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Appendix B: Landscape reconstruction Rhine-Meuse delta AD 100

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Appendix B: Landscape reconstruction Rhine-Meuse delta AD 100

0 5 10 20

Kilometers

Reworked by younger rivers;

mined peat;

covered / partially eroded by young sea ingression

!

Settlements

!

Active channels

Active sandy crevasse splays

Inherited sandy crevasse splays (4 - 2 ka) Active channel belts

Inherited channel belts (4 - 2 ka)

Levees and crevasse splays (active or inherited 4 - 2 ka) Floodbasins

Pleistocene outcrops

Inactive channels (depressions)

Legend

Peat swamp

Geomorphological reconstructions of the late-Roman and early-medieval landscape in the Rhine-Meuse delta

H.J. Pierik

1)

, K.M. Cohen

1,2)

& E. Stouthamer

1)

1) Department of Physical Geography, Faculty of Geosciences, Utrecht University, Heidelberglaan 2, 3584 CS, Utrecht. - Corresponding author: h.j.pierik@uu.nl 2) Deltares | TNO Geological Survey of the Netherlands, Princetonlaan 6, 3584 CB, Utrecht

Natural levees are important elements in delta plain geomorphology for understanding delta architecture, landscape evolution and settlement patterns. The data-rich Rhine- Meuse delta, The Netherlands, has a long tradition of integrated digital reconstruction maps and databases.

For this delta we present a new generation of digital map products with natural levees mapped at delta scale. In this contribution, we present the integrative map showing the patterns of levee distribution at AD 100, 500 and 900 and a palaeo-topography reconstruction of the levees. We outline the method of compiling these maps and

analyse the levee patterns of different channel belts and delta segments. At delta scale, tectonic setting and delta plain configuration are important in determining the width and orientation of natural levees. At smaller scale, time of evolution, orientation of the channel belt relative to the delta plain gradient overprint these delta scale trends.

The resulting palaeogeographical maps are integrative products created for a very data- rich research area that will yield new insights on delta evolution and past delta hydrology.

They provide new opportunities for palaeoenvironmental and archaeological maps to study changes in the Late Holocene landscape and the interaction with past habitation.

Palaeo elevation reconstruction AD 100 Geomorphological reconstructions

Cultural Heritage Agency of the Netherlands Ministry of Education, Culture and

Science

Conclusions and outlook

Draw levee boundaries with

queries from >100,000 boreholes

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