Ray Mine, Scott Mountain area, Mineral Creek District (Ray District), Dripping Spring Mts, Pinal Co., Arizona, USA
|Latitude & Longitude (WGS84):||33° 10' 39'' North , 110° 56' 45'' West|
|Latitude & Longitude (decimal):||33.17750,-110.94583|
|Other regions containing this locality:||Sonoran Desert, North America|
|Köppen climate type:||Csa : Hot-summer Mediterranean climate|
A Cu-Ag-Au-Mo-Pb-Zn mine located in all of sec. 10, T3S, R13E (Sonora 7.5 minute topo map), about 2¾ miles SSW of Scott Mountain, about 3¾ miles S of Hot Tamale Peak, and about 4 miles NNW of Kelvin. Discovered 1846. First produced 1911. NOTE: This mine, named after the mining town of Ray, subhumed that town (which no longer exists). Residents were moved to the new mining company built town of Kearny; however, Kelvin is the nearest municipality to the mine.
Mineralisation is a porphyry copper deposit hosted in Pinal Schist, Granite Mountain Porphyry, Pioneer Shale of the Apache group, and Dripping Spring Quartzite. Ore control was the intersection of NW and NE fault zones, permeability & type of host rock. Ore concentration was secondary enrichment. Alteration is sericitic, propylitic, biotite-clay, chloritisation, and epidote. Area structures include the Broken Hill fault, West End fault, North End fault and numerous others, mostly normal.
Mineral ListMineral list contains entries from the region specified including sub-localities
54 valid minerals.
Rock Types Recorded
Rock list contains entries from the region specified including sub-localities
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Entries shown in red are rocks recorded for this region.
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
|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. 
|Serpukhovian - Early Cambrian|
323.2 - 541 Ma
|Mississippian, Devonian, and Cambrian sedimentary rocks|
Age: Paleozoic (323.2 - 541 Ma)
Description: Brown to dark gray sandstone grades upward into green and gray shale, overlain by light to medium gray or tan limestone and dolostone. This unit includes the Tapeats Sandstone, Bright Angel Shale, Muav Limestone, Temple Butte Formation and Redwall Limestone in northern Arizona, and the Bolsa Quartzite, Abrigo Formation, Martin Formation, and Escabrosa Limestone in southern Arizona. These rocks record intermittent sea-level rise and inundation in early Paleozoic time. (330-540 Ma)
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.