Temescal dacite porphyry of Dudley (1935) is renamed Temescal Wash dacite porphyry. Exposed over wide area few mi southeast of Puente Hills [see Larsen (1948) for distribution]. Is dark-colored rock with plagioclase and quartz phenocrysts and inconspicuous biotite or hornblende. Occurs as rare constituent of conglomerate in Puente Hills.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Temescal dacite porphyry of Dudley (1935) is renamed Temescal Wash quartz latite porphyry since name Temescal was preoccupied and microscopic study and chemical analysis showed rock is quartz latite. Nearly black porphyritic rock forms several large bodies in Corona and Elsinore 30' quads chiefly east of Temescal Wash, Riverside Co, CA; underlies about 21 sq mi. Latite shows dark-gray, rugged, angular outcrops with sharp cliffs and steep, deep stream gorges. Intruded by Estelle tonalite. Is older than Woodson Mountain granodiorite (new) and Bonsall tonalite. Age given as Jurassic(?),
Source: GNU records (USGS DDS-6; Menlo GNULEX).
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