The Warner Range lies in the northeastern corner of California, near the Oregon and Nevada borders (see yellow box in Figure 1). Mt. Shasta sits approximately 100 miles to the west (orange circle in Figure 1) and is visible from the top of the range. The Surprise Valley, adjacent to the steep eastern flank of the range, hosts the town of Cedarville.
Geologically, the Warner Range marks a border between two provinces with very different histories: the Basin and Range to the east and the Modoc Plateau to the west. Because of this unqiue geological setting, we are interested in learning more about the structure of the crust in this area and how that structure has changed through time.
The Stanford project in the Warner Range - Surprise Valley region consists of three major components:
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