Gold-in-Alabama

Gold in Clay County Alabama

Gold In Clay County Alabama

Clay County, Alabama has 166 records of mines listed by the United States Geological Survey (USGS). Placer gold is found in many streams in the county including Crooked Creek, Wesobulga Creek and the Tallapoosa River.

Erin, Alabama

South of Erin, Alabama in gravel bars of Gold Mines Creek, you will find placer gold, with sillimanite, pyrope garnets and talc.

Gold Mines in Clay County Alabama

Alabama Gold & Mica Co. Mine

33.3259461, -85.866908

33.32654, -85.86802

Past Producer in Clay county in Alabama, United States with commodity Gold. The Alabama Gold And Mica Company Mine is near Pyriton, Alabama. Historically the site has been associated with the Idaho Gold Mining District which is now part of the Talladega National Forest. The Alabama Gold And Mica Company Mine was closed at the time of data entry with no known plans to re-open. Production size when active was considered to be small. The ore mined is composed of gold. The host rock in this area is mica schist from the Upper Cretaceous epoch 100.50 to 66.00 million years ago. The Piedmont Upland of the Appalachian Highlands characterize the geomorphology of the surrounding area.

Amason Prospect

Ashland Mining Company Gold Prospect

33.3218°N 85.9527°W

The Ashland Mining Company Gold Prospect is near Chandler Springs, Alabama. Historically the site has been associated with the Idaho Gold Mining District which is now part of the Talladega National Forest. The ore mined is composed of gold. The ore body is linear in form of unknown dimensions. The mineralization at this location is from the Upper Cretaceous epoch 100.50 to 66.00 million years ago. The Piedmont Upland of the Appalachian Highlands characterize the geomorphology of the surrounding area.

Benjamin Prospect

33.2592828, -85.6541243

Dean, Lewis S. and Otis M. Clarke, Jr. Mineral Resources of Clay County, Alabama: Special Map 212. Tuscaloosa, Alabama: Geological Survey of Alabama, 1988.

Brown Prospect

33.3165°N 85.8943°W

The Brown Gold Prospect is near Ashland, Alabama. Historically the site has been associated with the Idaho Gold Mining District which is now part of the Talladega National Forest. Preliminary development has taken place such as surface trenching, adits, shafts, drill holes, geophysics, geochemistry, or geological mapping. Enough data has been gathered to estimate grade and tonnage. The size of the deposit is estimated to be small. The ore mined is composed of gold. The ore body is linear in form of unknown dimensions. The mineralization at this location is from the Upper Cretaceous epoch 100.50 to 66.00 million years ago. The Piedmont Upland of the Appalachian Highlands characterize the geomorphology of the surrounding area.

California Lode

33.2876°N 85.9027°W

The California Lode Prospect is near Ashland, Alabama. Historically the site has been associated with the Idaho Gold Mining District which is now part of the Talladega National Forest. The ore mined is composed of gold with waste material consisting primarily of quartz. The ore body is linear in form of unknown dimensions. The host rock in this area is schist. The Piedmont Upland of the Appalachian Highlands characterize the geomorphology of the surrounding area.

Latitude: 33.2890025
Longitude: -85.9044094
GNIS ID: 151100

Carter Prospect

33.2140059, -85.6952364

The Chinca Pina Property

33.3307°N 85.9180°W

An open cut, inclined shaft, with several prospect holes, with best panning in surface gravel contained placer gold. The Haraldson Mine was an old mine. The California Property was the site of 10 stamp mill and had gold obtainable by crushing and panning. South of Lineville, Alabama, in area streams emptying into Crooked Creek, the placers are said to be very rich.

Cockrell Placer Mine

33.2534495, -85.6616245

Crucible Prospect

33.3070576, -85.8902425

Cragford District

Cragford district is located along the far east side of Clay county and far west side of Randolph County.

Dawkins Property

Between forks of White Oak and Wesobulga creeks you will find the Dawkins Property, which was the site of old 10 stamp mill and produced lode gold saved by amalgamation.

Dawkin’s Lode

33.2240058, -85.674958

Eley Gold Mine

The Eley Gold Mine is near Pyriton, Alabama. Historically the site has been associated with the Idaho Gold Mining District which is now part of the Talladega National Forest. The Eley Gold Mine was closed at the time of data entry with no known plans to re-open. Production size when active was considered to be small. The Piedmont Upland of the Appalachian Highlands characterize the geomorphology of the surrounding area. On lower valley slope of tributary to hunting creek on logging road. Massive quartz vein exposed in one pit.

Source: Gold deposits of the southern Piedmont.

33.34598, -85.89579

Farrar-Wallace Prospect

33.2401165, -85.6741248

Franklin Mine

33.3168°N 85.9020°W

The Franklin Gold Mine is near Ashland, Alabama. Historically the site has been associated with the Idaho Gold Mining District which is now part of the Talladega National Forest. The Franklin Gold Mine was closed at the time of data entry with no known plans to re-open. Production size when active was considered to be medium. Mine operations consist of surface and underground workings. There is one known shaft. The ore mined is composed of gold. The ore body is linear in form of unknown dimensions. Associated rock in this area is pegmatite from the Upper Cretaceous epoch 100.50 to 66.00 million years ago. The Piedmont Upland of the Appalachian Highlands characterize the geomorphology of the surrounding area.

The Farrar Property

had a deep shaft and crosscut tunnel, worked before 1860 for lode gold.

The Goldberg Mine

The Goldberg Mine was an open cut, inclined pit, with veins 6-15 inches thick that contained gold with antimony, copper, traces of arsenic.

Grizzel Prospect

The Grizzell Gold Prospect is near Cragford, Alabama. It has veins in quartz to 30 feet deep and you could find rich specimen ore near surface, the mine was famous for free milling gold.

33°15’58.4″N 85°39’42.9″W

Haraldson Mine

33.3332°N 85.9213°W

The Haraldson Gold Mine is near Chandler Springs, Alabama. Historically the site has been associated with the Idaho Gold Mining District which is now part of the Talladega National Forest. The Haraldson Gold Mine was closed at the time of data entry with no known plans to re-open. The Piedmont Upland of the Appalachian Highlands characterize the geomorphology of the surrounding area.

Harall Gold Prospect

33.1821°N 85.8916°W

The Harall Gold Prospect is near Millerville, Alabama. Historically the site has been associated with the Idaho Gold Mining District which is now part of the Talladega National Forest. The ore mined is composed of gold. The ore body is described as tabular shaped of unknown dimensions. The mineralization at this location is from the Lopingian epoch 259.80 to 252.17 million years ago. The Piedmont Upland of the Appalachian Highlands characterize the geomorphology of the surrounding area.

Harold Gold Mine

33.2445°N 86.0055°W

The Harold Gold Mine is near Millerville, Alabama. Historically the site has been associated with the Idaho Gold Mining District which is now part of the Talladega National Forest. The Harold Gold Mine was closed at the time of data entry with no known plans to re-open. The ore mined is composed of gold. The ore body is linear in form of unknown dimensions. The host rock in this area is mica schist. The Piedmont Upland of the Appalachian Highlands characterize the geomorphology of the surrounding area.

Harwell Prospect

33.1821°N 85.8916°W

The Harwell Gold Prospect is near Millerville, Alabama. Historically the site has been associated with the Idaho Gold Mining District which is now part of the Talladega National Forest. The Harwell Gold Prospect was closed at the time of data entry with no known plans to re-open. Production size when active was considered to be small. The Piedmont Upland of the Appalachian Highlands characterize the geomorphology of the surrounding area.

Hobbs Prospect

33.3168°N 85.9070°W

The Hobbs Gold Prospect is near Ashland, Alabama. Historically the site has been associated with the Idaho Gold Mining District which is now part of the Talladega National Forest. The Hobbs Gold Prospect is a surface mining operation. The ore mined is composed of gold. The ore body is linear in form of unknown dimensions. Associated rock in this area is pegmatite from the Upper Cretaceous epoch 100.50 to 66.00 million years ago. The Piedmont Upland of the Appalachian Highlands characterize the geomorphology of the surrounding area.

Horn’s Peak Mine

33.314835, -85.9155211

The Horns Peak Mine is near Chandler Springs, Alabama. Historically the site has been associated with the Idaho Gold Mining District which is now part of the Talladega National Forest. The Horns Peak Mine is a underground mining operation. The ore mined is composed of gold. The host rock in this area is mica schist from the Upper Cretaceous epoch 100.50 to 66.00 million years ago. The Piedmont Upland of the Appalachian Highlands characterize the geomorphology of the surrounding area.o0p9i.;/,,,,,

The H. S. Bradley

The H.S. Bradley land had prospects that contained free milling gold. The Manning Placer, consist of old diggings along tributaries of Crooked creek, which were landmarks of 1830’s and 40’s. You will find thin quartz veins nearby that produce placer and lode gold.

Idaho Mine

33.316224, -85.8994094

Knight’s Mill Prospect

33.2334499, -85.6741247

Lashley Property Prospect

Fisher Mine, Cragford Mining District

Laurel Prospect

33.3170°N 85.9154°W

The Laurel Gold Prospect is near Chandler Springs, Alabama. Historically the site has been associated with the Idaho Gold Mining District which is now part of the Talladega National Forest. The Laurel Gold Prospect was closed at the time of data entry with no known plans to re-open. Production size when active was considered to be small. The ore mined is composed of gold with waste material consisting primarily of quartz. The ore body is linear in form reaching 1.52 meters (4.99 feet) in width. The mineralization at this location is from the Lopingian epoch 259.80 to 252.17 million years ago. The Piedmont Upland of the Appalachian Highlands characterize the geomorphology of the surrounding area.

Laurel Prospect National Forest

Little Samson Lode

33.3195572, -85.8980206

The Manning Placer

The Manning Placer consist of old diggings along tributaries of Crooked creek, which were landmarks of 1830’s and 40’s. You will find thin quartz veins nearby that produce placer and lode gold.  The Tallapoosa River shoal sands show placer gold.

McLellan Mine

33.3301125, -85.8849646

Mitchell Prospect Number One

33.2315056, -85.6635688

The Morris Property

The Morris Property contained ore in formation that was traceable 1 mile northeast to the Tallapoosa River. The Tallapoosa River shoal sands show placer gold.

Old Gold Mine

33.3070°N 85.9374°W

The Old Gold Mine is near Chandler Springs, Alabama. Historically the site has been associated with the Idaho Gold Mining District which is now part of the Talladega National Forest. The Old Gold Mine was closed at the time of data entry with no known plans to re-open. Production size when active was considered to be small. The Piedmont Upland of the Appalachian Highlands characterize the geomorphology of the surrounding area.

Pyriton Area National Forest

The Pyriton Mines are near Pyriton, Alabama. Historically the area has been associated with the Pyriton Mining District which is now part of the Talladega National Forest. The Pyriton Mines was closed at the time of data entry with no known plans to re-open. Production size when active was considered to be medium. Mine operations consist of 2 distinct surface and underground workings extending 1.00 hectares (2.47 acres). There is one known shaft. The mining method is strip-level. Mine capacity in 1977 was 1000 mt ore/day with a production unit cost of 14 $/mt ore. As of 1982 there was one documented tabular shaped ore body extending 2,774 meters (9,101 feet) long, 324 meters (1,062 feet) wide, and 2 meters (6 feet) thick. The Piedmont Upland of the Appalachian Highlands characterize the geomorphology of the surrounding area.

The Teakle Property

at Wildcat Hollow consisted of a deep shaft known as the Orum Pit, produced lode gold. Adjacent to Wildcat Hollow, the Bradford Fraction produced lode gold.

Walker Prospect

33.2265057, -85.6674578

Whatley Gold Mine

33.3140016, -85.9394106

The Whatley Gold Mine is near Pyriton, Alabama. Historically the site has been associated with the Idaho Gold Mining District which is now part of the Talladega National Forest. The Whatley Gold Mine was closed at the time of data entry with no known plans to re-open. Production size when active was considered to be small. Mine operations consist of surface and underground workings. There is one known shaft. The ore mined is composed of gold. The ore body is linear in form of unknown dimensions. Associated rock in this area is pegmatite from the Upper Cretaceous epoch 100.50 to 66.00 million years ago. The Piedmont Upland of the Appalachian Highlands characterize the geomorphology of the surrounding area. On forested hill crest adjacent to south side of south Yadkin River.

Wildcat Hollow Prospect

At Wildcat Hollow, the Teakle Property consisted of a deep shaft known as the Orum Pit, produced lode gold.

The W. D. Mitchell’s Pine Hill Prospect

was an 80 foot deep inclined shaft and pits along strike in ore body 14 ft. thick. The Bradford Ridge Mine was the most extensively prospected mine in the district and was the site of a 10 stamp mill contained gold, with some arsenopyrite.

Worthy-Walker Mine

Cragford, Alabama

33.2277, -85.6403

33°13’39.7″N 85°38’25.1″W

33.227700, -85.640300

The Worthy-Walker Mine is near Cragford, Alabama. Historically the site has been part of the Cragford Mining District. The Worthy-Walker Mine is a underground mining operation. Mine operations consist of underground workings. There is one known shaft. The mining method is other combined methods. The ore mined is composed of gold. As of 1982 there were two known tabular shaped ore bodies one of which extends 10 meters (32 feet) long, 1 meter (2 feet) wide, and 1 meter (2 feet) thick. The host rock in this area is phyllite from the Upper Cretaceous epoch 100.50 to 66.00 million years ago. The Piedmont Upland of the Appalachian Highlands characterize the geomorphology of the surrounding area.
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Clay County Alabama Gold Map

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