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