Field Trip Guide
INQUA International Summer School on Active Tectonics and Tectonic Geomorphology 24-27 September 2019, Prague Field Trip Guide 26-27 September 2019 Flašar J. (ed.), Coubal M., Hartvich F., Burda J., Fischer T., Štěpančíková P., Tábořík P. Field trip overview map 2 Thursday 26th September 3 Friday 27th September 4 Field Trip Programme: Thursday 26th September 2019 Departure: IRSM Prague, conference venue 1a) Introduction to the Eger Rift (Coubal, M.) 1b) Tuchořice: southern marginal fault, slickensides and their measurement (Coubal, M.) 2a) Poláky - Hořenická (Erdbrandová) rokle: fluvial sediments embedded into the fault zone, paleostress analysis of the slickenside planes (Coubal, M.) 2b) Poláky: landslide (Hartvich F.) 3a) Nechranice dam: outcrop of the central rift fault (Střezov fault) (Coubal, M.) 3b) Nechranice dam: Slumps and rockfalls+ UAV remote sensing demonstration (Hartvich. F.) 4) Vysoká Pec: Landslides along the foot of the Krušné Hory Mts. (Hartvich F., Burda, J.) Accommodation: Nový Drahov Friday 27th September 2019 1 ) Introduction to the Cheb Basin 2 ) Soos 3a) Skalná: Geodynamic observatory and seismic station in Skalná (Fischer, T.) 3b) Skalná: Fault monitoring using TM-71 3D dilatometer (Hartvich, F.) 4a) Kopanina – Paleoseismic trenching site (backfilled trenches results) (Štěpančíková, P.) 4b) Kopanina ERT and DEMP measurement method (Tábořík, P.) 5)Hartoušov and Bublák moffette field (Fischer, T.) Dinner: Chodová Planá Return to IRSM Prague, conference venue 5 Thursday 26th September 1a) Introduction to the Eger Rift Origin of the Eger Rift The Eger Rift is the deep-based volcanic/tectonic structure in the northern part of Bohemian Massif, which has been formed in several phases. There have been a discussion, whether the Eger Rift is or is not the real continental rift, however Kopecký (1971) described the structure as a proper rift and today, the Eger Rift is generally accepted as a part of the European Cenozoic Rift System – ECRIS (Dezés et al., 2004).
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