Harriman Exit
The first stop on this field trip is an exit off of I-80 that comes about 13 miles before Vedauwoo. It is Exit 342 and it is approximately 18 miles from our home. There is a quarry at this exit where the “Miocene Ogallala Formation, gently laps onto Precambrian granite” (Lageson 41). This location is important because a lot of mining takes place here. The quarries dig into the 1.4 billion-year-old Sherman granite. This granite is able to be used to make ballast. Ballast is a crushed aggregate that railroads use for “weighting and holding rail ties in place” (Lageson 41). The pictures below were taken from a distance because the quarry was blocked off so the camera zoom was relied upon. Unfortunately, we were unable to get a closer look.
Langeson, David R, Spearing, Darwin R. Roadside Geology of Wyoming. Mountain Press Publishing Company: Missoula. 1988.
No comments:
Post a Comment