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Plate 1. Hydrogeologic Map and Cross Sections, White Pine County, Nevada, and Adjacent Areas in Nevada

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Plate 1. Hydrogeologic Map and Cross Sections, White Pine County, Nevada, and Adjacent Areas in Nevada U.S. DEPARTMENT OF THE INTERIOR Prepared in cooperation with the SCIENTIFIC INVESTIGATIONS REPORT 2007-5261 U.S. GEOLOGICAL SURVEY BUREAU OF LAND MANAGEMENT Hydrogeologic map and cross sections—PLATE 1 science for a changing world Welch, A.H., Bright, D.J., Knochenmus, L.A., Editors, 2008, Water Resources of the Basin and Range Carbonate-Rock Aquifer System, White Pine County, Nevada, and Adjacent Areas in Nevada and Utah 116° 115°30' 115° 114°30' 114° 113°30' EUREKA COUNTY ALT OREGON IDAHO WYOMING 93 93 UTAH CHERRY NEVADA NEVADA UTAH CREEK Plate location ELKO COUNTY ARIZONA RANGE WHITE PINE COUNTY CALIFORNIA EXPLANATION Boundary of study area Carbonate-rock province DIAMOND MOUNTAINS E RANGE G A' N 40° Steptoe A Valley R TOOELE COUNTY MAVERICK SPRINGS RANGE JUAB COUNTY Tippett CREEK K B E Valley E R C DEEP L KERN MOUNTAINS Butte Valley E G L Southern E BUTTE MOUNTAINS N H Part A C R Buck S A Mountain B' Long Valley N Eureka Spring 50 A G Valley 39°30' E SNAKE Snake Valley RANGE Newark Jakes CONFUSION Butte synclinorium RANGE Valley Valley Ely Sacramento WHITE PINE RANGE Pass EUREKA COUNTY 6 50 PANCAKE RANGE Steptoe Baker Valley Little Smoky Rattlesnake 39° Valley Knoll Northern Confusion Range synclinorium NEEDLE RANGE Part Little Smoky Lund Valley E Central Part G N A R E FORTIFICATION White G River N Valley A RANGE R HORSE MILLARD COUNTY Spring RANGE BEAVER COUNTY Valley K CNCC E Limestone N Lake C E Central Nevada A Hills 38°30' Cave R Valley G Caldera Complex Sunnyside C Dutch John E Valley Mountain C' Grassy Pass RANGE L L E H Mule C Shoe S Valley GRANT 6 IPCC SEAMAN RANGE Indian Peak Caldera Complex NYE COUNTY LINCOLN COUNTY 38° IRON COUNTY 93 CCC WASHINGTON COUNTY 0 10 20 30 40 50 MILES Caliente Caldera Complex 0 10 20 30 40 5 KILOMETERS Map compiled from digital versions of the Nevada (Stewart and Carlson, 1978; Raines and others, 2003) and Utah (Hintze and others, 2000) state geologic maps at 1:500,000-scale. Caldera boundaries modified after Williams and others (1997), Loucks and others (1989), Raines and others (1996), Workman and others (2002), and Gans and others (1989). Boundaries of highly extended terrains modified after Wernicke. Base from U.S. Geological Survey digital data 1:100,000, 1978-1989; Universal Transverse Mercator projection, Zone 11. Shaded relief base from 1:250,000-scale Digital Elevation Model; sun illumination from northwest at 30 degrees above horizon. ’ B-B EXPLANATION EUREKA CO. SW SECTION NE WHITE PINE CO. Zone of low-angle A A' FEET Lone Northern FEET METERS Butte synclinorium normal faults Antelope 12,000 Mountain Cherry Creek Schell Creek 12,000 4,000 Hydrogeologic unit Structural features Diamond Buck Butte Butte Range Spring Range Newark Mountain Range 3,000 8,000 Diamond Valley Mountains Valley Long Valley Mountains Valley Steptoe Valley Valley 8,000 2,000 Normal fault 4,000 4,000 Fine-grained younger sedimentary rock unit 1,000 (primarily lacustrine and playa deposits); FYSU 0 0 0 1,000 Inferred normal fault 4,000 4,000 2,000 Coarse-grained younger sedimentary rock 8,000 8,000 unit(alluvial and fluvial deposits); CYSU 3,000 Low angle normal or detachment fault 12,000 12,000 4,000 16,000 16,000 5,000 Older sedimentary rock unit (consolidated VERTICAL EXAGGERATION APPROXIMATELY X 5 Cenozoic rocks, variety of grain sizes and Low angle normal or detachment fault, inferred depositional environments); OSU Thrust fault ’ Volcanic flow unit (basalt, andesite, dacite A-A and rhyolite lava flows); VFU NW SE FEET B B' FEET METERS Zone of low-angle normal faults UTAH Syncline 12,000 Schell Creek NEVADA 12,000 4,000 Butte SECTION Egan Kern Range Range Mountains Mountains Confusion 3,000 8,000 Butte synclinorium Steptoe Valley Spring Valley Snake Valley 8,000 Volcanic tuff unit (ash-flow tuffs); VTU Confusion synclinorium Range 2,000 4,000 4,000 Inferred syncline 1,000 0 0 0 1,000 Mesozoic sedimentary rock unit (limestones, Caldera boundaries 4,000 4,000 sandstones and siltstones); MSU 2,000 8,000 8,000 3,000 Highly extended terranes 12,000 12,000 4,000 Upper carbonate rock unit (Mississippian 16,000 16,000 5,000 to Permian carbonate rocks); UCU 6,000 20,000 20,000 Transverse zones Northern Snake Range 7,000 detachment fault 24,000 24,000 8,000 Upper siliciclastic rock unit (Mississippian 9,000 siliciclastic rocks); USCU A'A 28,000 28,000 Line of hydrogeologic section 10,000 32,000 32,000 11,000 Lower carbonate rock unit (Cambrian to 36,000 36,000 12,000 Boundary of study area VERTICAL EXAGGERATION APPROXIMATELY X 5 Devonian predominantly carbonate rocks); LCU Jakes Boundary of hydrographic area Valley Lower siliciclastic rock unit (Early Cambrian and name and older siliciclastic rocks); LSCU Boundary of subbasin Symbols that appear on hydrogeologic and seismic cross sections Contact between hydrogeologic units NYE CO. Intrusive unit (Jurassic to Tertiary granitic Thickness of Cenozoic deposits W LINCOLN CO. E FEET C C' FEET METERS rocks); IU 1 mile Form line indicating general attitude of bedding within hydrogeologic unit 6,000 Cave Muleshoe Lake 6,000 2,000 Egan Range Valley White River Valley Valley —114°40' 2 mile —114°50' 4,000 Grant Range Valley —115° 4,000 Elevation of pre-Cenozoic rocks; modeled from gravity data (section A-A’ ) —115°10' 1,000 Geophysically determined faults 2,000 2,000 Fault (sections A-A’ and B-B’ ); arrow shows relative sense of offset 0 0 0 Fault (section C-C’) 2,000 Symmetric 2,000 graben 1,000 4,000 4,000 Fault, inferred (section C-C’ ) 6,000 6,000 2,000 Interpreted base of the Cenozoic basin fill (section C-C’ ) 8,000 Asymmetric grabens 8,000 3,000 10,000 10,000 12,000 12,000 4,000 VERTICAL AND HORIZONTAL SCALE APPROXIMATE VERTICAL EXAGGERATION APPROXIMATELY X 10 HYDROGEOLOGIC MAP AND CROSS SECTIONS, WHITE PINE COUNTY, NEVADA, AND ADJACENT AREAS IN NEVADA AND UTAH By Donald S. Sweetkind, Lari A. Knochenmus, David A. Ponce, Alan R. Wallace, Daniel S. Scheirer, Janet T. Watt, and Russell W. Plume 2008.
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