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Number of items: 9.

March 2014

Wilson, Andrew and Lavé, Jérôme (2014) Convergent evolution of abrading flow obstacles: Insights from analogue modelling of fluvial bedrock abrasion by coarse bedload. Geomorphology, 208. pp. 207-224. ISSN ISSN 0169-555X DOI :10.1016/j.geomorph.2013.11.024

September 2013

Roberts, G. G. and White, N. J. and Shaw, B. (2013) An uplift history of crete, greece, from inverse modeling of longitudinal river profiles. Geomorphology, 198. pp. 177-188. ISSN ISSN 0169-555X DOI

March 2013

Wilson, Andrew and Lavé, Jérôme (2013) The legacy of impact conditions in morphometrics of percussion marks on fluvial bedrock surfaces. Geomorphology, 186. pp. 174-180. ISSN ISSN 0169-555X DOI

January 2013

Wilson, Andrew and Hovius, Niels and Turowski, Jens M. (2013) Upstream-facing convex surfaces: Bedrock bedforms produced by fluvial bedload abrasion. Geomorphology, 180–18. pp. 187-204. DOI


Turowski, J. M. and Hovius, N. and Wilson, A. and Horng, M. J. (2008) Hydraulic geometry, river sediment and the definition of bedrock channels. Geomorphology, 99 (1-4). pp. 26-38. DOI


Hughes, P. D. and Gibbard, P. L. and Woodward, J. C. (2007) Geological controls on Pleistocene glaciation and cirque form in Greece. Geomorphology, 88 (3-4). pp. 242-253.

March 2006

Jin, Z. D. and Li, F. C. and Cao, J. J. and Wang, S. M. and Yu, J. M. (2006) Geochemistry of Daihai Lake sediments, Inner Mongolia, north China: Implications for provenance, sedimentary sorting, and catchment weathering. Geomorphology, 80 (3-4). pp. 147-163. ISSN ISSN 0169-555X DOI


Chen, H. and Dadson, S. and Chi, Y. G. (2006) Recent rainfall-induced landslides and debris flow in northern Taiwan. Geomorphology, 77 (1-2). pp. 112-125.

17 January 2005

Cunha, P. P. and Martins, A. A. and Daveau, S. and Friend, P. F. (2005) Tectonic control of the Tejo river fluvial incision during the late Cenozoic, in Ródão - central Portugal (Atlantic Iberian border). Geomorphology, 64 (3-4). pp. 271-298. DOI

This list was generated on Wed Oct 5 12:36:14 2022 BST.

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