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造型优美的钟乳状孔雀石一般都生长在地下的空洞里,它是原生含铜矿物氧化后经过淋滤作用最后沉积结晶而成。孔雀石晶形呈细针状,通常以放射状由中心向外缘构成钟乳状、肾状、葡萄状集合体形态产出。钟乳状孔雀石常见于洞顶和洞壁上,这是由于含碳酸铜溶液在重力作用下淋滤渗透的结果。钟乳状孔雀石一般长几厘米到十几厘米,其末端多为圆形,很少为圆锥形;其横断面为圆形或椭圆形,直径0.3～2厘米不等。圆心常具有0.5～2毫米的圆形或扁圆形
The graceful bell-shaped malachite generally grows underground in the hollow, it is the primary copper-containing minerals after oxidation by the final deposition of crystallization and crystallization. Malachite crystal fine needle-shaped, usually radially from the center to the outer edge of the composition of bell-shaped, kidney-shaped, grape-shaped aggregate output. Bell milk malachite common in the top and cave walls, which is due to the solution containing copper carbonate leaching infiltration under the action of gravity. Bell malachite generally grow a few centimeters to ten centimeters, the end of mostly round, rarely conical; its cross-section is round or oval, diameter of 0.3 to 2 cm. The center of the circle usually has a circle of 0.5 to 2 mm or oblate