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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

  • Czech description

Classification

  • Type

    J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)

  • CEP classification

    DB - Geology and mineralogy

  • OECD FORD branch

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

  • 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