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- W16903105 abstract "The 1977-1978 eruptions of Mt. Usu, Hokl<aiclo, altered erosion regime of its summit atrio through destruction of pre-existing vegetation, new tephra deposition and crustal cleformation, resulting in heavy rilling and gullying. Slope erosion rate in the atrio culminated on slopes of 150-30e owing to severe gullying. The 4th Crater catchment, located on sumrnit atrio, represented an extraordlnarily high erosion rate at 13.6cmlyr when averaged ever the 4 post-eruption years. However, the erosion rate was deceleratecl within 3 years after the latest tephra deposition and before revegetation and erosion control worl<s were done. The pattem, initial rapid erosion £ollowed by an exponential decline, was observed for several other volcanoes, indicating rapid adjustment of a slope to the new erosion-sedimentation regime." @default.
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- W16903105 date "1986-08-20" @default.
- W16903105 modified "2023-09-23" @default.
- W16903105 title "Surface Erosion Associated with Tephra Deposition on Mt. Usu and Other Volcanoes" @default.
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