Angelite (Anhydrite) – Peru

£1.50£8.00 ex VAT

Angelite is a popular trade name for a variety of Anhydrite that is light blue-grey in colour, semi-transparent, fine grained and marketed as gem material. These specimens, along with most angelite, are from Lima, Peru and were collected near the Casapalca Mine at Casapalca, Huarochiri Province, Lima Department, Peru.

 

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  •  Delivery & Return

    Delivery

    We ship to all 50 states, Washington DC.
    All orders are shipped with a UPS tracking number.
    Always free shipping for orders over US $200.
    During sale periods and promotions the delivery time may be longer than normal.

    Return

    Elessi will accept exchanges and returns of unworn and unwashed garments within 30 days of the date of purchase (14 days during the sales period), on presentation of the original till receipt at any store where the corresponding collection is available within the country of purchase.

    Your return will usually be processed within a week to a week and a half. We’ll send you a Return Notification email to notify you once the return has been completed.
    Please allow 1-3 business days for refunds to be received to the original form of payment once the return has been processed.

    Help

    Give us a shout if you have any other questions and/or concerns.
    Email: contact@mydomain.com
    Phone: +1 (23) 456 789

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Angelite is a popular trade name for a variety of Anhydrite that is light blue-grey in colour, semi-transparent, fine grained and marketed as gem material. These specimens, along with most angelite, are from Lima, Peru and were collected near the Casapalca Mine at Casapalca, Huarochiri Province, Lima Department, Peru.

The Casapalca mineral deposits were initially mined to a limited extent by the Spaniards in the 1600s. Over the past century, they have served as a significant source of silver, copper, lead, and zinc. However, amidst these metal deposits, the presence of a unique variety of anhydrite known as “angelite” stands out. Surprisingly, “angelite” formation is unrelated to the metal minerals in the area.

Angelite was created when solutions rich in sulphate interacted with calcite in limestone, leading to the formation of massive anhydrite. This anhydrite possesses a striking blue colour due to trace amounts of divalent (ferrous) iron. These anhydrite formations took shape as nodules within altered limestone layers. Interestingly, when the surface of these anhydrite nodules came into contact with chemically neutral groundwater, they underwent rehydration and transformed into gypsum, resulting in a white coating on “angelite” specimens.

These specimens are ideal for both collectors and educational use, available in a range of sizes. They come supplied in a white card tray with an information label.

Weight N/A
Size

1.5" x 1.5", 2" x 2", 3" x 2", 4" x 3"

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