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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Trench 7--Divide Zone Prospect (Bonanza Hill), Nome Mining District, Nome Census Area, Alaska, USAi
Regional Level Types
Trench 7--Divide Zone Prospect (Bonanza Hill)Prospect
Nome Mining DistrictMining District
Nome Census AreaCensus Area
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
64° 34' 59'' North , 165° 23' 38'' West
Latitude & Longitude (decimal):
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Nome3,806 (2018)9.1km
Mindat Locality ID:
200419
Long-form identifier:
mindat:1:2:200419:1
GUID (UUID V4):
0


Location: The Trench 7--Divide deposit is at an elevation of 450 to 465 feet about 1,200 to 1,500 feet due east of the rounded top of Bonanza Hill. The map location is in the northwest corner of section 36, T. 10 S., R. 34 W., Kateel River Meridian, and it is accurate.
Geology: The Trench 7--Divide deposit was identified from exploration by BHP in 1990 and by Newmont Mining Company in 1992; there are some old trenches and cuts of uncertain age on the deposit. The area was mapped by Thomas Borovicka for Newmont in 1992; his map was modified for Kennecott Exploration Company by C.C. Hawley in 1993 and 1994. The Trench 7--Divide deposit appears to be bounded on the northwest by a steep fault that strikes N 50 E. The apparent displacement, evidenced by offset of a calcareous quartz-mica schist layer, is about 10 feet. Southeast of the fault, the deposit is about 200 feet across. Locally, there are sheeted veins of calcite and quartz; older sloughed trenches show accumulations of vein quartz boulders. The deposit is irregular; locally it contains 0.05 to 0.07 ounce of gold per ton. It is possible that the deposit continues to the northeast to Placer Dome trenches 88-3, -4 and -5 (NM223). Bonanza Hill is mainly underlain by nearly horizontal calcareous quartz-muscovite schist and marble probably of early Paleozoic protolith age (Hummel, 1962 [MF 247]; Sainsbury, Hummel, and Hudson, 1972 [OFR 72-326]; Till and Dumoulin, 1994; Bundtzen and others, 1994).
Workings: This prospect has been explored by numerous trenches and shallow drill holes.
Age: Mid-Cretaceous; veins cross cut regionally metamorphosed schist; see NM207.

Commodities (Major) - Au
Development Status: None
Deposit Model: Low-sulfide Au-quartz veins (Cox and Singer, 1986; model 36a).

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


6 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
Gold1.AA.05Au
Group 2 - Sulphides and Sulfosalts
Pyrite2.EB.05aFeS2
Arsenopyrite2.EB.20FeAsS
Group 4 - Oxides and Hydroxides
Quartz4.DA.05SiO2
Group 5 - Nitrates and Carbonates
Calcite5.AB.05CaCO3
Group 9 - Silicates
Albite9.FA.35Na(AlSi3O8)

List of minerals for each chemical element

CCarbon
C CalciteCaCO3
OOxygen
O AlbiteNa(AlSi3O8)
O CalciteCaCO3
O QuartzSiO2
NaSodium
Na AlbiteNa(AlSi3O8)
AlAluminium
Al AlbiteNa(AlSi3O8)
SiSilicon
Si AlbiteNa(AlSi3O8)
Si QuartzSiO2
SSulfur
S ArsenopyriteFeAsS
S PyriteFeS2
CaCalcium
Ca CalciteCaCO3
FeIron
Fe ArsenopyriteFeAsS
Fe PyriteFeS2
AsArsenic
As ArsenopyriteFeAsS
AuGold
Au GoldAu

Other Databases

Link to USGS - Alaska:NM224

Other Regions, Features and Areas containing this locality

North AmericaContinent
North America PlateTectonic Plate

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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