By: magic-gigapans
Image: ahochstaedter ⧉
License: Copyright, All Rights Reserved

Uploaded: 10 Jul 2020
Last Updated: 10 Jul 2020

516 megapixels
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The Paleocene Carmelo conglomerate lies unconformably over the ~100 MA granodiorite of the Monterey Peninsula. A felsic diike intrudes the granodiorite, but does not intrude into the Carmelo conglomerate. Overlying both the granodiorite and the Carmelo conglomerate are marine terrace deposits, on which a soil has started to develop. This is a seacliff exposre in Pt Lobos State Natural Reserve.