Regional Geologic Setting of Rainbow BasinThe Rainbow Basin is located in the Calico Peaks in the Mojave Desert. The nature of the Mojave extension consists of sediments that were folded within the Barstow Syncline. The Basin is 8 miles to the north of Barstow where "Mud Hills" can be seen -- so-called because of the clay in the rock. Fossils are plentiful in the region, the remnants of life from the Miocene, along with plant remains, suggesting that the region was a coastal region in the past. The Basin itself gets its name from the colorful rocks -- whites, reds, greens, browns -- that come from the mineral deposits therein. Mudstone and sandstone make up most of the rock formations. The green coloring comes from the clay, while the white coloring is the effect of ash from volcanic activity on the Calico fault, which moves like the San Andreas fault. Its composition is rhyolitic.
The Garlock fault lies to the north of the Rainbow Basin. The San Andreas fault is to the southwest. The Basin is characterized by a badland type of topography. Extensive batholiths can be found beneath the sedimentary rock in the Basin, consisting of Cretaceous quartz monzonite layer (U.S. Department...
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