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conchoidal

[kong-koid-l]

adjective

Mineralogy.
  1. noting a shell-like fracture form produced on certain minerals by a blow.



conchoidal

/ kɒŋˈkɔɪdəl /

adjective

  1. (of the fracture of minerals and rocks) having smooth shell-shaped convex and concave surfaces

  2. (of minerals and rocks, such as flint) having such a fracture

“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

conchoidal

  1. Of or relating to a mineral or rock surface that is characterized by smooth, shell-like curves. Obsidian and quartz often have conchoidal fractures.

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Other Word Forms

  • conchoidally adverb
  • subconchoidal adjective
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Word History and Origins

Origin of conchoidal1

First recorded in 1660–70; conchoid + -al 1
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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.

These include the ‘conchoidal’ flaking that leaves a distinctive percussion mark; the production of several flakes from a single core, and the use of specific patterns of flake removal.

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Around the summit of Mount Tarn the ground is bare, but so covered with small decomposed fragments, that the solid rock only appears occasionally: it is very hard, and breaks with a conchoidal fracture: some of the specimens which we detached bore indistinct impressions of organic remains.

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The fracture of this stone has in all instances been found to be irregularly conchoidal, and on exposure to the atmosphere and subjection to fire it crumbled to pieces.

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The two legs of a hyperbolic branch may belong to different asymptotes, and in this case we have the forms which Newton 660 calls inscribed, circumscribed, ambigene, &c.; or they may belong to the same asymptote, and in this case we have the serpentine form, where the branch cuts the asymptote, so as to touch it at its two extremities on opposite sides, or the conchoidal form, where it touches the asymptote on the same side.

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It is of black colour; its fracture is conchoidal, and it has a lustrous surface.

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