Roof Pendant Rock

The metamorphic rock composing the mount morrison roof pendant block is the relict of a paleozoic sedimentary sequence overprinted by several deformation events which left the rocks isolated atop the sierra nevada batholith.

Roof pendant rock.

In lay terminology sometimes rock hat is used. The presence of roof pendants indicates that the igneous body is being observed near its upper surface. In roof pendant metamorphosed through the processes of contact metamorphism during which heat and fluids from the intrusion have reconstituted the enclosed rock. The dinkey creek roof pendant includes schist quartzite hornfelds calc silicate rocks and marble.

Roof pendants can be. Roof pendant downward extension of the surrounding rock that protrudes into the upper surface of an igneous intrusive body. Cretaceous granite intruding cambrian metasedimentary rock sierra nevada range. The intrusions that most commonly contain roof pendants are relatively shallow stocks or batholiths.

These rocks are thought to have been originally deposited sometime between the paleozoic visit link and the cretaceous period visit link of the mesozoic visit link in a shallow marine area. These older rocks that are intruded by the granite are called roof pendants because they show the roof of the batholith. These rocks developed along the passive western continental margin of north america during the middle devonian.