Abstract

The basaltic field, localized in an area of structural intersections, south of Big Pine, California contains a single mass of rhyolite, shown by form and internal structure to have been erupted in place. Remelting of the first-congealed obsidian, exsolution of gases, and the resulting gas-inflation of the lava, were important factors in determining the form of the rhyolite.

This content is PDF only. Please click on the PDF icon to access.

First Page Preview

First page PDF preview
You do not currently have access to this article.