Mineral Point, Wisconsin his family who settled a few miles away from Mineral Point. During the following year, large quantities of galena, or lead ore, were discovered around the settlement in shallow deposits. Lead had many uses at the time, and settlers began to flock to the region hoping to make a living by extracting the easily accessible mineral. Lead deposits extended throughout an area that also included Dubuque, Iowa and Galena, Illinois, but Mineral Point became the center of lead mining operations within the bounds of present-day Wisconsin (then part of Michigan Territory). By 1829, the region's growing population led to the
Broken Hill ore deposit hornblende schists. The ore consists of massive, recrystallised sphalerite-rich, galena-sphalerite and galena-rich sulfide lenses in folded horizons, known as No. 2 Lens Formation and No.3 Lens Formation. Both have distinctive metal ratios and gangue minerals. The ore boundaries are parallel to the bedding planes. According to Gustafson, "There is evidence that the ore has been introduced into an old, already folded, rock and has replaced certain favourable layers of that rock, particle by particle, with large tonnages of garnet, rhodonite, fluorite, marmatite (and wurtzite), galena, and other minerals that constitute the orebodies." The Potosi-Footwall Gneiss is found on both sides