The record of historic earthquakes in lake sediments of Central Switzerland

• Published in: Tectonophysics Vol. 394; no. 1; pp. 21 - 40
• Main Authors: Monecke, Katrin, Anselmetti, Flavio S., Becker, Arnfried, Sturm, Michael, Giardini, Domenico
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 02.12.2004
• Subjects: Central Switzerland; Freshwater; Historic earthquakes; Lake deposits; Paleoseismology; Switzerland; Lake deposits; Historic earthquakes; Central Switzerland; Paleoseismology
• ISSN: 0040-1951; 1879-3266
• DOI: 10.1016/j.tecto.2004.07.053

Deformation structures in lake sediments in Central Switzerland can be attributed to strong historic earthquakes. The type and spatial distribution of the deformation structures reflect the historically documented macroseismic intensities thus providing a useful calibration tool for paleoseismic investigations in prehistoric lake sediments. The Swiss historical earthquake catalogue shows four moderate to strong earthquakes with moment magnitudes of M w=5.7 to M w=6.9 and epicentral intensities of I 0=VII to I 0=IX that affected the area of Central Switzerland during the last 1000 years. These are the 1964 Alpnach, 1774 Altdorf, 1601 Unterwalden, and 1356 Basel earthquakes. In order to understand the effect of these earthquakes on lacustrine sediments, four lakes in Central Switzerland (Sarner See, Lungerer See, Baldegger See, and Seelisberg Seeli) were investigated using high-resolution seismic data and sediment cores. The sediments consist of organic- and carbonate-rich clayey to sandy silts that display fine bedding on the centimeter to millimeter scale. The sediments are dated by historic climate and environmental records, 137Cs activity, and radiocarbon ages. Deformation structures occur within distinct zones and include large-scale slumps and rockfalls, as well as small-scale features like disturbed and contorted lamination and liquefaction structures. These deformations are attributed to three of the abovementioned earthquakes. The spatial distribution of deformation structures in the different lakes clearly reflects the historical macroseismic dataset: Lake sediments are only affected if they are situated within an area that underwent groundshaking not smaller than intensity VI to VII. We estimate earthquake size by relating the epicentral distance of the farthest liquefaction structure to earthquake magnitude. This relationship is in agreement with earthquake size estimations based on the historical dataset.