“Cave pearl”的意思、由来-开放百科全书

A cave pearl is a small, usually spherical, speleothem (cave formation) found in limestone caves. Cave pearls are formed by a concretion of calcium salts that form concentric layers around a nucleus. Exposure to moving water polishes the surface of cave pearls, making them glossy; if exposed to the air, cave pearls can degrade and appear rough.

Composition

A cave pearl is composed primarily of calcite. Cave pearls are generally not considered to be a type of oolite. Other minerals found in small quantities in cave pearls include quartz, apatite, iron, aluminum, and magnesium.^[1]{{Dead link|date=February 2019}}^[2]

Formation

Cave pearls form when water dripping into a cave loses carbon dioxide and precipitates calcite. A cave pearl forms when the water is moving too vigorously to form a stalagmite. A nucleus of matter (such as a grain of sand) becomes coated with calcite, and the current then provides a rotation to the nucleus in such a way that it is coated evenly. In this manner, concentric layers build up over time, in much the same way that a biological pearl forms within a mollusc. There may be microbial action involved in the formation of cave pearls.^[3]

The existence of an actual pool may not be necessary for cave pearls to form, as long as the deposit is kept wet and agitated by water dripping or trickling through.^[4]{{Dead link|date=February 2019}} If the cave pearl sinks to the bottom of a pool or is otherwise in direct contact with moving water, the motion of the water buffs it to a high gloss. Although the motion of the water often keeps cave pearls from adhering, sometimes cave pearls will stick to one another or to the bottom of a pool.

Nucleus

A cave pearl forms around a nucleus of matter. The nucleus of a cave pearl is typically very small, such as a grain of sand, but can be larger.^[5]{{Dead link|date=February 2019}} Some nuclei are made of foreign matter (such as quartz sand, wood, bone, or even plastic), whereas others are made of calcified clay or limestone.^[1]

Shape

Cave pearls are usually spherical but can also have other shapes. The reason cave pearls tend to be round is not their rotation, but rather that their growth is steady and uniform. Because a spherical shape allows the greatest amount of deposition for the smallest surface area, a cave pearl tends to end up spherical even if its nucleus is highly irregular. Sometimes several cave pearls stick together to form a shape that resembles a bunch of grapes. In addition to the typical spherical shape, cave pearls can be cylindrical, elliptical, cubical, hexagonal, discoid, or irregular.^[6]

Size

Most cave pearls are smaller than {{convert|1|cm|abbr=on}} wide. Large cave pearls grow as big as {{convert|20|cm|abbr=on}} in diameter. The world's largest cave, Son Doong Cave in Vietnam, has cave pearls "the size of baseballs".^[7]

Frequency

Cave pearls are relatively common in caves but are typically present in low abundance.

In Tabasco, Mexico, the Gruta de las Canicas (Cave of the Marbles) is highly unusual in that it contains a tremendous quantity of pearls: an estimated 200 million pearls were discovered on the cave floor, in some areas to a depth of a meter or more. The mechanism for the formation of this vast quantity of pearls has not been determined.^[2]

The Rookery, in Carlsbad Caverns, New Mexico, has so many cave pearls that they were at one time handed out to visitors as souvenirs.^[6]

References

1. ^¹{{cite journal|last=|first=|date=1956|title=|url=http://www.karstportal.org/FileStorage/NSS_news/1956-v014-008.pdf|journal=NSS News|publisher=National Speleological Society|volume=14|issue=8|pages=|via=}}
2. ^¹{{Cite journal|last=Houston|first=Shari|last2=Mozley|first2=Peter S.|last3=Campbell|first3=Andrew R.|last4=Boston|first4=Penny|date=|title=Petrology and Chemistry of Cave Pearls from Gruta De Las Canicas (Cave of the Marbles), Tabasco, Mexico|url=https://gsa.confex.com/gsa/2008AM/finalprogram/abstract_150967.htm|dead-url=|journal=Abstracts with Programs|publisher=Geological Society of America|volume=40|issue=6|pages=479|archive-url=|archive-date=|via=}}
3. ^{{cite journal|last=Onac|first=Bogdan P.|last2=Forti|first2=Paolo|date=July 2011|title=Minerogenetic mechanisms occurring in the cave environment: an overview|url=http://scholarcommons.usf.edu/cgi/viewcontent.cgi?article=1016&context=ijs|journal=International Journal of Speleology|volume=40|issue=2|pages=79–98|doi=10.5038/1827-806X.40.2.1|via=}}
4. ^{{cite journal|last=|first=|date=1958|title=|url=http://www.karstportal.org/FileStorage/NSS_news/1958-v016-010.pdf|journal=NSS News|publisher=National Speleological Society|volume=16|issue=10|pages=|via=}}
5. ^{{cite journal|last=|first=|date=1955|title=|url=http://www.karstportal.org/FileStorage/NSS_news/1955-v013-010.pdf|journal=NSS News|publisher=National Speleological Society|volume=13|issue=10|pages=|via=}}
6. ^¹{{cite web|url=http://www2.nature.nps.gov/views/KCs/CaveKarst/HTML/ET_Underground.htm|title=Underground: What and Who are in Caves?|last=|first=|date=|website=|publisher=National Park Service|archiveurl=https://web.archive.org/web/20130225044147/http://www2.nature.nps.gov/views/KCs/CaveKarst/HTML/ET_Underground.htm|archivedate=February 25, 2013|deadurl=yes|accessdate=September 9, 2013}}
7. ^{{cite web|url=http://ngm.nationalgeographic.com/2011/01/largest-cave/jenkins-text/1|title=Vietnam Cave|last=Jenkins|first=Mark|date=January 2011|website=National Geographic|page=7|archive-url=https://web.archive.org/web/20101220095335/http://ngm.nationalgeographic.com/2011/01/largest-cave/jenkins-text/1|archive-date=December 20, 2010|dead-url=Yes|access-date=}}