July 29, 2013
Photographer: Peter Burgess
Summary Author: Peter Burgess
This wonderful spot on the North Devon coast (UK) shows strata of Mid to Upper Carboniferous (Mississippian to Pennsylvanian), deep-water turbidites. They were laid down about 320 million years ago by turbulent flow of sand and mud down into a deep sea basin. The marine basin was formed in front of an advancing mountain belt that was created ultimately by the collision of the African and Eurasian plates -- an event known as the Variscan orogeny. After the strata were deposited, buried and lithified to form rocks, they were caught up in the bulldozing effect of the advancing mountain front and buckled and folded into the fascinating geometries visible on the North Devon coast today. Their presence provides spectacular evidence of plate tectonics in action. The students in the foreground are MSc Petroleum Geoscience students studying at Royal Holloway University of London. Photo taken on May 22, 2013.
Photo details: Camera Maker: SONY; Camera Model: NEX-5; Lens: E 18-55mm F3.5-5.6 OSS; Focal Length: 18mm (35mm equivalent: 27mm); Aperture: f/11.0; Exposure Time: 0.0050 s (1/200); ISO equiv: 200.