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Geologic Unit: Segovia
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Map showing publication footprint
  • Usage in publication:
    • Segovia Formation
  • Modifications:
    • Original reference
  • Dominant lithology:
    • Limestone
    • Dolomite
  • AAPG geologic province:
    • Kerr basin
    • Permian basin
Publication:

Rose, P.R., 1972, Edwards Group, surface and subsurface, central Texas: University of Texas-Austin, Bureau of Economic Geology Report of Investigations, no. 74, 198 p.


Summary:

Pg. 34-43. Segovia Formation of Edwards Group. Chiefly marly limestone, dolomite, biosparite limestone. Thickness 64 m at type section. Includes Burt Ranch Member, Allen Ranch Breccia Member, informal "Gryphaea bed" [not included in this lexicon], Orr Ranch Bed, and Black Bed. Overlies Fort Terrett Formation of Edwards Group; underlies Del Rio Clay. Age is Early Cretaceous (Comanchean).
Type section: Joy Creek composite section in roadcuts of U.S. Highway I-10 from 8 to 16 km southeast of Segovia, Kimble Co., TX.

Source: US geologic names lexicon (USGS Bull. 1520, p. 275).


Map showing publication footprint
  • Usage in publication:
    • Segovia Member
  • Modifications:
    • Areal extent
  • AAPG geologic province:
    • Kerr basin
    • Permian basin
Publication:

Barnes, V.E. (project director), 1977, Geologic atlas of Texas, Del Rio sheet: University of Texas-Austin, Bureau of Economic Geology Geologic Atlas of Texas, 1 sheet, scale 1:250,000, Robert Thomas Hill memorial edition


Summary:

Is upper member of two of Edwards Limestone (Lower Cretaceous). Is mapped in northernmost part of sheet from Pecos River valley and eastward in Val Verde and Edwards Cos, TX (Permian basin) and Real Co, TX (Kerr basin). Overlies Fort Terrett Member of Edwards. Overlain by Del Rio Clay or Buda Limestone. Map unit described as limestone and dolomite; in upper part--cherty, light-gray, miliolid, shell fragment, rudistid limestone; in middle--dolomite, medium brownish-gray, porous, massive to thin-bedded, cherty, collapse breccia; in lower part--light yellowish-gray miliolid limestone and marl and marly limestone with EXOGYRA TEXANA and oxytropidocerid ammonites; key bed mapped is "Calvert's Zone"; thickness 300-380 ft, thickens southward. Is not mapped south of [what appears to be an arbitrary] east-west line that separates the unit from the Devils River Limestone. In map explanation, is schematically depicted to be equivalent to upper part of Devils River Limestone, upper part of McKnight Formation, Salmon Peak Limestone, upper part of Sue Peaks Formation, and Santa Elena Limestone.

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


Map showing publication footprint
  • Usage in publication:
    • Segovia Member
  • Modifications:
    • Mapped 1:250k
  • AAPG geologic province:
    • Kerr basin
Publication:

Barnes, V.E. (project director), 1982, Geologic atlas of Texas, San Antonio sheet [revision of 1974 ed.]: University of Texas-Austin, Bureau of Economic Geology Geologic Atlas of Texas, 1 sheet, [9 p., revised 1983], scale 1:250,000, Robert Hamilton Cuyler memorial edition


Summary:

Segovia Member of Edwards Limestone. Is upper member of Edwards Limestone. Overlies Fort Terrett Member of Edwards; underlies Del Rio Clay. Age is Early Cretaceous.
Exposed on plateau in northwestern part of map sheet, in Real, Bandera, and Kerr Counties, southern Texas. Not mapped beyond apparent arbitrary limit in southern Real County.

Source: Publication.


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

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