11 November 2010
Microfaults-a-million
Posted by Callan
I got to Pittsburgh around 1:30pm yesterday, which meant I had several free hours before the opening reception for new Fine Fellows. I took a bunch of photos of the exhibits there, but my traveling laptop doesn’t have the image processing software that I usually employ to resize these things, so for now I’ll just share this one. It’s a sandstone from South Dakota, age unknown, which shows beautiful parallel small faults. Viewed from this angle, the top has moved to the right relative to the bottom. I like the little lens-shaped zone in the middle where the strain is more pronounced. Reminds me of something I’ve seen elsewhere. You can click through to make it much bigger.


Callan Bentley is an assistant professor of geology at Northern Virginia Community College in Annandale, Virginia. He is particularly interested in structural geology and the evolution of the Appalachian mountain belt. Callan draws cartoons and writes for EARTH magazine. He lives in the Fort Valley of Virginia.









Steve Stokowski said on 15 November 2010
I think that the rock may be from Calico Canyon, which is near Buffalo Gap, SD. The rock is the Fall River (Dakota) Sandstone, which is Cretaceous.