Goat Haven

The Goat Haven is a copper mine located in Snohomish county, Washington at an elevation of 4,800 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: Goat Haven  

State:  Washington

County:  Snohomish

Elevation: 4,800 Feet (1,463 Meters)

Commodity: Copper

Lat, Long: 47.96667, -121.46667

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 Goat Haven

Goat Haven MRDS details

Site Name

Primary: Goat Haven


Commodity

Primary: Copper
Secondary: Molybdenum


Location

State: Washington
County: Snohomish
District: Sultan District


Land Status

Not available


Holdings

Not available


Workings

Not available


Ownership

Not available


Production

Not available


Deposit

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


Physiography

General Physiographic Area: Pacific Mountain System
Physiographic Province: Cascade-Sierra Mountains
Physiographic Section: Northern Cascade Mountains


Mineral Deposit Model

Model Name: Polymetallic veins


Orebody

Form: UNKNOWN


Structure

Not available


Alterations

Not available


Rocks

Not available


Analytical Data

Analytical Data: PB RATIOS GIVEN IN CHURCH AND OTHERS


Materials

Ore: Chalcopyrite
Ore: Molybdenite


Comments

Comment (Location): ACCURACY OF LOCATION IN CHURCH AND OTHERS IS UNKNOWN. UNABLE TO FIND ANY OTHER REFERENCE TO PROPERTY

Comment (Deposit): CHURCH AND OTHERS INDICATE THAT THIS IS A PORPHYRY TYPE DEPOSIT BUT THERE IS TOO LITTLE INFORMATION ABOUT IT FOR INDICATING THAT HERE

Comment (Geology): IF LOCATED CORRECTLY, DEPOSIT APPEARS TO LIE ALONG CONTACT OF INDEX BATHOLITH WITH SWAUK FORMATION SEDIMENTARY ROCKS


References

Reference (Deposit): CHURCH, S.E., LEHURAY, A.P., GRANT, A.R., DELEVAUX, M.H., AND GRAY, J.E., 1986, LEAD-ISOTOPIC DATA FROM SULFIDE MINERALS FROM THE CASCADE RANGE, OREGON AND WASHINGTON: GEOCHIMICA ET COSMOCHIMICA ACTA, V. 50, P. 317-328.

Reference (Deposit): TABOR, R.W., FRIZZELL, V.A., JR., BOOTH, D.B., WHETTEN, J.T., WAITT, R.B., JR., AND ZARTMAN, R.E., 1982, PRELIMINARY GEOLOGIC MAP OF THE SKYKOMISH RIVER 1:100,000 QUADRANGLE, WASHINGTON: U.S. GEOLOGICAL SURVEY OPEN-FILE REPORT 82-747, SCALE 1:100,000.


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