Excursion Materials Saxonian Cretaceous Basin Startigraphy of the Elbsandsteingebirge 09.05.2017 Introduction The...
by the fresh,
yellowish color of the sandstones. At the level of the γ3 horizon, a circular path leads around the three
Fig. 2. Distal – proximal correlation of the Strehlen Limestone (lower Strehlen Formation, mid-Upper
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...
Uranium Mine. Thickness of fluvial
deposits in the Pirna valley decreases from about 30 m to zero towards the margins of the catchment
area. The above following units of the Oberhäslich and the Dölzschen formations show
Česká geologická služba Mathematical Modelling of the RESIBIL Project 3D geological model...
of geological model for public:
a) Model of Cretaceous sediments on Upper Paleozoic to
determine of slope instability
b) Model of Quternary sediments (aquifer) in Labe area
with the volume calculation of groundwater horizons
Nevertheless, the contact of the
Hochwald sandstone to the older units is unknown, because the slopes of the Hochwald
Mountain are covered by volcanic debris of a major phonolithe body on top of the mountain.
ResiBil – Bilance vodních zdrojů ve východní části česko-saského pohraničí a hodnocení...
Fig. 8: Correlation of the Lower Turonian in Saxony on the base of borehole descriptions. The vertical extent of
the profiles is not true to scale (does not correspond to the thickness) but to the extent of the
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
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
Integrating Geological Mapping in the Saxon-Czech Border Region
local geological situations
proof of existing fault systems
in pilot areas
identification of the cretaceous
and tertiary sediments base
determination of hydrogeological conditions
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
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