Vote for your favorite mineral in #MinCup26! - Quartz vs. Asagiite
It's a classic vs a newbie as the most common named mineral in the crust Quartz is up against an exceedingly-rare sea foam-green mineral discovered just a few years ago Asagiite.
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Casca Zinc Prospect, Black Mining District, Southeast Fairbanks Census Area, Alaska, USAi
Regional Level Types
Casca Zinc ProspectProspect
Black Mining DistrictMining District
Southeast Fairbanks Census AreaCensus Area
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
65° 19' 19'' North , 141° 4' 44'' West
Latitude & Longitude (decimal):
Köppen climate type:
Mindat Locality ID:
196828
Long-form identifier:
mindat:1:2:196828:9
GUID (UUID V4):
0


This property lies on Doyon, Limited selected or conveyed land. For more information, contact Doyon, Limited. This site is within the Yukon-Charley Rivers National Preserve.
Location: The Casca Zinc prospect is at about 2,600 feet elevation, approximately 1/3 mile southwest of Tindir Creek, in the NE1/4 section 26, T. 6 N., R. 32 E., of the Fairbanks Meridian. This prospect is on land selected by or conveyed to Doyon, Limited. The location is accurate.
Geology: The mineralization at Casca Zinc prospect is hosted by limestone of the Lower Cambrian Funnel Creek Formation (Brabb and Churkin, 1969). The deposits consists of fracture and open-space fillings that locally contain specular hematite, barite, and sphalerite. The sphalerite is typically massive, very fine grained, and compact, but is also found disseminated throughout the limestone (DiMarchi and others, 1993). Alteration consists mainly of silicification of fossiliferous limestone, but iron oxides and specular hematite can be locally abundant. Most of the iron oxide, alteration, and sulfide mineralization is confined to fault and fracture zones. Soil sampling programs starting in the mid-1970s have outlined areas of anomalous zinc and lead. Rock samples from Casca Zinc prospect yield as much as 18.9 percent Zn (DiMarchi and others, 1993).
Workings: Several soil and rock sampling programs have been carried out on the property, beginning in the mid-1970s. In 1993, a detailed mapping program was completed by ASA Inc. This property lies on Doyon, Limited selected or conveyed land.
Age: Early Cambrian or younger, based on the age of the host rocks.
Alteration: Iron oxide, sulfides, and silicification occur mainly along fault and fracture zones (DiMarchi and others, 1993).

Commodities (Major) - Pb, Zn; (Minor) - Ba
Development Status: None
Deposit Model: Carbonate-hosted Zn-Pb; Appalachian Zn (Schmidt, 1997; Cox and Singer, 1986; m

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
Galena2.CD.10PbS
Group 4 - Oxides and Hydroxides
Hematite4.CB.05Fe2O3
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
Baryte7.AD.35BaSO4

List of minerals for each chemical element

OOxygen
O BaryteBaSO4
O HematiteFe2O3
SSulfur
S BaryteBaSO4
S GalenaPbS
S SphaleriteZnS
FeIron
Fe HematiteFe2O3
ZnZinc
Zn SphaleriteZnS
BaBarium
Ba BaryteBaSO4
PbLead
Pb GalenaPbS

Other Databases

Link to USGS - Alaska:CY005

Other Regions, Features and Areas containing this locality


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