Midnight Mine [1], Midnight vein, Oatman, Oatman Mining District, Black Mountains, Mohave County, Arizona, USAi
| Regional Level Types | |
|---|---|
| Midnight Mine [1] | Mine |
| Midnight vein | Vein |
| Oatman | Town |
| Oatman Mining District | Mining District |
| Black Mountains | Mountain Range |
| Mohave County | County |
| Arizona | State |
| USA | Country |
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Latitude & Longitude (WGS84):
35° 2' 22'' North , 114° 25' 24'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Oatman | 135 (2011) | 3.9km |
| Mesquite Creek | 416 (2011) | 15.5km |
| Bullhead City | 39,445 (2017) | 17.8km |
| Mohave Valley | 2,616 (2011) | 19.2km |
| Laughlin | 7,323 (2011) | 19.7km |
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
Local clubs are the best way to get access to collecting localities
| Club | Location | Distance |
|---|---|---|
| Silvery Colorado River Rock Club | Bullhead City, Arizona | 18km |
| Mohave County Gemstoners | Kingman, Arizona | 38km |
Other/historical names associated with this locality:
Midnight group; Leo and Gemni Mine
A former Ag-Au occurrence/mine located in the NE¼NE¼ sec. 17, T19N, R20W, G&SRM, about 2¼ miles NW of Oatman, on Bureau of Land Management administered land. Started about 1900 and owned by the Mohave Gold Mining Co. Produced 1900 to 1907 and 1935. The USGS MRDS database stated accuracy for this locality is 500 meters.
MIDNIGHT MINE.
The Midnight mine is situated in the hills 1½ miles northwest of Vivian, at an elevation of 2,500 feet, and is accessible by wagon road. It is owned by the Mohave Gold Mining Company, and has been producing moderately since about 1900. For some time it paid the running expenses of the Leland mine, which were large.
The mine is developed to a depth of 50 feet by inclined shaft, drifts, and stopes and is equipped with a gasoline hoist; the management has just begun sinking the shaft 300 feet deeper.
The country rock is the green chloritic andesite. It is intruded by basic and acidic dikes near by and is cut by a marked sheeting which trends N. 10° W. and dips 75° W. and by a close cross sheeting which dips steeply to the north. One of the basic dikes, a fine-grained greenish rock, about 40 feet in width, forms the foot wall. About 300 feet northeast of the mine, on higher ground, occurs a closely banded bluish to light-gray and greenish mottled 2 to 3 foot vein composed of fine-grained siderite containing some lime and manganese. It resembles rhyolite with banded or flow structure and may have replaced a dike in the fissure it now occupies.
The Midnight vein, which is the foot-wall member of a north-south lode, 100 feet wide, strikes N. 15° W. and dips 30° to 40° W. It is about 3½ feet in width and consists principally of quartz, with some calcite, fluorite, and adularia. Its foot-wall, portion, for a width of 3 or 4 inches, contains crudely banded red and green fluorspar, and toward the foot wall the quartz becomes dark and dense, of a flinty nature, and contains a few crystals of pyrite.
The vein has been worked from the surface almost to the bottom of the mine and longitudinally for a distance of about 120 feet, mainly on the south side of the shaft, and in this extent has averaged about $18 a ton in gold. The production has been considerable for a mine of its size, that on one side of the shaft alone amounting to $18,000. Where now worked in the bottom of the mine the ore is of low grade, running about $7 in gold to the ton, and consists of a mixture of partly altered soft country rock traversed by stringers and veinlets of calcite and quartz.
The Midnight mine is situated in the hills 1½ miles northwest of Vivian, at an elevation of 2,500 feet, and is accessible by wagon road. It is owned by the Mohave Gold Mining Company, and has been producing moderately since about 1900. For some time it paid the running expenses of the Leland mine, which were large.
The mine is developed to a depth of 50 feet by inclined shaft, drifts, and stopes and is equipped with a gasoline hoist; the management has just begun sinking the shaft 300 feet deeper.
The country rock is the green chloritic andesite. It is intruded by basic and acidic dikes near by and is cut by a marked sheeting which trends N. 10° W. and dips 75° W. and by a close cross sheeting which dips steeply to the north. One of the basic dikes, a fine-grained greenish rock, about 40 feet in width, forms the foot wall. About 300 feet northeast of the mine, on higher ground, occurs a closely banded bluish to light-gray and greenish mottled 2 to 3 foot vein composed of fine-grained siderite containing some lime and manganese. It resembles rhyolite with banded or flow structure and may have replaced a dike in the fissure it now occupies.
The Midnight vein, which is the foot-wall member of a north-south lode, 100 feet wide, strikes N. 15° W. and dips 30° to 40° W. It is about 3½ feet in width and consists principally of quartz, with some calcite, fluorite, and adularia. Its foot-wall, portion, for a width of 3 or 4 inches, contains crudely banded red and green fluorspar, and toward the foot wall the quartz becomes dark and dense, of a flinty nature, and contains a few crystals of pyrite.
The vein has been worked from the surface almost to the bottom of the mine and longitudinally for a distance of about 120 feet, mainly on the south side of the shaft, and in this extent has averaged about $18 a ton in gold. The production has been considerable for a mine of its size, that on one side of the shaft alone amounting to $18,000. Where now worked in the bottom of the mine the ore is of low grade, running about $7 in gold to the ton, and consists of a mixture of partly altered soft country rock traversed by stringers and veinlets of calcite and quartz.
Mineralization is a vein deposit hosted in trachyte and andesite. The ore body strikes N15W and dips 35W at a width of 1.07 meters. The vein represents the footwall member of a wide lode. It strikes N015ºW and dips 30º to 40ºW. It occurs in Oatman Andesite and probably also in Alcyone Trachyte. The vein filling is quartz, calcite and fluorite. Associated rocks include Pliocene mafic intrusive rock. Local rocks include Middle Miocene to Oligocene granitic/volcanic rocks.
Regional geologic structures include a NNW- to WNW-trending vein and fault system in Tertiary volcanic rocks.
Workings include underground openings with a length of 36.58 meters and an overall depth of 15.24 meters, and are comprised of stopes from the surface to 50 feet deep at 120 feet long and 3½ feet wide.
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Standard Detailed Gallery Strunz Chemical ElementsCommodity List
This is a list of exploitable or exploited mineral commodities recorded at this locality.Mineral List
3 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 DiagramGallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 3 - Halides | |||
|---|---|---|---|
| ⓘ | Fluorite | 3.AB.25 | CaF2 |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Quartz | 4.DA.05 | SiO2 |
| Group 5 - Nitrates and Carbonates | |||
| ⓘ | Calcite | 5.AB.05 | CaCO3 |
List of minerals for each chemical element
| C | Carbon | |
|---|---|---|
| C | ⓘ Calcite | CaCO3 |
| O | Oxygen | |
| O | ⓘ Calcite | CaCO3 |
| O | ⓘ Quartz | SiO2 |
| F | Fluorine | |
| F | ⓘ Fluorite | CaF2 |
| Si | Silicon | |
| Si | ⓘ Quartz | SiO2 |
| Ca | Calcium | |
| Ca | ⓘ Calcite | CaCO3 |
| Ca | ⓘ Fluorite | CaF2 |
Other Databases
| Link to USGS MRDS: | 10027901 |
|---|---|
| Link to USGS MRDS: | 10259588 |
Other Regions, Features and Areas containing this locality
North AmericaContinent
North America PlateTectonic Plate
- Basin and Range BasinsBasin
- Mojave DomainDomain
- Southern Basin and RangeWide Rift
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Midnight Mine [1], Midnight vein, Oatman, Oatman Mining District, Black Mountains, Mohave County, Arizona, USA