Floods, floodplains, delta plains—a satellite imaging approach

JPM Syvitski, I Overeem, GR Brakenridge… - Sedimentary Geology, 2012 - Elsevier
Thirty-three lowland floodplains and their associated delta plains are characterized with data
from three remote sensing systems (AMSR-E, SRTM and MODIS). These data provide new …

A great wave: the Storegga tsunami and the end of Doggerland?

J Walker, V Gaffney, S Fitch, M Muru, A Fraser, M Bates… - Antiquity, 2020 - cambridge.org
Around 8150 BP, the Storegga tsunami struck North-west Europe. The size of this wave has
led many to assume that it had a devastating impact upon contemporaneous Mesolithic …

Submerged prehistory

J Benjamin, A Fischer, C Pickard, C Bonsall - 2011 - torrossa.com
COST–the acronym for European Cooperation in Science and Technology–is the oldest and
widest European intergovernmental network for cooperation in research. Established by the …

Holocene transgression of the Rhine river mouth area, The Netherlands/Southern North Sea: palaeogeography and sequence stratigraphy

MP Hijma, KM Cohen - Sedimentology, 2011 - Wiley Online Library
This study presents a detailed reconstruction of the palaeogeography of the Rhine valley
(western Netherlands) during the Holocene transgression with systems tracts placed in a …

Dealing with biases: three geo-archaeological approaches to the hidden landscapes of Italy

H Feiken - 2014 - torrossa.com
Following earlier methodological studies (Van Leusen 1996; 2001; 2002) Martijn van
Leusen in 2005 began a new project in both regions–the Hidden Landscapes Project (HLP) …

Organic‐facies determination: a key for understanding facies distribution in the basal peat layer of the Holocene Rhine‐Meuse delta, The Netherlands

IJ Bos, FS Busschers, WZ Hoek - Sedimentology, 2012 - Wiley Online Library
Peat and gyttja (organic lake sediment) are important indicators for past environmental
conditions; they form in areas where the supply of clastic sediment is insufficient to fill the …

[HTML][HTML] Lithological control on scour hole formation in the Rhine-Meuse Estuary

Y Huismans, H Koopmans, A Wiersma, T de Haas… - Geomorphology, 2021 - Elsevier
River deltas commonly have a heterogeneous substratum of alternating peat, clay and sand
deposits. This has important consequences for the river bed development and in particular …

[PDF][PDF] Paleo-coastline of the Central Eastern Adriatic Sea, and Paleo-Channels of the Cetina and Neretva rivers during the last glacial maximum

M Sikora, H Mihanović, I Vilibić - Acta Adriatica, 2014 - hrcak.srce.hr
Paleo-coastline of the Central Eastern Adriatic Sea, and Paleo-Channels of the Cetina and
Neretva rivers during the last glacial Page 1 Paleo-coastline of the Central Eastern Adriatic …

Understanding and managing the morphology of branches incising into sand-clay deposits in the Dutch Rhine Delta

K Sloff, A Van Spijk, E Stouthamer, A Sieben - International Journal of …, 2013 - Elsevier
Abstract In the Rhine-Meuse delta in the south-western part of the Netherlands, the
morphology of the river branches is highly dependent on the erodibility of the subsoil …

Tributaries of the Elbe palaeovalley: features of a hidden palaeolandscape in the German Bight, North Sea

DA Hepp, U Warnke, D Hebbeln, T Mörz - Under the Sea: archaeology …, 2017 - Springer
Prior to postglacial global sea-level rise in the present North Sea area, Mesolithic hunters
and gatherers were able to settle in the coastal lowland landscape between England …