Reactivation of mass movements in Dessie graben, the example of an active landslide area in the Ethiopian Highlands

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F15%3A10312456" target="_blank" >RIV/00216208:11310/15:10312456 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/67985831:_____/15:00450963 RIV/26619954:_____/15:#0000065

Výsledek na webu

<a href="http://dx.doi.org/10.1007/s10346-015-0613-2" target="_blank" >http://dx.doi.org/10.1007/s10346-015-0613-2</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1007/s10346-015-0613-2" target="_blank" >10.1007/s10346-015-0613-2</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Reactivation of mass movements in Dessie graben, the example of an active landslide area in the Ethiopian Highlands

Popis výsledku v původním jazyce

Dessie town is located in a tectonic depression along the western rift margin with a young, high energy relief. Study area is known for numerous landslides in the past. These landslides are of different types, from shallow soil creeping to huge deep-seated landslides with appreciable consequences. Landslides endanger the quickly growing regional centre of Dessie and its infrastructure. Four typical recent landslides have been selected and studied in detail using both remote sensing and field observations from 2013. The described reactivation and new landslide events have been caused by a combination of natural influences and anthropogenic activities. Since seasonal rainfall is the main external triggering factor, precipitation data from Dessie weatherstation were analysed. The degree of negative human impact on slope instability was also discussed. Endangered zones and the actual risk in the studied localities were identified, and adequate measures were proposed.

Název v anglickém jazyce

Reactivation of mass movements in Dessie graben, the example of an active landslide area in the Ethiopian Highlands

Popis výsledku anglicky

Dessie town is located in a tectonic depression along the western rift margin with a young, high energy relief. Study area is known for numerous landslides in the past. These landslides are of different types, from shallow soil creeping to huge deep-seated landslides with appreciable consequences. Landslides endanger the quickly growing regional centre of Dessie and its infrastructure. Four typical recent landslides have been selected and studied in detail using both remote sensing and field observations from 2013. The described reactivation and new landslide events have been caused by a combination of natural influences and anthropogenic activities. Since seasonal rainfall is the main external triggering factor, precipitation data from Dessie weatherstation were analysed. The degree of negative human impact on slope instability was also discussed. Endangered zones and the actual risk in the studied localities were identified, and adequate measures were proposed.

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DE - Zemský magnetismus, geodesie, geografie

OECD FORD obor

—

Projekt

<a href="/cs/project/GCP209%2F12%2FJ068" target="_blank" >GCP209/12/J068: Výzkum svahových pohybů a eroze jako indikátoru morfotektonické aktivity Etiopské vysočiny založený na DPZ</a><br>

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2015

Kód důvěrnosti údajů

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

Název periodika

Landslides

ISSN

1612-510X

e-ISSN

—

Svazek periodika

12

Číslo periodika v rámci svazku

5

Stát vydavatele periodika

DE - Spolková republika Německo

Počet stran výsledku

12

Strana od-do

985-996

Kód UT WoS článku

000361983500011

EID výsledku v databázi Scopus

2-s2.0-84942984438