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.

This fold is bounded on the east and west by faults. Most minor folds in this roof pendant however are steeply plunging and related to apparent lateral movement along faults. Rocks of the mount morrison roof pendant. These rocks developed along the passive western continental margin of north america during the middle devonian.

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. 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. 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.

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. The tight folds range in amplitude from a few inches to several tens of feet. In the mount morrison pendant structures produced during the morrison orogeny apparently were later refolded twice prior to sinistral displacement on the laurel convict fault which cross cuts. Morrison s summit pendant a lower paleozoic roof pendant usgs professional paper 1145 is composed of dolomite and marble basically metamorphosed limestone.

Type section locality area and or origin of name. Mount morrison consists of a roof pendant that underlies an area of 62 km 2 24 sq mi.