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  1. 25 Geotourism / Geoturystyka
  2. 5 Studia Geomorphologica Carpatho-Balcanica
  3. 3 Acta Geologica Polonica
  4. 2 Przegląd Geodezyjny
  5. 1 Acta Geophysica
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  1. 18 Krobicki Michał
  2. 8 Golonka Jan
  3. 4 Starzec Krzysztof
  4. 3 Barmuta Jan
  5. 3 Ratschbacher Lothar
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  1. 1 2026
  2. 26 2024
  3. 2 2023
  4. 2 2022
  5. 1 2021
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1
Content available The uppermost Jurassic–Lower Cretaceous (Tithonian–Aptian) of the Raptawicka Gate section (High-Tatric succession, Poland): integrated stratigraphy and microfacies
Lodowski Damian Gerard, Kowal-Kasprzyk Justyna, Waśkowska Anna, Granier Bruno, Grabowski Jacek
Acta Geologica Polonica
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2026
|
Vol. 76, no. 2
art. no. e84
EN
This study presents the results of research conducted on material coming from the Raptawicka Gate section of the High-Tatric autochthonous succession (Kościeliska Valley, West Tatra Mts, Central West Carpathians, Poland). It utilizes biostratigraphic (calpionellids, calcareous dinocysts, foraminifers), quantitative microfacies, and geochemical (stable carbon and oxygen isotopes, main and trace elements concentrations) techniques. The section documents the transition between the Raptawicka Turnia Limestone (RTL) Fm and the Wysoka Turnia Limestone (WTL) Fm, with an erosional gap in between them. The RTL Fm part contains the Malmica–Remanei microfossil zones, and therefore belongs to the middle lower–upper Tithonian; the WTL Fm part contains a foraminiferal assemblage which characterizes the Barremian/Aptian transition and the lower Aptian, whereas the δ13C record largely conforms with the characteristics of Oceanic Anoxic Event 1a (OAE 1a). Correlation with the Giewont composite section (High-Tatric allochthonous unit) enables the presentation of a coherent record of Tithonian sedimentation in both areas. It also allows the inference that the topmost beds of the RTL Fm in the Raptawicka Gate section are younger than those in the Giewont composite section. Furthermore, the stratigraphic gap between the topmost Jurassic and the Lower Cretaceous sediments in the High-Tatric autochthonous cover (Raptawicka Gate) is significantly larger (topmost Tithonian–basal Aptian) than that within the Giewont Nappe (cf. topmost Tithonian–Berriasian). Ultimately, microfacies analysis allows the recognition of biotic events/processes documented in other western Tethys sections; these are thought to reflect major-scale environmental perturbations.
2
Content available Evolution of the form of small tourist shelters in the mountain landscape – selected issues
Kronowski Dariusz
Przestrzeń i Forma
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2024
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nr 58
21--56
PL
Architektura gór kieruje się własnymi prawami. Projektanci realizujący standardowe opracowania starają się tworzyć wytrzymałe obiekty w trudnym terenie, zwykle z materiałów rodzimych, łącząc je ze współczesnymi możliwościami budownictwa. Detal to proste elementy wywodzące się od funkcji, oraz lokalizacji, wspierane technologią betonu, szkła oraz lekkiego drewna, wtapiają się w teren lub dominują. Architektura górska to nie tylko obiekty monumentalne, również należy wyróżnić małe schronienia o kształcie charakterystycznym dla formy terenu, mniej natury regionalnej, chociaż z niej się wywodzące. Poszukiwanie niepowtarzalnego piękna krajobrazu – wszystko to świadczy, że górska architektura nie jest tylko rzemiosłem o zakreślonych granicach, ale sztuką twórczą i nieskrępowaną.
EN
Mountain architecture follows its own rules. Designers implementing standard designs try to create durable objects in difficult terrain, often from native materials, combining them with modern construction possibilities. Details are simple elements derived from function and location, supported by the technology of concrete, glass and light wood, they blend into the terrain or dominate. Mountain architecture is not only about monumental objects, there are also small shelters with a shape characteristic of the landform, less regional in nature, although derived from it. The search for the unique beauty of the landscape - all this proves that mountain architecture is not just a craft with defined boundaries, but a creative and unrestrained art.
3
Content available Spring water resources in the Tatra Mountains
Bojarczuk Anna, Rajwa-Kuligiewicz Agnieszka, Siwek Janusz, Żelazny Mirosław, Szubert-Pufelska Marta
Journal of Water and Land Development
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2024
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no. 62
166--173
EN
The Tatra Mountains stand out as the wettest and most water-rich region in Poland. Despite this, limited studies addressed this issue, and current knowledge largely relies on data obtained in the mid-20th century, with a substantial lack of current estimates. This study aims to fill this gap by evaluating the contemporary water resources of springs in the Tatra Mountains. The study bases on the most recent hydrological mapping of 1,018 springs. The spring resources were evaluated using parameters such as the number of springs, specific runoff, and crenological index, analysed across different physiographic regions, tectonic units, and altitudinal zones. Our studies showed that the highest number of springs occurs in the Western Tatras (66%) between 1000 and 1400 m a.s.l., especially within the Sub-Tatric unit. Springs with discharges ranging from 0.1-1.0 dm3 ∙s-1 constitute approximately 70% of all springs but they contribute to only 8.1% of spring water resources. Total spring discharge amounted to 2726 dm3 ∙s-1 and was higher in the Western Tatras (1982.5 dm3 ∙s-1) than in the High Tatras (743.5 dm3 ∙s-1). The specific runoff amounted to 12.9 dm3 ∙s-1 ∙km-2 with the highest total runoff at altitudes occupied by the most abundant karst springs (1000-1100 m a.s.l.). The crenological index amounted to 4.8 springs∙km-2 and was higher in the Western Tatras (6.5 springs∙km-2) than in the High Tatras (4.9 springs∙km-2). The analysis revealed that the only five largest karst springs, constituting a mere 0.5% of all springs, account for 65% of spring water resources in the Tatras.
4
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
5
Content available Tatra Mountains (Figs 53–57)
Krobicki Michał, Golonka Jan
Geotourism / Geoturystyka
|
2024
|
nr 1-2 (76-77)
63--67
6
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
7
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
8
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
9
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
10
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
11
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
12
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
13
Content available Stop 20 – Kraków vicinity – Middle-Upper Jurassic and Upper Cretaceous deposits
Geotourism / Geoturystyka
|
2024
|
nr 1-2 (76-77)
69
14
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
15
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
16
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
17
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
18
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
19
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
20
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
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