63 citations as recorded by crossref.

1. A Review of Tsunami Hazards in the Makran Subduction Zone A. Rashidi et al. 10.3390/geosciences10090372
2. Major typhoon phases in the upper Gulf of Thailand over the last 1.5 millennia, determined from coastal deposits on rock islands J. Terry et al. 10.1016/j.quaint.2018.04.022
3. Unveiling the history and nature of paleostorms in the Holocene K. Minamidate & K. Goto 10.1016/j.earscirev.2024.104774
4. Megaboulder Movement by Superstorms: A Geomorphological Approach A. Scheffers & D. Kelletat 10.2112/JCOASTRES-D-19-00112.1
5. Ancient high-energy storm boulder deposits on Ko Samui, Thailand, and their significance for identifying coastal hazard risk J. Terry et al. 10.1016/j.palaeo.2016.04.046
6. Limitations to U/Th dating of reef-platform carbonate boulders produced by high-energy marine inundations in the Tuamotu Archipelago (French Polynesia) C. Remy et al. 10.1007/s00338-018-1732-8
7. Sediment analysis and historical context of the 2018 Palu-Donggala tsunami deposit, Indonesia J. Majewski et al. 10.1016/j.margeo.2023.107159
8. Surf beat-induced overwash during Typhoon Haiyan deposited two distinct sediment assemblages on the carbonate coast of Hernani, Samar, central Philippines J. Soria et al. 10.1016/j.margeo.2017.08.016
9. Ice melt, sea level rise and superstorms: evidence from paleoclimate data, climate modeling, and modern observations that 2 °C global warming could be dangerous J. Hansen et al. 10.5194/acp-16-3761-2016
10. Paleo-Typhoon Events as Indicated by Coral Reef Boulder Deposits on the Southern Coast of Hainan Island, China L. Zhou et al. 10.3389/fmars.2021.746773
11. Multiple severe storms revealed by coral boulders at Pasuquin, northwestern Luzon, Philippines S. Gong et al. 10.1016/j.palaeo.2022.111195
12. A Numerical Modeling Approach for Better Differentiation of Boulders Transported by a Tsunami, Storm, and Storm‐Induced Energetic Infragravity Waves M. Watanabe et al. 10.1029/2023JF007083
13. Boulder displacements along rocky coasts: A new deterministic and theoretical approach to improve incipient motion formulas N. Nandasena et al. 10.1016/j.geomorph.2022.108217
14. Clustered, Stacked and Imbricated Large Coastal Rock Clasts on Ludao Island, Southeast Taiwan, and Their Application to Palaeotyphoon Intensity Assessment J. Terry et al. 10.3389/feart.2021.792369
15. Monitoring of Coastal Boulder Movements by Storms and Calculating Volumetric Parameters Using the Volume Differential Method Based on Point Cloud Difference Y. Yao et al. 10.3390/rs15061526
16. Occurrence of 1 ka-old corals on an uplifted reef terrace in west Luzon, Philippines: Implications for a prehistoric extreme wave event in the South China Sea region N. Ramos et al. 10.1186/s40562-017-0078-3
17. Coral boulders on Melekeok reef in the Palau Islands: An indicator of wave activity associated with tropical cyclones C. Hongo et al. 10.1016/j.margeo.2018.02.004
18. Multiple dating approach (14C, 230Th/U and 36Cl) of tsunami-transported reef-top boulders on Bonaire (Leeward Antilles) – Current achievements and challenges G. Rixhon et al. 10.1016/j.margeo.2017.03.007
19. INVESTIGATING DISTRIBUTION CHARACTERISTIC OF STORM BOULDERS AT OKINOSHIMA ISLAND, JAPAN BASED ON NUMERICAL MODELING M. WATANABE et al. 10.2208/kaigan.76.2_I_1165
20. Factors responsible for the limited inland extent of sand deposits on Leyte Island during 2013 Typhoon Haiyan M. Watanabe et al. 10.1002/2016JC012023
21. Tsunami and storm sediments in Oman: Characterizing extreme wave deposits using terrestrial laser scanning B. Schneider et al. 10.1007/s11852-018-0663-4
22. Giant palaeotsunami in Kiribati: Converging evidence from geology and oral history J. Terry et al. 10.1111/iar.12417
23. Finding Coastal Megaclast Deposits: A Virtual Perspective D. Ruban 10.3390/jmse8030164
24. Storm Waves May Be the Source of Some “Tsunami” Coastal Boulder Deposits A. Kennedy et al. 10.1029/2020GL090775
25. Is Bangkok at risk of marine flooding? Evidence relating to the historical floods of AD 1785 and 1983 J. Terry et al. 10.1007/s11069-020-04347-4
26. A laboratory experiment on the incipient motion of boulders by high‐energy coastal flows L. Bressan et al. 10.1002/esp.4461
27. Sea-level change and superstorms; geologic evidence from the last interglacial (MIS 5e) in the Bahamas and Bermuda offers ominous prospects for a warming Earth P. Hearty & B. Tormey 10.1016/j.margeo.2017.05.009
28. Significance of boulder shape, shoreline configuration and pre‐transport setting for the transport of boulders by tsunamis J. Oetjen et al. 10.1002/esp.4870
29. The Safi boulders (Morocco): Evidence of past extreme wave events O. Khalfaoui et al. 10.1016/j.margeo.2024.107265
30. Strongly aligned coastal boulders on Ko Larn island (Thailand): a proxy for past typhoon‐driven high‐energy wave events in the Bay of Bangkok J. Terry & J. Goff 10.1111/1745-5871.12342
31. Coral boulder transport and gravel bar formation by storms in Lumaniag village, Batangas, northwestern Philippines A. Gallentes et al. 10.1016/j.geomorph.2020.107554
32. Assessment of hydrodynamic competence in extreme marine events through application of Boussinesq–Green–Naghdi models Y. Zhang et al. 10.1016/j.apor.2017.06.001
33. Magnitudes of nearshore waves generated by tropical cyclone Winston, the strongest landfalling cyclone in South Pacific records. Unprecedented or unremarkable? J. Terry & A. Lau 10.1016/j.sedgeo.2017.10.009
34. Maximal Heights of Nearshore Storm Waves and Resultant Onshore Flow Velocities N. Bujan & R. Cox 10.3389/fmars.2020.00309
35. Cliff-top boulder morphodynamics on the high–energy volcanic rocky coast of the Reykjanes Peninsula (SW Iceland) R. Autret et al. 10.1016/j.margeo.2022.106984
36. Evaluating optically stimulated luminescence rock surface exposure dating as a novel approach for reconstructing coastal boulder movement on decadal to centennial timescales D. Brill et al. 10.5194/esurf-9-205-2021
37. Progress in Tsunami Science: Toward an Improved Integration of Hydrodynamical Modeling and Geomorphic Field Evidence A. Scheffers & W. Erdmann 10.3390/geosciences12050209
38. Atoll islets reshaping processes induced by extreme cyclonic waves and calm weather. Evidence from two centuries of megablocks emergences and coral rubble displacements in Anaa, Rangiroa and Tikehau atolls (western Tuamotu archipelago - French Polynesia) R. Canavesio et al. 10.1016/j.margeo.2023.107140
39. Reconsidering the seawater-density parameter in hydrodynamic flow transport equations for coastal boulders J. Terry & S. Malik 10.1080/00288306.2020.1716815
40. Digital mapping of coastal boulders – high‐resolution data acquisition to infer past and recent transport dynamics F. Boesl et al. 10.1111/sed.12578
41. Data of boulder transport experiment in super-large wave flume M. Watanabe et al. 10.4096/jssj.79.15
42. Typhoon Haiyan's sedimentary record in coastal environments of the Philippines and its palaeotempestological implications D. Brill et al. 10.5194/nhess-16-2799-2016
43. Morphological controls and statistical modelling of boulder transport by extreme storms M. Oliveira et al. 10.1016/j.margeo.2020.106216
44. Tsunami deposits of the Caribbean – Towards an improved coastal hazard assessment M. Engel et al. 10.1016/j.earscirev.2016.10.010
45. Extreme block and boulder transport along a cliffed coastline (Calicoan Island, Philippines) during Super Typhoon Haiyan A. Kennedy et al. 10.1016/j.margeo.2016.11.004
46. Field Studies of Megagravel Transport: Relevance for Coastal Infrastructure Engineering R. Cox & V. Pakrashi 10.1002/cepa.2211
47. On a ~210 t Caribbean coastal boulder: The huracanolito seaward of the ruins of the Bucanero resort, Juragua, Oriente, Cuba K. Pedoja et al. 10.1002/esp.5682
48. The role of hydrodynamic impact force in subaerial boulder transport by tsunami—Experimental evidence and revision of boulder transport equation H. Lodhi et al. 10.1016/j.sedgeo.2020.105745
49. Long–term variability of supratidal coastal boulder activation in Brittany (France) R. Autret et al. 10.1016/j.geomorph.2017.12.028
50. Imbricated Coastal Boulder Deposits are Formed by Storm Waves, and Can Preserve a Long-Term Storminess Record R. Cox et al. 10.1038/s41598-019-47254-w
51. High‐energy inundation events versus long‐term coastal processes – room for misinterpretation M. Spiske et al. 10.1111/sed.12524
52. Boulder transport by storms – Extreme-waves in the coastal zone of the Irish west coast W. Erdmann et al. 10.1016/j.margeo.2018.02.003
53. A systematic review of geological evidence for Holocene earthquakes and tsunamis along the Nankai-Suruga Trough, Japan E. Garrett et al. 10.1016/j.earscirev.2016.06.011
54. Topographical Analysis of the 2013 Typhoon Haiyan Storm Surge Flooding by Combining the JMA Storm Surge Model and the FLO-2D Flood Inundation Model L. Dasallas & S. Lee 10.3390/w11010144
55. A mid-Holocene candidate tsunami deposit from the NW Cape (Western Australia) S. May et al. 10.1016/j.sedgeo.2015.11.010
56. Very large boulders were moved by storm waves on the west coast of Ireland in winter 2013–2014 R. Cox 10.1016/j.margeo.2018.07.016
57. Size-frequency distributions of scleractinian coral (Porites spp.) colonies inside and outside a marine reserve in Leyte Gulf, central Philippines S. Boco et al. 10.1016/j.rsma.2020.101147
58. Boulder emplacement and remobilisation by cyclone and submarine landslide tsunami waves near Suva City, Fiji A. Lau et al. 10.1016/j.sedgeo.2017.12.017
59. Extraordinary boulder transport by storm waves (west of Ireland, winter 2013–2014), and criteria for analysing coastal boulder deposits R. Cox et al. 10.1016/j.earscirev.2017.12.014
60. Megagravel deposits on the west coast of Ireland show the impacts of severe storms R. Cox 10.1002/wea.3677
61. Extreme waves in the British Virgin Islands during the last centuries before 1500 CE B. Atwater et al. 10.1130/GES01356.1
62. Coastal boulder deposit as evidence of an ocean‐wide prehistoric tsunami originated on the Atacama Desert coast (northern Chile) M. Abad et al. 10.1111/sed.12570
63. Systematic Review Shows That Work Done by Storm Waves Can Be Misinterpreted as Tsunami-Related Because Commonly Used Hydrodynamic Equations Are Flawed R. Cox et al. 10.3389/fmars.2020.00004