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Bentonite usually forms from weathering of volcanic ash, most often in the presence of water. However, the term bentonite, as well as a similar clay called tonstein, have been used for clay beds of uncertain origin. For industrial purposes, two main classes of bentonite exist: sodium bentonite and calcium bentonite.
Bentonite layers from an ancient deposit of weathered volcanic ash tuff in Wyoming Gray shale and bentonites (Benton Shale; Colorado Springs, Colorado). Bentonite (/ ˈ b ɛ n t ə n aɪ t / BEN-tə-nyte) [1] [2] is an absorbent swelling clay consisting mostly of montmorillonite (a type of smectite) which can either be Na-montmorillonite or Ca-montmorillonite.
Underground room and pillar mining began in 1936. Leased storage began in 1986. Used by the U.S. Department of Defense for storage of 10,000,000 MRE meals, by Bridgestone for storage of 400,000 tires, and by Controlled Pharming Ventures for growing tomatoes and corn. Indiana is the Limestone Capital of the world.
The Tioga Bentonites are a series of ash bed layers occurring in three Sedimentary basins in the eastern and midwestern United States. The primary basin they are found in is the Appalachian Basin, as well as the Illinois Basin and the Michigan Basin.
Indiana limestone is a more common term for Salem Limestone, a geological formation primarily quarried in south central Indiana, USA, between the cities of Bloomington and Bedford. It has been called the best quarried limestone in the United States. Indiana limestone, like all limestone, is a rock primarily formed of calcium carbonate.
Bentonite mines (1 C) Pages in category "Bentonite" The following 6 pages are in this category, out of 6 total. This list may not reflect recent changes. ...
Several different types of bentonite can be found; however, potassium bentonite is the main one associated with the Deicke and Millbrig eruptions. The Deicke and Millbrig K-bentonite layers can be found from Alabama to New York to Minnesota. These K-bentonite layers are up to a meter thick in some locations. [8] Such thickness is unique.
The Monument Mountain in Wyandotte Caves, Indiana, is a cluster of large stalagmites on a breakdown pile. The ceiling is a classic tension dome. Wyandotte Caves began to form in the Pliocene Era, about 2 million years ago. [3] Like most of Southern Indiana's caves, the caves were formed when water dissolved limestone, causing hollow caves to form.