301 Mine, Cherokee County, Georgia, USAi
| Regional Level Types | |
|---|---|
| 301 Mine | Mine |
| Cherokee County | County |
| Georgia | State |
| USA | Country |
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Latitude & Longitude (WGS84):
34° 10' 16'' North , 84° 31' 31'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Holly Springs | 10,719 (2017) | 2.2km |
| Woodstock | 29,898 (2017) | 7.8km |
| Canton | 25,469 (2017) | 8.0km |
| Mountain Park | 578 (2017) | 14.5km |
| Waleska | 802 (2017) | 16.3km |
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 |
|---|---|---|
| Cobb County Gem and Mineral Society | Marietta, Georgia | 24km |
| Georgia Mineral Society, Inc. | Norcross, Georgia | 38km |
Other/historical names associated with this locality:
Three-O-One Mine; Doctor's Mine; Kolb Mine; Farrar Mine
The 301 (Doctor's, Kolb, Farrar) mine, on lot 301 in the fifteenth district, near Holly Springs, is controlled by a group of Atlanta businessmen. When visited it was being worked under the supervision of W. H. Fluker. The mine is opened by a shaft about 143 feet deep, from which two levels have been driven at depths at 80 and 140 feet. A short tunnel, several old stopes, and some other old workings were partly accessible.
The country rock near the lode is a mica schist. About 100 feet southeast of the main workings is a few feet of interlayered mica schist and dark-green amphibole gneiss, and lighter-colored feldspathic amphibole gneiss crops out farther to the southeast. The foliation planes in the schist and gneiss strike N. 40° to 50° E. and dip 65° to 75° SE. Few exposures of solid rock are to be found except in the mine workings and in some road cuts, the surface being nearly everywhere covered with soil and saprolite.
The lode consists of numerous quartz layers and stringers, generally parallel to the foliation of the country rock. Near the collar of the shaft 15 quartz layers, each less than an inch thick, occur within a width of 28 inches. The number of quartz layers changes abruptly, and in places they are nearly absent. The rock adjoining them and forming part of the lode consists mainly of fine grained quartz and sericite. A little pyrite and chalcopyrite are usually present; the gold is said to be in the pyrite. The sulfides are almost completely oxidized on the 80-foot level, but the rock in the lower (140-foot) level appears fresh.
Only a little exploration work had been done in depth up to the time of the visit, 1934-35, and the results were not encouraging. The property is said to have been core drilled, but the results were not available.
The country rock near the lode is a mica schist. About 100 feet southeast of the main workings is a few feet of interlayered mica schist and dark-green amphibole gneiss, and lighter-colored feldspathic amphibole gneiss crops out farther to the southeast. The foliation planes in the schist and gneiss strike N. 40° to 50° E. and dip 65° to 75° SE. Few exposures of solid rock are to be found except in the mine workings and in some road cuts, the surface being nearly everywhere covered with soil and saprolite.
The lode consists of numerous quartz layers and stringers, generally parallel to the foliation of the country rock. Near the collar of the shaft 15 quartz layers, each less than an inch thick, occur within a width of 28 inches. The number of quartz layers changes abruptly, and in places they are nearly absent. The rock adjoining them and forming part of the lode consists mainly of fine grained quartz and sericite. A little pyrite and chalcopyrite are usually present; the gold is said to be in the pyrite. The sulfides are almost completely oxidized on the 80-foot level, but the rock in the lower (140-foot) level appears fresh.
Only a little exploration work had been done in depth up to the time of the visit, 1934-35, and the results were not encouraging. The property is said to have been core drilled, but the results were not available.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsCommodity List
This is a list of exploitable or exploited mineral commodities recorded at this locality.Mineral List
6 valid minerals.
Rock Types Recorded
Note: data is currently VERY limited. Please bear with us while we work towards adding this information!
Select Rock List Type
Alphabetical List Tree DiagramDetailed Mineral List:
| ⓘ Allanite-(Ce) Formula: (CaCe)(AlAlFe2+)O[Si2O7][SiO4](OH) References: |
| ⓘ 'Amphibole Supergroup' Formula: AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
| ⓘ Chalcopyrite Formula: CuFeS2 |
| ⓘ 'Limonite' |
| ⓘ Muscovite Formula: KAl2(AlSi3O10)(OH)2 |
| ⓘ Muscovite var. Sericite Formula: KAl2(AlSi3O10)(OH)2 |
| ⓘ Native Gold Formula: Au |
| ⓘ Pyrite Formula: FeS2 |
| ⓘ Quartz Formula: SiO2 |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 1 - Elements | |||
|---|---|---|---|
| ⓘ | Native Gold | 1.AA.05 | Au |
| Group 2 - Sulphides and Sulfosalts | |||
| ⓘ | Chalcopyrite | 2.CB.10a | CuFeS2 |
| ⓘ | Pyrite | 2.EB.05a | FeS2 |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Quartz | 4.DA.05 | SiO2 |
| Group 9 - Silicates | |||
| ⓘ | Allanite-(Ce) | 9.BG.05b | (CaCe)(AlAlFe2+)O[Si2O7][SiO4](OH) |
| ⓘ | Muscovite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
| ⓘ | var. Sericite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
| Unclassified | |||
| ⓘ | 'Amphibole Supergroup' | - | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
| ⓘ | 'Limonite' | - | |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Allanite-(Ce) | (CaCe)(AlAlFe2+)O[Si2O7][SiO4](OH) |
| H | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
| H | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| H | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| O | Oxygen | |
| O | ⓘ Allanite-(Ce) | (CaCe)(AlAlFe2+)O[Si2O7][SiO4](OH) |
| O | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
| O | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| O | ⓘ Quartz | SiO2 |
| O | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| F | Fluorine | |
| F | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
| Al | Aluminium | |
| Al | ⓘ Allanite-(Ce) | (CaCe)(AlAlFe2+)O[Si2O7][SiO4](OH) |
| Al | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
| Al | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Al | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Si | Silicon | |
| Si | ⓘ Allanite-(Ce) | (CaCe)(AlAlFe2+)O[Si2O7][SiO4](OH) |
| Si | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
| Si | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Si | ⓘ Quartz | SiO2 |
| Si | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| S | Sulfur | |
| S | ⓘ Chalcopyrite | CuFeS2 |
| S | ⓘ Pyrite | FeS2 |
| Cl | Chlorine | |
| Cl | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
| K | Potassium | |
| K | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| K | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Ca | Calcium | |
| Ca | ⓘ Allanite-(Ce) | (CaCe)(AlAlFe2+)O[Si2O7][SiO4](OH) |
| Ti | Titanium | |
| Ti | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
| Fe | Iron | |
| Fe | ⓘ Allanite-(Ce) | (CaCe)(AlAlFe2+)O[Si2O7][SiO4](OH) |
| Fe | ⓘ Chalcopyrite | CuFeS2 |
| Fe | ⓘ Pyrite | FeS2 |
| Cu | Copper | |
| Cu | ⓘ Chalcopyrite | CuFeS2 |
| Ce | Cerium | |
| Ce | ⓘ Allanite-(Ce) | (CaCe)(AlAlFe2+)O[Si2O7][SiO4](OH) |
| Au | Gold | |
| Au | ⓘ Native Gold | Au |
Other Databases
| Link to USGS MRDS: | 10240693 |
|---|
Other Regions, Features and Areas containing this locality
North AmericaContinent
North America PlateTectonic Plate
- PedmontiaAccretionary Complex
- Piedmontia DomainDomain
USA
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301 Mine, Cherokee County, Georgia, USA