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diabase

American  
[dahy-uh-beys] / ˈdaɪ əˌbeɪs /

noun

Petrology.
  1. a fine-grained gabbro occurring as minor intrusions.

  2. British. a dark igneous rock consisting essentially of augite and feldspar; an altered dolerite.


diabase British  
/ ˈdaɪəˌbeɪs /

noun

  1. an altered dolerite

  2. another name for dolerite

"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

diabase Scientific  
/ dīə-bās′ /
  1. A dark-gray to black, medium-grained igneous rock consisting mainly of labradorite and pyroxene. Diabase is compositionally similar to andesite, but has coarser grains. It is commonly found in sills and dikes.

  2. Also called dolerite


Other Word Forms

Etymology

Origin of diabase

1810–20; < French, equivalent to dia- (error for di- two) + base base 1

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:

At Carrock Fell, N.E. of Skiddaw, is an extremely interesting complex of volcanic rocks, and in many other places are diabase and other forms, e.g. the well-known rock at Castle Head, Keswick.

From Encyclopaedia Britannica, 11th Edition, Volume 7, Slice 8 "Cube" to "Daguerre, Louis" by Various

The terms diabase and dolerite are employed really to designate distinct facies of the same set of rocks.

From Encyclopaedia Britannica, 11th Edition, Volume 8, Slice 3 "Destructors" to "Diameter" by Various

Numerous rounded diabase bowlders, varying in size from a few inches to several feet in diameter, are also scattered over the surface of the soil.

From History and Comprehensive Description of Loudoun County, Virginia by James William Head

Away from the ranges, the bowlders are generally of some crystalline rock, such as granite and diabase.

From The Geography of the Region about Devils Lake and the Dalles of the Wisconsin by Wallace W. Atwood

The ore minerals are believed to have been deposited by hot solutions emanating from deep magmatic sources after the intrusion of the diabase.

From The Economic Aspect of Geology by C. K. (Charles Kenneth) Leith

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