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National Geologic Map Database
Map showing publication footprint
  • Usage in publication:
    • Mountain Meadows dacite porphyry*
  • Modifications:
    • Named
  • Dominant lithology:
    • Dacite
    • Porphyry
  • AAPG geologic province:
    • Transverse Ranges province
Publication:

Woodford, A.O., Shelton, J.S., and Moran, T.G., 1944, Stratigraphy and oil possibilities of Puente and San Jose Hills, California: U.S. Geological Survey Oil and Gas Investigations Map, OM-23, 1 sheet, scale approx. 1:64,000


Summary:

Shown on geologic map in northeast extremity of San Jose Hills, Los Angeles Co, CA. Porphyry has mass of 5500 ft by 2500 ft. Intrudes gneissic bedrock. Unconformably underlies massive and fragmental volcanic rocks of Tertiary age. Age is uncertain.

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


Map showing publication footprint
  • Usage in publication:
    • Mountain Meadows dacite porphyry*
  • Modifications:
    • Areal extent
  • AAPG geologic province:
    • Transverse Ranges province
Publication:

Shelton, J.S., 1946, Geology of northeast margin of San Gabriel basin, Los Angeles County, California: U.S. Geological Survey Oil and Gas Investigations Map, OM-63, 1 sheet, scale 1:24,000


Summary:

Mapped undivided with basement rocks in northeast margin of San Gabriel basin. Age of undivided rocks given as Mesozoic.

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


Map showing publication footprint
  • Usage in publication:
    • Mountain Meadows dacite porphyry*
  • Modifications:
    • Areal extent
  • AAPG geologic province:
    • Transverse Ranges province
Publication:

Woodford, A.O., Moran, T.G., and Shelton, J.S., 1946, Miocene conglomerates of Puente and San Jose Hills, California: American Association of Petroleum Geologists Bulletin, v. 30, no. 4, p. 514-560. [Available online, with subscription, from AAPG archives: http://www.aapg.org/datasystems or http://search.datapages.com]


Summary:

Mountain Meadows dacite porphyry described as pale greenish or yellowish rock with phenocrysts of euhedral oligoclase and biotite and less abundant resorbed quartz. Named for largest exposed mass at Mountain Meadows Country Club just northwest of Pomona. Is 2000 ft across and intrusive into basement complex. Occurs as swarms of dikes and masses in San Gabriel Mountains between San Gabriel Canyon and Cucamonga Canyon. Also occurs in subsurface. Probably unconformably underlies Glendora volcanics. Sketch map shows age as uncertain.

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


Map showing publication footprint
  • Usage in publication:
    • Mountain Meadows dacite
  • Modifications:
    • Redescribed
    • Age modified
  • AAPG geologic province:
    • Transverse Ranges province
Publication:

Shelton, J.S., 1955, Glendora volcanic rocks, Los Angeles basin, California: Geological Society of America Bulletin, v. 66, no. 1, p. 45-90, (incl. geologic map, scale 1:24,000)


Summary:

Mountain Meadows dacite porphyry of Woodford and others (1940) referred to as Mountain Meadows dacite. Described as biotite dacite porphyry considerably more extensive underground than at the surface. Shown on geologic map of Glendora volcanic rocks as pre-middle Miocene in age.

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


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

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