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

This review article provides an overview of dry granular flows and particle fluid mixtures,
including experimental and numerical modeling at the laboratory scale, large scale …

Scaling plays a crucial role in designing experiments aimed at understanding the behavior
of landslides, debris flows, and other geomorphic phenomena involving grain-fluid mixtures …

Debris-flow impact against rigid obstacle involves instant redirection of flow velocity and
elevation of flow depth, and could serve as a stringent approach for verification of the two …

Understanding the impact forces exerted by debris flows is limited by a lack of direct field
measurements and validated numerical models. In this study, we use real‐time impact‐force …

Debris flows are typically a saturated mixture of poorly sorted particles and interstitial fluid,
whose density and flow properties depend strongly on the presence of suspended fine …

A systematic set of flume experiments is used to investigate the features of velocity profiles
within the body of coarse‐grained debris flows and the dependence of the transport …

Debris flows can grow greatly in size by entrainment of bed material, enhancing their runout
and hazardous impact. Here, we experimentally investigate the effects of debris‐flow …

The internal deformation within debris flows holds essential information on dynamics and
flow resistance of such mass‐wasting processes. Systematic measurements of velocity …

It has been reported that, in submarine landslides down a slope, only a small part of the
landslide momentum was transferred to the tsunami while most was lost in the further …