Cabarrus County is a county located in the south-central part of the U.S. state of North Carolina. As of the 2020 census, the population was 225,804, making it the 9th-most populous county in North Carolina. The county seat is Concord, which was incorporated in 1803. Cabarrus County is included in the Charlotte-Concord-Gastonia, NC-SC Metropolitan Statistical Area.
Dahlonega is the county seat of Lumpkin County, Georgia, United States. As of the 2010 census, the city had a population of 5,242, and in 2018 the population was estimated to be 6,884.
A gold rush or gold fever is a discovery of gold—sometimes accompanied by other precious metals and rare-earth minerals—that brings an onrush of miners seeking their fortune. Major gold rushes took place in the 19th century in Australia, Greece, New Zealand, Brazil, Chile, South Africa, the United States, and Canada while smaller gold rushes took place elsewhere.
The Dahlonega Mint was a former branch of the United States Mint built during the Georgia Gold Rush to help the miners get their gold assayed and minted, without having to travel to the Philadelphia Mint. It was located at in Dahlonega, Lumpkin County, Georgia. Coins produced at the Dahlonega Mint bear the "D" mint mark. That mint mark is used today by the Denver Mint, which opened in 1906, over four decades after the Dahlonega Mint closed. All coins from the Dahlonega Mint are gold, in the $1, $2.50, $3, and $5 denominations, and bear dates in the range 1838–1861.
Placer mining is the mining of stream bed deposits for minerals. This may be done by open-pit mining or by various surface excavating equipment or tunneling equipment.
The Reed Gold Mine is located in Midland, Cabarrus County, North Carolina, and is the site of the first documented commercial gold find in the United States. It has been designated a National Historic Landmark because of its importance and listed on the National Register of Historic Places
Auraria is a ghost town in Lumpkin County, Georgia, United States, southwest of Dahlonega. Its name derives from aurum, the Latin word for gold. In its early days, it was also known variously as Dean, Deans, Nuckollsville, and Scuffle Town.
The Calhoun Mine is perhaps the oldest and best-known mine in Lumpkin County, Georgia. When gold was discovered in Lumpkin County in 1828, which led to the Georgia Gold Rush in 1829, it was discovered on 239 acres (0.97 km2) owned by Robert Obar. After at least two intermediary sales, the land was purchased by Senator John C. Calhoun of South Carolina, who later served as the 7th Vice President of the United States. Calhoun started a mining company to mine the land and later allowed his son-in-law Thomas Green Clemson, the founder of Clemson University, to manage it. The ore deposit was a very rich deposit and, according to an 1856 letter from Clemson to his brother-in-law, was still producing significant quantities of gold nearly 30 years after its initial discovery on the land. This mine - along with the Consolidated Mine and the Loud Mine - were some of the most productive mines in the Georgia Gold Belt.
The Consolidated Mine was a gold mine in Lumpkin County, Georgia, United States, just east of Dahlonega. Like most of the area around Dahlonega, the placer mining on the land on which the mine is located probably started during the Georgia Gold Rush. By 1880, the placer deposits were exhausted and the land was down to hard rock. Gold was soon discovered in a huge quartz vein system, and mined. "The richest acre" was mined deep into the ground, and the resulting shaft became known as the "Glory Hole.”
Crisson Mine was a gold mine in Lumpkin County, Georgia, USA, located just east of Dahlonega. Like many mines in the area, the property probably started as a placer mine during the Georgia Gold Rush. Once the placer deposits had been exhausted, an open pit gold mine was established in 1847 and commercial operations continued until the early 1980s. A small stamp mill was also established here. Much of the gold used for the gold leaf dome of the Georgia State Capitol was mined at this mine, which was among the most productive mines in the Georgia Gold Belt. The mine is located just north of the site of the Consolidated Mine, which is itself north of the Calhoun Mine.
The largest quantities of gold found in the eastern United States were found in the Georgia Gold Belt, extending from eastern Alabama to Rabun County, Georgia. The biggest concentration of gold was found in White, Lumpkin, and northern Cherokee counties in Georgia. The gold in the Georgia Gold Belt was close to 24 karat (100%) purity. Most of the gold was found in eroded rock (saprolite) and mixed in with quartz.
The Denver Mint is a branch of the United States Mint that struck its first coins on February 1, 1906. The mint is still operating and producing coins for circulation, as well as mint sets and commemorative coins. Coins produced at the Denver Mint bear a D mint mark. The Denver Mint is the single largest producer of coins in the world.
The Charlotte Mint was the first United States branch mint. It was located in Charlotte, North Carolina and specialized in gold coinage.
The Dahlonega Gold Museum Historic Site is a Georgia state historic site located in Dahlonega that commemorates America's first gold rush and the mining history of Lumpkin County. The museum is housed in the historic Old Lumpkin County Courthouse built in 1836 and located in the center of the town square. It is the oldest surviving county courthouse in the state. The museum houses many artifacts from the gold rush of 1836, including gold nuggets, gold coins, and gold panning equipment, as well as an educational film and gift shop.
The Georgia Gold Rush was the second significant gold rush in the United States and the first in Georgia, and overshadowed the previous rush in North Carolina. It started in 1829 in present-day Lumpkin County near the county seat, Dahlonega, and soon spread through the North Georgia mountains, following the Georgia Gold Belt. By the early 1840s, gold became difficult to find. Many Georgia miners moved west when gold was found in the Sierra Nevada in 1848, starting the California Gold Rush. Since the 16th century, American Indians in Georgia told European explorers that the small amounts of gold which they possessed came from mountains of the interior. Some poorly documented accounts exist of Spanish or French mining gold in North Georgia between 1560 and 1690, but they are based on supposition and on rumors passed on by Indians. In summing up known sources, W.S. Yeates observed: "Many of these accounts and traditions seem to be quite plausible. Nevertheless, it is hardly probable that the Spaniards would have abandoned mines which were afterwards found to be quite profitable, as those in North Georgia."
In the United States, gold mining has taken place continually since the discovery of gold at the Reed farm in North Carolina in 1799. The first documented occurrence of gold was in Virginia in 1782. Some minor gold production took place in North Carolina as early as 1793, but created no excitement. The discovery on the Reed farm in 1799 which was identified as gold in 1802 and subsequently mined marked the first commercial production.
Gold mining in Alaska, a state of the United States, has been a major industry and impetus for exploration and settlement since a few years after the United States acquired the territory in 1867 from the Russian Empire. Russian explorers discovered placer gold in the Kenai River in 1848, but no gold was produced. Gold mining started in 1870 from placers southeast of Juneau, Alaska.
Recreational gold mining and prospecting has become a popular outdoor recreation in a number of countries, including New Zealand, Australia, South Africa, Wales, in Canada and in the United States especially. Recreational mining is often small-scale placer mining but has been challenged for environmental reasons. The disruption of old gold placer deposits risks the reintroduction of post gold rush pollution, including mercury in old mining deposits and mine tailings.
The case of Woodruff v. North Bloomfield Gravel Mining Company was a lawsuit brought to California courts in 1882 where a group of local farmers sued North Bloomfield Mining and Gravel Company over damages caused to farmland in the Central Valley. The farmers who brought the suit claimed that the company's hydraulic mining operations resulted in the disposal of excess sediment, debris, and chemicals in local rivers. Prosecutors argued that the debris raised river beds and restricted flow in the rivers leading to heavy man-made flooding. In the years prior, flooding of debris and chemicals had destroyed a large portion of the valley's agriculture.
The Silver Hill Mine was the first silver mine in the United States, later used primarily as a source of lead and zinc. Discovered during the Carolina gold rush at a Davidson County, North Carolina location later named Silver Hill, operations began at the site in 1839 under the Washington Mining Company. Increasing difficulties extracting the silver from ore heavy in lead and zinc led to the introduction of various new metallurgical processes and equipment. These were unable to fully stem losses of silver in refinement, and an increasingly convoluted production chain led to closure of the mine in 1852.
