“…More recently, geomorphological research in these areas has made it possible to date soils, given the presence of windblown silts (loess) which are highly fertile and can be accurately dated by sediment luminescence (Stevens et al, 2020: 3-4), in turn allowing for a better understanding of the historic formation of lynchets and increased potential of soil erosion (Evans et al, 2017: 49-51;Verhegge & Delvoie, 2021: 1-2). A greater understanding of formation processes and prehistoric land use across the chalklands of southern Britain (Bell, 1986: 72-73;Johnston et al, 2020Johnston et al, , 2021) and continental Europe (Rommens et al, 2007: 784-87;Fuchs & Lang, 2009: 22-24;Turner et al, 2021: 784-87), mapping, and morphological assessments of buried soils and lynchets have documented the progressive development, erosion, and redeposition of brown earth soils, calcareous colluvium, and agricultural horizons across these landscapes (Ford et al, 1990: 44-51;Macphail et al, 1990: 53-69;Allen, 1992: 37-52;Bell et al, 2020: 1-8).…”