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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Unnamed Occurrence (ARDF - MM088; East Fork of Glen Creek), Kantishna Mining District, Denali Borough, Alaska, USAi
Regional Level Types
Unnamed Occurrence (ARDF - MM088; East Fork of Glen Creek)- not defined -
Kantishna Mining DistrictMining District
Denali BoroughBorough
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
63° 33' 23'' North , 150° 44' 34'' West
Latitude & Longitude (decimal):
Köppen climate type:
Mindat Locality ID:
201356
Long-form identifier:
mindat:1:2:201356:8
GUID (UUID V4):
0


The boulder deposits and their presumed bedrock source are in Denali National Park and Preserve.
Location: This is an inferred location for a proximate bedrock source of rhodonite boulders that have long been known to occur in Glen Creek (MM108). The location of the boulders is in the East Fork of Glen Creek about a half-mile above its confluence with the West Fork. It is somewhat upstream of occurrence 76 of Thornsberry, McKee, and Salisbury (1984), cited as a rhodonite boulder locality, but seems to agree more closely with their text description of the locality.
Geology: Manganiferous boulders have long been known in Glen Creek. The boulders contain rhodonite and rhodochrosite, and are stained with a black oxide, probably pyrolusite. An early-reported location of the boulders is on socalled Claim No. 9, where black-stained pebbles and small boulders of rhodonite accompanied placer gold and galena (Capps, 1919, p. 84). It is not certain whether this claim is in the East Fork or in Glen Creek below the junction of the two forks. Rhodonite on Glen Creek was also reported by Wells (1933, p. 355-356; p. 372); and Bundtzen, Smith, and Tosdal (1976, p. 9) reported that some of the rhodonite in Glen Creek is of gem quality. The country rock near the boulder locality consists partly of marble of the Spruce Creek sequence, a possible host for replacement(?) deposits of manganese minerals.
Workings: The manganiferous boulders may have been discovered in 1916, when they were reported in sluice box concentrate on Claim No. 9 (Capps, 1919). They were also noted in 1931 (Wells, 1933), and in recent mining operations (Bundtzen, Smith, and Tosdal, 1976; Thornsberry, McKee, and Salisbury, 1984).
Age: The boulder deposit is Holocene.
Alteration: Oxidation of manganese mineral.
Production: Small amounts of the rhodonite have probably been sold as gem material.

Commodities (Major) - Rhodonite (as a gem mineral, not as an ore o; (Minor) - Mn
Development Status: None

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


3 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 4 - Oxides and Hydroxides
Pyrolusite4.DB.05Mn4+O2
Group 5 - Nitrates and Carbonates
Rhodochrosite5.AB.05MnCO3
Group 9 - Silicates
Rhodonite9.DK.05CaMn3Mn[Si5O15]

List of minerals for each chemical element

CCarbon
C RhodochrositeMnCO3
OOxygen
O PyrolusiteMn4+O2
O RhodochrositeMnCO3
O RhodoniteCaMn3Mn[Si5O15]
SiSilicon
Si RhodoniteCaMn3Mn[Si5O15]
CaCalcium
Ca RhodoniteCaMn3Mn[Si5O15]
MnManganese
Mn PyrolusiteMn4+O2
Mn RhodochrositeMnCO3
Mn RhodoniteCaMn3Mn[Si5O15]

Other Databases

Link to USGS - Alaska:MM088

Other Regions, Features and Areas containing this locality


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