Scolecite is a member of the zeolite group, and is closely related to Natrolite and Mesolite. It forms a series with those two minerals, and is the calcium-rich end member. Chemical analysis or optical tests may be required to distinguish Scolecite from Natrolite, and a single crystal may even contain part of each mineral within different zones of the same crystal.
Scolecite can be very brittle, so care should be exercised when handling specimens. Scolecite is named after the Greek term "skolec", which means "worm", alluding to its worm-like reaction to a blowpipe test.
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Crystal Forms & Aggregates
Striking Features
Environment
Uses
Noteworthy Localities
India is the most important producer of Scolecite, where excellent specimens are found in the basalts of the Deccan Traps in the state of Maharashtra. The districts that have produced excellent Scolecite include Nasik, Pune (Poona), Ahmadnagar, Jalgaon, and Mumbai. A recent outstanding find of large radiating clusters associated with Stilbite is Rankhamb, Maharashtra, India.
Other worldwide localities include the Das Antas tunnel, Veranópolis, Rio Grande Do Sul, Brazil; Teigarhorn, Berufjördur, Iceland; Arvigo, Grisons, Switzerland; and several deposits in the Ossola Valley, Piedmont, Italy. In the U.S., Scolecite come from Elk Mountain, northeast of Pigeon Springs, Cowlitz Co., Washington.
