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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 my recent research has concentrated on the well-exposed metamorphosed
supracrustal rocks that are part of a large tectonic mélange 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. | |
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Beartooth Mtn. research at LSU |
Beartooth Mtn. resources |
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Metamorphic petrology studies of the eastern Beartooth Mountains
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Geologic
overview of the eastern Beartooth Mountains |
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Darrell Henry
is the Campanile
Charities Professor of Geology and
Geophysics at Louisiana State University whose research specialty is metamorphic
petrology. Further details of his professional background are included in an accompanying
vita or faculty profile. This page was last updated on 04/17/06. |
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