Golden Lily Deposit

The Golden Lily Deposit is a fluorine-fluorite mine located in Dona Ana county, New Mexico at an elevation of 5,121 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: Golden Lily Deposit  

State:  New Mexico

County:  Dona Ana

Elevation: 5,121 Feet (1,561 Meters)

Commodity: Fluorine-Fluorite

Lat, Long: 32.44722, -106.50556

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 Golden Lily Deposit

Golden Lily Deposit MRDS details

Site Name

Primary: Golden Lily Deposit
Secondary: The Deposit Is Shown As the H and H Mine On the Organ Quadrangle


Commodity

Primary: Fluorine-Fluorite
Tertiary: Copper


Location

State: New Mexico
County: Dona Ana
District: Organ Mountains-San Andres Mountains Area


Land Status

Land ownership: Military Reservation
Note: the land ownership field only identifies whether the area the mine is in is generally on public lands like Forest Service or BLM land, or if it is in an area that is generally private property. It does not definitively identify property status, nor does it indicate claim status or whether an area is open to prospecting. Always respect private property.


Holdings

Not available


Workings

Not available


Ownership

Owner Name: H. A. Heuer
Home Office: Las Cruces, N.M.
Years: 1966 -


Production

Not available


Deposit

Record Type: Site
Operation Category: Occurrence
Operation Type: Unknown
Year First Production: 1946
Year Last Production: 1946
Discovery Year: 1946
Discovery Method: Ore-Mineral In Place
Years of Production:
Organization:
Significant: N
Deposit Size: S


Physiography

General Physiographic Area: Intermontane Plateaus
Physiographic Province: Basin And Range Province
Physiographic Section: Mexican Highland


Mineral Deposit Model

Not available


Orebody

Form: IRREGULAR


Structure

Type: L
Description: N-S To N60e Trending Faults And Fractures


Alterations

Not available


Rocks

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

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


Analytical Data

Analytical Data: GRAB SAMPLE NEAR SHAFT CONTAINED 61.2% CAF2
Analytical Data: 6 FT CHIP SAMPLE ON ADIT FACE CONTAINED 41.2% CAF2


Materials

Ore: Fluorite


Comments

Comment (Location): PROSPECT MAY BE REACHED BY TRAVELING 18.8 MI EAST FROM LAS CRUCES ON US 70, AND THEN 1 MI NORTH. PROSPECT IS ON THE WHITE SANDS MISSILE RANGE. ; INFO FROM LAND.ST :(1976)

Comment (Development): PROSPECT CONSISTS OF FOUR CONTIGUOUS UNPATENTED CLAIMS.

Comment (Workings): WORKINGS CONSIST OF TWO ADITS, ONE 75 FT IN LENGTH, THE OTHER 390 FT IN LENGTH, AND A 15 FT DEEP EXPLORATORY PIT.

Comment (Geology): PRECAMBRIAN GRANITE TRAVERSED BY DIORITE DIKES AND PEGMATITES CONSTITUTES THE HOST ROCK. AND IRON-STAINED VEIN CONTAINING COPPER MINERALS FOLLOWS ONE OF THE DIKES. A 75 FT LONG ADIT BRIEFLY EXPLORED THE VEIN ABOUT 100 FT ABOVE A GULCH. A MINOR AMOUNT OF FLUORSPAR OCCURS IN SMALL STRINGERS IN FRACTURES EXPOSED BY THE ADIT. MANY COMPLEX FAULTS CUT THE GRANITE. ONE GROUP TRENDS N60E, WHILE ANOTHER GROUP TRENDS NORTH. FLUORSPAR OCCURS IN THESE FAULTS AS DENSE FISSURE-FILLING VEINLETS AND AS GRANULAR CEMENTING MATERIAL FOR FAULT BRECCIA FRAGMENTS. THE FLUORITE IS WHITE TO PALE GREEN AND SHOWS CUBIC CRYSTALLINE FORM LOCALLY. A 390 FT ADIT DRIVEN 20 FT ABOVE THE GULCH INTERSECTED A 6 FT WIDE BRECCIA ZONE CONTAINING FLUORSPAR FINELY DISSEMINATED WITH APLITE BRECCIA FRAGMENTS.


References

Reference (Deposit): WILLIAMS, FE, 1966, USBM 8307, P. 23-24

Reference (Production): WILLIAMS, FE, 1966, P. 23.


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