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Ray, Mineral Creek District (Ray District), Dripping Spring Mts, Pinal Co., Arizona, USA

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Latitude & Longitude (WGS84): 33° 11' 0'' North , 110° 59' 51'' West
Latitude & Longitude (decimal): 33.18339,-110.99761
Other regions containing this locality:Sonoran Desert, North America
Köppen climate type:Csa : Hot-summer Mediterranean climate


The town of Ray was subhumed by the Ray Mine of ASARCO. It was located at what is now the N end of the Ray Mine. Prior to its demise, the then owner of the mine, Kennicott Copper, built the nearby town of Kearny to move everyone who was displaced into a nice, sterile, company designed town. Since Ray no longer exists, its continued use is for historical purposes only.


Mineral List


14 valid minerals.

Regional Geology

This geological map and associated information on rock units at or nearby to the coordinates given for this locality is based on relatively small scale geological maps provided by various national Geological Surveys. This does not necessarily represent the complete geology at this locality but it gives a background for the region in which it is found.

Click on geological units on the map for more information. Click here to view full-screen map on Macrostrat.org

Quaternary - Miocene
0 - 23.03 Ma



ID: 3185380
Cenozoic sedimentary rocks

Age: Cenozoic (0 - 23.03 Ma)

Lithology: Sedimentary rocks

Reference: Chorlton, L.B. Generalized geology of the world: bedrock domains and major faults in GIS format: a small-scale world geology map with an extended geological attribute database. doi: 10.4095/223767. Geological Survey of Canada, Open File 5529. [154]

Statherian
1600 - 1800 Ma



ID: 2853721
Early Proterozoic metasedimentary rocks

Age: Statherian (1600 - 1800 Ma)

Stratigraphic Name: Pinal Schist; Yavapai Supergroup; Tonto Basin Supergroup; Vishnu Schist

Description: Metasedimentary rocks, mostly derived from sandstone and shale, with minor conglomerate and carbonate rock. Includes quartz-rich, mostly nonvolcanic Pinal Schist in southeastern Arizona and variably volcanic-lithic sedimentary rocks in the Yavapai and Tonto Basin supergroups in central Arizona. (1600-1800 Ma)

Lithology: Major:{metasedimentary,schist}, Minor:{conglomerate,carbonate,sedimentary}

Reference: Horton, J.D., C.A. San Juan, and D.B. Stoeser. The State Geologic Map Compilation (SGMC) geodatabase of the conterminous United States. doi: 10.3133/ds1052. U.S. Geological Survey Data Series 1052. [133]

Data and map coding provided by Macrostrat.org, used under Creative Commons Attribution 4.0 License



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