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[[File:Kämmenkivi stone in Pisa, Kuopio, Finland.jpg|thumb|''Kämmenkivi'' stone on the Pisa hill in [[Kuopio]], Finland]] |
[[File:Kämmenkivi stone in Pisa, Kuopio, Finland.jpg|thumb|''Kämmenkivi'' stone on the Pisa hill in [[Kuopio]], Finland]] |
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In [[geology]], a '''boulder''' (or rarely '''bowlder''')<ref>{{Cite book |title= |
In [[geology]], a '''boulder''' (or rarely '''bowlder''')<ref>{{Cite book |title=Webster's New International Dictionary of the English Language |publisher=G. & C. Merriam Company |year=1913 |location=Springfield, Massachusetts}}</ref> is a [[rock (geology)|rock]] fragment with size greater than {{Convert|25.6|cm|in|1|abbr=on}} in diameter.<ref name="Glossary2005">{{cite book | title=Glossary of Geology | publisher=American Geological Institute | editor-last1=Neuendorf | editor-first1=K.K.E. | editor-last2=Mehl | editor-first2=J.P. Jr. | editor-last3=Jackson | editor-first3=J.A. | year=2005 | location=Alexandria, Virginia | page=79 | isbn=978-0922152896| edition=5th }}</ref> Smaller pieces are called [[cobble (geology)|cobbles]] and [[pebble]]s. While a boulder may be small enough to move or roll manually, others are extremely massive.<ref name="Boulder">{{cite dictionary|title=Boulder|url=http://dictionary.reference.com/browse/boulder|dictionary=[[Dictionary.com]]|access-date=24 August 2013}}</ref> In common usage, a boulder is too large for a person to move. Smaller boulders are usually just called [[rock (geology)|rock]]s or stones. |
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== Etymology == |
== Etymology == |
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Revision as of 23:42, 5 July 2024
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In geology, a boulder (or rarely bowlder)[1] is a rock fragment with size greater than 25.6 cm (10.1 in) in diameter.[2] Smaller pieces are called cobbles and pebbles. While a boulder may be small enough to move or roll manually, others are extremely massive.[3] In common usage, a boulder is too large for a person to move. Smaller boulders are usually just called rocks or stones.
Etymology
The word boulder derives from boulder stone, from Middle English bulderston or Swedish bullersten.[4]
About
In places covered by ice sheets during ice ages, such as Scandinavia, northern North America, and Siberia, glacial erratics are common. Erratics are boulders picked up by ice sheets during their advance, and deposited when they melt.[3] These boulders are called "erratic" because they typically are of a different rock type than the bedrock on which they are deposited. One such boulder is used as the pedestal of the Bronze Horseman in Saint Petersburg, Russia.
Some noted rock formations involve giant boulders exposed by erosion, such as the Devil's Marbles in Australia's Northern Territory, the Horeke basalts in New Zealand, where an entire valley contains only boulders, and The Baths on the island of Virgin Gorda in the British Virgin Islands.
Boulder-sized clasts are found in some sedimentary rocks, such as coarse conglomerate and boulder clay.
See also
- Bouldering, free climbing performed on small rock formations or artificial climbing walls
- Moeraki Boulders, unusually large spherical boulders found in New Zealand
- Monolith, a geological feature consisting of a single massive rock
References
- ^ Webster's New International Dictionary of the English Language. Springfield, Massachusetts: G. & C. Merriam Company. 1913.
- ^ Neuendorf, K.K.E.; Mehl, J.P. Jr.; Jackson, J.A., eds. (2005). Glossary of Geology (5th ed.). Alexandria, Virginia: American Geological Institute. p. 79. ISBN 978-0922152896.
- ^ a b "Boulder". Dictionary.com. Retrieved 24 August 2013.
- ^ boulder. (n.d.) Online Etymology Dictionary. Retrieved December 9, 2011, from Dictionary.com website.
External links
Media related to Boulders at Wikimedia Commons
