Guidebook; Death Valley Region, California and Nevada
Prepared for 70th Annual Meeting of the Cordilleran Section, the Geological Society of America, Field Trip Number 1
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Whilst the greatest effort has been made to ensure the quality of this text, due to the historical nature of this content, in some rare cases there may be minor issues with legibility. The carbonate formations can be followed through the Spring Mountains with little lithologic change: some are cut out by unconformities. Facies changes occur between the Spring Mountains and Frenchman Mountain, but the general characteristics of the formations are maintained. All the car bonate formations that have been studied suggest deposition in shallow marine or marginal marine environments (gans.
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