C Kasse
Biographic Data
| ID | 5652102 |
|---|---|
| NAME | C Kasse |
| GIVEN NAMES | C |
| FAMILY NAME | Kasse |
| SIGNATURE | KASSE C |
| AFFILIATIONS | Vrije Universiteit Amsterdam |
| ORCID | 0000-0002-1466-1016 |
| VERIFIED | Yes |
| TOTAL WORKS | 7 |
| TOTAL CITATIONS | 12 |
| AUTHOR COUNT | 7 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2013 |
| LATEST PUBLICATION YEAR | 2025 |
| H-INDEX | 3 |
Topography and Substrate Lithology Control the Position of Fluvial Channels on a Drained Lake Floor, the Case of the Postglacial Ain Valley (Eastern France)
The development of fluvial systems over long time scales is a complex interplay of tectonic, climatic, and lithological factors. The initiation and location of fluvial channels in the landscape is less well understood. Recently exposed surfaces provide opportunities to determine factors controlling fluvial channel initiation. During the Würm Last Glacial Maximum (c. 20 ka), the Ain valley in eastern France transformed into a large proglacial lake…
Unravelling a Neanderthal landscape rich in bifacial tools at Esbeek-Diessen, the Netherlands
Esbeek-Diessen represents a significant late Middle Palaeolithic surface site, recent surveys show the effectiveness of GPR in Palaeolithic landscape archaeology, Neanderthal stone artefacts are found in association with a thermokarst landscape
Spatial and temporal variations in river terrace formation, preservation, and morphology in the Lower Meuse Valley, The Netherlands
The Lower Meuse Valley crosses the Roer Valley Rift System and provides an outstanding example of well-preserved late glacial and Holocene river terraces. The formation, preservation, and morphology of these terraces vary due to reach-specific conditions, a phenomenon that has been underappreciated in past studies. A detailed palaeogeographic reconstruction of the terrace series over the full length of the Lower Meuse Valley has been performed. T…
Specifying the External Impact on Fluvial Lowland Evolution: The Last Glacial Tisza (Tisa) Catchment in Hungary and Serbia
External impact on the development of fluvial systems is generally exerted by changes in sea level, climate and tectonic movements. In this study, it is shown that a regional to local differentiation of fluvial response may be caused by semi-direct effects of climate change and tectonic movement; for example, vegetation cover, frozen soil, snow cover and longitudinal gradient. Such semi-direct effects may be responsible for specific fluvial activ…
News from the north: A late Middle Palaeolithic site rich in handaxes on the Drenthe–Frisian till plateau near Assen, the Netherlands; first results of a trial excavation
From natural to human-dominated floodplain geoecology - A Holocene perspective for the Dijle catchment, Belgium
Sensitivity of floodplain geoecology to human impact: A Holocene perspective for the headwaters of the Dijle catchment, central Belgium
Floodplain deposition rates have increased markedly under influence of human impact throughout the late Holocene in many western and central European catchments. Consequently the geomorphology and ecology of many floodplains changed. In this study we discuss this human impact and its influence on the floodplain geoecology during the middle and late Holocene for the headwaters of the Dijle catchment, located in the Belgian loess belt. The floodpla…
News from the north: A late Middle Palaeolithic site rich in handaxes on the Drenthe–Frisian till plateau near Assen, the Netherlands; first results of a trial excavation
Sensitivity of floodplain geoecology to human impact: A Holocene perspective for the headwaters of the Dijle catchment, central Belgium
Floodplain deposition rates have increased markedly under influence of human impact throughout the late Holocene in many western and central European catchments. Consequently the geomorphology and ecology of many floodplains changed. In this study we discuss this human impact and its influence on the floodplain geoecology during the middle and late Holocene for the headwaters of the Dijle catchment, located in the Belgian loess belt. The floodpla…
From natural to human-dominated floodplain geoecology - A Holocene perspective for the Dijle catchment, Belgium
Sensitivity of floodplain geoecology to human impact: A Holocene perspective for the headwaters of the Dijle catchment, central Belgium
Floodplain deposition rates have increased markedly under influence of human impact throughout the late Holocene in many western and central European catchments. Consequently the geomorphology and ecology of many floodplains changed. In this study we discuss this human impact and its influence on the floodplain geoecology during the middle and late Holocene for the headwaters of the Dijle catchment, located in the Belgian loess belt. The floodpla…
From natural to human-dominated floodplain geoecology - A Holocene perspective for the Dijle catchment, Belgium
News from the north: A late Middle Palaeolithic site rich in handaxes on the Drenthe–Frisian till plateau near Assen, the Netherlands; first results of a trial excavation
Specifying the External Impact on Fluvial Lowland Evolution: The Last Glacial Tisza (Tisa) Catchment in Hungary and Serbia
External impact on the development of fluvial systems is generally exerted by changes in sea level, climate and tectonic movements. In this study, it is shown that a regional to local differentiation of fluvial response may be caused by semi-direct effects of climate change and tectonic movement; for example, vegetation cover, frozen soil, snow cover and longitudinal gradient. Such semi-direct effects may be responsible for specific fluvial activ…
Spatial and temporal variations in river terrace formation, preservation, and morphology in the Lower Meuse Valley, The Netherlands
The Lower Meuse Valley crosses the Roer Valley Rift System and provides an outstanding example of well-preserved late glacial and Holocene river terraces. The formation, preservation, and morphology of these terraces vary due to reach-specific conditions, a phenomenon that has been underappreciated in past studies. A detailed palaeogeographic reconstruction of the terrace series over the full length of the Lower Meuse Valley has been performed. T…
Topography and Substrate Lithology Control the Position of Fluvial Channels on a Drained Lake Floor, the Case of the Postglacial Ain Valley (Eastern France)
The development of fluvial systems over long time scales is a complex interplay of tectonic, climatic, and lithological factors. The initiation and location of fluvial channels in the landscape is less well understood. Recently exposed surfaces provide opportunities to determine factors controlling fluvial channel initiation. During the Würm Last Glacial Maximum (c. 20 ka), the Ain valley in eastern France transformed into a large proglacial lake…
Unravelling a Neanderthal landscape rich in bifacial tools at Esbeek-Diessen, the Netherlands
Esbeek-Diessen represents a significant late Middle Palaeolithic surface site, recent surveys show the effectiveness of GPR in Palaeolithic landscape archaeology, Neanderthal stone artefacts are found in association with a thermokarst landscape
Geography (5 works) · Geology (5 works) · Geology and Paleoclimatology Research (5 works) · Geomorphology (5 works) · Fluvial (4 works) · Holocene (4 works) · Hydrology and Sediment Transport Processes (4 works) · Physical geography (4 works) · Archaeology (3 works) · Drainage basin (3 works)