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Title
Leffingwell Landing Cambria
Artist
Barbara Snyder
Medium
Photograph - Photographs
Description
Also available as a Digital Painting under the same title in our FASGallery.com gallery.
Cambria is built on the Cambria Slab, a 5,000 ft. thick late-Cretaceous sandstone in a rather enigmatic geologic setting, completely surrounded by Franciscan Formation rocks, mostly melange. The Cambria Slab extends from Villa Creek in Estero Bluffs State Park to San Simeon Creek, holding up the high coastal ridge between Cayucos and San Simeon State Park. The sandstones are massively bedded. Bedding is only occasionally visible, as at the Leffingwell Landing bridge on Moonstone Beach. Compositionally, they are a feldspathic graywacke. The rocks in places are distorted and sheared (for example, below the high bluff at the north end of Moonstone Beach), and in a few areas injected by Franciscan melanges and serpentinites (as on the beach below the high bluff at the north end of the Bluff Trail in the Fiscalini Ranch preserve). The Slab was deposited in an area of active subduction during the plate-tectonic assembly of today's coastal California
Uploaded
August 17th, 2016
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Viewed 331 Times - Last Visitor from Fairfield, CT on 04/23/2024 at 9:27 PM
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