Regional Metamorphic Isograds
Have you ever wanted to traverse the regional metamorphic isograds, from biotite up throughsillimanite gradeand beyond? Well, a drive from Loveland up to Estes Park offers that opportunity. Prof. Bill Braddock and his students at the University of Colorado mapped the different metamorphic zones in pelitic rocks in this part of the northern Front Range. The map below starts in low-grade, greenschist facies (pink) on the east and advances through the garnet zone (blue), staurolite zone (orange), and into thesillimanite zone (green), before crossing into the microcline zone near the granitic batholith.