Proterozoic evolution of the western margin of the Wyoming craton: implications for the tectonic and magmatic evolution of the northern Rocky Mountains

Overview of attention for article published in Canadian Journal of Earth Sciences, October 2006

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The geology of the Rocky Mountains is that of a discontinuous series of mountain ranges with distinct geological origins.

The Grouse Creek block is a block of 2.5 to 2.6 billion year old orthogneisses (a type of gneiss) and similar metasedimentary rocks.

The Geology of Idaho is complex, with outcroppings of differing ages of volcanics, undifferentiated metamorphics and sedimentary structures.

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