Bloodstone (African Bloodstone)

African Bloodstone’s unique color pattern results from specific mineral inclusions, while its formation requires unique geological conditions. The green base of African Bloodstone is rich in chlorite and sometimes amphibole minerals, which give it the characteristic dark green color. The hallmark red spots are caused by iron oxide (often hematite). These inclusions form due to iron-rich minerals present in groundwater or surrounding rock, which oxidize and create the vibrant red flecks over thousands or even millions of years. African Bloodstone is typically found in hydrothermal veins, sedimentary beds, and alluvial deposits.

These formations occur when silica-rich solutions percolate through cracks in the Earth’s crust, depositing minerals like quartz and chalcedony. The high iron content in the surrounding rock leads to the red spots as iron oxidizes in contact with air or water. African Bloodstone is primarily mined in regions across Africa, with significant deposits in South Africa, Madagascar, and Namibia. These regions provide the necessary geological conditions for its formation, such as silica-rich deposits and iron-bearing mineral environments. African Bloodstone has a rich history that dates back centuries, entwined with myths and cultural traditions worldwide.

While the stone’s colors are stable, long periods in direct sunlight can reduce its luster.