BACKGROUND INFORMATION ON THE BEARTOOTH MOUNTAINS
The rocks of the Beartooth Mountains of Montana and Wyoming span 4 billion years of earth history. The geologic features range from the more recent spectacular glaciation of the Beartooth Plateau and the volcanism and thermal activity of the Yellowstone area (south of the Beartooth Mountains) to the ancient crust containing constituents that are over 4 billion years old.
Most of recent research has concentrated on the well-exposed metamorphosed supracrustal rocks that are part of a large tectonic melange caught up in the areally extensive, 2.8 billion year old granitoid plutons of the eastern Beartooth Mountains. One reason that these rocks are particularly significant is that some of the detrital zircons in the quartzites are 4 billion years old. The metamorphosed supracrustal rocks have at least two high grade metamorphic events superimposed on them: (1) an initial granulite facies event accompanied by deformation that was probably no older than 3.2 billion years old and (2) a second upper amphibolite/granulite facies overprint with no deformation that was associated with the thermal effects of the massive granitoid intrusions at 2.8 billion years. These rocks are part of one of oldest pieces of crust in North America and provide many insights into early crustal formation on the Earth.
Summary of the geologic history of the eastern Beartooth Mountains
COMPARISON OF BIOTITE AND AMPHIBOLE CHEMISTRY
IMAGES OF LOCATIONS OF SAMPLES USED FOR THE PET ROCK PROJECT
BEARTOOTH RECONNAISSANCE SAMPLES AND FIELD VIEWS
HELLROARING PLATEAU
QUAD CREEK AND ROCK CREEK