PL
 |
EN
Ograniczanie wyników
Czasopisma help
  1. 24 Geotourism / Geoturystyka
  2. 11 Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie
  3. 3 Geoturystyka
  4. 3 Volumina Jurassica
  5. 2 Acta Geologica Polonica
Więcej...
Autorzy help
  1. 18 Krobicki Michał
  2. 8 Golonka Jan
  3. 8 Krobicki M.
  4. 6 Wierzbowski A.
  5. 4 Starzec Krzysztof
Więcej...
Lata help
  1. 1 2026
  2. 24 2024
  3. 1 2022
  4. 1 2018
  5. 1 2015
Więcej...
Preferencje help
Polish version English version Język
Widoczny [Schowaj] Abstrakt
Liczba wyników

Znaleziono wyników: 51

Liczba wyników na stronie
first rewind previous Strona / 3 next fast forward last
Wyniki wyszukiwania
Wyszukiwano:
w słowach kluczowych:  Pieniński Pas Skałkowy
help Sortuj według:

help Ogranicz wyniki do:
first rewind previous Strona / 3 next fast forward last
1
Content available Use of the electrical conductivity of water and the electrical resistivity tomography of rocks in the recognition of groundwater circulation and discharge in strongly tectonized carbonate massifs
Humnicki Włodzimierz, Mieszkowski Radosław, Szostakiewicz-Hołownia Marzena
Acta Geologica Polonica
|
2026
|
Vol. 76, no. 1
art. no. e73
EN
In protected mountainous areas, groundwater surveys are usually restricted to studies of their recharge by springs and streams. In the case of fissured rocks, which represent a highly heterogeneous medium, classical hydrogeological methods may be supplemented by electrical resistivity tomography (ERT) techniques. The studies presented here were focused on explaining issues related to groundwater circulation and recharge in such a complex structure, based on the study of Gorczyński Ravine situated within the Pieniny Klippen Belt. The groundwater of that area is recharged by the Macelowy Stream and its spring. Electrical conductivity of water (EC) measurements have indicated the existence of a privileged groundwater recharge zone of the stream and a different groundwater recharge zone of the spring. ERT surveys were used to explain the observed EC measurements. The analysed rock massif is clearly heterogenic, as documented by the wide range of electrical resistivity values, from c. 50 Ωm to above 19 000 Ωm. Interpretation of the results was limited by the lack of documentation from wells, which would have allowed precise correlation between geoelectrical layers and geological units. Despite these restrictions, ERT surveys facilitated the explanation of the observed hydrogeological phenomena and supplied new data on the complex structure of this part of the Pieniny Klippen Belt.
2
Content available The position of the West Carpathians in the Alpine-Carpathian fold-and-thrust belt
Golonka Jan, Krobicki Michał
Geotourism / Geoturystyka
|
2024
|
nr 1-2 (76-77)
5--11
3
Content available Tatra Mountains (Figs 53–57)
Krobicki Michał, Golonka Jan
Geotourism / Geoturystyka
|
2024
|
nr 1-2 (76-77)
63--67
4
Content available Stop 9 – Flaki range – Jurassic deposits of the Branisko Succession (Figs 35, 37, 38)
Krobicki Michał
Geotourism / Geoturystyka
|
2024
|
nr 1-2 (76-77)
43--45
5
Content available Stop 8 – Wżar Mount (Miocene andesites and panoramic view) (Figs 12, 35, 36)
Golonka Jan, Krobicki Michał
Geotourism / Geoturystyka
|
2024
|
nr 1-2 (76-77)
41--43
6
Content available Stop 7 – Klubina quarry – siliciclastic flysch (upper Eocene) (Figs 8, 13, 31–34)
Starzec Krzysztof, Barmuta Jan, Ratschbacher Lothar, Seyedi Saeideh Asal, Łapcik Piotr
Geotourism / Geoturystyka
|
2024
|
nr 1-2 (76-77)
39--41
7
Content available Stop 6 – Janoszka stream in Kamesznica villagesandy-to-gravelly debris flow deposits (Upper Cretaceous–Paleocene) (Figs 8, 13, 27–30)
Starzec Krzysztof
Geotourism / Geoturystyka
|
2024
|
nr 1-2 (76-77)
34--39
8
Content available Stop 5 – Wisła quarry – siliciclastic flysch (upper Cretaceous) (Figs 8, 13, 23–26)
Starzec Krzysztof, Barmuta Jan, Ratschbacher Lothar, Seyedi Saeideh Asal
Geotourism / Geoturystyka
|
2024
|
nr 1-2 (76-77)
29--24
9
Content available Stop 4 – Baška village – part of the Hradiště Formation with so-called teschenite volcanics (including pillov lavas) (Figs 8, 21)
Skupien Petr, Vašíček Zdeněk
Geotourism / Geoturystyka
|
2024
|
nr 1-2 (76-77)
28--29
10
Content available Stop 3 – Dolní Líštná near Třinec (Moravian part of the Czech Republic) – rare fossil polychelid lobsters in turbiditic palaeoenvironments (Lower Cretaceous, Valanginian) (Figs 8, 13)
Krobicki Michał
Geotourism / Geoturystyka
|
2024
|
nr 1-2 (76-77)
27
11
Content available Stop 20 – Kraków vicinity – Middle-Upper Jurassic and Upper Cretaceous deposits
Geotourism / Geoturystyka
|
2024
|
nr 1-2 (76-77)
69
12
Content available Stop 2 – Leszna Górna quarry – carbonate flysch (lowermost Cretaceous, Berriasian) (Figs 8, 13, 14, 19, 20)
Barmuta Jan, Starzec Krzysztof, Kowal-Kasprzyk Justyna, Ratschbacher Lothar, Krobicki Michał
Geotourism / Geoturystyka
|
2024
|
nr 1-2 (76-77)
25--27
13
Content available Stop 19 – Liliowe pass – Lower Triassic, nappe structures (Figs 54, 55)
Krobicki Michał, Golonka Jan
Geotourism / Geoturystyka
|
2024
|
nr 1-2 (76-77)
67--68
14
Content available Stop 18 – Szczawnica (“Orlica”) – history of the discovery of nappes in the Carpathians (Figs 35, 50–52)
Krobicki Michał
Geotourism / Geoturystyka
|
2024
|
nr 1-2 (76-77)
60--62
15
Content available Stop 17 – Sromowce-Szczawnica, Dunajec River rafting – uppermost Jurassic/Lower Cretaceous Maiolica limestones (Figs 9, 11, 35, 48)
Golonka Jan, Krobicki Michał
Geotourism / Geoturystyka
|
2024
|
nr 1-2 (76-77)
57--60
16
Content available Stop 16 – Sromowce, Macelowa – Upper Cretaceous Scaglia Rossawith clastics (Figs 11, 35, 48, 49)
Krobicki Michał, Golonka Jan
Geotourism / Geoturystyka
|
2024
|
nr 1-2 (76-77)
57
17
Content available Stop 15 – Czorsztyn Castle Jurassic-Cretaceous deposits of the Czorsztyn Succession (Figs 9, 35, 46, 47)
Krobicki Michał, Wierzbowski Andrzej, Kwietniak Anna
Geotourism / Geoturystyka
|
2024
|
nr 1-2 (76-77)
53--57
18
Content available Stop 14 – Jaworki village, below church – Maastrichtian/Paleocene sedimentary breccia of the Jarmuta Formation (Figs 11, 35, 45)
Krobicki Michał
Geotourism / Geoturystyka
|
2024
|
nr 1-2 (76-77)
53
19
Content available Stop 13 – Biała Woda valley – “mid”-Cretaceous basaltic olistolith (Figs 35, 43, 44)
Oszczypko Nestor, Krobicki Michał, Salata Dorota
Geotourism / Geoturystyka
|
2024
|
nr 1-2 (76-77)
51--52
20
Content available Stop 12 – Biała Woda valley (waterfall) – Berriasian crinoidal limestones, synsedimentary breccia and Valanginian crinoidal limestones (Figs 35, 42)
Krobicki Michał, Wierzbowski Andrzej
Geotourism / Geoturystyka
|
2024
|
nr 1-2 (76-77)
49--51
first rewind previous Strona / 3 next fast forward last
JavaScript jest wyłączony w Twojej przeglądarce internetowej. Włącz go, a następnie odśwież stronę, aby móc w pełni z niej korzystać.