description Chabazite Overview
Chabazite is a zeolite mineral that usually occurs as clear, white, pink, or pale-colored crystals in cavities of volcanic rocks. Its crystals commonly have rhombohedral forms that can appear pseudo-cubic, and its structure contains channels capable of holding exchangeable ions and water. Those properties make chabazite relevant to mineral collectors and to technical uses involving ion exchange, adsorption, and molecular separation.
help Chabazite FAQ
What is chabazite?
Chabazite is a zeolite mineral that commonly forms in cavities in volcanic rocks. Its crystals may be clear, white, pink, or another pale color.
What shape do chabazite crystals have?
Chabazite crystals commonly have rhombohedral forms that can look almost cubic. Their appearance can therefore resemble a cube even though the underlying crystal form is different.
Why is chabazite considered a zeolite?
Its structure contains channels and spaces that can hold exchangeable ions and water. That open framework is a key feature of zeolite minerals and gives them useful ion-exchange properties.
Where does chabazite usually occur?
It is usually found lining cavities and cracks in volcanic rocks. The mineral forms when mineral-rich fluids alter or fill spaces in the rock.
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