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Never-Get-Left Mine (Never-Get-Left prospect), Gold Basin Mining District, White Hills, Mohave County, Arizona, USAi
Regional Level Types
Never-Get-Left Mine (Never-Get-Left prospect)Mine
Gold Basin Mining DistrictMining District
White HillsGroup of Census-designated Places
Mohave CountyCounty
ArizonaState
USACountry

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Latitude & Longitude (WGS84):
35° 47' 38'' North , 114° 12' 54'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
White Hills323 (2011)17.6km
Dolan Springs2,033 (2011)23.1km
Meadview1,224 (2011)26.7km
Chloride271 (2011)42.2km
Valle Vista1,659 (2017)53.2km
Mindat Locality ID:
39558
Long-form identifier:
mindat:1:2:39558:5
GUID (UUID V4):
0
Other/historical names associated with this locality:
Josephine patent 1034a; Southern Pride patent 1034a; Golden Butterfly Mine; South Dog Hole Mine


A former Au-Ag-Cu-Zn-Mo occurrence/mine located in the SE¼ sec. 20, SW¼ sec. 21, and in the N½N½NW¼ sec. 28, T28N, R18W, G&SRM, in the eastern White Hills, 10 miles W of Garnet Mountain, on Bureau of Land Management administered land. Past operators include Henry Buly, Kent August, Manna & Lester. Owned by Ralph G. Godfrey, Arizona (1979). The USGS MRDS database stated accuracy for this locality is 500 meters.

NEVER-GET-LEFT MINE.

The Never-get-left mine is located in the upper part of a cliff or fault scarp that overlooks the Eldorado mine on the east, from which it is but a few hundred yards distant. It is situated at about 4,500 feet elevation, or 1,600 feet above Hualpai Valley. It is owned by Henry Paully, of Basin, and is developed principally by an adit drift, shallow shafts, and open cuts, aggregating several hundred feet of work.

The country rock is dark gneissoid schist. The structure dips about 50° W., but the principal deposit dips about 80° N. It has a width of 6 or 8 feet and contains mainly iron-stained or copper-stained crushed gold-bearing quartz. The country rock is greatly disturbed by jointing, fracturing, and-faulting, and its true character is somewhat doubtful. The mine has been a small producer for some years and was shipping ore in April, 1906.


Mineralization is a fault vein hosted in schist. The ore body dips 80N at a width of 2.44 meters and is comprised of massive white quartz veins. Alteration is propyllitic. Locally, the schist dips 50ºW and is greatly disturbed by jointing, fracturing and faulting. Associated rocks include Late Cretaceous-Neoproterozoic quartz monzonite, pegmatite and granite. Local rocks include Early Proterozoic metamorphic rocks.

Workings include surface and underground openings with a length of 213.36 meters and comprised of a 9 meter long by 0.6 to 3.1 meter deep open cut, an adit, drift, and shallow shafts.

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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.

Rock Types Recorded

Note: data is currently VERY limited. Please bear with us while we work towards adding this information!

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Alphabetical List Tree Diagram

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
Chalcopyrite2.CB.10aCuFeS2
Galena2.CD.10PbS
Pyrite2.EB.05aFeS2
Group 4 - Oxides and Hydroxides
Quartz4.DA.05SiO2
var. Milky Quartz4.DA.05SiO2

List of minerals for each chemical element

OOxygen
O QuartzSiO2
O Quartz var. Milky QuartzSiO2
SiSilicon
Si QuartzSiO2
Si Quartz var. Milky QuartzSiO2
SSulfur
S ChalcopyriteCuFeS2
S GalenaPbS
S PyriteFeS2
FeIron
Fe ChalcopyriteCuFeS2
Fe PyriteFeS2
CuCopper
Cu ChalcopyriteCuFeS2
PbLead
Pb GalenaPbS

Other Databases

Link to USGS MRDS:10102558
Link to USGS MRDS:10259501

Other Regions, Features and Areas containing this locality


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References

 
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