Itacolumite

A photograph of a slab of Itacolumite

Itacolumite is a naturally occurring sandstone that is flexible when cut into relatively thin slabs. It occurs at Itacolomi, its eponym, in the southern portion of Minas Gerais, Brazil. The stone is porous, and often yellow in color. It is also found in Kaliana village (Charkhi Dadri district, Haryana, India),[1] the U.S. state of Georgia, and Stokes and McDowell counties of North Carolina. It is the best and most widely known example of a flexible sandstone, and is a source of diamonds found in the Minas Gerais area of Brazil.[2]

On the split faces of the slabs, scales of greenish mica are visible, but in other respects, the rock seems to be a remarkably pure specimen consisting of quartz. If a slab measuring 30-60 centimetres long and few centimetres thick is cut and then placed so that it is supported at its ends only, it will gradually bend due to its own weight. If it is then turned over it will straighten and bend in the opposite direction. Flakes a millimetre or two thick can be bent between the fingers and are said to give out a creaking sound, but specimens showing this property form only a small part of the whole mass of the rock.[2]

  1. ^ Kumar, P.; Sharma, M.C.; Singh, Y; Singh, N.; Kumar, P.; Chopra, S. (2019). "Itacolumite (Flexible Sandstone) From Kaliana, Charkhi Dadri District, Haryana, India". Journal of the Geological Society of India. 93 (3): 278–284. doi:10.1007/s12594-019-1174-0. S2CID 135301911.
  2. ^ a b One or more of the preceding sentences incorporates text from a publication now in the public domainFlett, John Smith (1911). "Itacolumite". In Chisholm, Hugh (ed.). Encyclopædia Britannica. Vol. 14 (11th ed.). Cambridge University Press. p. 887.

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