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2.35" Green Kolwezite on Vibrant Cobaltoan Dolomite - DR Congo
This is a glistening cobaltoan (cobalt-bearing) dolomite crystal cluster that features an aggregation of rare, sage green, acicular kolwezite crystals coating many of the cobaltoan dolomite crystals. It was collected from the Kansalawile Open Pit at the Tenk-Fungurume Mines, located in the Democratic Republic of the Congo.
Comes with an acrylic display stand.
Comes with an acrylic display stand.
Dolomite is an anhydrous carbonate mineral composed of calcium magnesium carbonate (CaMg(CO3)2).
The mineral dolomite crystallizes in the trigonal-rhombohedral system. It forms white, tan, gray, or pink crystals. Dolomite is a double carbonate, having an alternating structural arrangement of calcium and magnesium ions. It does not rapidly dissolve in dilute hydrochloric acid as calcite does. Crystal twinning is common.
Dolomite was first described by Carl Linnaeus in 1768, and in 1791 it was described as a rock by the French naturalist and geologist Déodat Gratet de Dolomieu. He first recognized the material in buildings of the old city of Rome, and later as samples collected in the mountains known as the Dolomite Alps of northern Italy.
The mineral dolomite crystallizes in the trigonal-rhombohedral system. It forms white, tan, gray, or pink crystals. Dolomite is a double carbonate, having an alternating structural arrangement of calcium and magnesium ions. It does not rapidly dissolve in dilute hydrochloric acid as calcite does. Crystal twinning is common.
Dolomite was first described by Carl Linnaeus in 1768, and in 1791 it was described as a rock by the French naturalist and geologist Déodat Gratet de Dolomieu. He first recognized the material in buildings of the old city of Rome, and later as samples collected in the mountains known as the Dolomite Alps of northern Italy.
SPECIES
Kolwezite & Dolomite var. Cobalt-Bearing
LOCATION
Kansalawile Open Pit, Tenk-Fungurume Mines, Lualaba, Democratic Republic of the Congo
SIZE
2.35 x 2.2"
CATEGORY
ITEM
#305706
