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Page 5202, results 130026 - 130050

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Maps showing aeromagnetic data and interpretation for the Kalmiopsis Wilderness, southwestern Oregon
Richard J. Blakely, Norman J. Page, Floyd Gray, Lisa Senior, Holly F. Ryan
1983, Miscellaneous Field Studies Map 1240-D
The distinctive magnetic properties of the major rock types in the Kalmiopsis Wilderness of southwestern Oregon facilitate interpretation of aeromagenetic data. The region is composed of tectonic slices of magnetic ultramafic, gabboric, and other ophiolitic rocks faulted against  the realitively nonmagnetic Dothan Formation, the equivalent of the Franciscan Complex of...
Maps showing the distribution and relationships of selected metals in heavy-mineral concentrates of the Hells Hole Further Planning Area (RARE II), Greenlee County, Arizona, and Grant County, New Mexico
J.R. Hassemer, K. C. Watts, C.L. Forn, E. L. Mosier
1983, Miscellaneous Field Studies Map 1344-D
The Wilderness Act (Public Law 99-577, Sept. 3, 1964) and related acts require the U.S. Geological Survey and the U.S. Bureau of Mines to survey certain areas on Federal lands to determine their mineral resource potential.  Results must be made available to the public and be submitted to the President...
Water resources data, New Mexico, water year 1982
Water Resources Division, U.S. Geological Survey
1983, Water Data Report NM-82-1
Water resources data for the 1982 water year for New Mexico consist of records of discharge and water quality of streams; stage, contents and water quality of lakes and reservoirs; and water levels and water quality in wells and springs. This report contains discharge records for 197 gaging stations; stage and...
Mineral resource potential map of the Lye Brook Wilderness, Bennington and Windham counties, Vermont
R. A. Ayuso, D. K. Harrison
1983, Miscellaneous Field Studies Map 1609-C
The Lye Brook Wilderness contains no significant mineral deposits. Although the Cheshire Quartzite is a potential source of low-grade silica sand and crops out in a large area within the wilderness, its degree of induration and relative inaccessibility make its use prohibitive. No major concentation of base metals exist within the Precambrian rocks,...