Słomka, Tadeusz
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Item type:Interactive Resource, Access status: Metadata only , Geologia. Ziemia i procesy endogeniczne(Akademia Górniczo-Hutnicza im. St. Staszica w Krakowie, 2022) Golonka, Jan; Słomka, Tadeusz; Waśkowska, Anna; Słomka, Tadeusz
Wydział Geologii, Geofizyki i Ochrony Środowiska; Centrum e-Learningu i Innowacyjnej DydaktykiE-podręcznik poświęcony jest omówieniu podstawowych zagadnień wchodzących w zakres geologii, jednej z najważniejszych nauk o Ziemi. Porusza zagadnienia podstawowe, związane z budową Ziemi, geotektoniką oraz z procesami endogenicznymi, czyli magmatyzmem, epejrogenezą, trzęsieniami ziemi oraz metamorfizmem. Przedstawiono genezę tych procesów, środowiska w jakich zachodzą, mechanizmy oraz ich efekty, ze szczególnym uwzględnieniem skał magmowych i metamorficznych. Wskazana została komplementarność procesów geologicznych, które w czasie geologicznym wpływają na zmiany w konfiguracji Ziemi.Item type:Article, Access status: Open Access , Litostratygrafia osadów górnej jury i dolnej kredy zachodniej części Karpat zewnętrznych (propozycja do dyskusji)(Wydawnictwa AGH, 2008) Golonka, Jan; Vašíček, Zdenĕk; Skupien, Petr; Waśkowska, Anna; Krobicki, Michał; Cieszkowski, Marek; Ślączka, Andrzej; Słomka, TadeuszUpper Jurassic-Lower Cretaceous deposits are part of the Outer Carpathians nappes: Magura, Silesian and Sub-Silesian-Żdanice-Waschberg, and are known in olistholites, which occur within different units of the Outer Carpathians. Authors systematized lithostratigraphical units according to their primary position in sedimentary basins and other sedimentary areas. Magura Basin originated in Middle Jurassic and proto-Silesian Basin in Late Jurassic-Early Cretaceous times together with syn- and post-rift deposits. Sub-Silesian-Żdanice sedimentary area originated in Late Cretaceous, and during Jurassic and Early Cretaceous times was northern part of the proto-Silesian Basin. The source areas for olistholites have been northern slope and shelf of the proto-Silesian Basin and submerged intra-oceanic ridges (cordilleras).Item type:Article, Access status: Open Access , The geotourist attractions in the vicinity of Szczawnica spa(2014) Golonka, Jan; Waśkowska, Anna; Doktor, Marek; Krobicki, Michał; Słomka, TadeuszThe main aim of this paper is presentation of the most characteristic outcrops/geological monuments, which occur in Szczawnica spa vicinity and are perfect geotouristic objects. These objects are presented with short geological/geomorphological remarks about their origin, development and significance in natural sciences. They provide the excellent inanimate natural monuments (geotourist trail in Pieniny Mountains from Szczawnica to Červený Kláštor, Palenica Mountain, Zawiasy area, Bryjarka Mountain, Jarmuta Mountain and Zaskalnik Waterfall), which can be used for better understanding of the history of our Earth and numerous geological processes, which „sculptured” its surface, especially very complicated geological story of the Pieniny Klippen Belt.Item type:Article, Access status: Open Access , Rocky forms in the Yamna Sandstone (Skyba Nappe, Outer Carpathians, Ukraine)(Wydawnictwa AGH, 2019) Waśkowska, Anna; Hnylko, Svitlana; Bakayeva, Sofia; Golonka, Jan; Słomka, Tadeusz; Heneralova, LarysaInteresting objects - the rocky forms and waterfall thresholds, built of Yamna Sandstone occur in the vicinity of Skole town. Beside the esthetic positive aspects related the morphological variety of the rocky forms and occurrence of the diversified weathering structures, the objects have a substantial cognitive value encompassing the lithology and sedimentological processes of the thick-bedded turbidites. The sandstone rocky forms usually occur in the groups distributed on slopes and forming so-called rocky towns. Their number and distribution allow observation of the changing structural and textural features both lateral and vertical within the 100-m thick composed profiles. The excellent degree of rocks outcropping, variety of structural and textural features and spectrum of possible observations indicates the high geotouristic potential of the investigated objects.Item type:Interactive Resource, Access status: Metadata only , Geologia. Ziemia i procesy egzogeniczne(Akademia Górniczo-Hutnicza im. St. Staszica w Krakowie, 2023) Golonka, Jan; Słomka, Tadeusz; Waśkowska, Anna; Waśkowska, Anna
Wydział Geologii, Geofizyki i Ochrony ŚrodowiskaE-podręcznik przedstawia podstawowe zagadnienia wchodzące w zakres geologii dynamicznej, które dotyczą procesów egzogenicznych, czyli tych które kształtują naszą Planetę pozyskując energię pozaziemską. Porusza zagadnienia związane z działalnością wód we wszystkich stanach skupienia, prądów powietrznych, powierzchniowych ruchów masowych oraz uczestnictwa w procesach geologicznych atmosfery i biosfery. Przedstawia genezę procesów egzogenicznych, środowiska w jakich przebiegają, ich mechanizmy oraz ich efekty, ze szczególnym uwzględnieniem ich roli morfotwórczej i akumulacyjnej, wraz z charakterystyką podstawowych typów skał osadowych.Item type:Article, Access status: Open Access , Utwory formacji wierzowskiej na tle wczesnokredowych warunków sedymentacji w zachodniej części basenu protośląskiego (Morawy, Republika Czeska)(Wydawnictwa AGH, 2009) Strzeboński, Piotr Andrzej; Golonka, Jan; Waśkowska, Anna; Krobicki, Michał; Słomka, Tadeusz; Skupien, Petr; Vašíček, ZdenĕkSedimentological development of the Verovice Formation (Czech Moravia) is presented, according to Early Cretaceous geotectonic-eustatic changes in the proto-Silesian Basin. Those processes were a consequence of a gradual rebuilding the architecture of the Alpine-Carpathian realm. The geological events well correspond with the global sequence stratigraphy.Item type:Article, Access status: Open Access , Koncepcja projektu: »Geostrada Sudecka - studium geologiczno-krajobrazowe z inwentaryzacją obiektów dziedzictwa przyrody nieożywionej«(Wydawnictwa AGH, 2009) Słomka, Tadeusz; Bartuś, Tomasz; Mastej, Wojciech; Łodziński, Marek; Mayer, Wojciech; Strfaniuk, Michał; Doktor, Marek; Koźma, Jacek; Cwojdziński, Stefan; Stachowiak, AndrzejThe aim of the paper is presentation of geological and landscape studies with the inventarization of abiotic nature objects located along proposed trail »The Leszek Sawicki Sudetic Geostrada«. Through detailed descriptions of the trail and proposals of development of selected, most attractive geosites of geological-mining heritage, the project should aim to spread geological knowledge of the Sudety Mts. among the non-professionals. Using the passable roads, the trail was led along the main ridges of the Sudety Mts. in both the Polish and the Czech parts, through less popular and rarely visited but also interesting parts of the Sudety Mts. and their foreland. Polish parts of the Geostrada (ca 285 km) were such determined to reach as much the most attractive geosites as possible in the 10-kilometers-wide zone ($\pm$ 5 km from both sides of the trail).Item type:Article, Access status: Open Access , A record of Eocene subaqueous large-scale mass movements in the external Tethys Ocean (Skyba Nappe, Outer Carpathians, Ukraine)(Wydawnictwa AGH, 2025) Waśkowska, Anna; Hnylko, Svitlana; Kowal-Kasprzyk, Justyna; Golonka, Jan; Słomka, Tadeusz; Hnylko, Oleh; Heneralova, Larysa; Pilarz, MonikaStudies were carried out on the Popeli Beds, which were mainly deposited by mass movements along the northern slope of the Tethys Ocean and form an olistostrome sequence occurring within Paleogene deposits. The analysis focuses on the deposits exposed in the northern limb of the Pobuk Syncline – the structural element of the Oriv Skyba – in the external zones of the Skyba (Skole) Nappe. Structural, lithological, sedimentological and paleontological studies allowed for the identification and characterisation of the olistostrome sequence and revealed its structure. Six individual olistostrome complexes were distinguished and described in detail. Five of these are gravelly mudstoneswith oversized clasts, overlain by medium-bedded mudstones and sandstones, the last one consists of deformed packages of thin bedded mudstones and sandstones. The olistostrome sequence is composed of a wide range of lithological and stratigraphic components, including Tithonian – Berriasian shallow- water limestones (so-called Štramberk-type limestones), Upper Cretaceous limestones, sandstones, and siliceous rocks, as well as Paleogene mudstones, sandstones, limestones, and marls. Biostratigraphic analysis of foraminifera indicates the Bartonian as the time of displacement. The olistostrome niche migrated downslope from a lower shelf-upper slope position characterized by marl sedimentation, to slope areas dominated by turbidite sedimentation.Item type:Article, Access status: Open Access , Atrakcje geoturystyczne Geostrady Wschodniosudeckiej(Wydawnictwa AGH, 2009) Słomka, Tadeusz; Doktor, Marek; Bartuś, Tomasz; Mastej, Wojciech; Łodziński, MarekThe Eastern Sudetic Geostrada (Geotrail) constitutes only a small, eastermost fragment of the whole »Sudetic Geostrada« tourist trail project. Hence, the number of geosites selected along the trail is rather limited. The westernmost site is the famous Sławniowice quarry. Here, in 16 active and inactive pits the Precambrian marbles and accompanying rocks (mica schists, amphibolites and pegmatites) have been quarried since the XIIIth century. Stones extracted there are well-known in Poland and in Germany, usually as facings. However, the most intrising part of the Eastern Sudetic Geostrada is the vicinity of Głuchołazy. In the town itself and in the valley of the Biała Głuchołaska River as well as in the adjacent Jeseniki and Zlaté Hory mountains in the Czech Republic gold has been mined from alluvial deposits as well as from quartz and quartz-feldspar lodes. The relics of this mining operations are numerous adits and shafts, which can be recently seen along the promenade accompanying the Biała Głuchołaska River bank. Other sites attractive for the Earth-science enthusiasts are: granitoids of the Strzelin-Žulova Massif in Jarnołtów, Precambrian marbles in Gierałcice and biotitic schists in Burgrabice. The last site in the Polish sector of the Eastern Sudetic Geostrada is the operating slate quarry in Jarnołtówek where phyllitic schists are extracted and used as roof tiles.Item type:Article, Access status: Open Access , Stanowiska najstarszych skał osadowych w polskich Karpatach fliszowych jako obiekty geoturystyczne(Wydawnictwa AGH, 2008) Waśkowska, Anna; Krobicki, Michał; Golonka, Jan; Słomka, Tadeusz; Ślączka, Andrzej; Doktor, MarekThe popularization of educational aspects linked to the geological history of Earth is one of the goals of geotourism, dynamically developing recently. The present paper contains the description of the classic localities exposing the oldest deposits of the Outer Flysch Carpathians. Firstly, these are initial Late Jurassic-Early Cretaceous basinal facies originated during early carbonate flyschoidal stages within the developing proto-Silesian Basin (Goleszów - Vendryne Formation, Soła River valley in Żywiec and Jasieniowa Mt and Leszna Górna - Cieszyn Limestone Formation). Secondly, these are different size limestone blocks, olistoliths in origin, known as Andrychów Klippen (Targanice, Roczyny and Inwałd) represent Jurassic reef and circum-reef environments originated in shallow-water condition on the Baska-Inwałd submarine ridge.