TERRIUM — A mineralogy cabinet


Creedita

Creedita is a mineral with formula Ca₃Al₂(SO₄)(F,OH)(SO₄)₃·2H₂O, in the Sulfatos group. This specimen comes from Mina Navidad, Mapimí, Durango, México and joined the Terrium collection in 2001.

Creedita from Mina Navidad, Mapimí, Durango, México — Terrium

Description

Specimen with a small geode showing internal crystal growth. Intense orange colour, with crystals of good lustre and habit.

History of this specimen

I bought it just after a conversation with Rudolfbel, who has followed my work on LinkedIn for years and turned out to have been director of Mina Navidad from 2019 to 2022, the classic source of creedite. I liked the coincidence and the unexpected connection: we both grew up in coal-mining areas and perhaps knowing from the inside the harshness of that work makes us relate to others in a very similar way. The piece is associated with all this synchronicity.

About Creedita

Creedite is a rare hydrated calcium-aluminium fluorosulphate that forms in the oxidised zones of complex sulphide deposits. It commonly occurs with fluorite because, as the latter partially dissolves, it supplies the fluorine required for crystallisation. Well-crystallised creedite specimens were extremely rare until they were found at Mina Navidad, Mapimí.

About the locality

Mina Navidad is world-famous for its orange creedite. Mining has been irregular, often carried out by "gambusinos" (artisanal miners), and today the availability of high-quality specimens is very limited because it is, in practice, closed to this type of extraction.

Technical data

Catalogue No.
0011
Composition
Ca₃Al₂(SO₄)(F,OH)(SO₄)₃·2H₂O
Name
Creedita
Group
Sulfatos
Category
Asteris Explosio
Matrix
Floater
Mine
Mina Navidad
District / Municipality
Mapimí
Region
Durango
Country
México
Size (cm)
4 x 3 x 3
Weight
17.5 g
Acquired
2001
Ex-collection
Sergio Petretich
Etymology
From English "Creede", the original description locality (Colorado, USA), with the mineral suffix "-ite".
Quality
Muy buena
Value trend
Al alza

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