My week

This week is “Wyoming Energy Resources field trip” week! Day Start End Destination August 1st Sheridan, WY Lander, WY Gas Hills Uranium District August 2nd Lander, WY Lander, WY Green River Basin Oil Shale and South Pass/ Atlantic City Mining District August 3rd Lander, WY Newcastle, WY Smith Ranch-Highland Uranium ISR Mine and Mill near … Read more

Commonality contest

Here’s a contest for you: tell me what all the following items have in common. Though there are several sub-themes (readily apparent), I’m looking for the one overriding commonality for all the following 105 items: Hi-Lo Inferno The Good Life Country Squire Wildcat Wilderness Challenger Flair Catalina Sport Alpine Coach Designer Carriage Maxum Wildlife Artic … Read more

A faulted chert nodule

Here is a trio of concentrically-zoned chert nodules in Mississippian Castle Reef Dolostone, exposed at Sun River Canyon, Montana, just downstream from the roadside outcrop of the French Thrust: If you look closely at the lowermost of the three chert nodules, you’ll see it’s been split and offset by a small fault. Here are close-up … Read more

Friday fold: Pete’s purty pet

That’s my Rockies co-instructor Pete Berquist, in the regulation uniform of an orange down vest, holding a subtly-folded slab of sandstone (it’s a very slight “S”), rescued from amid the shaley wastes of the Blackleaf Formation, the Cretaceous aged sedimentary rocks beneath the Lewis Thrust on the Blackfoot Reservation, just east of Glacier National Park. … Read more

Friday fauxld: liesegang banding at Giant City

Today, the Friday fold is a fake! Looks like a nice set of asymmetric antiforms and synforms, right? But it ain’t! It’s naturally wiggly; primary not tectonic. The photo shows nothing more than differential erosion of hematite that was deposited by groundwater in permeable sandstone. It’s Liesegang banding! These hematite blobs are in the sandstone … Read more

Stylolites in Mississippian limestone

Stylolites (pressure solution seams) in limestone of Mississippian age, exposed on the side of a rounded boulder in Hyalite Canyon, Gallatin Range, Montana. These stylolites, like most, are bedding-parallel, and thus most likely formed due to the weight of the overlying rock. Calcite, the dominant mineral, goes into solution under pressure, and insoluble material, like … Read more

Cascade Canyon

Following up on Friday’s fold, I wanted to share a few other images from our hike last week in Cascade Canyon of Grand Teton National Park.  Lots of cool exposures of Archean basement rock there. Folds in gneissic banding: Big, angular mafic blocks in a felsic soup: Swarm of granite dikes on a mountainside: Asymmetric … Read more

Friday fold: west Bighorn monocline

While out in the field with Butch Dooley last week, making major discoveries like I do, I was very impressed with the landscape-scale west Bighorn monocline, which takes formerly horizontal Madison limestone and skews it to a westward dip where the mountains end and the intermontane basin begins. It’s totally sweet. Check it out in photo form and gigapan, too.

Block Mountain basalt flow

This year, for the first time ever, I took students to map at Block Mountain, a classic field camp mapping site near Dillon, Montana. Here’s a quick look (enlarge it by a gazillion-fold by clicking through) of some columnar jointing in the Eocene Block Mountain basalt flow, a paleo-drainage turned mountain through the miracle of … Read more