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David Favis‐mortlock

Biographic Data

ID4510695
NAMEDavid Favis‐mortlock
GIVEN NAMESDavid
FAMILY NAMEFavis‐mortlock
SIGNATUREMORTLOCK D F
AFFILIATIONSUniversity of Oxford
ORCID0000-0002-9801-3787
VERIFIEDYes
TOTAL WORKS2
TOTAL CITATIONS8
WORKS AS AUTHOR2
WORKS AS EDITOR0
FIRST PUBLICATION YEAR1993
LATEST PUBLICATION YEAR1997
H-INDEX2
  • Modelling long-term anthropogenic erosion of a loess cover

    Open Access•David Favis‐mortlock, David Favis-Mortlock et al.•ARTICLE•The Holocene•1997•Cited by: 5•References: 3

    There is growing archaeological evidence that erosion induced by prehistoric agricultural activities has, in many parts of Europe, greatly thinned an original thick loess cover. The evidence for this is, however, almost entirely observational and qualitative. Whether in the time available, anthropogenic activity could have produced modern thin loessial soils has not been quantitatively evaluated. This study adopts a novel modelling approach in th…

  • Climate Change and Soil Erosion in Britain

    J Boardman, D T Favis-Mortlock et al.•ARTICLE•Geographical Journal•1993•Cited by: 3•References: 1

    The recent increase in soil erosion in Britain is the result of continued intensification of farming and a major land-use change from spring-planted to autumn-planted cereals. Field studies of erosion and computer models are the basis of this attempt to predict changes of rates under future climate conditions. Increases in winter rainfall, summer storm frequency, the area of irrigated land, and the introduction of new erosion-susceptible crops su…

  • Modelling long-term anthropogenic erosion of a loess cover

    Open Access•David Favis‐mortlock, David Favis-Mortlock et al.•ARTICLE•The Holocene•1997•Cited by: 5•References: 3

    There is growing archaeological evidence that erosion induced by prehistoric agricultural activities has, in many parts of Europe, greatly thinned an original thick loess cover. The evidence for this is, however, almost entirely observational and qualitative. Whether in the time available, anthropogenic activity could have produced modern thin loessial soils has not been quantitatively evaluated. This study adopts a novel modelling approach in th…

  • Climate Change and Soil Erosion in Britain

    J Boardman, D T Favis-Mortlock et al.•ARTICLE•Geographical Journal•1993•Cited by: 3•References: 1

    The recent increase in soil erosion in Britain is the result of continued intensification of farming and a major land-use change from spring-planted to autumn-planted cereals. Field studies of erosion and computer models are the basis of this attempt to predict changes of rates under future climate conditions. Increases in winter rainfall, summer storm frequency, the area of irrigated land, and the introduction of new erosion-susceptible crops su…

  • Climate Change and Soil Erosion in Britain

    J Boardman, D T Favis-Mortlock et al.•ARTICLE•Geographical Journal•1993•Cited by: 3•References: 1

    The recent increase in soil erosion in Britain is the result of continued intensification of farming and a major land-use change from spring-planted to autumn-planted cereals. Field studies of erosion and computer models are the basis of this attempt to predict changes of rates under future climate conditions. Increases in winter rainfall, summer storm frequency, the area of irrigated land, and the introduction of new erosion-susceptible crops su…

  • Modelling long-term anthropogenic erosion of a loess cover

    Open Access•David Favis‐mortlock, David Favis-Mortlock et al.•ARTICLE•The Holocene•1997•Cited by: 5•References: 3

    There is growing archaeological evidence that erosion induced by prehistoric agricultural activities has, in many parts of Europe, greatly thinned an original thick loess cover. The evidence for this is, however, almost entirely observational and qualitative. Whether in the time available, anthropogenic activity could have produced modern thin loessial soils has not been quantitatively evaluated. This study adopts a novel modelling approach in th…

Climate change (2 works) · Environmental Science (2 works) · Erosion (2 works) · Geography (2 works) · Geology (2 works) · Geomorphology (2 works) · Geotechnical engineering (2 works) · Hydrology (agriculture (2 works) · Oceanography (2 works) · Physical geography (2 works)

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