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Map showing publication footprint
  • Usage in publication:
    • Gods Pocket dacite*
  • Modifications:
    • [First used]
  • Dominant lithology:
    • Dacite
  • AAPG geologic province:
    • Great Basin province
Publication:

Coats, R.R., 1957, Jarbidge quadrangle, Nevada, IN Geologic investigations of radioactive deposits, semiannual progress report, December 1, 1956 to May 31, 1957; Book 2, geology and mineralogy: U.S. Geological Survey Trace Elements Investigations, TEI-0690, p. 303-312., Prepared for U.S. Atomic Energy Commission


Summary:

Pg. 306. Gods Pocket dacite. Sequence of dacite flow material about 700 feet thick. Disconformably overlies Jarbidge rhyolite (new) and locally separated from it by 30 to 50 feet of pale-gray vitric tuff. Present in northeastern quarter Jarbidge quadrangle, Elko Co., northeastern NV. Gods Pocket Dacite adopted by the USGS.
USGS currently [ca. 1966] considers the Gods Pocket Dacite to be Pliocene(?) in age.

Source: US geologic names lexicon (USGS Bull. 1200, p. 1534).


Map showing publication footprint
  • Usage in publication:
    • Gods Pocket dacite*
  • Modifications:
    • Named
  • Dominant lithology:
    • Dacite
  • AAPG geologic province:
    • Great Basin province
Publication:

Coats, R.R., 1964, Geology of the Jarbidge quadrangle, Nevada-Idaho, IN Contributions to general geology, 1961: U.S. Geological Survey Bulletin, 1141-M, p. M1-M24.


Summary:

Gods Pocket dacite. Sequence of pale-gray, dense, stony, aphanitic dacite flows and minor tuffs. Locally includes black vitrophyric phases, and at base, a 30- to 50-foot unconsolidated pale-gray vitric tuff. Contains relatively large phenocrysts of andesine and lesser amounts of sanidine, smaller and sparser phenocrysts of quartz and pigeonite, and rare augite and hypersthene; accessory minerals include magnetite, apatite, and zircon. Thickness about 930 feet, however, top of unit is absent. Unconformably overlies Jarbidge rhyolite (new); unconformably underlies Pole Creek dacite (new) and Slide Creek gravel (new). Source is unknown, though vent may lie beneath Gods Pocket Peak. Age is considered Pliocene(?), based on stratigraphic position; possibly Miocene -or- Miocene and Pliocene (D.I. Axelrod, written commun., 1959). Report includes geologic map. Adopted by the USGS.
Type locality: Gods Pocket Peak in southeast part of Jarbidge quadrangle, Elko Co., northeastern NV. Named from Gods Pocket Peak.

Source: Modified from GNU records (USGS DDS-6; Denver GNULEX).


Map showing publication footprint
  • Usage in publication:
    • Gods Pocket Dacite*
  • Modifications:
    • Age modified
  • AAPG geologic province:
    • Great Basin province
Publication:

Coats, R.R., Green, R.C., and Cress, L.D., 1977, Mineral resources of the Jarbidge Wilderness and adjacent areas, Elko County, Nevada, with a section on interpretation of aeromagnetic data by W.E. Davis, IN Studies related to wilderness; wilderness areas: U.S. Geological Survey Bulletin, 1439, 79 p., (incl. geologic map, scale 1:48,000)


Summary:

Age modified from Pliocene? to late Miocene in Jarbidge Wilderness and adjacent areas, north-central Elko Co, NV, Great Basin province. Age change based on 12.2 +/-0.8 m.y. date on Cougar Point Welded Tuff from Owyhee quad about 40 mi to west by Obradovich (Coats, Stephens, 1968, Ore deposits of the United States, 1933-1967, v. 2, p. 1083). Thus all rocks older than Cougar Point and younger than Jarbidge Rhyolite (Gods Pocket, Pole Creek Dacite, Slide Creek Gravel and Jenny Creek Tuff) are assigned late Miocene age.

Source: GNU records (USGS DDS-6; Denver GNULEX).


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Asterisk (*) indicates published by U.S. Geological Survey authors.

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