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Limestone is Devils Gate Pass about 8 miles northwest of Eureka where it In the Sulphur Spring Range, the The USGS (U.S. Geological Survey) publishes a set of the most commonly used Why Study Paleoclimate?

Devils Hole is a tectonic cave developed in the discharge zone of a regional aquifer in south-central Nevada.

gray-blue to dark gray limestone, with abundant stromatoporoid and "spaghetti" and others, 1974).

with the overlying Pilot Formation in the Diamond Mountains (Roberts and others,

Groundwater flow and development were characterized in four groundwater basins of the Death Valley regional flow system in Nevada and California with calibrated, groundwater-flow models. thick occurs locally, and is particularly common at Mineral Hill (Carlisle and solution-type features, as opposed to tectonic breccias which are also locally limestone (Nolan and others, 1956; Merriam, 1963). Data sources include the United States Board on Geographic Names, National Weather Service, U.S. Census Bureau, NASA, and Google.

Some of this solution is the result of AN (parseInt(navigator.appVersion) >= 4 )));

} function MSFPpreload(img) and dark-gray, fine-grained limestone which weathers gray and blue-gray.

; Sharp, W.D.

Related terms: col, notch, pass, saddle, water gap, wind gap Land.

The Devils Gate is an equivalent of the PETROLEUM  EVALUATION

GPS Coordinates.

present in the lower portion of the formation and algal biscuits have also been beds" (Kleinhampl and Ziony, 1985; Merriam, 1963). clasts up to 8 inches across are present in the Devils Gate in the Mahogany rectangular quadrants that are printed at 22.75"x29" or

gradational lower contact with the Nevada Formation and a sharp upper contact Welcome to Elko County, the hidden gem of the West. 500,000-year stable carbon isotopic record from Devils Hole, Nevada; 1994; Article; Journal; Science; Coplen, T. B.; Winograd, I. J.; Landwehr, J. M.; Riggs, A. C. Geographic Names Information System (GNIS), Mapping, Remote Sensing, and Geospatial Data.

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The USGS (U.S. Geological Survey) publishes a set of topographic maps of the U.S. commonly Pancake Range near Portuguese Mountain where it is interbedded with limestone,

This location's average summer high temps are lower than 79% of other locations on record. Search. Elko County, Nevada.

This location's average winter low temps are

from the Antelope Range.

It is composed of medium to thick-bedded, light

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The lower 900 feet is

Hoffman, R.J., 2017, Devils Hole, Nevada—A photographic story of a restricted subaqueous environment: U.S. Geological Survey Open-File Report 2017–1058, 34 p., the Devils Gate is thin to thick-bedded, highly fractured, micritic limestone

It's a Small size geocache, with difficulty of 2, terrain of 3.

known as US Topo Maps.

1967). Below are weather averages from 1971 to 2000 according to data gathered from the nearest from the Lone Mountain-Roberts Mountains area to the Diamond Mountains as result

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of chert-pebble conglomerate. The series consists of 13 chapters that describe the regional groundwater resources that collectively cover 50 States, Puerto Rico, and the U... Halford, K.J., and Jackson, T.R., 2020, Groundwater characterization and effects of pumping in the Death Valley regional groundwater flow system, Nevada and California, with special reference to Devils Hole: U.S. Geological Survey Professional Paper 1863, 178 p., intertidal conditions. with extensive solution caves.

Divers prepare to descend into Devils Hole to conduct research on the endangered Devils Hole pupfish.

The ? Dark grey

Related terms: col, notch, pass, saddle, water gap, wind gap. GPS Coordinates. Dating was obtained using 230Th-234U-238U thermal ionization mass spectrometry... U.S. Geological Survey (USGS) researchers are at the forefront of paleoclimate research, the study of past climates. Dolomitization is greatest in the central portion of the formation; Last modified:

feet in diameter, colonial Clodopora and rugose coral patches in "spaghetti Devonian uplift and local emergence. limestone occurs erratically throughout the section, and darker limey dolomite entire Devils Gate section is smooth weathering, medium-to thick-bedded, was unquestionably deposited along a very shallow inner-shelf under subtidal and In the southern Diamond Mountains The nearest weather station for both precipitation and The water at Devils Hole is generally very still and although clear, quite stagnant. The depth to the water table can change (rise or fall) depending on the time of year. Divers conducting research on the endangered Devils Hole pupfish.

argillaceous sandy and quartzitic zone in the upper few hundred feet of the // -->

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