Paga No. 3 Mine, PAGA Mine, Cartersville Mining District, Bartow County, Georgia, USAi
| Regional Level Types | |
|---|---|
| Paga No. 3 Mine | Mine |
| PAGA Mine | Mine |
| Cartersville Mining District | Mining District |
| Bartow County | County |
| Georgia | State |
| USA | Country |
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Latitude & Longitude (WGS84):
34° 8' 30'' North , 84° 46' 1'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Emerson | 1,535 (2017) | 2.0km |
| Cartersville | 20,319 (2017) | 4.2km |
| Acworth | 22,131 (2017) | 11.7km |
| Euharlee | 4,261 (2017) | 15.3km |
| White | 724 (2017) | 15.8km |
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 | 29km |
| Rome Georgia Mineral Society Inc. | Rome, Georgia | 39km |
Other/historical names associated with this locality:
Peruvian Ochre Company Mine, Georgia Peruvian Ochre Company Mine, Renfroe Mine
The Paga No. 3 mine is on lots 677 and 692, 4th district, 3d section, 1 1/4 miles north-northwest of Emerson, and a quarter of a mile east of Etowah River. The washer is in the southeast corner of lot 677 and the open-cut is in the northeast corner of lot 692. Both are on the south side of the Dixie Highway. The property belongs to the Georgia Peruvian Ocher Company, R. C. May, agent, Cartersville, except a little more than 4 acres comprising the extreme northeast corner of lot 692, which belongs to Mrs. Kittie P. Larey.
Although the deposit had been prospected some time previously, it was not opened and worked until July, 1917. P. C. Renfroe, of Cartersville, leased and operated the mine from 1917 to the first part of 1919. In 1919 the Paga Mining Company acquired Renfroe's interest in the property and the mine became known as Paga No. 3.
Barytes particles and fragments ranging in thickness from a fraction of an inch to more than a foot have been found on the surface and in test pits throughout a distance of approximately 300 yards south of the Dixie Highway, up to an elevation of about 780 feet above sea level. Nodules also occur 150 yards southeast of the cut in the direction of the Nulsen mine. Water-worn quartz pebbles are abundant in places on the hillside up to an elevation of 860 feet above sea level or about 175 feet higher than the river. Small open-cuts and entries have been made in brown iron ore at elevations of 900 and 960 feet on the hillside.
Although the deposit had been prospected some time previously, it was not opened and worked until July, 1917. P. C. Renfroe, of Cartersville, leased and operated the mine from 1917 to the first part of 1919. In 1919 the Paga Mining Company acquired Renfroe's interest in the property and the mine became known as Paga No. 3.
Barytes particles and fragments ranging in thickness from a fraction of an inch to more than a foot have been found on the surface and in test pits throughout a distance of approximately 300 yards south of the Dixie Highway, up to an elevation of about 780 feet above sea level. Nodules also occur 150 yards southeast of the cut in the direction of the Nulsen mine. Water-worn quartz pebbles are abundant in places on the hillside up to an elevation of 860 feet above sea level or about 175 feet higher than the river. Small open-cuts and entries have been made in brown iron ore at elevations of 900 and 960 feet on the hillside.
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:
| ✪ Baryte Formula: BaSO4 |
| ⓘ 'Brown Iron Ore' |
| ⓘ 'Clay minerals' |
| ⓘ Goethite Formula: Fe3+O(OH) |
| ⓘ Hematite Formula: Fe2O3 |
| ⓘ Hematite var. Iridescent Hematite Formula: Fe2O3 |
| ⓘ Lepidocrocite Formula: Fe3+O(OH) |
| ⓘ 'Limonite' |
| ⓘ Pyrite Formula: FeS2 |
| ⓘ Quartz Formula: SiO2 |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 2 - Sulphides and Sulfosalts | |||
|---|---|---|---|
| ⓘ | Pyrite | 2.EB.05a | FeS2 |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Goethite | 4.00. | Fe3+O(OH) |
| ⓘ | Hematite | 4.CB.05 | Fe2O3 |
| ⓘ | var. Iridescent Hematite | 4.CB.05 | Fe2O3 |
| ⓘ | Quartz | 4.DA.05 | SiO2 |
| ⓘ | Lepidocrocite | 4.FE.15 | Fe3+O(OH) |
| Group 7 - Sulphates, Chromates, Molybdates and Tungstates | |||
| ⓘ | Baryte | 7.AD.35 | BaSO4 |
| Unclassified | |||
| ⓘ | 'Clay minerals' | - | |
| ⓘ | 'Limonite' | - | |
| ⓘ | 'Brown Iron Ore' | - | |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Goethite | Fe3+O(OH) |
| H | ⓘ Lepidocrocite | Fe3+O(OH) |
| O | Oxygen | |
| O | ⓘ Baryte | BaSO4 |
| O | ⓘ Goethite | Fe3+O(OH) |
| O | ⓘ Hematite | Fe2O3 |
| O | ⓘ Lepidocrocite | Fe3+O(OH) |
| O | ⓘ Quartz | SiO2 |
| O | ⓘ Hematite var. Iridescent Hematite | Fe2O3 |
| Si | Silicon | |
| Si | ⓘ Quartz | SiO2 |
| S | Sulfur | |
| S | ⓘ Baryte | BaSO4 |
| S | ⓘ Pyrite | FeS2 |
| Fe | Iron | |
| Fe | ⓘ Goethite | Fe3+O(OH) |
| Fe | ⓘ Hematite | Fe2O3 |
| Fe | ⓘ Lepidocrocite | Fe3+O(OH) |
| Fe | ⓘ Pyrite | FeS2 |
| Fe | ⓘ Hematite var. Iridescent Hematite | Fe2O3 |
| Ba | Barium | |
| Ba | ⓘ Baryte | BaSO4 |
Other Regions, Features and Areas containing this locality
North AmericaContinent
North America PlateTectonic Plate
- Appalachian BasinBasin
- SCAB DomainDomain
- Southern and Central ApplachianAccretionary Complex
USA
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