Difference between revisions of "Concretion"
Jump to navigation
Jump to search
m (Text replace - "== Authority ==" to "== Sources Checked for Data in Record ==") |
|||
Line 20: | Line 20: | ||
</gallery> | </gallery> | ||
− | + | ==Resources and Citations== | |
− | == | ||
* G.S.Brady, ''Materials Handbook'', McGraw-Hill Book Co., New York, 1971 | * G.S.Brady, ''Materials Handbook'', McGraw-Hill Book Co., New York, 1971 |
Revision as of 11:04, 4 July 2022
Description
In geology, concretion is an anomalous mass of mineral matter found in Sandstone, Clay, or other Sedimentary rock. Concretions are form by the deposition of Silica, Calcite, Gypsum, or other chemical compound. They are often found in concentric layers surrounding an original nucleus.
Synonyms and Related Terms
agglomerate; concrétion (Fr.);concrecion (Esp.); concreção (Port.); Konkretion (Deut.); concretie (Ned.)
Additional Images
Resources and Citations
- G.S.Brady, Materials Handbook, McGraw-Hill Book Co., New York, 1971
- Van Nostrand's Scientific Encyclopedia, Douglas M. Considine (ed.), Van Nostrand Reinhold, New York, 1976
- Random House, Webster's Encyclopedic Unabridged Dictionary of the English Language, Grammercy Book, New York, 1997
- The American Heritage Dictionary or Encarta, via Microsoft Bookshelf 98, Microsoft Corp., 1998