west of the inactive spreading center represented by the Mathematician Seamounts. It rises ∼3,900 m above the surrounding sea floor to within 50 m of present-day sea level. The area of Shimada Seamount should be volcanically dormant, because
Authors
J. V. Gardner, Walter E. Dean, Richard J. Blakely
Addresses, topics of interest, and geographic distribution of professors working on landslides in the United States
No abstract available.
Authors
E. E. Brabb, Ann R. FitzSimmons
Wilderness mineral potential: Assessment of mineral-resource potential in U.S. Forest Service lands studied in 1964-1984: Volume 1
Under the provisions of the Wilderness Act (Public Law 88-577, September 3, 1964) and subsequent related legislation, the U.S. Geological Survey (USGS) and the U.S. Bureau of Mines (USBM) have been conducting mineral surveys of wilderness and primitive areas, and of other national forest lands being considered for wilderness designation. The Wilderness Act directs that the results of these surveys
United States Geological Survey Yearbook, fiscal year 1983
The fiscal year 1983 Yearbook summarizes the activities of the U.S. Geological Survey in response to its scientific and regulatory missions.
Authors
Weaver Bally Roadless Area, California
The Weaver Bally Roadless Area includes approximately 22 sq mi in the Shasta-Trinity National Forest, Trinity County, California. A mineral survey indicates that an area of less than 1 sq mi in the northern part of the Weaver Bally Roadless Area has a substantiated mineral-resource potential for gold and silver; a much larger area has a probable mineral-resource potential for the same elements. Th
Authors
M. C. Blake, T. J. Peters
Yolla Bolly-Middle Eel Wilderness And Big Butte-Shinbone, East Fork, Murphy Glade, and Wilderness contiguous roadless areas, California
A mineral survey of the Yolla Bolly-Middle Eel Wilderness, California identified a mine with inferred resources of manganese and an occurrence with inferred resources of nickel. The adjacent Big Butte-Shinbone Roadless Area to the west has an area of probable potential for the occurrence of chromium-nickel-cobalt resources and mines with demonstrated and inferred resources of manganese and chrome-
Authors
M. C. Blake, A. M. Leszcykowski
Preliminary geologic map of the Red Bluff 1:100,000 Quadrangle, California
No abstract available.
Authors
M. C. Blake, D. S. Harwood, E. J. Helley, W. P. Irwin, A. S. Jayko, D. L. Jones
Preliminary geologic map of the Colville Indian Reservation, Ferry and Okanogan Counties, Washington, with a table of potassium-argon ages
No abstract available.
Authors
Brian F. Atwater, Robert J. Fleck
Geological Survey research, fiscal year 1981
A summary of recent significant scientific and economic results accompanied by a list of geologic, hydrologic, and cartographic investigations in progress.
Authors
Proceedings of Conference XXIV; A workshop on Geologic Hazards in Puerto Rico
No abstract available.
Authors
Walter W. Hays, Carls J. Kitzmiller, Lynne N. Downer
Statistical relations among earthquake magnitude, surface rupture length, and surface fault displacement
In order to refine correlations of surface-wave magnitude, fault rupture length at the ground surface, and fault displacement at the surface by including the uncertainties in these variables, the existing data were critically reviewed and a new data base was compiled. Earthquake magnitudes were redetermined as necessary to make them as consistent as possible with the Gutenberg methods and results,
Authors
M. G. Bonilla, R. K. Mark, J. J. Lienkaemper