2022
DOI: 10.1016/j.geomorph.2022.108461
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The Trendermarsch polder (North Frisia, Germany) - Geophysical and geoarchaeological investigations of an anthropogenic medieval coastal landscape and its vulnerability against natural hazards

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Cited by 6 publications
(9 citation statements)
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“…TRE ( [37]) is an example from the Wadden Sea area of northern Germany (North Frisia), comprising mainly sandy, silty and organic layers from tidal flats and marshlands. 7.…”
Section: Dp Test Modelsmentioning
confidence: 99%
“…TRE ( [37]) is an example from the Wadden Sea area of northern Germany (North Frisia), comprising mainly sandy, silty and organic layers from tidal flats and marshlands. 7.…”
Section: Dp Test Modelsmentioning
confidence: 99%
“…But the systematic large-scale reclamation and major transformation of natural coastal conditions into a cultural landscape had only begun around 1100 AD. Unlike in neighbouring Wadden Sea regions, prevailing amphibious conditions had restricted permanent human settlement for a long time 22 . Pleistocene outcrops and Holocene beach ridges had mostly kept out open North Sea conditions during the post-glacial sea level rise 2 , 25 .…”
Section: Introductionmentioning
confidence: 99%
“…Pleistocene outcrops and Holocene beach ridges had mostly kept out open North Sea conditions during the post-glacial sea level rise 2 , 25 . Instead, quiescent shallow water conditions and wide marshes emerged since c. 2000 BC, traversed by tidal channels and succeeded by extensive peat formation that lasted at least until the first millennium AD 22 , 25 , 26 . Yet, only two centuries of intense human interventions by medieval colonization increased the region’s vulnerability in a way that the devastating effects of the 1362 AD storm flood destroyed much of North Frisia’s low-lying coastal areas 11 , 21 , 27 .…”
Section: Introductionmentioning
confidence: 99%
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“…Many geophysical methods, namely electrical resistivity tomography (ERT), ground penetrating radar (GPR), induced polarization (IP), controlled source audio frequency magnetotelluric (CSAMT), seismic refraction tomography (SRT), self-potential (SP), magnetic and gravity are widely carried out in geotechnical, environmental and groundwater studies 1,6,15,17,18,[23][24][25][26][27][28][29][30][31][32][33][34][35][36][37] . Compared to the borehole approaches, geophysical methods offer volumetric measurements of the subsurface 28,38 .…”
mentioning
confidence: 99%