The rock formations at Vasquez Rocks Natural Area Park were formed by rapid erosion during uplift about 25 million years ago and later exposed by activity along the San Andreas Fault. The iconic “hogback” ridges of steeply inclined strata are a geographical demonstration of the significant fault activity in the area.
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Aperture: ƒ/8 Camera: ILCE-7RM2 Taken: 24 December, 2016 Exposure bias: -1EV Flash fired: no Focal length: 28mm ISO: 50 Shutter speed: 1s
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EXIF Data Below Applies Only To The Featured Photo In This Post
