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Neither in the quarried rock nor in the exposures along the stream nor in the pebbled of its bed were any fossils observed.
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In passing along the line of the narrow guage[sp?] railway from San Luis Obispo to Point Harford much the same series of rocks as those just described were observed. Toward the sea the sandstones and slaty rocks appear and are more or less contorted and crushed. Inland the schists predominate