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Jordanów – the town's genesis, urban layout and heritage protection. Initial remarks

Kuśnierz Kazimierz

Technical Transactions

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2019

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Vol. 116, iss. 11

41--49

EN

This article discusses the history of the spatial development of the town of Jordanów, as well as the cultural heritage sites located inside the territory of this urban centre. Jordanów, currently located within the administrative area of the Lesser Poland Voivodship, in the district of Sucha, was founded as a private town in 1564 and issued a charter by the Krakow Voivod Spytek Jordan of Zakliczyn. The urban centre is an example of a town which was founded in cruda radice–i.e. on previously undepeveloped land–during the early modern period but whose model bears a similarity to traditional urban forms used in previous centuries.

PL

Niniejszy artykuł dotyczy problematyki historii rozwoju przestrzennego miasta Jordanów oraz zabytków dziedzictwa kulturowego zlokalizowanych na terenie tego ośrodka. Jordanów, położony obecnie w granicach województwa małopolskiego, w powiecie suskim, został założony jako miasto prywatne w 1564 roku z fundacji wojewody krakowskiego Spytka Jordana z Zakliczyna. Ośrodek jest przykładem miasta, które lokowano na surowym korzeniu w okresie nowożytnym, ale jego rozplanowanie nawiązuje do tradycyjnych form urbanistycznych stosowanych w wiekach wcześniejszych.Niniejszy artykuł dotyczy problematyki historii rozwoju przestrzennego miasta Jordanów oraz zabytków dziedzictwa kulturowego zlokalizowanych na terenie tego ośrodka. Jordanów, położony obecnie w granicach województwa małopolskiego, w powiecie suskim, został założony jako miasto prywatne w 1564 roku z fundacji wojewody krakowskiego Spytka Jordana z Zakliczyna. Ośrodek jest przykładem miasta, które lokowano na surowym korzeniu w okresie nowożytnym, ale jego rozplanowanie nawiązuje do tradycyjnych form urbanistycznych stosowanych w wiekach wcześniejszych.

2

Origin of serpentinite-related nephrites from Gogołów-Jordanów Massif, Poland

Gil G., Barnes J. D., Boschi Ch., Gunia P., Szakmány G., Bendő Z., Raczyński P., Péterdi B.

Geological Quarterly

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2015

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Vol. 59, No. 3

457--472

EN

The Gogołów-Jordanów Massif (GJM) in the Fore-Sudetic Block, SW Poland, hosts nephrites traditionally interpreted as serpentinite-related (ortho-nephrite). This contribution confirms the serpentinite-related origin of the nephrites on the basis of mineralogy, bulk-rock chemistry, and O and H isotopes. Rock-forming amphiboles from nephrites of the GJM have 7.73–7.99 Si apfu, comparable to 7.76–8.03 Si apfu of serpentinite-related Crooks Mountain nephrite amphibole (Granite Mountains, Wyoming, USA). The GJM amphiboles also have Mg/(Mg + Fe2+) values ranging from 0.82 to 0.94, similar to serpentinite-related Crooks Mountain and New Zealand nephrites amphiboles with Mg/(Mg + Fe2+) values of 0.86–0.90 and 0.91 to 0.92, respectively. The GJM nephrite amphiboles differ from the Val Malenco dolomite-related nephrite (Italy) amphibole, e.g., Val Malenco has a higher Si content (~8.0 Si apfu), although it overlaps with some of the GJM nephrite samples, and ~1.0 Mg/(Mg + Fe2+), also higher than the GJM samples. Also, apatite in the nephrite studied from the GJM has a slightly higher Ca content than apatite from dolomite-related nephrite. Chlorites found in the Jordanów nephrite have similar compositions to that of chlorites in the serpentinite-related nephrites and also to chlorites associated with serpentinisation/rodingitisation. The bulk-rock FeO vs. Fe/(Fe + Mg), Cr, Ni, and Co are also typical of the serpentinite-related nephrites. The d18O values range from +6.1 to +6.7‰ (±0.1‰), and the average dD values = –61‰, corresponding with the serpentinite-related nephrites range. Based on petrographic observations, we suggest four crystallisation stages (including rodingitisation prior to nephrite formation): 1 – leucogranite rodingitisation and black-wall formation; 2 – tremolite formation at the expense of rodingite diopside and black-wall chlorite (nephritisation) and garnet break-down, with spinel and chlorite formation (chlorite can be a product of garnet break-down or spinel with serpentine reaction); 3 – prehnite vein formation; 4 – tremolite formation at the expense of prehnite veins and actinolite veins formation. Spinels composed of 0.29–1.96 wt.% MgO, 24.87–29.67 wt.% FeO, 8.72–22.82 wt.% Fe2O3, 3.11–4.36 wt.% Al2O3, and 39.07–54.46 wt.% Cr2O3 suggest nephritisation in the greenschist to lower-amphibolite-facies conditions.

3

Petrographic and geochemical investigation of a stone adze made of nephrite from the site Balatonőszöd – Temetői dűlő (Hungary)

Péterdi B., Szakmány G., Judik K., Dobosi G., Kasztovszky Z., Szilágyi V., Maróti B., Bendő Z., Gil G.

Geological Quarterly

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2014

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Vol. 58, No. 1

181--192

EN

The present study reports on results of petrographic and geochemical analyses on a stone adze from the archaeological site Balatonőszöd – Temetői dűlő (Hungary). This is the largest excavated site of the Baden Culture in Hungary (more than 200.000 m2) and has the longest continuous settlement history. In the site, features of the Balaton-Lasinja Culture (Middle Copper Age) and the Boleraz Culture were also found. Altogether 500 stone artefacts were found and registered. The present study reports on the results of the investigation of a unique stone adze made of nephrite, found on the site. The nephrite adze found in Balatonőszöd – Temetői dűlő has proved to be the first find made of nephrite having an established archaeological context in Hungarian prehistory. By applying detailed petrographic, geochemical and petrophysical methods as well as comparing data from technical literature we located the origin of the raw material of the nephrite adze. Its most probable source is the Northern part of the Bohemian Massif, Lower Silesia, a geological site near Jordanów (Poland).

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Petrographic and microprobe study of nephrites from Lower Silesia (SW Poland)

Gil G.

Geological Quarterly

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2013

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Vol. 57, No. 3

395--404

EN

Lower Silesia hosts important European nephrite deposits of Jordanów and less-known of Złoty Stok. Nephrite artifacts were discovered in archaeological sites dated back to the Neolithic period, across Eurasia. Especially artifacts found in Poland, Italy and Bulgaria may originate from Polish nephrites. Nowadays, only one artifact is precisely linked to Jordanów. Petrographic study of nephrites and chemical analyses of constituents by means of EMPA allow accurate identification of the nephrites. The characteristic phases of Jordanów tremolite nephrite are rotated and cataclased diopside porphyroblasts with pressure shadows, chlorite layers and nests with interlocking non-pseudomorphic texture and prehnite veins. The presence of hydrogrossular, grossular, titanite, apatite with monazite inclusions, and zircon with pleochroic haloe is typical. Chlorites are usually represented by penninite, and minor clinochlore and diabantite. The characteristic features of Złoty Stok actinolite nephrite are löllingite and diopside crystals usually visible by the naked eye, with the presence of quartz and carbonates. Löllingite is chemically inhomogeneous and gold bearing. Most of the mineralogical-petrological features can be obtained using non-destructive methods.