˜yÐÄvlog

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pegmatite

[ peg-muh-tahyt ]

noun

Petrology.
  1. a coarsely crystalline granite or other high-silica rock occurring in veins or dikes.


pegmatite

/ ˈpɛɡməˌtaɪt; ˌpɛɡməˈtɪtɪk /

noun

  1. any of a class of exceptionally coarse-grained intrusive igneous rocks consisting chiefly of quartz and feldspar: often occurring as dykes among igneous rocks of finer grain
“Collins English Dictionary — Complete & Unabridged†2012 Digital Edition © William Collins Sons & Co. Ltd. 1979, 1986 © HarperCollins Publishers 1998, 2000, 2003, 2005, 2006, 2007, 2009, 2012

pegmatite

/ ±èÄ•²µâ€²³¾É™-³ÙÄ«³Ù′ /

  1. Any of various coarse-grained igneous rocks that often occur as wide veins cutting across other types of rock. Pegmatites form from water-rich magmas or lavas that cool slowly, allowing the crystals to grow to large sizes. Although pegmatites can be compositionally similar to a number of rocks, they most often have the composition of granite.
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Derived Forms

  • pegmatitic, adjective
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Other ˜yÐÄvlog Forms

  • ±è±ð²µÂ·³¾²¹Â·³Ù¾±³Ù·¾±³¦ [peg-m, uh, -, tit, -ik], adjective
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˜yÐÄvlog History and Origins

Origin of pegmatite1

1825–35; < Greek ±èŧ²µ³¾²¹³Ù- (stem of ±èê²µ³¾²¹ ) anything fastened together, a bond (compare ±èŧ²µ²Ôý±ð¾±²Ô to stick) + -ite 1
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˜yÐÄvlog History and Origins

Origin of pegmatite1

C19: from Greek pegma something joined together
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Example Sentences

Examples have not been reviewed.

Primary sources for lithium like pegmatites and volcanic clays are well understood, but finding other stores that are safe and economical to exploit would be helpful.

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The pegmatites in the Spruce Pine Mineral District, an area about 25 miles long and 10 miles wide, were formed hundreds of millions of years ago under intense heat and pressure.

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Some of the most visually striking – the emeralds, garnets, topazes and aquamarines that Busse seeks – are pegmatites that form when magma forces its way into underground cracks, then cools slowly.

From

Piedmont Lithium says it would be the nation’s only hard-rock mine, extracting lithium from a mineral, spodumene, that is found in rock called pegmatite.

From

The resulting folds are easy to see, because molten pegmatite penetrated the voids.

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