Extreme block and boulder transport along a cliffed coastline (Calicoan Island, Philippines) during Super Typhoon Haiyan

This paper presents data and analysis for block and boulder transport during Super Typhoon Haiyan along a 4.5km long, low (5–12m) cliffed coastline in Calicoan Island, Eastern Samar, Philippines. Wave runup exceeding 15.2m elevation above mean sea level drove large limestone clasts, with volumes up to ~83m3, up to ~280m inland. A few very large clasts with volumes 65–132m3 were not transported by the waves. When combined with recent transport reported in May et al. (2015), Cox et al. (2016), and other literature, it is becoming increasingly clear that the largest blocks transported by storms overlie much of the tsunami transport range, increasing the difficulty in attributing the transport source without additional evidence. Comparison of present results with a global database of storm boulder transport shows a mass-elevation envelope outside of which no transport is observed. Initiation of motion criteria were extended to include non-rectangular cross-sections, which significantly reduces inferred velocities, particularly for overturning motion. These new relations were applied to the largest observed sliding and overturning boulders while considering coefficient uncertainties, and resulting velocity uncertainty was large enough that direct inference of wave heights would be problematic. Estimates of initiation velocities for cliff-edge boulders computed using lifting/joint-bounded relations were unreasonably large when compared to those for sliding and overturning boulders, suggesting that processes other than Bernoulli lift forces dominated at cliff edges. •Waves from Super Typhoon Haiyan transported clifftop boulders with volumes up to ~83m3 in Calicoan Island, Philippines.•Non-rectangular boulder cross-sections reduce predicted initiation of motion velocities, particularly in overturning.•Initiation of velocity estimates for lifting motion are much larger than those found for other modes of transport.•The mass-elevation ranges of storm-transported boulders overlie much of the tsunami transport range.•Upper size and elevation ranges for tsunami transport exceed those from storms.