California produced more than 106 million
troy ounces of gold between 1848 and 1965, of which the Mother Lode district contributed more than 13 million ounces through 1959. Three successive extraction methods dominated:
placer mining from 1848 (panning and sluicing surface gravels),
hydraulic mining from the 1850s (high-pressure water jets eroding gold-bearing gravel banks), and hard-rock
lode mining from the 1860s onward (underground tunnels following quartz veins). Lode mining became the dominant source from the 1880s to 1918;
dredge operations began in 1898 and continued through the 1960s. The
Empire Mine in
Grass Valley, the state's longest-operating gold mine (1850–1956), produced 5.8 million ounces from 367 miles of underground passages. The term "mother lode" has been applied to principal ore deposits worldwide. The
veta madre of
Guanajuato, Mexico, a
epithermal silver vein system discovered in 1548, produced an estimated 37,000 metric tonnes of silver between 1701 and 2004. In Australia, the goldfields at
Ballarat and
Bendigo in
Victoria yielded more than 22 million ounces of gold after their discovery in 1851, though their geology — gold in quartz saddle reefs within folded
Ordovician sandstone — differs from the fault-hosted veins of the California Mother Lode. The
Witwatersrand basin in South Africa, source of an estimated 40 percent of all gold ever mined, contains gold in
Precambrian sedimentary
conglomerate rather than hydrothermal veins. In the
Klondike district of
Yukon, Canada, more than 20 million ounces of placer gold have been recovered since 1896, but the bedrock source — the mother lode in its literal sense — has never been found. == In popular culture ==