Bottle Spring Prospect

The Bottle Spring Prospect is a iron mine located in Gila county, Arizona at an elevation of 6,401 feet.

About the MRDS Data:

All mine locations were obtained from the USGS Mineral Resources Data System. The locations and other information in this database have not been verified for accuracy. It should be assumed that all mines are on private property.

Mine Info

Name: Bottle Spring Prospect  

State:  Arizona

County:  Gila

Elevation: 6,401 Feet (1,951 Meters)

Commodity: Iron

Lat, Long: 34.17611, -110.82639

Map: View on Google Maps

Satelite View

MRDS mine locations are often very general, and in some cases are incorrect. Some mine remains have been covered or removed by modern industrial activity or by development of things like housing. The satellite view offers a quick glimpse as to whether the MRDS location corresponds to visible mine remains.


Satelite image of the Bottle Spring Prospect

Bottle Spring Prospect MRDS details

Site Name

Primary: Bottle Spring Prospect


Commodity

Primary: Iron


Location

State: Arizona
County: Gila


Land Status

Not available


Holdings

Not available


Workings

Not available


Ownership

Not available


Production

Not available


Deposit

Record Type: Site
Operation Category: Occurrence
Deposit Type: Replacement
Operation Type: Unknown
Years of Production:
Organization:
Significant: N
Deposit Size: S


Physiography

Not available


Mineral Deposit Model

Not available


Orebody

Form: IRREGULAR


Structure

Not available


Alterations

Not available


Rocks

Name: Diabase
Role: Associated
Age Type: Associated Rock
Age Young: Neoproterozoic

Name: Diabase
Role: Associated
Age Type: Host Rock
Age Young: Neoproterozoic


Analytical Data

Analytical Data: 0.34 % PHOSPHORUS, 0.10 % SULFUR, AND 21.0 % SILICA
Analytical Data: A CHARACTER SAMPLE CONTAINED 51.8 % IRON, 0.1 % MN, 0.4 % TITANIA


Materials

Ore: Hematite


Comments

Comment (Production): NO PRODUCTION AS OF 1961

Comment (Workings): PROPERTY HAS BEEN DEVELOPED BY A FEW SHALLOW OPEN PITS AND CUTS

Comment (Geology): THE DEPOSIT SHOULD BE CONSIDERED PART OF THE HEMATITE MINERALIZATION OF A GREAT AREA OF THE PRE CAMBRIAN, MESCAL LIMESTONE BY CONTACT-METAMORPHIC PROCESSES ASSOCIATED WITH WIDESPREAD INVASION BY GREAT DIABASE INTRUSIONS


References

Reference (Deposit): HARRER, C. M.; 1964 ; RECONNAISSANCE OF IRON RESOURCES IN ARIZONA: USBM INFORMATION CIRCULAR 8236 , P. 28


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