Excursion Materials Saxonian Cretaceous Basin Startigraphy of the Elbsandsteingebirge 09.05.2017 Introduction The...
the elevation and erosion of the Lusatian Block and the flexural subsistence of the edged trough is
supposed to be intensified in the mid-Turoniam stage. Most of the layers from the overburden of the
Guidebook Excursion, May, 28 th-29th 2018 German part Geology of the western...
to the activity of the
Lausitz Thrust. From the bridge across the Kirnitzsch, the tilted Hohe Liebe Block can be
observed in sandstones of the Postelwitz Formation (about 20°) at the western part of the
valley, while the
Guidebook Excursion, September, 11 th-12th 2019 Base of cretaceous sediments at Elbe...
onlap on the basement. Even the marly lower Turonian Briesnitz Formation is absent on the heights of
the paleo-morphology. All units disappear in the subground of the Zehistaer Wände. Further to the
ResiBil – Bilance vodních zdrojů ve východní části česko-saského pohraničí a hodnocení...
yellowish color of the sandstones. At the level of the γ3 horizon, a
circular path leads around the three peaks of the Kaiserkrone. From the northern summit, the
Postelwitz formation can be recognized very nicely at the
Guidebook Czech part Excursion 9. - 10. 5. 2017 ResiBil – Bilance...
Lusatian granitic massif lying in the north from the sandstones of the Bohemian Cretaceous
Basin in the south (Fig. 13). The granodiorites of the Lusatian Massif in the mid part of the
valley protrude towards the valley´s
crassus it represents the highest Lower Coniacian
and is therefore younger than the sections at the Lausche. Nevertheless, the contact of the
Hochwald sandstone to the older units is unknown, because the slopes of the Hochwald
unit in the Czech Republic
the total thickness of predominantly sandstone
sediments is up to 1000 m
The highest yields in the order of tens of l / s
have aquifers on the border with Germany
Until now, the use of these
Ohne Zweitlogo: Titel der Präsentation Arial 26
in the area of Hřensko it
would be possible to increase the pumping of the maximum
permitted consumption up to 115%, ie on the Czech side to
125.9 l/s and at the same time on the German side to 80.5 l/s,
including dry periods.
we are not able to quantify the effect of the part of the
catchment North of the Lausitz thrust
Groundwater model input:
• outputs are valid for the model
• time series relevant for the
Integrating Geological Mapping in the Saxon-Czech Border Region
different stratigraphic systems
to develop a transborder legend
Creating a innovative transborder
geological map with a scale of 1:100.000
for the saxon-bohemian cretaceous basin
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