One of the most striking features in the Sierra Nevada is a sinuous set of flat-topped ridges in the Stanislaus River watershed. About 28 km (18 miles) long, these mesas rise above a generally flat and featureless plain. Table Mountain in the Stanislaus River watershed. Table Mountain starting from the upper-left corner of the image, passing by New Melones Reservoir, and ending at the bottom-right corner. The peculiar shape of these ridges is due to their geologic origin. About 10 million years ago, lava erupted from a vent near the crest of the Sierra Nevada and poured down a river bed. As the lava cooled, it assumed the shape of the river. Over time, the material surrounding the hardened lava eroded away, leaving behind the imprint of the river. A report by J.D. Whitney, published in 1865, was the first to describe the formation of Table Mountain. In this report, Whitney included a cross-section of Table Mountain, at the Buckeye Tunnel Mine, that has since been reproduced in numero