U.S. Geological Survey Home AASG Logo USGS HOME CONTACT USGS SEARCH USGS
National Geologic Map Database
Map showing publication footprint
  • Usage in publication:
    • Campbell Mountain rhyolite*
  • Modifications:
    • Original reference
  • Dominant lithology:
    • Rhyolite
  • AAPG geologic province:
    • San Juan Mountains province
Publication:

Emmons, W.H., and Larsen, E.S., 1923, Geology and ore deposits of the Creede district, Colorado: U.S. Geological Survey Bulletin, 718, 198 p., (incl. geologic map, scale 1:24,000) [http://ngmdb.usgs.gov/Prodesc/proddesc_25596.htm]


Summary:

Campbell Mountain rhyolite of Alboroto group of Potosi volcanic series. Overlying the Willow Creek rhyolite rather irregularly is a rhyolite flow breccia here named Campbell Mountain rhyolite. In most places no evidence was seen of more than one flow, but on East Willow Creek two flows of this type are separated by a few hundred feet of Phoenix Park quartz latite. Thickness 0 to 1,000 feet. Upper contact of Campbell Mountain rhyolite is everywhere sharp, but some of overlying rocks so closely resemble it that separation was somewhat difficult. Age is Miocene.
Named from Campbell Mountain, Creede district, [San Luis Peak 7.5-min quadrangle], Mineral Co., southwestern CO.

Source: US geologic names lexicon (USGS Bull. 896, p. 325).


Map showing publication footprint
  • Usage in publication:
    • Campbell Mountain Member*
  • Modifications:
    • Revised
  • AAPG geologic province:
    • San Juan Mountains province
Publication:

Steven, T.A., and Ratte, J.C., 1964, Revised Tertiary volcanic sequence in the central San Juan Mountains, Colorado; Article 132, IN Geological Survey Research 1963; short papers in geology and hydrology; Articles 122-170: U.S. Geological Survey Professional Paper, 475-D, p. D54-D63. [Available online from the USGS PubsWarehouse: http://pubs.er.usgs.gov/pubs/pp/pp475D]


Summary:

Campbell Mountain Member of Bachelor Mountain Rhyolite. In the San Juan Mountain province, Campbell Mountain Rhyolite of Emmons and Larsen (1923) is reduced in stratigraphic rank and assigned to the Bachelor Mountain Rhyolite as its middle member. Age is middle or late Tertiary.

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


Map showing publication footprint
  • Usage in publication:
    • Campbell Mountain Bed*
  • Modifications:
    • Revised
    • Age modified
  • AAPG geologic province:
    • San Juan Mountains province
Publication:

Steven, T.A., Lipman, P.W., and Olson, J.C., 1974, Ash-flow stratigraphy and caldera structures in the San Juan volcanic field, southwestern Colorado, IN Cohee, G.V., and Wright, W.B., Changes in stratigraphic nomenclature by the U.S. Geological Survey, 1972: U.S. Geological Survey Bulletin, 1394-A, p. A75-A82.


Summary:

Pg. A8-A9, A79. Campbell Mountain Bed of Bachelor Mountain Member of Carpenter Ridge Tuff. Reduced in stratigraphic rank from Campbell Mountain Member of Bachelor Mountain Tuff to Campbell Mountain Bed, middle bed of Bachelor Mountain Member (revised) of Carpenter Ridge Tuff (revised). Overlies Willow Creek Bed (revised) of Bachelor Mountain; underlies Windy Gulch Bed (revised) of Bachelor Mountain. Age is changed from Oligocene --to-- late Oligocene.

Source: Publication.


Map showing publication footprint
  • Usage in publication:
    • Campbell Mountain zone*
  • Modifications:
    • Revised
  • AAPG geologic province:
    • San Juan Mountains province
Publication:

Lipman, P.W., Sawyer, D.A., and Hon, K., 1989, Central San Juan caldera cluster; Road log 3, South Fork to Lake City, IN Chapin, C.E., and Zidek, Jiri, eds., Field excursions to volcanic terranes in the western United States; Volume 1, Southern Rocky Mountain region: New Mexico Bureau of Mines and Mineral Resources Memoir, no. 46, p. 330-349., Produced for the International Association of Vocanology and Chemistry of the Earth's Interior (IAVCEI) General Assembly held in Santa Fe, New Mexico, June 25 - July 1, 1989


Summary:

Revised to informal status and is referred to as middle of three zones within Bachelor Mountain Member of Carpenter Ridge Tuff. Restudy of Creede area, Mineral Co, CO, San Juan Mountain province, has shown that within central part of Bachelor caldera in San Juan volcanic field, unit represents middle zone of upward sequence of progressively less welded zones within thick rhyolitic caldera fill. At margins of caldera welding zones, alternate and interfinger complexly. Unit previously thought to be a discrete eruptive deposit. Grades downward into Willow Creek zone (revised to informal status) of Bachelor Mountain; grades upward into Windy Gulch zone (revised to informal status) of Bachelor Mountain. Oligocene age (27.35 Ma).

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


Search archives

For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.

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

"No current usage" (†) implies that a name has been abandoned or has fallen into disuse. Former usage and, if known, replacement name given in parentheses ( ).

Slash (/) indicates name conflicts with nomenclatural guidelines (CSN, 1933; ACSN, 1961, 1970; NACSN, 1983, 2005, 2021). May be explained within brackets ([ ]).