Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
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Transcription
Wea. TUES. MAY 18, 1909 Ther.
So much of the Brinowski has shallow depressions from 1 to 2 inches across. I can think these mainly of by crm rippling. After storming away the mantle bed shows lifting by the sources and healing up of lights and dark layers owing to the mantles effect. In those pits was laid down a very fine dolomitic and sand.