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Journal of the Geological Society; 2001; v. 158; issue.6; p. 885-893;
DOI: 10.1144/0016-760000-198
© 2001 Geological Society of London

Regular Article

Lateral erosion (‘toe-cutting’) of alluvial fans by axial rivers: implications for basin analysis and architecture

M. R. LEEDER1 & G. H. MACK2

1 1School of Environmental Sciences, University of East Anglia, Norwich, Norfolk NR4 7TJ, UK (e-mail: M.Leeder@uea.ac.uk)
2 2Department of Geological Sciences, New Mexico State University, Las Cruces, New Mexico 88003, USA

Abstract: We document the neglected phenomenon of lateral erosion (‘toe-cutting’) of alluvial fans by non-incising axial river channels. Field examples from the Holocene of the Big Lost River basin, Idaho and the Plio-Pleistocene of the Rio Grande Rift, New Mexico help to establish architectural models with more general application to basin analysis. The process of toe-cutting can lead to complete fan destruction and may be a response to climate change, tectonic tilting, fault propagation or a combination of these variables. It gives rise to: near horizontal erosion surfaces cut in fan sediment; steep fan-margin scarps; progressive up-fan incision from the scarp by a network of channels; soil formation up-fan away from the incised channel network; a deposit of axial alluvium that overlies the erosion surface and onlaps the scarp. Once avulsion occurs to take the axial channel away from the bajada margin, distinctive ‘healing-wedges’ of fan alluvium prograde across abandoned axial river channel and floodplain deposits, gradually onlapping the eroded scarp and its upstream network of incised channels. Toe-cutting has important stratigraphic basin analysis and economic consequences: bajada deposits subject to the process exhibit appreciable extra groundwater and petroleum reservoir potential in the intercalations of more porous and permeable axial fluvial sediments.


Keywords: Idaho, Rio Grande, alluvial fans, erosion, basin analysis.




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