Triangles: 500k
Vertices: 253.7k
More model informationComplexly deformed, thin-bedded chert from the Miocene Monterey Formation, Lompoc Landing, Santa Barbara County. Black layers are quartz-phase chert and white are opal-CT. Folding occurs by brittle fracturing of thin chert laminations into fragments that are free to translate and rotate an a flexible manner contributing to an overall fold. https://www.researchgate.net/profile/Richard-Behl/publication/285379806_The_origin_of_chert_in_the_Monterey_Formation_of_California_USA/links/5669a37908aea0892c49b094/The-origin-of-chert-in-the-Monterey-Formation-of-California-USA.pdf
Photography by Anthony Temprano | 3D Modeling by Sara Olson
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