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Tytuł:
Pleistocene deposits in the western part of the Holy Cross Mountains
Autorzy:
Lindner, Leszek
Dzierżek, Jan
Powiązania:
https://bibliotekanauki.pl/articles/2025105.pdf
Data publikacji:
2019
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Quaternary deposits
Holy Cross Mts.
glacial palaeogeography
interglacial records
Opis:
The paper presents characteristics of the Pleistocene sediments in the western part of the Holy Cross Mountains. They are subdivided into four complexes and their stratigraphic setting is referred to the updated scheme for the Pleistocene of Poland. The Preglacial Complex includes fluvial sediments characteristic for its lack of Scandinavian material. Sediments of three main glaciations (Nidanian, Sanian 1 and Sanian 2) within the South Polish Complex, are referred also as the South Polish Glaciations. The oldest of these glaciations (Nidanian) is separated from the middle glaciation (Sanian 1) by sediments of the Podlasian Interglacial, represented by clay at the Kozi Grzbiet Cave that contains faunal remains and record of the Brunhes/Matuyama palaeomagnetic boundary. During the middle (Sanian 1) and youngest glaciation (Sanian 2), the Holy Cross Mountains were almost completely covered by the Scandinavian ice sheet, forming glacial deposits separated by fluvial series of the Ferdynandovian Interglacial. The Middle Polish Complex begins with sediments of the Mazovian Interglacial, represented by a pollen record from the Zakrucze site. They are followed by deposits of periglacial and fluvial origin of the Liwiecian Glaciation, Zbójnian Interglacial, Krznanian Glaciation and Lublinian Interglacial. The following glaciation (Odranian) is represented by the youngest glacial deposits that document presence of the Scandinavian ice-sheet in the westernmost part of the Holy Cross Mountains. The North Polish Complex is composed of a climatic warming (Eemian Interglacial) and cooling (Vistulian Glaciation), and is represented by valley and periglacial deposits. The last cooling of the Pleistocene is recorded in faunal remains in the Raj Cave.
Źródło:
Studia Quaternaria; 2019, 36; 75-85
1641-5558
2300-0384
Pojawia się w:
Studia Quaternaria
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Od geologicznego parku krajobrazowego do geoparku globalnego (1991–2021)
From a geological landscape park to a global geopark (1991-2021)
Autorzy:
Wróblewski, Tomasz
Powiązania:
https://bibliotekanauki.pl/articles/2076176.pdf
Data publikacji:
2021
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
geodziedzictwo
geokonserwacja
geopark
Góry Świętokrzyskie
geoheritage
geoconservation
Holy Cross Mts.
Opis:
The Chęiny-Kielce Geological Landscape Park was proposed to be created in 1991, in order to protect the geological heritage of supra regional value, as well for educational purposes and development of geotourism. It was established in 1996 as the Chęciny-Kielce Landscape Park (ChKLP). The key adjective (Geological) was missing from its name due to the lack of relevant legislation (despite this, the ChKLP was promoted as a geological park, i.a., during the International ProGEO workshops in 1997 and 2003). At the beginning of 21st century, when a Global Geoparks Network was being organized, the ChKLP, as meeting all UNESCO geopark requirements, was proposed to be included in the network. The Geopark Kielce Centre (an institution previously established for geoheritage promotion purposes) was crucial in the foundation of the new geopark (on the basis on ChKLP), and preparing an application according to UNESCO instructions. The Chęciny-Kielce Geopark, eventually called Holy Cross Mountains Geopark (as its area was extended) was established and included in the Global Geoparks Network in 2021. It should be emphasized that the Polish Geological Institute also played a key role in the whole process, because both innovative ideas (the geological landscape park and the centre of geological education) originated in its Holy Cross Mts. Branch.
Źródło:
Przegląd Geologiczny; 2021, 69, 5; 287--293
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Nowe dane o litologii i biostratygrafii akritarchowej skał kambryjskich na Łysicy, najwyższym szczycie Gór Świętokrzyskich
New data on the lithology and acritarch biostratigraphy of Cambrian rocks of Łysica Mt., the highest summit of the Holy Cross Mountains
Autorzy:
Szczepanik, Z.
Malec, J.
Powiązania:
https://bibliotekanauki.pl/articles/2075672.pdf
Data publikacji:
2017
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
kambr
litologia
arkritarchy
biostratygrafia
Holy Cross Mts.
Cambrian
lithology
acritarchs
biostratigraphy
Holy Cross Mountains
Opis:
The southern slope of Łysica Mountain, which is the highest elevation of the Holy Cross Mountains, is comprised of three lithological complexes divided by parallel fault zones. The uppermost part of the succession consists of quartzitic sandstone of the Wiśniówka Formation. The formation is underlain by a complex of sandstone with mudstone interbeds, with black claystone underneath, which is exposed in the upper part of the Glęboczka ravine succession. The strata of the first and the third complexes dip northward, whereas those of the second complex dip southward. In the fault-bound zone between the second and the third complexes, there are concentrations of weathering iron ore. The black claystone, which is lithologically similar to this of the Pepper Mountains Formation, contains a taxonomically rich assemblage of organic-walled microfossils (acritarchs) diagnostic of the Upper Cambrian (Lower Furongian) successions. The new record of microfossils allows determining the age of the succession composing the Łysogóry Mountains for the first time in the history of regional geological investigation.
Źródło:
Przegląd Geologiczny; 2017, 65, 9; 564--575
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Cyclic ecological replacement of brachiopod assemblages in the top-Eifelian Dobruchna Brachiopod Shale Member (Skały Formation) of the Holy Cross Mountains (Poland)
Autorzy:
Woźniak, Paweł
Halamski, Adam T.
Racki, Grzegorz
Powiązania:
https://bibliotekanauki.pl/articles/2182172.pdf
Data publikacji:
2022
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
Brachiopods
palaeoecology
Eifelian
Kačák Event
Skały Formation
Devonian
Holy Cross Mts
Opis:
The palaeoecology of fossiliferous shales, belonging to the upper part of the Dobruchna Brachiopod Shale Member (= set XIV) of the Skały Formation (northern Holy Cross Mountains), was studied quantitatively in a succession in the transient (1989) trench A, 5.6 m thick, near the village of Skały. The top-Eifelian strata, recording the carbonate crisis during the global Kačák Bioevent, are well known for having a particularly diverse brachiopod fauna. The four brachiopod assemblages, recognised herein, were mainly controlled by the evolving bottom-sediment properties of the outer carbonate ramp basin. Soft, unstable substrates were inhabited by the poorly-diversified Poloniproductus assemblage, associated with a distinctive, ‘incumbent’ set of largely semi-infaunal, generalist species. The pioneer community, as a result of progressive consolidation of bioclast-enriched sediment, evolved toward a more diverse biota. This consequent stabilisation of the substrate resulted in the progressive growth of crinoid thickets or bryozoan-dominated biostromes and patches, associated with rich, subordinate, sessile and vagile benthos. In this stage, diverse brachiopod assemblages were dominated by the pedunculate, eurytopic, ribbed spiriferide Eleutherokomma or specialized orthides (Aulacella, Costisorthis) in the Dobruchna Mbr, and by the expansive, large, free-lying orthotetide Xystostrophia in the overlying set XV of the Skały Fm The cyclic ecological replacement, with the characters of ecological succession in the final phase, was evidently stimulated by an irregular transition from soupy muds to a mosaic of bioclast-rich and firmer, biogenic sediments, within the cyclic pattern of distal tempestite sedimentation. The three episodes of variously reduced deposition rate, recorded in the more diverse benthos, culminated in the pioneer bryozoan/coral reef growth and abundance of epibionts, alternating with times of destructive storm activity and deposition from suspension clouds in the muddy habitats.
Źródło:
Annales Societatis Geologorum Poloniae; 2022, 92, 4; 445--463
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Xenotime from the Podwiśniówka mine pit, Holy Cross Mountains (South-Central Poland)
Autorzy:
Migaszewski, Zdzisław M.
Gałuszka, Agnieszka
Powiązania:
https://bibliotekanauki.pl/articles/2086505.pdf
Data publikacji:
2010
Wydawca:
Polskie Towarzystwo Mineralogiczne
Tematy:
xenotime
Wiśniówka Sandstone Fm
Podwiśniówka mine pit
Holy Cross Mts
Polska
TESZ
Opis:
This report presents the results of petrographical and mineralogical (optical microscopy, SEM/EDS) study of xenotime derived from the Upper (Middle?) Cambrian rocks (Wiśniówka Sandstone Fm.) of the abandoned Podwiśniówka mine pit. This is the first work on this mineral from the Holy Cross Mts. The authigenic xenotime occurs primarily as overgrowths around/on zircon in siliciclastic rocks. Moreover, this mineral is characterized by the large size of the overgrowths reaching 50 μm long and 20 μm wide. The presence of pyritecoated zircon/xenotime aggregates indicates that the xenotime formed prior to hydrothermal quartz-pyrite mineralization. The apparent lack of xenotime and vein pyrite in the tuff-bearing series, compared to the other two series displaying hydrothermal signature (pyrite, hematite, nacrite, jarosite), as well as considerable variations of the xenotime overgrowths in size and morphology, and their dominant irregular patchy-zonal microtexture may provide evidence for direct precipitation of this mineral from hydrothermal fluids.
Źródło:
Mineralogia; 2010, 41, 1/2; 3--9
1899-8291
1899-8526
Pojawia się w:
Mineralogia
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Xenotime from the Podwiśniówka mine pit, Holy Cross Mountains (South-Central Poland)
Autorzy:
Migaszewski, Z. M.
Gałuszka, A.
Powiązania:
https://bibliotekanauki.pl/articles/2086545.pdf
Data publikacji:
2010
Wydawca:
Polskie Towarzystwo Mineralogiczne
Tematy:
xenotime
Wiśniówka Sandstone Fm
Podwiśniówka mine pit
Holy Cross Mts
Polska
TESZ
Opis:
This report presents the results of petrographical and mineralogical (optical microscopy, SEM/EDS) study of xenotime derived from the Upper (Middle?) Cambrian rocks (Wiśniówka Sandstone Fm.) of the abandoned Podwiśniówka mine pit. This is the first work on this mineral from the Holy Cross Mts. The authigenic xenotime occurs primarily as overgrowths around/on zircon in siliciclastic rocks. Moreover, this mineral is characterized by the large size of the overgrowths reaching 50 μm long and 20 μm wide. The presence of pyritecoated zircon/xenotime aggregates indicates that the xenotime formed prior to hydrothermal quartz-pyrite mineralization. The apparent lack of xenotime and vein pyrite in the tuff-bearing series, compared to the other two series displaying hydrothermal signature (pyrite, hematite, nacrite, jarosite), as well as considerable variations of the xenotime overgrowths in size and morphology, and their dominant irregular patchy-zonal microtexture may provide evidence for direct precipitation of this mineral from hydrothermal fluids.
Źródło:
Mineralogia; 2010, 41, 1/2; 3--9
1899-8291
1899-8526
Pojawia się w:
Mineralogia
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Middle Devonian Skały Formation in the Holy Cross Mountains (Poland) : formal description and subdivision based on new field data
Autorzy:
Racki, Grzegorz
Wójcik, Krystian
Halamski, Adam T.
Narkiewicz, Marek
Powiązania:
https://bibliotekanauki.pl/articles/2182148.pdf
Data publikacji:
2022
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
lithostratigraphy
Skały Formation
Dobruchna Member
Middle Devonian
Łysogóry Region
Holy Cross Mts
Opis:
The well-known fossiliferous and lithologically variable clay-carbonate series in the Łysogóry Region (northern part of the Holy Cross Mts, central Poland), enclosed between the Middle Devonian Amphipora dolomites and limestones (Kowala Formation) and siliciclastics (Świętomarz Beds), is defined formally as the Shaly-Calcareous Skały Formation. This Upper Eifelian to Middle Givetian, ca. 250–280 m thick unit, consists of marly and clay shales, interbedded many times with various limestone types (including encrinite and biohermal varieties), as well as with marls and siltstones. Its diagnostic feature is the presence of variable skeletal accumulations, formed by exceptionally numerous, well-preserved and diverse macrofauna (including brachiopods, corals, crinoids, bryozoans), described since the 19th century. The stratotype is located in the eastern slope of the Dobruchna stream near the Skały village and belongs to the Silurian to Upper Devonian Grzegorzowice-Skały section. Compared to the previously used term, Skały Beds sensu Pajchlowa (1957), the lower boundary is redefined, owing to a new exposure in the active Skała Quarry, and placed higher, at the base of the famous brachiopod shales (set XIV of Pajchlowa), instead of the formerly accepted lower boundary at the base of set XIII. Set XIV is formally distinguished as the Dobruchna Brachiopod Shale Member. The higher part of the Skały Fm (sets XV–XXVA) is not subdivided further, as the poorly exposed succession, including in particular the type area, precludes a more accurate recognition of lithological variability. The upper boundary of the Skały Fm is placed at the top of set XXV sensu Pajchlowa (1957), corresponding to the boundary between subsets XXVA and XXVB sensu Malec and Turnau (1997). A hypostratotype of the upper boundary is selected in the outcrop M0 at Miłoszów, 2.5 km westwards from the type section, allowing recognition of the diachroneity of lithological change defining the transition from the Skały Fm to Świętomarz Beds. A borehole situated in a key location would be an obvious next step in the further elucidation of the stratigraphic sequence of the Łysogóry Region.
Źródło:
Annales Societatis Geologorum Poloniae; 2022, 92, 4; 425--444
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Problematyka dotycząca uzyskania zgody na wydobycie surowców skalnych poniżej zwierciadła wód podziemnych na przykładzie wybranych kopalń w regionie świętokrzyskim
Problems related to obtaining the mining concessions for extraction of industrial minerals beneath the groundwater table -examples from selected quarries in the Holy Cross Mts.
Autorzy:
Białecka, Katarzyna
Kos, Marcin
Powiązania:
https://bibliotekanauki.pl/articles/2076057.pdf
Data publikacji:
2020
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
kopalnie odkrywkowe
odwadnianie kopalni
region świętokrzyski
opencast mines
mine dewatering
Holy Cross Mts. region
Opis:
The Holy Cross Mts. region is a very important mining district of industrial minerals used in the building industry, road construction and cement/lime manufacturing. Due to high demand for construction aggregates, the owners of mineral deposits apply to local authorities for permits to extract industrial minerals from beneath the groundwater table. However, some local authorities do not grant such permits in order to prevent the impact of mine drainage related to such extraction on admissible volumes of groundwater in local intakes. The paper presents the consecutive stages of administrative procedure, starting from the entry of mining operations (beneath the groundwater table) to the local zoning plan until the granting of the legal permit for specified use of inland waters (i.e. for mine drainage). Problems encountered during the granting procedure of the permit are presented as case studies of selected quarries from the Łagów region and of the "Celiny” limestone quarry.
Źródło:
Przegląd Geologiczny; 2020, 68, 4; 237--241
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Permian to Triassic paleokarst of the Świętokrzyskie (Holy Cross) Mts, central Poland
Permsko-triasowy kras kopalny Gór Świętokrzyskich, Polska środkowa
Autorzy:
Urban, J.
Powiązania:
https://bibliotekanauki.pl/articles/183335.pdf
Data publikacji:
2007
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:
kras kopalny
perm
trias
paleogeografia
Góry Świętokrzyskie
paleokarst
Permian
Triassic
paleogeography
Świętokrzystkie (Holy Cross) Mts.
Opis:
This paper presents classification of the Permian and Triassic paleokarst forms in the Świętokrzyskie Mts, systematic description of the groups of forms and their fillings as well as conclusions concerning environmental conditions of their development. Four groups were distinguished among paleokarst forms developed before the deposition of the Buntsandstein whereas five ones developed during the Buntsandstein deposition (proceeding diachronically) and/or the Middle Triassic time. The Permian-Triassic paleokarst was conditioned by the Variscan tectonic movements and up-lift as well as subsequent formation of the Danish-Polish Trough. The Permian karst developed in the area of mountainous morphology and were often connected with hydrothermal processes. The Triassic karst formed due to tectonic activity stimulating morphological rejuvenation of the region. Wide and low passages representing one of the Triassic paleokarst group presumably formed in fresh and sea waters mixing zone.
Artykuł prezentuje klasyfikację permskich i triasowych form paleokrasowych w Górach Świętokrzyskich, systematyczny opis poszczególnych typów tych form oraz ich wypełnień, jak również wnioski dotyczące warunków ich rozwoju. Wyróżniono cztery typy form pseudokrasowych powstałych przed sedymentacją osadów pstrego piaskowca oraz pięć typów tworzących się w trakcie sedymentacji pstrego piaskowca (następującej diachronicznie) oraz/lub środkowego triasu. Permsko--triasowy kras kopalny był warunkowany waryscyjskimi ruchami tektonicznymi oraz wyniesieniem regionu, a następnie tworzeniem się niecki duńsko-polskiej. Kras permski rozwijał się na obszarze o górskiej rzeźbie i był często związany z procesami hydrotermalnymi. Kras triasowy powstał w rezultacie aktywności tektonicznej powodującej odnowienie rzeźby regionu. Szerokie i niskie kanały reprezentujące jedną z generacji krasu triasowego utworzyły się prawdopodobnie w strefie mieszania się wód słodkich i słonych.
Źródło:
Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie; 2007, 33, 1; 5-50
0138-0974
Pojawia się w:
Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Osiemdziesiąt lat Oddziału Świętokrzyskiego Państwowego Instytutu Geologicznego w służbie polskiej geologii : osiągnięcia w geologii stosowanej
Eighty years of the Holy Cross Branch of the Polish Geological Institute in the survey of Polish geology : achievements in applied geology
Autorzy:
Szczepanik, Zbigniew
Białecka, Katarzyna
Giełżecka-Mądry, Dorota
Kos, Marcin
Wieczorek, Dariusz
Złonkiewicz, Zbigniew
Powiązania:
https://bibliotekanauki.pl/articles/2076169.pdf
Data publikacji:
2021
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Góry Świetokrzyskie
historia badań
kartografia geologiczna
geologia stosowana
hydrogeologia
Holy Cross Mts.
history of investigations
geological cartography
applied geology
hydrogeology
Opis:
This article presents the achievements of the employees of the Holy Cross Mts. Branch of the Polish Geological Institute in the field of applied geology: geological cartography, geology of natural resources and hydrogeology. The area of the Holy Cross Mts. is located in central Poland and for hundreds of years was the main source of metal ores and rock raw materials for the Polish state. Investigating the possibility of using these minerals and raw materials in the modern economy was the reason for establishing the Polish Geological Institute in Kielce. Shortly before World War II, a department of the Institute was established in Kielce for a detailed geological study of this interesting area, where the full profile of the Phanerozoic deposits is present, from the oldest Cambrian to Quaternary. The basic work performed by geologists in Kielce was the preparation of geological maps. During the 80 years of the Institute's activity in Kielce, geological maps on various scales were made, ranging from 1:300,000 to 1:50,000. Currently, detailed mapping at the 1:50,000 and 1: 25,000 scales are being prepared. The search for deposits of iron, copper and other metals, conducted by the Kielce Institute, did not lead unfortunately to discovery of economically useful deposits. On the other hand, large deposits of rock building materials have been identified and documented and are currently exploited mainly for road construction. The region of the Holy Cross Mountains and their vicinity is unique in comparison to other regions of Poland because the entire population and economy are supplied with water from underground sources. Taking care of resources and adequate water quality is the main goal of the hydrogeologists employed at the Holy Cross department of the Polish Geological Institute. They organized and supervise a network that controls the water level and its quality, the impact of quarry activities on the groundwater levels, and prepare various types of hydrogeological maps.
Źródło:
Przegląd Geologiczny; 2021, 69, 3; 185--196
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
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