Hemimorphite is known for its unique crystal structure, which sets it apart from many other minerals. The crystals can vary in color and may be transparent, translucent, or opaque. Common colors include white, yellow, blue, green, and gray, with blue being the most sought after.
One of the distinctive characteristics is its botryoidal or globular habit. This means that it often forms rounded, bubbly-looking aggregates with a smooth, waxy, or vitreous luster. These formations can resemble bunches of grapes or cauliflower-like clusters.
Hemimorphite is primarily composed of zinc, silicon, oxygen, and hydrogen. It forms in the oxidation zones of zinc ore deposits, where it occurs as a secondary mineral. It is commonly associated with other minerals such as smithsonite, calcite, and willemite.
This mineral has been found in various locations around the world, including the United States, Mexico, Australia, China, and Namibia.
MEASUREMENT DETAILS:
Mineral #1 - 3" L X 2.25" W X 1.50" H
Mineral #2 - 2" L X 2.25" W X 1 1/8" H
Mineral #3 - 1.75" L X 1.25" W X 0.75" H
Mineral #4 - 2.75" L X 2" W X 1" H
Mineral #5 - 1.50" L X 1.75" W X 1" H
