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Teschenite is a type of coarse or medium grained , akin to or , that contains essential . Its name is derived from the region of , where it was discovered. The term crinanite has previously been used as a synonym for teschenite (particularly for deposits with increased analcime content), but there have been attempts to standardise terminology by stopping its use. Rocks related to teschenite are referred to as rocks of the teschenite association.


Geological composition
Teschenite is typically composed of essential -, , and small quantities of and may include ; the presence of analcime is a key characteristic of teschenites and its presence is a factor that differentiates it from other similar rocks.
(1894). 9780559745102, Engelmann. .

Teschenite also has subtypes such as and .


History
Teschenite was first described and named by in 1861. Hohenegger used the term to describe masses of near , which up until that point were listed as a range of minerals, such as , , or , among others. Later in 1866 Hohenegger's definition of the mineral was further refined by Gustav Tschermak, who differentiated between the darker, basalt-like deposits rich in and what is now called teschenite as he identified the former as .

Until 1892 the name in use for the rock was tchesenit, which is derived from the German name for Český Těšín. The name teschenite ( těšínit in Czech) was first used by mineralogist


Location of occurrence
Teschenite has been found in many parts of the world, some examples include Scotland, Portugal, the Caucasus Mountains, , Kenya, Myanmar, Taiwan, Australia and New Zealand.

In the Czech Republic, teschenite is primarily found in the volcanic region of the which stretch from the borders of to regions east of Český Těšín. Specific documented deposits are in Tichá, in the basin of the Ostravice river, in the Řepiště municipality and in a quarry near Žermanice Reservoir. Historically, olivine-rich teschenite has also been mined in an old quarry in Straník.


See also

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