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National Geologic Map Database
Map showing publication footprint
  • Usage in publication:
    • Oakville Sandstone
  • Modifications:
    • Mapped 1:250k
  • Dominant lithology:
    • Sandstone
    • Clay
  • AAPG geologic province:
    • Gulf Coast basin
Publication:

Barnes, V.E. (project director), 1974, Geologic atlas of Texas, Seguin sheet: University of Texas-Austin, Bureau of Economic Geology Geologic Atlas of Texas, 1 sheet, scale 1:250,000, Donald Clinton Barton memorial edition


Summary:

Oakville Sandstone. Sandstone and clay; sandstone, medium-grained, calcareous, light yellowish gray to light gray, thick-bedded, some cross-bedding, locally contains fossil wood, quartz and chert pebbles, vertebrate fossils, and reworked Cretaceous invertebrate fossils; clay, calcareous, yellowish gray; forms cuesta of smoothly rounded hills. Thickness 200 to 500 feet. Overlies Catahoula Formation (Miocene); underlies Fleming Formation (Miocene). Age is Miocene.
Mapped in De Witt, Karnes, Gonzales, Lavaca, and Fayette Cos., southeastern TX.

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


Map showing publication footprint
  • Usage in publication:
    • Oakville Sandstone
  • Modifications:
    • Areal extent
  • AAPG geologic province:
    • Gulf Coast basin
Publication:

Barnes, V.E. (project director), 1976, Geologic atlas of Texas, Crystal City-Eagle Pass sheet: University of Texas-Austin, Bureau of Economic Geology Geologic Atlas of Texas, 1 sheet, scale 1:250,000, Dolan Hoye Eargle memorial edition


Summary:

Oakville Sandstone. Sandstone and clay; sandstone, medium-grained, calcareous, light yellowish gray to light gray, thick-bedded, some cross-bedding, locally contains fossil wood, quartz and chert gravel, and vertebrate fossils; clay, calcareous, yellowish gray. [Thickness not stated.] Lies above Catahoula Formation and below Fleming Formation. Age is Miocene.
Not separately mapped. Mapped with Fleming Formation [in Duval, Live Oak, Bee, and Karnes Cos., southern TX].

Source: Publication.


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