Bottom-current and wind-pattern changes as indicated by Late Glacial and Holocene sediments from western Lake Geneva (Switzerland)
- 1 January 2003
- book chapter
- Published by Springer Nature
Abstract
No abstract availableKeywords
This publication has 15 references indexed in Scilit:
- Late-glacial and Holocene vegetation history and dynamics as shown by pollen and plant macrofossil analyses in annually laminated sediments from Soppensee, central SwitzerlandVegetation History and Archaeobotany, 1999
- 1822 earthquake‐triggered homogenite in Lake Le Bourget (NW Alps)Terra Nova, 1999
- The Effects of Shallow Gas on Seismic Reflection ProfilesPublished by Springer Nature ,1997
- Sediment drifts and erosional surfaces in the central Mediterranean: seismic evidence of bottom-current activitySedimentary Geology, 1993
- Dust transport and palaeoclimate during the Oldest Dryas in Central Europe — implications from varves (Lake Constance)Climate Dynamics, 1992
- Holocene lake‐level fluctuations in Jura and the northern subalpine ranges, France: regional pattern and climatic implicationsBoreas, 1992
- Horizontal Transport and Sedimentation by Interflows and Turbidity Currents in Lake GenevaPublished by Springer Nature ,1990
- Slumps and their deposits in fan delta front and slopeGeology, 1984
- The influence of wind, fetch, and water depth on the distribution of sediments in Lake Vänern, SwedenCanadian Journal of Earth Sciences, 1977
- Palynological and oxygen isotope investigations on Late‐Glacial sediment cores from Swiss lakesBoreas, 1976