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3321 results.

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Page 46, results 1126 - 1150

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Reconnaissance geochemical maps of mineralized rocks in the Dragoon Mountains Roadless Area, Cochise County, Arizona
Harald Drewes
1984, Miscellaneous Field Studies Map 1521-D
The Dragoon Mountains of central Cochise County are one of a group of northwest-trending ranges in southeastern Arizona. The Dragoon Mountains have a broad, low southeastern part; a narrow, moderately high central part; and a broad, high, northwestern part. The Dragoon Mountains Roadless Area, about 55 mi2 (104 km2) in...
Summary geochemical maps, Hoover Wilderness and adjacent study area, Mono and Tuolumne counties, California
M.A. Chaffee, R. H. Hill, S. J. Sutley
1984, Miscellaneous Field Studies Map 1101-B
The Hoover Wilderness and the adjacent Hoover Extension (East), Hoover Extension (West), and Cherry Creek A Roadless Areas (the adjacent study area) encompass approximately 153,900 acres (241 mi2; 623 km2) in the Inyo, Stanislaus, and Toiyabe Naitonal Forests, Mono and Tuolumne Counties, Calif. These two areas lie along and mostly...
Bathymetric map of Lydonia Canyon, U.S. Atlantic Outer Continental Shelf
Bradford Butman, John A. Moody
1984, Miscellaneous Field Studies Map 1710
Lydonia Canyon is one of several large submarine canyons that indent the eastern U.S. Continental Shelf along the southern flank of Georges Bank (Index map).  This bathymetric map of the upper part of Lydonia Canyon (water depths shallower than about 2,00 m) was prepared as part of a study of...
Illinois landslide inventory map
M. M. Killey (compiler), J.K. Hines, P. B. Du Montelle, Earl Braff
1984, Miscellaneous Field Studies Map 1691
No abstract available. ...
Maps showing geomorphic and geologic evidence for Late Quaternary displacement along the Surprise Valley and associated faults, Modoc County, California
Charles W. Hedel
1984, Miscellaneous Field Studies Map 1429
The maps in this report are designed to show the location, nature, and age of fault traces and lineaments that are interpreted to be the result of late Quaternary movement along the Surprise Valley and associated faults. These characteristics are important to scientists and engineers who study the surface faulting...