Tuerto Formation
The Tuerto Formation is a geologic formation exposed around the Ortiz Mountains of New Mexico. It is estimated to be of Pliocene to Pleistocene age, and forms the gravel cap of the Ortiz surface, one of the first pediment surfaces recognized by geologists.
Description
The Tuerto Formation consists primarily of conglomerate with minor sandstone. The clasts making up the conglomerate consist largely of hornfels and Ortiz porphyry eroded off the Ortiz Mountains and Cerrillos Hills and deposited as a thin alluvial fan in the Hagan basin. Beds containing limestone clasts eroded off the east slopes of the Sandia Mountains are sometimes also included in the formation. The formation is informally divided into a lower well-cemented cliff-forming member and an upper poorly cemented member.The formation lies with angular unconformity on the Blackshare Formation. It is distinguished from the coeval Ancha Formation in containing mostly volcanic clasts, while the Ancha Formation is rich in granite clasts.
The unit underlies the Ortiz surface, one of the first pediment surfaces recognized, by I.H. Ogilvie in 1905.