${session.getAttribute("locale")} 5 Hydrogeomorphic processes and scaling issues in the continuum from soil pedons to catchments Fri 18 Oct 2019 13:17:52 AEST ]]> Water and watersheds Fri 14 Jun 2019 13:48:40 AEST ]]> Evaluating factors for controlling sediment connectivity of landslide materials: A flume experiment 50% of landslide sediment was transported downstream, indicating the occurrence of a debris flow. The amount of sediment deposited at the junction angle was greater for pyroclastic sediment followed by weathered granite, weathered sedimentary rock, and finally, sand and shale. Our connectivity index suggests that a threshold exists between landslide dam formation and debris flow occurrence associated with topographic conditions, water content, and types of sediment.]]> Fri 14 Jun 2019 13:47:41 AEST ]]> Hydrogeomorphic Characteristics of Fissures Developed during 2016 Kumamoto Earthquake Fri 14 Jun 2019 13:47:37 AEST ]]> The continuum of chronic to episodic natural hazards: Implications and strategies for community and landscape planning Fri 14 Jun 2019 13:47:10 AEST ]]> Assessing spatially distributed infiltration capacity to evaluate storm runoff in forested catchments: Implications for hydrological connectivity Fri 14 Jun 2019 13:47:00 AEST ]]> Discovery of zero-order basins as an important link for progress in hydrogeomorphology Fri 14 Jun 2019 13:46:19 AEST ]]>