Roof Pendants Sierra Nevada

Paleozoic metasedimentary rocks are present in numerous roof pendants and wall rock septa in the eastern sierra nevada of east central california.

Roof pendants sierra nevada.

As the roof rocks were intruded by the granite heat from the intrusions metamorphosed the overlying rocks. They are generally various types of sedimentary rocks metamorphosed from contact metamorphism high temp due to magma chambers in close proximity. It lies midway between mono lake on the north and bishop california on the south. There are other roof pendants in the sierra nevada including several on the sierra national forest.

One of these features is in the form of what are known as roof pendants. These older rocks that are intruded by the granite are called roof pendants because they show the roof of the batholith. Roof pendants span through the central and southern portions of the eastern sierra nevada. The sierra nevada mountain range consists of a vast array of different geologic features.

Yes there are a ton of metamorphic roof pendants all over the east side of the sierra at least as far north as lake tahoe. A classic well documented example of a roof pendant is the strata that comprise mount morrison within the sierra nevada in mono and fresno counties california. Rocks in the major roof pendants of the eastern sierra nevada have been mapped in various degrees of detail to bet ter understand their stratigraphy internal structure and geologic history and. Cretaceous granite intruding cambrian metasedimentary rock sierra nevada range.

In our mapping of the major pendants in this.