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clastic

American  
[klas-tik] / ˈklæs tɪk /

adjective

  1. Biology. breaking up into fragments or separate portions; dividing into parts.

  2. pertaining to an anatomical model made up of detachable pieces.

  3. Geology. noting or pertaining to rock or rocks composed of fragments or particles of older rocks or previously existing solid matter; fragmental.


clastic British  
/ ˈklæstɪk /

adjective

  1. (of sedimentary rock, etc) composed of fragments of pre-existing rock that have been transported some distance from their points of origin

  2. biology dividing into parts

    a clastic cell

  3. able to be dismantled for study or observation

    a clastic model of the brain

"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

Other Word Forms

Etymology

Origin of clastic

1870–75; < Greek klastós broken in pieces ( klas- variant stem of klân to break + -tos verbal adjective suffix) + -ic

Vocabulary lists containing clastic

Example Sentences

Examples are provided to illustrate real-world usage of words in context. Any opinions expressed do not reflect the views of Dictionary.com.

See Examples For:

These are mostly unmetamorphosed clastic rocks deposited in rivers and lakes during the middle Proterozoic, at around 1,400 Ma, while Laurentia was still part of the supercontinent Columbia.

From Textbooks Jan. 1, 2015

In both cases, the rocks are mostly clastic, with both terrestrial and marine deposition.

From Textbooks Jan. 1, 2015

While clastic and carbonate sediments were accumulating along the western edge of Laurentia, much of the interior of the continent was submerged under inland seas that were connected to ocean most of the time.

From Textbooks Jan. 1, 2015

It’s important not to assume that mechanical weathering leads only to clastic sedimentary rocks, while chemical weathering leads only to chemical sedimentary rocks.

From Textbooks Jan. 1, 2015

The original clastic characters of the strata are obscured and the rocks between Arrochar and Inverarnan in Glen Falloch merge into quartz-biotite gneisses and albite schists.

From Encyclopaedia Britannica, 11th Edition, Volume 8, Slice 8 "Dubner" to "Dyeing" by Various

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