Mount Morrison Roof Pendant

Metasedimentary rocks of the mount morrison roof pendant just south of long valley caldera gave 87 sr 86 sr values that range from 0 7090 to 0 7250 goff et al 1991.

Mount morrison roof pendant.

The tight folds range in amplitude from a few inches to several tens of feet. Type area is along john muir trail between mount morrison roof pendant and wheeler crest and pine creek septa on east and potter pass septum on west sierra nevada ca bateman 1992. 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 of the mount morrison roof pendant.

The age is pre cambrian making it some of the oldest rock in the sierra. 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. 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. Numerous metavolcanic rocks from the ritter range pendant gave 87 sr 86 sr values that range from 0 7053 to 0 7264 most of them 0 709 kistler and swanson 1981.

This fold is bounded on the east and west by faults. Type section locality area and or origin of name. These rocks developed along the passive western continental margin of north america during the middle devonian. Morrison s summit pendant a lower paleozoic roof pendant usgs professional paper 1145 is composed of dolomite and marble basically metamorphosed limestone.

These rocks developed along the passive western continental margin of north america during the middle devonian. It lies midway between mono lake on the north and bishop california on the south.