Since all Zeolites are alteration products of volcanic glass present in tuff (a rock containing consolidated volcanic ash) or tuff breccia (rock consists of volcanic rocks cemented together by large amount of volcanic ash), the ore does not consist solely of zeolite, and thus it is appropriate to be called zeolite-containing tuff.
Zeolite resources can be found in sedimentary layers or rocks of volcanic ash throughout the world. Natural zeolite deposits have recently been discovered in the Pacific Rim countries, including New Zealand and countries of Mediterranean coast. Among these countries, Japan has been leading the rest of the world in the exploration and development of natural zeolite and has been the world’s major producing countries.
Localities of Natural zeolite in the United States are distributed mainly in the western states such as Oregon, Nevada, California and Idaho. Most of the mines produce clinoptilolite and mordenite
Apart from United States and Japan, zeolite is also discovered in Eastern European countries which include eastern part of Czechoslovakia, the north-eastern part of Hungary, the north-western part of Yugoslavia, and south-eastern part of Bulgaria. And also countries like Italy, Cuba, Brazil, South Africa and China are all recorded as zeolite producing countries.
Australia recently started producing natural zeolite in Werris Creek, South of Tamworth in New South Wales as well as Cranky Corner near Singleton.
Zeolite is purified differently depending on the nature of the ores and is associated to the processes of granulation, drying, milling, screening (sizing) and bagging. Special applications such as filler for high-quality paper, after milling, the zeolite is subject to wet process of bleaching, concentration, filtering and finally drying.
Reference:
Boiling stone (zeolite), Zeolite Dynamics, Lecture Notes.
Roskill Report (1990)
Annual Reports of Various Companies
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