Pg. 224, 228. Tentatively called Alamo formation. Overlies with slight unconformity Neroly formation. Underlies Orinda formation. Contains abundant poorly preserved leaf impressions of typical San Pablo species. Age is Pliocene. [Mentioned in abstract by Huey, 1937 (GSA Proc. 1936, p. 335) where correlated with shaly facies of upper part of Neroly formation.]
Occurs in vicinity of Mount Diablo Country Club on southwest side of Mount Diablo, [Diablo 7.5-min quadrangle], Contra Costa Co., northern CA.
Source: US geologic names lexicon (USGS Bull. 1200, p. 36); GNU records (USGS DDS-6; Menlo GNULEX).
Pg. 213. †Alamo formation (of early Pliocene age) as used by B.L. Clark [abs.], 1940 (GSA Bull, v. 51, no. 12, pt. 2, p. 1957) abandoned. Name preoccupied. Unit here is renamed Diablo formation for exposures near Diablo Post Office. Well preserved early Pliocene flora occur in brown semi-cherty mudstone near base of this unit.
[B.L. Clark concurs; see p. 585, chart 11, IN C.E. Weaver and others, 1944, GSA Bull., v. 55, no. 5.]
Source: US geologic names lexicon (USGS Bull. 1200, p. 36); GNU records (USGS DDS-6; Menlo GNULEX).
†Alamo formation abandoned; formation renamed Diablo.
Source: US geologic names lexicon (USGS Bull. 1200, p. 36).
Pg. 76. Alamo formation. Mentioned as 1,000 feet of marine beds deposited above Neroly beds during [early] Pliocene.
Source: US geologic names lexicon (USGS Bull. 1200, p. 36).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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