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Kamień w zabytkowej architekturze Szydłowa

Fijałkowska-Mader Ania, Złonkiewicz Zbigniew, Król Paweł

Przegląd Geologiczny

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2019

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Vol. 67, nr 9

736--748

EN

The historical city of Szydłów, located in the southeastern part of the Świętokrzyskie province, has preserved its medieval urban layout. It is surrounded by stone walls, hence the town is named the "Polish Carcasonne”. There are castle remains in the western part of the city. Two monumental objects discussed in the article - defensive walls with the Krakowska Gate and the St. Władysław church were built during the reign of King Casimir the Great. The All Saints Church can be older, because it contains Romanesque features. The time of construction of the castle palace is uncertain but its design may indicate the later period of the reign of Władysław Jagiełło and Anna Andegaweńska. The church and Holy Spirit sheltered-hospital originated in the early 16th century. All these buildings were made of local stone - organogenic-detritic limestones of the Chmielnik Formation (Late Badenian-Early Sarmatian), in the stoneworkers’ language called "Szydłów stone/sandstone”. Architectural details, such as portals, window frames or cornices, were carved from fine-grained limestones, similar to the Pińczów Limestones of Badenian age. The unambiguous lithostratigraphic classification of these stones requires a more datail petrographic research. Despite the Szydłów Limestones, common in Szydłów and its vicinity, were exploited here throughout centuries in many local quarries. It is currently impossible to indicate the local deposit in which the Pińczów Limestones were excavated. It is possible that they were transported from the Pińczów area.

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Burial crypts in solid rock – a geophysical case study of a small church with a unique polychrome in Szydłów (S Poland)

Zieliński Artur, Łyskowski Mikołaj, Mazurkiewicz Ewelina, Lubarska Kinga Wiktoria

Geology, Geophysics and Environment

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2019

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Vol. 45, no. 2

89--97

EN

Lesser Poland (Małopolska) is a historic region of Poland. The presented case study was undertaken in the All Saints’ Church in the town of Szydłów, in which conservation and restoration works were carried out to preserve Gothic wall paintings by identifying and eliminating the causes of their degradation, and these efforts were supported by geophysical surveying. The conducted studies constitute a step not only to determine the age of the construction of the Szydłów temple, but also to improve knowledge of medieval architecture and mural paintings in Lesser Poland. The geophysical research with application of GPR (Ground Penetrating Radar) helped to locate previously unknown structures under the temple floor. This survey indicated four, possibly connected, structural objects clearly visible in GPR profiles. Carried out works confirmed that anomalies visible on radargrams mark two crypts. This discovery of the hidden construction elements emphasizes and strengthens the earlier suppositions of the unique character of this temple.

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Uwagi o wieku osadów miocenu środkowego okolic Szydłowa [południowe obrzeżenie Gór Świętokrzyskich]

Stachacz M.

Przegląd Geologiczny

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2007

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Vol. 55, nr 2

168-168, 174

EN

The Middle Miocene sediments outcropping between Szydłów and Brzeziny are represented by the Pińczów Beds and the Chmielnik Beds. The Pińczów Beds are developed as the Heterostegina sands with intercalations of red algal limestones. These sediments contain numerous fossils of foraminifera, bryozoans, bivalves, ostracods, echinoids, crustaceans and corallinacean red algae. Foraminifera [Amphistegina, Heterostegina, Orbulina suturalis] point to the early Badenian age of the Pińczów Beds. The Chmielnik Beds contain mainly organodetritical limestones, which are composed mainly of grains eroded from the Badenian red algal limestones. The organodetritical limestones contain pebbles and blocks of microbial-serpulid limestones, Abra limestones, marls and rare lenses of quartz sands. Numerous pectenids, other small bivalves, gastropods, foraminifera and rhodolites occur here. The fossils point to mainly Anomalinoides dividens Zone. New literature data show that this zone, commonly accepted as diagnostic for the beginning of Sarmatian, is diachronic. Therefore, the Badenian-early Sarmatian age is suggested for the Chmielnik Beds. The presence or absence of normal-marine biota as an age criterium for the Badenian-Sarmatian boundary, the commonly accepted idea for the brackish Sarmatian basin of the central Paratethys has been challenged recently. Both Badenian (not redeposited) and Sarmatian fossils occur in the Chmielnik Beds. Therefore, part of deposits in the Szydłów area assumed so far to be of Sarmatian age, can in fact represent late Badenian age.

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Szydłów – niezwykły krajobraz warowny w skali Europy

Myczkowski Z.

Wiadomości Konserwatorskie

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2006

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Nr 19

38--44