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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
cyclones
Turbidity currents regulate the transport and settling of microplastics in a deep-sea submarine canyon Available to Purchase
Landslide Warning Area Delineation through Seismic Signals and Landslide Characteristics: Insights from the Silabaku Landslide in Southern Taiwan Available to Purchase
Potential of Cave Sediments as a Proxy for Tropical Cyclone and Storm Activity Available to Purchase
200 Years of Fossil Fuels and Climate Change (1900-2100) Available to Purchase
Sediment routing in an incised valley during Hurricane Harvey (2017) in Houston, Texas, USA: Implications for modern sedimentation Open Access
Characteristics of Background Noise in the Oldest‐1 Array Deployed on the Oldest Part of the Pacific Plate Available to Purchase
Geological controls on dispersal and deposition of river flood sediments on the Hidaka shelf, Northern Japan Available to Purchase
Abstract The distribution and characteristics of marine surface sediments are a basic marine geological information. Large river floods are a frequent natural hazard that transport substantial terrigenous sediments into the marine environment. In August 2003, TY ETAU (0310) caused heavy rainfall in the southern coast of Hokkaido, north Japan, where some mountainous rivers in the Hidaka region flooded. Two deposition modes for the 2003 flood sediments can be identified by comparing the pre- and post-flood surface sediment distribution. Shore-normal shallow depressions off the mouth of the Saru and Atsubetsu rivers served as channels for the discharged floodwater preventing dispersion and maintaining the necessary water density to transport the materials as density bottom currents. This action also promoted long-distance transport of flood materials across the continental shelf. Absence of depression on the inner shelf off the mouth of the Niikappu and Shizunai rivers may have dispersed floodwaters near the river mouth and deposited the flood materials close to the shore. Marine geological mapping suggests that the differences in submarine topography (the presence or absence of shallow depressions) are closely related to the regional geological structure. Thus, submarine geology is a controlling factor of the seafloor environments influenced by the river flood.