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Implications of geomorphological research for recent and prehistoric avalanches and related hazards at Huascaran, Peru

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11320%2F09%3A00014311" target="_blank" >RIV/00216208:11320/09:00014311 - isvavai.cz</a>

  • Alternative codes found

    RIV/67985891:_____/09:00336510 RIV/00216208:11310/09:00014311

  • Result on the web

    <a href="https://verso.is.cuni.cz/pub/verso.fpl?fname=obd_publikace_handle&handle=PBODTx-enC" target="_blank" >https://verso.is.cuni.cz/pub/verso.fpl?fname=obd_publikace_handle&handle=PBODTx-enC</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1007/s11069-008-9330-7" target="_blank" >10.1007/s11069-008-9330-7</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Implications of geomorphological research for recent and prehistoric avalanches and related hazards at Huascaran, Peru

  • Original language description

    Article gives new evidences for prehistoric rock debris avalanche, its magnitude and related hazard in the area of the Yungay city bellow Huascarán, Peru. Detailed research of superficial deposits below the northern peak of Huascaran (Cordillera Blanca) provides new information on the limits of a paleo-avalanche originating from this mountain. Geomorphological mapping of the sediments identified glacial deposits, deposits from historical rock-debris avalanches and huge boulders from a paleo-avalanche. Schmidt Hammer rock-hardness tests were used to distinguish between the several generations of rock-debris avalanches, but largely failed to distinguish between the much older moraine and the paleo-avalanche sediments. Thus, only the field geomorphological mapping proved to be reliable for identifying the limits of the paleo-avalanche. The limits identified as granite boulders deposited over volcanic rocks were found to extend 30 m further up the opposite valley slope than previously had been mapped. This larger extent implies a greater volume and/or greater mobility for the prehistoric event.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10508 - Physical geography

Result continuities

  • Project

    <a href="/en/project/LC06024" target="_blank" >LC06024: Jaroslav Hájek Center for Theoretical and Applied Statistics</a><br>

  • Continuities

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Others

  • Publication year

    2009

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Natural Hazards

  • ISSN

    0921-030X

  • e-ISSN

  • Volume of the periodical

    50

  • Issue of the periodical within the volume

    1

  • Country of publishing house

    US - UNITED STATES

  • Number of pages

    17

  • Pages from-to

    193-209

  • UT code for WoS article

    000266831100014

  • EID of the result in the Scopus database

    2-s2.0-67649411666