Fig. 5From: Variations in volumetric erosion rates of bedrock cliffs on a small inaccessible coastal island determined using measurements by an unmanned aerial vehicle with structure-from-motion and terrestrial laser scanningChanges in the occurrences of potential triggering factors and cliff erosion between survey periods. a Wave height at Bosohanto-oki. b Earthquake at Choja, Misaki-machi, Ishumi-shi. c Erosion rate of the cliff. d Relationships between potential triggering factors and eroded volume. Blue-colored circles are wave datasets and brown-colored x-marks are earthquake datasetsBack to article page