Pico del Caballo southern ridge is Tajo de los Machos, 3088m. At the middle of the two ridges starts the river Rio Lanjaron, 400 m lower. Rio Lanjaron flows several km down towards the town of Lanjaron. There is also a few lakes in this wide mountain valley. Pico del Caballo Pico del Caballo, Cerro del Caballo or simply Caballo ("horse") is 3,011 m high mountain in the Sierra Nevada, Spain. It is the westernmost three thousander of the range. Caballo mountain can be accessed from the towns of Lanjaron, Durcal and also from the Sierra Nevada Ski Resort. The Ski Resort is
Caballo Mountains another unconformity. Above that is the Love Ranch Formation of conglomerate, mudstone and sandstone, which was deposited in the Paleocene to early Eocene. During the Eocene, a wave of arc volcanism was felt across southern New Mexico. In the Caballo Mountains, this can be seen in the Palm Park Formation, a thick layer of andesitic or tuffaceous mudstones, sandstones, and breccia. Next is the Bell Top Formation, which consists of rhyolite, basalt flows, and tuffaceous sandstones. In the southern part of the Caballo Mountains, there are remnants of a region wide sheet of flood basalts and andesite, which was laid