97 citations as recorded by crossref.

1. Preservation and transportation of large landslide deposits under decadal and millennial timescales in the Taiwan orogenic belt C. Chen et al. 10.1016/j.geomorph.2022.108402
2. Lithological control on the geomorphic evolution of the Shillong Plateau in Northeast India C. Strong et al. 10.1016/j.geomorph.2019.01.016
3. Multiband (X, C, L) radar amplitude analysis for a mixed sand- and gravel-bed river in the eastern Central Andes B. Purinton & B. Bookhagen 10.1016/j.rse.2020.111799
4. Glacial-interglacial climate changes recorded by debris flow fan deposits, Owens Valley, California M. D'Arcy et al. 10.1016/j.quascirev.2017.06.002
5. Modelling of sediment supply from torrent catchments in the Western Alps using the sediment contributing area (SCA) approach M. Altmann et al. 10.1002/esp.5046
6. Does soil erosion rejuvenate the soil phosphorus inventory? A. Eger et al. 10.1016/j.geoderma.2018.06.021
7. Predicting post‐fire debris flow grain sizes and depositional volumes in the Intermountain West, United States S. Wall et al. 10.1002/esp.5480
8. The gravel-sand transition and grain size gap in river bed sediments E. Dingle et al. 10.1016/j.earscirev.2021.103838
9. Variable‐Threshold Behavior in Rivers Arising From Hillslope‐Derived Blocks C. Shobe et al. 10.1029/2017JF004575
10. Sediment size on talus slopes correlates with fracture spacing on bedrock cliffs: implications for predicting initial sediment size distributions on hillslopes J. Verdian et al. 10.5194/esurf-9-1073-2021
11. Sand, Gravel, Cobbles, and Boulders: Detrital Thermochronology Shows that One Size Does Not Tell All C. Lukens et al. 10.1029/2023JF007192
12. An automated knickzone selection algorithm (KZ‐Picker) to analyze transient landscapes: Calibration and validation A. Neely et al. 10.1002/2017JF004250
13. Local topography and erosion rate control regolith thickness along a ridgeline in the Sierra Nevada, California E. Gabet et al. 10.1002/esp.3754
14. The grain size of sediments delivered to steep debris‐flow prone channels prior to and following wildfire A. Neely et al. 10.1002/esp.5819
15. Evidence for Self‐Similar Bedload Transport on Andean Alluvial Fans, Iglesia Basin, South Central Argentina R. Harries et al. 10.1029/2017JF004501
16. Formation of waterfalls by intermittent burial of active faults L. Malatesta & M. Lamb 10.1130/B31743.1
17. Controls on Pebbles’ Size and Shape in Streams of the Swiss Alps C. Litty & F. Schlunegger 10.1086/689183
18. Geomorphic response of a mountain gravel-bed river to an extreme flood in Aberdeenshire, Scotland D. Fieman et al. 10.1144/sjg2019-005
19. Measuring the grain‐size distributions of mass movement deposits E. Harvey et al. 10.1002/esp.5337
20. Fluvial geomorphology of the Yan Shan in North China: Implications for drainage evolution and seismic activity X. Yu & A. Yin 10.1016/j.jhydrol.2024.130810
21. Characterizing the transient geomorphic response to base‐level fall in the northeastern Tibetan Plateau H. Zhang et al. 10.1002/2015JF003715
22. Effects of Mass Wasting on the Physiochemical Properties of Fluvial Sediments in Puerto Rico Following Hurricane Maria N. Webb et al. 10.1029/2021JF006509
23. The size, distribution, and mobility of landslides caused by the 2015 Mw7.8 Gorkha earthquake, Nepal K. Roback et al. 10.1016/j.geomorph.2017.01.030
24. Does Pebble Abrasion Influence Detrital Age Population Statistics? A Numerical Investigation of Natural Data Sets C. Lavarini et al. 10.1029/2018JF004610
25. Fracture density and grain size controls on the relief structure of bedrock landscapes R. DiBiase et al. 10.1130/G40006.1
26. How many grains are needed for quantifying catchment erosion from tracer thermochronology? A. Madella et al. 10.5194/gchron-4-177-2022
27. Soil organic carbon and mineral interactions on climatically different hillslopes X. Wang et al. 10.1016/j.geoderma.2018.02.021
28. Straight from the source's mouth: Controls on field‐constrained sediment export across the entire active Corinth Rift, central Greece S. Watkins et al. 10.1111/bre.12444
29. Arrested development: Erosional equilibrium in the southern Sierra Nevada, California, maintained by feedbacks between channel incision and hillslope sediment production R. Callahan et al. 10.1130/B35006.1
30. Coarse sediment supply sets the slope of bedrock channels in rapidly uplifting terrain: Field and topographic evidence from eastern Taiwan L. Lai et al. 10.1002/esp.5200
31. Landslides after wildfire: initiation, magnitude, and mobility F. Rengers et al. 10.1007/s10346-020-01506-3
32. Fluvial archives, a valuable record of vertical crustal deformation A. Demoulin et al. 10.1016/j.quascirev.2016.11.011
33. River profile response to normal fault growth and linkage: an example from the Hellenic forearc of south-central Crete, Greece S. Gallen & K. Wegmann 10.5194/esurf-5-161-2017
34. Post-Miocene topographic rejuvenation in an elevated passive continental margin not characterized by a sharp escarpment (northern end of the Mantiqueira Range, Brazil) S. Calegari et al. 10.1016/j.geomorph.2021.107946
35. Canyon shape and erosion dynamics governed by channel-hillslope feedbacks R. Glade et al. 10.1130/G46219.1
36. Grain size from source to sink – modern and ancient fining rates T. Reynolds 10.1016/j.earscirev.2024.104699
37. The Lasting Legacy of Megaflood Boulder Deposition in Mountain Rivers S. Morey et al. 10.1029/2023GL105066
38. Denudation systematics inferred from in situ cosmogenic 10Be concentrations in fine (50–100 µm) and medium (100–250 µm) sediments of the Var River basin, southern French Alps A. Mariotti et al. 10.5194/esurf-7-1059-2019
39. A New Data‐Driven Bayesian Inversion of Fluvial Topography Clarifies the Tectonic History of the Corinth Rift and Reveals a Channel Steepness Threshold S. Gallen & D. Fernández‐Blanco 10.1029/2020JF005651
40. Possible threshold controls on sediment grain properties of Peruvian coastal river basins C. Litty et al. 10.5194/esurf-5-571-2017
41. Controls on the grain size distribution of landslides in Taiwan: the influence of drop height, scar depth and bedrock strength O. Marc et al. 10.5194/esurf-9-995-2021
42. Spatial variation of surface erosion rate in a fault zone and its controlling factors X. Li et al. 10.1016/j.geomorph.2023.108802
43. Grain size bias in cosmogenic nuclide studies of stream sediment in steep terrain C. Lukens et al. 10.1002/2016JF003859
44. Temporal variability in detrital <sup>10</sup>Be concentrations in a large Himalayan catchment E. Dingle et al. 10.5194/esurf-6-611-2018
45. Reconceptualising flood risk assessment by incorporating sediment supply H. Liu et al. 10.1016/j.catena.2022.106503
46. Effects of deep‐seated versus shallow hillslope processes on cosmogenic 10Be concentrations in fluvial sand and gravel S. Tofelde et al. 10.1002/esp.4471
47. Long-profile evolution of transport-limited gravel-bed rivers A. Wickert & T. Schildgen 10.5194/esurf-7-17-2019
48. Investigation of stochastic-threshold incision models across a climatic and morphological gradient C. Desormeaux et al. 10.5194/esurf-10-473-2022
49. Consistent mineral-associated organic carbon chemistry with variable erosion rates in a mountainous landscape X. Wang et al. 10.1016/j.geoderma.2021.115448
50. The influence of coarse particle abundance and spatial distribution on sediment transport and cluster evolution in steep channels under sediment-starved conditions W. Li et al. 10.1016/j.catena.2023.107199
51. Developing, choosing and using landscape evolution models to inform field‐based landscape reconstruction studies A. Temme et al. 10.1002/esp.4162
52. Scale dependent spatial structuring of mountain river large bed elements maximizes flow resistance J. Wiener & G. Pasternack 10.1016/j.geomorph.2022.108431
53. Automated detecting, segmenting and measuring of grains in images of fluvial sediments: The potential for large and precise data from specialist deep learning models and transfer learning D. Mair et al. 10.1002/esp.5755
54. The influence of lithology on channel geometry and bed sediment organization in mountainous hillslope‐coupled streams M. Fratkin et al. 10.1002/esp.4885
55. Slope, grain size, and roughness controls on dry sediment transport and storage on steep hillslopes R. DiBiase et al. 10.1002/2016JF003970
56. The effect of fragmentation on the distribution of hillslope rock size and abundance: Insights from contrasting field and model data A. Román-Sánchez et al. 10.1016/j.geoderma.2019.06.014
57. Grain size of fluvial gravel bars from close-range UAV imagery – uncertainty in segmentation-based data D. Mair et al. 10.5194/esurf-10-953-2022
58. Grain-size variability in debris flows of different runout lengths, Wenchuan, China E. Harvey et al. 10.1130/B37027.1
59. Hillslope‐derived blocks retard river incision C. Shobe et al. 10.1002/2016GL069262
60. Rock properties and sediment caliber govern bedrock river morphology across the Taiwan Central Range J. Carr et al. 10.1126/sciadv.adg6794
61. Grain Size in Landscapes L. Sklar 10.1146/annurev-earth-052623-075856
62. Water in the critical zone: soil, water and life from profile to planet M. Kirkby 10.5194/soil-2-631-2016
63. Post-Wildfire Debris Flow and Large Woody Debris Transport Modeling from the North Complex Fire to Lake Oroville T. Wasklewicz et al. 10.3390/w15040762
64. Introducing <i>PebbleCounts</i>: a grain-sizing tool for photo surveys of dynamic gravel-bed rivers B. Purinton & B. Bookhagen 10.5194/esurf-7-859-2019
65. The problem of predicting the size distribution of sediment supplied by hillslopes to rivers L. Sklar et al. 10.1016/j.geomorph.2016.05.005
66. Impact of climate on landscape form, sediment transfer and the sedimentary record R. Harries et al. 10.1002/esp.5075
67. How does landslide debris grain size control sediment transport and dynamics? J. Xie et al. 10.1016/j.geomorph.2023.109050
68. Modelling the evolution of debris flows after the 2008 Wenchuan earthquake F. Yang et al. 10.1016/j.enggeo.2023.107152
69. Climate and topography control the size and flux of sediment produced on steep mountain slopes C. Riebe et al. 10.1073/pnas.1503567112
70. Tracking Downstream Variability in Large Grain‐Size Distributions in the South‐Central Andes B. Purinton & B. Bookhagen 10.1029/2021JF006260
71. Slip slidin' away: A post-glacial environmental history of the Waipaoa River basin B. Gomez & B. Rosser 10.1016/j.geomorph.2017.08.035
72. The story of a summit nucleus: hillslope boulders and their effect on erosional patterns and landscape morphology in the Chilean Coastal Cordillera E. Lodes et al. 10.5194/esurf-11-305-2023
73. Storage and export of soil carbon and mineral surface area along an erosional gradient in the Sierra Nevada, California X. Wang et al. 10.1016/j.geoderma.2018.02.008
74. Kinetically limited weathering at low denudation rates in semiarid climatic conditions J. Schoonejans et al. 10.1002/2015JF003626
75. Predicting river bed substrate cover proportions across New Zealand A. Haddadchi et al. 10.1016/j.catena.2017.12.014
76. Measuring alluvial fan sensitivity to past climate changes using a self‐similarity approach to grain‐size fining, Death Valley, California M. D'Arcy et al. 10.1111/sed.12308
77. Controls on the hydraulic geometry of alluvial channels: bank stability to gravitational failure, the critical-flow hypothesis, and conservation of mass and energy J. Pelletier 10.5194/esurf-9-379-2021
78. Bio-climate affects hillslope and fluvial sediment grain size along the Chilean Coastal Cordillera S. Terweh et al. 10.1016/j.geomorph.2021.107700
79. Dynamic bedrock channel width during knickpoint retreat enhances undercutting of coupled hillslopes E. Baynes et al. 10.1002/esp.5477
80. Human Management Decreased Suspended Particle Size in the Loess Plateau Rivers during the 1980s to the 2010s K. Li et al. 10.3390/su16020799
81. 陆相裂陷盆地深时源-汇系统关键地质问题及革新方向 Q. Liu et al. 10.3799/dqkx.2023.194
82. Peripheral gully and landslide erosion on an extreme anthropogenic landscape produced by mountaintop removal coal mining M. Reed & S. Kite 10.1002/esp.4867
83. Gully characteristics across linear troughs in the southern Daliangshan, and its implications for debris mitigation K. Li et al. 10.1007/s10064-023-03293-2
84. Drainage Area, Bedrock Fracture Spacing, and Weathering Controls on Landscape‐Scale Patterns in Surface Sediment Grain Size A. Neely & R. DiBiase 10.1029/2020JF005560
85. Fluvial evacuation of landslide material from bedrock-confined channels under controlled experimental conditions E. Baynes et al. 10.1016/j.geomorph.2020.107359
86. Downvalley fining of hillslope sediment in an alpine catchment: implications for downstream fining of sediment flux in mountain rivers L. Sklar et al. 10.1002/esp.4849
87. Understanding the Role of Rainfall and Hydrology in Determining Fluvial Erosion Efficiency E. Deal et al. 10.1002/2017JF004393
88. The role of infrequently mobile boulders in modulating landscape evolution and geomorphic hazards C. Shobe et al. 10.1016/j.earscirev.2021.103717
89. Spatial and temporal analysis of hillslope–channel coupling and implications for the longitudinal profile in a dryland basin K. Michaelides et al. 10.1002/esp.4340
90. Impact of recycling and lateral sediment input on grain size fining trends—Implications for reconstructing tectonic and climate forcings in ancient sedimentary systems R. Harries et al. 10.1111/bre.12349
91. Comparison of three grain size measuring methods applied to coarse-grained gravel deposits P. Garefalakis et al. 10.1016/j.sedgeo.2023.106340
92. Cosmogenic 10Be in river sediment: where grain size matters and why R. van Dongen et al. 10.5194/esurf-7-393-2019
93. Sediment size and abrasion biases in detrital thermochronology C. Lukens et al. 10.1016/j.epsl.2019.115929
94. The relationship between drainage density, erosion rate, and hilltop curvature: Implications for sediment transport processes F. Clubb et al. 10.1002/2015JF003747
95. Sediment controls on the transition from debris flow to fluvial channels in steep mountain ranges A. Neely & R. DiBiase 10.1002/esp.5553
96. Conglomerate recycling in the Himalayan foreland basin: Implications for grain size and provenance L. Quick et al. 10.1130/B35334.1
97. Lithological controls on hillslope sediment supply: insights from landslide activity and grain size distributions D. Roda‐Boluda et al. 10.1002/esp.4281