Chlorargyrite

Chlorargyrite, despite being an important ore of silver, is not well-represented in collections. This is because of its general lack of aesthetics, with the bulk of mined material being processed for the extraction of its silver content. Formerly called Cerargyrite, Chlorargyrite is the currently accepted name of this mineral today. An old miners term describing this mineral was Horn Silver.

Chlorargyrite forms a solid solution series with Bromargyrite, which contains the halogen bromine instead of chlorine. Chlorargyrite and Bromargyrite can be visually indistinguishable from one another, and will often form in the same deposits. The intermediary mineral of this series, known as Embolite, is usually considered to be a bromine-rich variety of Chlorargyrite.

Chlorargyrite is named after its chemical composition: "chlor" for chlorine, and "argyros" for the Greek word used for silver. Chlorargyrite often darkens upon exposure to light, and specimens should generally be stored in the dark.

One of the most important localities of Chlorargyrite is the famous silver mine at Broken Hill, New South Wales, Australia. This locality has produced some of the best examples of this mineral, in a lightly-colored, bromium-rich type. In the 1980's, highly regarded collector's examples of this mineral were found in the Kintore open cut of that mine.

In the U.S., unusual cubic Chlorargyrite crystals were found De Lamar Mine, near Silver City, Owyhee Co., Idaho. This find is regarded by many to have produced the most well-crystallized examples of this mineral. Waxy brown coatings of Chlorargyrite have come from Calico, San Bernardino Co., California; and small greasy crystals from the Silver Coin Mine, Valmy, Humboldt Co., Nevada. Other locations in the Western U.S. include Leadville, Lake Co., Colorado; the Tintic District, Utah Co., Utah; and Bisbee and Tombstone, Cochise Co., Arizona.