The Cowhole Mountains, near Baker, California, are an east-tilted remnant of the Jurassic magmatic arc that extends from western Nevada through southeastern California to Arizona and Sonora, Mexico. In Middle Jurassic time, two northeasterly trending grabens bounded by syndepositional faults accumulated 550 m and 700 m of predominantly eolian sandstone (Aztec Sandstone). Because east dip in one of the grabens increases from 30 degrees at the base of the sandstone section to 65 degrees at its top, we infer that structure to have developed during tilting to the west of east-dipping, listric normal faults. Westward tilting continued to accumulate during extrusion of an overly Middle Jurassic volcanic series (Cowhole volcanics). Felsic volcanic rocks that buried the grabens comprise ignimbrites, volcaniclastic rocks, and flow breccias, emplaced in a proximal but extra-caldera setting. Plutons and sills were intruded at shallow levels, possibly during both graben filling and extrusion of volcanics. Local magmatism of significant volume ended with the intrusion of a dike swarm that may be correlative with the Independence dike swarm (148 Ma). After the range tilted 90 degrees toward the east, small glide blocks and landslides detached from high portions of the eroding range and descended into the southern graben.
Our model suggests that two sets of high-angle normal faults, oriented nearly at right angles to each other, were active during the same Middle Jurassic interval. A modern analogue may be provided by the Central American arc graben, in which similar transtensional structures have developed perpendicular to the regional graben where it is intersected obliquely by the Chiapas shear zone.