Moore, R.C., 1933, Historical geology: McGraw-Hill Book Co., 673 p.
Pg. 325 (P.B. King credited). Glass Mountains formation. Underlies Bissett conglomerate and overlies Word formation. Divided, in eastern part of Glass Mountains, into (descending) Tessey massive limestone member, Gilliam thin-bedded limestone member, and Vidrio massive limestone member. In western part of Glass Mountains includes, in lower part, Altuda siliceous shale member. Is = Capitan limestone. [See 1931 and 1933 entries under Tessey dolomite.]
Source: US geologic names lexicon (USGS Bull. 896, p. 825).
Pg. 825. †Glass Mountains formation. This name being preoccupied, and the rocks being the southern extension of Capitan limestone (an older and well-established name), the USGS designates these rocks in Glass Mountains the Capitan limestone. (See P.B. King, 1934, GSA Bull., v. 45, p. 697-798).
Source: US geologic names lexicon (USGS Bull. 896, p. 825).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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