Morphological analysis and features of the landslide dams in the Cordillera Blanca, Peru

Result code in IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F86652079%3A_____%2F18%3A00490957" target="_blank" >RIV/86652079:_____/18:00490957 - isvavai.cz</a>

Alternative codes found

RIV/00216208:11310/18:10382116

Result on the web

<a href="http://dx.doi.org/10.1007/s10346-017-0888-6" target="_blank" >http://dx.doi.org/10.1007/s10346-017-0888-6</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1007/s10346-017-0888-6" target="_blank" >10.1007/s10346-017-0888-6</a>

Result language

angličtina

Original language name

Morphological analysis and features of the landslide dams in the Cordillera Blanca, Peru

Original language description

Global warming in high mountain areas has led to visible environmental changes as glacial retreat, formation and evolution of moraine dammed lakes, slope instability, and major mass movements. Landslide dams and moraine dams are rather common in the Cordillera Blanca Mountains Range, Peru, and have caused large damages and fatalities over time. The environmental changes are influencing the rivers' and dams' equilibrium, and the potential induced consequences, like catastrophic debris flows or outburst floods resulting from dam failures, can be major hazards in the region. The studies of past landslide dam cases are essential in forecasting induced risks, and specific works on this topic were not developed in the study region. Reflecting this research gap, a database of 51 cases and an evolution study of landslide dams in the Cordillera Blanca Mountains is presented. The main morphometric parameters and information of the landslide, the dam body, the valley, and the lake, if any, have been determined through direct and indirect survey techniques. Low variability in some of the main morphometric parameter distributions (valley width and landslide volume) has been shown, most likely due to an environmental control connected to the regional tectonic and glacial history. In order to analyze present and future landslide dam evolution, a morphological analysis was carried out using two recently developed geomorphological indexes employed on the Italian territory. The results of the Cordillera Blanca analysis have been compared with a large Italian landslide dam inventory, highlighting as much the differences as the similarities between the two datasets. The long-term geomorphological evolution changes are evaluated. Many of the stable dams are in disequilibrium with their surrounding environment and their classification result is of 'uncertain determination.'

Czech name

—

Czech description

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Type

J_imp - Article in a specialist periodical, which is included in the Web of Science database

CEP classification

—

OECD FORD branch

10505 - Geology

Project

<a href="/en/project/LO1415" target="_blank" >LO1415: CzechGlobe 2020 – Development of the Centre of Global Climate Change Impacts Studies</a><br>

Continuities

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

Publication year

2018

Confidentiality

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

Name of the periodical

Landslides

ISSN

1612-510X

e-ISSN

—

Volume of the periodical

15

Issue of the periodical within the volume

3

Country of publishing house

DE - GERMANY

Number of pages

15

Pages from-to

507-521

UT code for WoS article

000426656100011

EID of the result in the Scopus database

2-s2.0-85029146802