The Montana-Yellowstone Geologic Field Guide Database
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Integrating Research and Education > Montana-Yellowstone Geologic Field Guide Database > Search the Database > Volcanism and Plutonism at Shallow Crustal Levels: The Elkhorn Mountains Volcanics and the Boulder batholith, southwestern Montana

Volcanism and Plutonism at Shallow Crustal Levels: The Elkhorn Mountains Volcanics and the Boulder Batholith, Southwestern Montana

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Route

Start point

Helena, MT

End point

Butte, MT

Roads

U.S. 287/12, I-15, I-90, U.S. 2, Montana 393; other county, gravel, and Forest Service roads

Total distance

50.5 miles

Geology

Summary

The Upper Cretaceous Elkhorn Mountains Volcanics (EMV) and Boulder batholith of southwestern Montana provide an example of a large-volume, epizonal, volcanic-plutonic complex whose deep level of erosion has exposed the cogenetic intrusive rocks while preserving sizeable portions of the volcanic field. Such a volcanic-plutonic association provides a unique opportunity for evaluation of many aspects of the evolution of a shallow-crustal magmatic system, such as geochemical relations of both the volcanic and plutonic rocks and the nature of intrusive-extrusive relationships at the present level of exposure.

Key Lithologic Features

Structures

Landforms

Other Features


Reference

Rutland, C., Smedes, H.W., Tilling, R.I., and Greenwood, W.R., 1989, Volcanism and plutonism at shallow crustal levels: The Elkhorn Mountains volcanics and the Boulder batholith, southwestern Montana, in Hyndman, D.W., ed., Cordilleran volcanism, plutonism, and magma generation at various crustal levels, Montana and Idaho : 28th International Geological Congress, Field Trip Guidebook T337: Washington, D.C., American Geophysical Union, p. 16-31.

Availability

Order from the American Geophysical Union Bookstore. Go to the AGU On Line Book Catalog for ordering information.