Vote for your favorite mineral in #MinCup26! - Sphalerite vs. Anorthite
Both zinc ore Sphalerite and calcium plagioclase feldspar Anorthite have perfect cleavage that will split cleanly if you hit them with a hammer, but only one can claim a larger split of your votes!
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Unnamed Occurrence (ARDF - MH317; headwaters of the Chistochina River), Chistochina Mining District, Southeast Fairbanks Census Area, Alaska, USAi
Regional Level Types
Unnamed Occurrence (ARDF - MH317; headwaters of the Chistochina River)- not defined -
Chistochina Mining DistrictMining District
Southeast Fairbanks Census AreaCensus Area
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
63° 8' 43'' North , 144° 29' 23'' West
Latitude & Longitude (decimal):
Köppen climate type:
Mindat Locality ID:
201322
Long-form identifier:
mindat:1:2:201322:3
GUID (UUID V4):
0


Unpublished data cited is available for viewing by contacting Grayd Resources Inc. in Vancouver, B. C., Canada (www.grayd.com), or Northern Associates Inc. in Fairbanks, Alaska.
Location: This occurrence is at an elevation of about 4,400 feet, 8 miles southeast of Mount Kimball. It is on moraine at the foot of an unnamed glacier at the head of the Chistochina River at the northeast corner of section 29 T. 16 N., R. 5 E., Copper River Meridian. This location is accurate.
Geology: During reconnaissance work in 1978, Resource Associates of Alaska, Inc. discovered pyrite-rich float on a glacial moraine (R.A. Blakestad and others, unpublished Resource Associates of Alaska Inc. report, 1978). There is no indication of any follow-up work at this site. The occurrence is 2.5 miles down the glacier from the SM massive sulfide occurrence (MH316). The rocks of the Hayes Glacier unit that hosts this occurrence consist of fine-grained phyllitic schist and mylonite derived from sedimentary and volcanic protoliths. The rocks locally display intense structural deformation due to their proximity to Denali Fault. The basal part of the unit consists of mafic- to intermediate-composition metavolcanic rocks; they are overlain by interbedded felsic metavolcanic rocks and extensive pelitic and graphitic metasedimentary rocks (Dashevsky and others, 2003).
Workings:

Commodities (Major) - Cu, Zn; (Minor) - Pb
Development Status: None
Deposit Model: Kuroko massive sulfide (Cox and Singer, 1986; model

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Commodity List

This is a list of exploitable or exploited mineral commodities recorded at this locality.


Mineral List


4 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
Sphalerite2.CB.05aZnS
Chalcopyrite2.CB.10aCuFeS2
Galena2.CD.10PbS
Pyrite2.EB.05aFeS2

List of minerals for each chemical element

SSulfur
S ChalcopyriteCuFeS2
S GalenaPbS
S PyriteFeS2
S SphaleriteZnS
FeIron
Fe ChalcopyriteCuFeS2
Fe PyriteFeS2
CuCopper
Cu ChalcopyriteCuFeS2
ZnZinc
Zn SphaleriteZnS
PbLead
Pb GalenaPbS

Other Databases

Link to USGS - Alaska:MH317

Other Regions, Features and Areas containing this locality


This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders for access and that you are aware of all safety precautions necessary.

References

 
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