What is it about?
The study comprises main landslide-dams of Central Alborz, including those with saturated and dried lakes. Valasht, Chort, Shoormast, Evan, Tar, Havir and Imamza-e-Ali were the lakes discovered as being formed by a landslide-damming process. Several other ancient lakes were identified as the remnants of breached and dried landslide-dams. The geometry and structural setting of each case is described; however, more investigations are required to evaluate the potential hazards for downstream populations.
Featured Image
Why is it important?
This paper emphasizes the relationship between active faulting, fault valleys and slope instability that leads to fault valley blockage by landslide. The recommendation from this study is that more consideration of active structures is needed in tectonically active regions, where the fault damage zones are more susceptible to slope instability due to progressive deformation and earthquakes.
Read the Original
This page is a summary of: Geometrical and structural setting of landslide dams of the Central Alborz: a link between earthquakes and landslide damming, Bulletin of Engineering Geology and the Environment, February 2017, Springer Science + Business Media,
DOI: 10.1007/s10064-017-1021-8.
You can read the full text:
Contributors
The following have contributed to this page







