Mineral Resource of the Month: Zeolites

by U.S. Geological Survey
Friday, October 3, 2014

Robert Virta, a mineral commodity specialist for the U.S. Geological Survey, prepared the following information about the zeolite industry.

Chabazite is a common natural zeolite mineral. Credit: ©Didier Descouens, CC BY-SA 3.0.

Zeolites comprise a group of silicate minerals with very open crystalline structures that make them suitable for catalytic, ion exchange and molecular sieving applications. Aluminum, silicon and oxygen atoms are arranged in a 3-D framework of channels and cages. Water molecules and cations, such as calcium, sodium, potassium and magnesium, occupy these interconnected channels and cages. The cations can readily substitute for one another, and water molecules may be gained or lost without any major changes to the basic zeolite crystal structure.

For many years, zeolite minerals were thought to be uncommon and found only in vugs and fissures in volcanic rock. In the 1950s and early 1960s, however, zeolites were found in abundance in large deposits of altered volcanic tuff in the western U.S. and in altered volcanogenic marine tuffs in Italy and Japan. Similar deposits were later found worldwide.

Large-scale mining of natural zeolites in the U.S. began in the 1960s, with early efforts focusing on locating natural zeolites suitable for use in petroleum processing. When the materials' performance proved unsatisfactory, other markets were developed. Use in pet litter quickly became the leading market for natural zeolites — accounting for more than 50 percent of usage from the 1960s through 1995 — because of the minerals' capacity to absorb moisture. After 1995, sales of natural zeolites for pet litter began to decline. In 2013, animal feed applications, in which it is used as a flow control agent, dominated the U.S. natural zeolite market, followed by pet litter applications.

Globally, volcanic tuffs containing zeolites are used for high-tonnage applications such as dimension stone, lightweight aggregate, pozzolanic cement and general soil conditioners.

A large market also exists for synthetic zeolites, first created in the 1930s. Researchers looking for new ways to increase the efficiency of petroleum refining in the 1950s used zeolites to catalytically break down large organic molecules into specific petroleum products. In the 1970s, synthetic zeolites began to replace phosphate compounds in laundry detergent powders.

The high cost of synthetic zeolites precludes their use for most natural zeolite applications. Conversely, stringent product specifications prevent the large-scale use of natural zeolites for most synthetic zeolite applications.

For more information on zeolites and other mineral resources, visit: minerals.usgs.gov/minerals/.


In 2013, U.S. production was 69,500 metric tons, and consumption was 68,300 metric tons. Magor U.S. markets for natural zeolites are in animal feed, cement, odor-controlling materials, per litter, wastewater treatment and water-purification applications.

In 2013, world production of natural zeolite was estimated to be 2.7 million to 3.2 million metric tons, with China accounting for more than 70 percent of production.


The name “zeolite” is derived from Greek words meaning “boiling stones” because the minerals frothed when heated to high temperatures.

Zeolites give off heat when rehydrated. An old field test to determine if a rock sample contained zeolites was to see if a rock chip heated up when placed on the tongue.

Zeolites adsorb ethylene and are used to prolong the shelf-life of vegetables and fruit, which emit ethylene as they ripen.

Zeolites were used to adsorb radioactive isotopes from contaminated cooling water spilled at the Fukushima nuclear power plant after the plant was damaged in the March 2011 magnitude-9 earthquake in Japan.

Zeolite minerals have large surface areas because of their open crystal structure — 10 grams of chabazite has roughly the same surface area as a football field (about 5,350 square meters)

© 2008-2021. All rights reserved. Any copying, redistribution or retransmission of any of the contents of this service without the expressed written permission of the American Geosciences Institute is expressly prohibited. Click here for all copyright requests.