Difference between revisions of "Travertine"

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[[File:06.1883a-b-E1925CR-d1.jpg|thumb|]]
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[[File:06.1883a-b-E1925CR-d1.jpg|thumb|Offering table<br>MFA # 06.1883a-b]]
 
== Description ==
 
== Description ==
  
A light-colored, porous rock composed primarily of [http://cameo.mfa.org/materials/fullrecord.asp?name=calcite calcite]. Travertine is a variety of [http://cameo.mfa.org/materials/fullrecord.asp?name=limestone limestone] formed from multilayered [http://cameo.mfa.org/materials/fullrecord.asp?name=calcium%20carbonate calcium carbonate] deposits in pools by the slow precipitation of mineral-rich spring water. The "holes" characteristic of travertine were produced by trapped [http://cameo.mfa.org/materials/fullrecord.asp?name=carbon%20dioxide carbon dioxide] bubbles during its formation. Plant residues are often layered with the calcite deposits resulting in large elongated, often interconnected rings in the stone. Very porous, spongy travertine is called [http://cameo.mfa.org/materials/fullrecord.asp?name=tufa tufa]. Travertine polishes to a matte finish. It is used as an interior and exterior building material. Thick deposit of travertine occur near Tivoli, Italy, and Mammoth Hot Springs in Yellowstone National Park. Banded travertine from Mexico is called [http://cameo.mfa.org/materials/fullrecord.asp?name=Mexican%20onyx Mexican onyx] marble.
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A light-colored, porous rock composed primarily of [[calcite|calcite]]. Travertine is a variety of [[limestone|limestone]] formed from multilayered [[calcium%20carbonate|calcium carbonate]] deposits in pools by the slow precipitation of mineral-rich spring water. The "holes" characteristic of travertine were produced by trapped [[carbon%20dioxide|carbon dioxide]] bubbles during its formation. Plant residues are often layered with the calcite deposits resulting in large elongated, often interconnected rings in the stone. Very porous, spongy travertine is called [[tufa|tufa]]. Travertine polishes to a matte finish. It is used as an interior and exterior building material. Thick deposit of travertine occur near Tivoli, Italy, and Mammoth Hot Springs in Yellowstone National Park. Banded travertine from Mexico is called [[Mexican%20onyx|Mexican onyx]] marble.
  
 
[[File:Travertineemr1.jpg|thumb|Travertine]]
 
[[File:Travertineemr1.jpg|thumb|Travertine]]
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tufa limestone; false marble; Mexican onyx; Egyptian alabaster; frådsten (Dan.); kildekalk (Dan.); Travertin (Deut, Fr.); travertino (Esp., It.); (Ned.); (Pol.); (Port.); (Sven.); travertijn (Ned.)
 
tufa limestone; false marble; Mexican onyx; Egyptian alabaster; frådsten (Dan.); kildekalk (Dan.); Travertin (Deut, Fr.); travertino (Esp., It.); (Ned.); (Pol.); (Port.); (Sven.); travertijn (Ned.)
  
== Hazards and Safety ==
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== Risks ==
  
 
No significant hazards. Noncombustible.
 
No significant hazards. Noncombustible.
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[[File:travertinelarge.jpg|thumb|Travertine]]
  
== Additional Images ==
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== Resources and Citations ==
 
 
<gallery>
 
File:travertinelarge.jpg|Travertine
 
</gallery>
 
 
 
 
 
== Sources Checked for Data in Record ==
 
  
 
* Luciana and Tiziano Mannoni, ''Marble: the history of a culture'', Facts on File Publications
 
* Luciana and Tiziano Mannoni, ''Marble: the history of a culture'', Facts on File Publications
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* G.S.Brady, ''Materials Handbook'', McGraw-Hill Book Co., New York, 1971  Comment: p. 386
 
* G.S.Brady, ''Materials Handbook'', McGraw-Hill Book Co., New York, 1971  Comment: p. 386
  
* Website address 1  Comment: http://www.marble-institute.com
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* Website: http://www.marble-institute.com
  
* Wikipedia, the free encyclopedia, at http://www.wikipedia.com  Comment: http://en.wikipedia.org/wiki/Travertine (Accessed Nov. 9, 2005)
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* Wikipedia: http://en.wikipedia.org/wiki/Travertine (Accessed Nov. 9, 2005)
  
 
* Michael McCann, ''Artist Beware'', Watson-Guptill Publications, New York City, 1979
 
* Michael McCann, ''Artist Beware'', Watson-Guptill Publications, New York City, 1979

Latest revision as of 11:54, 22 August 2020

Offering table
MFA # 06.1883a-b

Description

A light-colored, porous rock composed primarily of Calcite. Travertine is a variety of Limestone formed from multilayered Calcium carbonate deposits in pools by the slow precipitation of mineral-rich spring water. The "holes" characteristic of travertine were produced by trapped Carbon dioxide bubbles during its formation. Plant residues are often layered with the calcite deposits resulting in large elongated, often interconnected rings in the stone. Very porous, spongy travertine is called Tufa. Travertine polishes to a matte finish. It is used as an interior and exterior building material. Thick deposit of travertine occur near Tivoli, Italy, and Mammoth Hot Springs in Yellowstone National Park. Banded travertine from Mexico is called Mexican onyx marble.

Travertine

Synonyms and Related Terms

tufa limestone; false marble; Mexican onyx; Egyptian alabaster; frådsten (Dan.); kildekalk (Dan.); Travertin (Deut, Fr.); travertino (Esp., It.); (Ned.); (Pol.); (Port.); (Sven.); travertijn (Ned.)

Risks

No significant hazards. Noncombustible.

Travertine

Resources and Citations

  • Luciana and Tiziano Mannoni, Marble: the history of a culture, Facts on File Publications
  • Anne Grimmer, Glossary of Building Stone Terms, A Glossary of Historic Masonry Deterioration Problems and Preservation Treatments, National Park Service, Washington DC, 1984
  • C.W.Chesterman, K.E.Lowe, Audubon Society Field Guide to North American Rocks and Minerals, Alfred A. Knopf, New York, 1979
  • G.S.Brady, Materials Handbook, McGraw-Hill Book Co., New York, 1971 Comment: p. 386
  • Michael McCann, Artist Beware, Watson-Guptill Publications, New York City, 1979
  • Dictionary of Building Preservation, Ward Bucher, ed., John Wiley & Sons, Inc., New York City, 1996
  • 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