Filed under: archean, folds, Friday Fold, metamorphism, montana, structure | 4 Comments »
Fine faulting
Check it out: In the canyon of the Jefferson River, Montana, you can find yourself some limestone (Mississippian Madison Group, I think of the Lodgepole Formation) that has seen a wee bit of faulting: And here’s an annotated copy… Both of these images are enlargeable by clicking through (twice): Note the quarter for scale: this [...]
Filed under: faults, limestone, mississippian (carboniferous), montana, structure | 3 Comments »
Friday fold: tight syncline in Montana
This fold is located on Highway 287, north of Wolf Creek, Montana. Annotated version: As with last week’s Friday Fold, this fold owes its existence to (a) deposition of sandstone and shale in the Western Interior Seaway, and (b) deformation under a giant thrust sheet during the thin-skinned compressional tectonics of the Sevier Orogeny. In [...]
Filed under: cretaceous, folds, Friday Fold, montana, structure | Comments Off
Friday fold: Cretaceous sandstone
Happy Friday, everyone!
Filed under: cretaceous, folds, Friday Fold, montana, paleogene, structure | 6 Comments »
Jointed Virgelle
One of the stops my Rockies students and I made this summer was a dinosaur paleontology tour through the Two Medicine Dinosaur Center in Bynum, Montana. The folks there are very accommodating, and at my request gave the class a bit of stratigraphic context for the dinosaur fossils. For instance, we visited the geologic formation [...]
Filed under: asia, cretaceous, geology, himalayas, joints, mongolia, montana, north america, rockies, russia, sandstone, structure | Comments Off
Rocks of Glacier National Park
This is the second of my Rockies course student projects that I wanted to share here on the blog: it is a guest post by Filip Goc. Enjoy! -CB —————————————————————————– The Rocks around Glacier National Park, Montana: Introduction to the formations The geology around Glacier National Park is great for beginners because the area is [...]
Filed under: art, faults, folds, mesoproterozoic, montana, national parks, primary structures, proterozoic, sediment, stromatolites, structure | Comments Off
Volcanic features of the Rockies trip
This weekend, I wanted to share some of the best work from this year’s Rockies field course students. Let’s start with a nice video by Marcelo Arispe: I thought this was a really nice job making a video using still images and a voiceover. The only thing I would change would be in the Gallatin [...]
Filed under: montana, teaching | 2 Comments »
In which I am eaten by a stromatolitic Pac-Man
Let this be a lesson to you, kids. Don’t get too close to wild stromatolites, even if they are Mesoproterozoic… These exceptionally large stromatolites are on the threshold of the Grinnell Glacier, in Glacier National Park, Montana. No stromatolites or geologists were harmed during the production of this blog post. Photos by NOVA Rockies student [...]
Filed under: mesoproterozoic, montana, national parks, stromatolites | 2 Comments »
The routine
It’s that time of year for me… summer’s here, and I’m winding up my duties at NOVA in preparation for some travels. We leave Sunday night for two weeks in Turkey, followed by my regional field geology course in Montana (also two weeks), followed by some family time and mountain climbing in New Hampshire (three [...]
Filed under: dc, lola, montana, new hampshire, travel, turkey | 3 Comments »
The LaHood Conglomerate
The Belt Supergroup is a series of sedimentary strata laid down in the Belt Sea, an inland sea (like modern Hudson Bay) that existed in the northwestern (by present coordinates) part of ancestral North America during the Mesoproterozoic era of geologic time. Estimates of the absolute age of these rocks range from 1470 to 1400 [...]
Filed under: mesoproterozoic, montana, rockies, sediment | 2 Comments »

