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Rapid fluvial response to meter-scale coseismic coastal uplift during the 2024 Noto Peninsula earthquake
The response of river profiles to relative base-level change is a key topic in earth surface processes, but observations capturing these changes on unconsolidated deposits at a 1–10 years timescales are scarce. We monitored geomorphic changes at the Hakka River mouth after the 3.5-meter base-level f
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