Cryogenic Cave Pearls In the Periglacial Zones of Ice Caves
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61389005%3A_____%2F13%3A00390419" target="_blank" >RIV/61389005:_____/13:00390419 - isvavai.cz</a>
Alternative codes found
RIV/67985831:_____/13:00390419
Result on the web
<a href="http://dx.doi.org/10.2110/jsr.2013.16" target="_blank" >http://dx.doi.org/10.2110/jsr.2013.16</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.2110/jsr.2013.16" target="_blank" >10.2110/jsr.2013.16</a>
Alternative languages
Result language
angličtina
Original language name
Cryogenic Cave Pearls In the Periglacial Zones of Ice Caves
Original language description
The Carpathian Mountains across Slovakia and Romania are home of several ice caves located at elevations between 700 and 1,200 m above sea level (asl). Although the mean surface annual temperature is above the freezing point, perennial ice deposits are common in caves and shafts with certain morphologies (large entrances followed by steep vertical or downward-sloping passages), into which the dense cold winter air sinks and remains trapped all year round. A particular type of cave pearls (cryogenic cavepearls, CCPs) occur in spatially restricted accumulations or extensive pearl fields (layers locally up to 0.5 m in thickness) within the scree covering the cave floor in the periglacial zone of these caves. The temperature in the periglacial zone oscillates around the freezing point, promoting seasonal ice formation. A similar type of pearl is observed in the entrance section of other caves that experience temporary freezing conditions during the cold season. When compared to pearls of
Czech name
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Czech description
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Classification
Type
J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)
CEP classification
DB - Geology and mineralogy
OECD FORD branch
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Result continuities
Project
<a href="/en/project/GAP210%2F10%2F1760" target="_blank" >GAP210/10/1760: Cryogenic cave carbonates: Mechanisms of formation and relationship to permafrost depth</a><br>
Continuities
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Others
Publication year
2013
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Journal of Sedimentary Research
ISSN
1527-1404
e-ISSN
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Volume of the periodical
83
Issue of the periodical within the volume
2
Country of publishing house
US - UNITED STATES
Number of pages
14
Pages from-to
207-220
UT code for WoS article
000317703200014
EID of the result in the Scopus database
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