Lot 71, Canton, Cherokee County, Georgia, USAi
| Regional Level Types | |
|---|---|
| Lot 71 | Property |
| Canton | Town |
| Cherokee County | County |
| Georgia | State |
| USA | Country |
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Latitude & Longitude (WGS84):
34° North , 84° West (est.)
Estimate based on other nearby localities or region boundaries.
Margin of Error:
~6km
Type:
Köppen climate type:
Other/historical names associated with this locality:
W. T. Worley property
The property of W. T. Worley, formerly owned by S. J. Blackwell, is located 7 miles east of Canton on lot 71, 4th district, and 2nd section. It is situated on a small ridge one-fourth of a mile off the public road.
The asbestos is associated with an intrusion of pyroxenite, probably enstatitite, which has a northeast-southwest trend and is at least a quarter of a mile long and 200 yards wide. Other outcrops of the same material are said to occur along the strike in both directions, but they were not visited. The pyroxenite is present as a local, basic segregation, as is demonstrated by its relationship to the enclosing hornblende gneiss.
On account of its size, when taken together with the hornblende gneiss, of which it is properly a part, the intrusion has not suffered as much metamorphism as have most other areas. There are no large quantities of talc or soapstone present; on the contrary, they are conspicuously absent. A large part of the mass has remained a pyroxenite with little alteration. Some local segregations of magnetite and corundum in pieces 3 to 4 inches in diameter have been found. At some places the pyroxenite is altered largely to amphibole; and along lines where movement has taken place slip-fiber asbestos is to be found. Hyalitic fragments, so characteristic of rocks of other more altered areas, have been found here to a slight extent.
This property was quite extensively prospected some years ago: a tunnel 80 feet long was driven in on the eastern side of the intrusion, in an attempt to follow a vein of slip-fiber asbestos; a shaft 30 feet deep was sunk nearby, but with no success; besides these, a few other small pits have been dug at various places over the intrusion.
The asbestos, although it occurs both as slip and cross fiber along fault planes, and also to a small extent as mass fiber, is developed to but a comparatively small extent.
The asbestos is associated with an intrusion of pyroxenite, probably enstatitite, which has a northeast-southwest trend and is at least a quarter of a mile long and 200 yards wide. Other outcrops of the same material are said to occur along the strike in both directions, but they were not visited. The pyroxenite is present as a local, basic segregation, as is demonstrated by its relationship to the enclosing hornblende gneiss.
On account of its size, when taken together with the hornblende gneiss, of which it is properly a part, the intrusion has not suffered as much metamorphism as have most other areas. There are no large quantities of talc or soapstone present; on the contrary, they are conspicuously absent. A large part of the mass has remained a pyroxenite with little alteration. Some local segregations of magnetite and corundum in pieces 3 to 4 inches in diameter have been found. At some places the pyroxenite is altered largely to amphibole; and along lines where movement has taken place slip-fiber asbestos is to be found. Hyalitic fragments, so characteristic of rocks of other more altered areas, have been found here to a slight extent.
This property was quite extensively prospected some years ago: a tunnel 80 feet long was driven in on the eastern side of the intrusion, in an attempt to follow a vein of slip-fiber asbestos; a shaft 30 feet deep was sunk nearby, but with no success; besides these, a few other small pits have been dug at various places over the intrusion.
The asbestos, although it occurs both as slip and cross fiber along fault planes, and also to a small extent as mass fiber, is developed to but a comparatively small extent.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsMineral List
2 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:
| ⓘ 'Amphibole Supergroup' Formula: AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
| ⓘ 'Asbestos' |
| ⓘ Corundum Formula: Al2O3 |
| ⓘ Magnetite Formula: Fe2+Fe3+2O4 |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 4 - Oxides and Hydroxides | |||
|---|---|---|---|
| ⓘ | Magnetite | 4.BB.05 | Fe2+Fe3+2O4 |
| ⓘ | Corundum | 4.CB.05 | Al2O3 |
| Unclassified | |||
| ⓘ | 'Amphibole Supergroup' | - | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
| ⓘ | 'Asbestos' | - | |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
| O | Oxygen | |
| O | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
| O | ⓘ Corundum | Al2O3 |
| O | ⓘ Magnetite | Fe2+Fe23+O4 |
| F | Fluorine | |
| F | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
| Al | Aluminium | |
| Al | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
| Al | ⓘ Corundum | Al2O3 |
| Si | Silicon | |
| Si | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
| Cl | Chlorine | |
| Cl | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
| Ti | Titanium | |
| Ti | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
| Fe | Iron | |
| Fe | ⓘ Magnetite | Fe2+Fe23+O4 |
Other Regions, Features and Areas containing this locality
North AmericaContinent
North America PlateTectonic Plate
- Laurentides DomainPassive Margin
- Piedmontia DomainDomain
USA
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