Landslides are generated by natural causes and by human action, causing various
geomorphological changes as well as physical and socioeconomic loss of the environment …

Debris flows can grow greatly in size and hazardous potential by eroding bed and bank
materials. However, erosion mechanisms are poorly understood because debris flows are …

In the Dolomitic region, abundant coarse hillslope sediment is commonly found at the toe of
rocky cliffs. Ephemeral channels originate where lower permeability bedrock surfaces …

The recent and growing development and availability of unmanned aerial vehicles/systems
(UAV, UAS, or “drones”) in volcanology has promoted a significant advance in volcanic …

Slit-type barriers serve as active countermeasures against debris flow. However, the
dynamic interaction between debris flows and slit-type barriers is extremely complicated. To …

Although the prediction of debris flow-prone areas represents a key step towards reducing
damages, modeling debris flow susceptibility is complicated. In addition, the role of debris …

Lateral erosion is a critical factor that influences the formation and amplification of debris
flows. However, our understanding of the bank retreat process in debris flow channels is …

滑坡运动路径具有普遍的复杂性, 体现为侧散, 转向, 分叉, 交织, 聚合与并联等复杂行为.
滑坡运动路径复杂性增大了滑坡危险性. 因而, 滑坡危险性评估对滑坡运动路径复杂度的量化和 …

Chronological data on recent debris-flow activity in the Eastern Meditteranean are
fragmentary, limiting a proper assessment of future geomorphic risk. This is especially true if …

Rainfall patterns that trigger debris flows may vary depending on the amount of sediment
storage in their initiation zones. However, the current literature did not fully explore the …