Rockies 5 concludes

My Rockies field course has wrapped up for another year – the fifth year in a row I’ve run this intermediate-level ‘regional field geology’ course in collaboration with Pete Berquist of Thomas Nelson Community College. We were fortunate to be joined by two other professional geologists this year: Chris Khourey of NOVA and Tom Biggs … Read more

Paleoproterozoic dikes in Archean granite, Laramie Range, Wyoming

At Morton Pass, where highway 34 crosses the crest of the Laramie Range, you can see a nice set of (younger) mafic dikes cutting (older) granite/gneiss basement complex. The pink stuff is Archean; the black stuff is Paleoproterozoic; around 2 billion years old. Click to enlarge I got to check out this outcrop on Tuesday … Read more

Monday macrobug: Jumping spiders that “Attack the Block”

A few weeks ago, I started seeing a new kind of jumping spider around our house. It was distinctive primarily because of its iridescent green chelicerae (think of them as “jaws”). I took a couple of blurry shots, but nothing I considered good enough for “Monday macrobug” treatment… These spiders reminded me of the unique … Read more

Headin’ west

Well, it’s that time of the year again. Tomorrow morning, I pack up the car and head west. I’m giving myself five days to drive out to Bozeman, Montana, with three stops along the way to see people I like and talk about interesting stuff. Next week, my family flies out to join me. It’ll … Read more

Dwyka Tillite in South Africa

My wonderfully named e-buddy Martin Bentley recently took a field trip to a quarry in South Africa (between Grahamstown and Fort Beaufort) where the Dwyka Formation is exposed: This poorly sorted sedimentary rock (a ‘diamictite’) is usually interpreted as glacial deposits (lithified till, or ’tillite’). Alfred Wegener cited these rocks and accompanying glacial striations (and … Read more

Another example of the perplexing mystery “fossil”

In April, I posted some images of an odd structure from some of the fossiliferous siltstones of the Fort Valley. Some of the commenters suggested it was no fossil, but simply a very small scale version of soft-sediment deformation. Now, another “Fortian” has shown me another example, and this one is better preserved. Its lobes … Read more