Terasy Wetliny w Bieszczadach (Karpaty Wschodnie) – próba porównania ich hipsometrii, budowy i wieku z doliną górnego Sanu

Kukulak, Józef

doi:10.12657/landfana.028.003

Cited by 4 publications

(4 citation statements)

References 7 publications

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“…Very comparable results were obtained in studies from river valleys of a similar mining and metallurgical district in Wallonia (Belgium), where the method of searching for macroand microscopic slag as well as for magnetic iron spherules was applied (Houbrechts, 2007;Houbrechts et al, , 2020, 2004. However, these results concerned only medieval and post-medieval metallurgical activities, as confirmed by historical materials.…”

Section: Discussionsupporting

confidence: 64%

“…Further research results from various areas proved, however, that these muds were deposited throughout the late glacial and Holocene, although at a different rate (Kalicki, 2006). Many authors, however, still closely associate the appearance and sedimentation of these muds with an anthropogenic factor (e.g., Klimek, 1988Klimek, , 2003Lipps, 1988;Hiller et al, 1991;Pastre et al, 1991;Litt, 1992;Brown, Keough, 1992a, 1992bAlexandrowicz, 1996), which undoubtedly had a strong influence from the Middle Ages (e.g., Schirmer, 1995;Klimek, 1996;Houben, 2003) and initiated such deposition in small mountain catchments in the last few centuries (e.g., Hong, 1995;Mäckel and Zollinger, 1995;Klimek et al, 2003;Kukulak, 2004).…”

Section: Introductionmentioning

confidence: 99%

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Sedimentological and geochemical traces of metallurgical activity in the Świślina River valley (central Poland) at the Doły Biskupie site

Przepióra,

Kalicki

2024

Quat. res.

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Prehistoric and historic iron metallurgy in the Holy Cross Mountains in central Poland developed along with human Przeworsk Culture activity (during the Roman period) and within the boundaries of the Old-Polish Industrial District (OPID) during the Middle Ages and during recent centuries. At the Świślina catchment, there are many archaeological sites showing intense prehistoric metallurgical activity. The later medieval and modern iron industry was significantly smaller. At the Doły Biskupie site, slags and microscopic iron spherules (hammerscales) were found in alluvia. The microscopic spherules separation method (MSS) enabled analysis of these small artefacts created during iron ore smelting and forging. Iron spherules were detected in floodplain sediments, which are characterized by increased content of trace elements. The presence of these artefacts in shallow sediment layers in the confluence section of the river may be an indicator of archaeologically confirmed prehistoric metallurgical activity in the catchment area. Study of these residues enabled an attempt to reconstruct the river valley environment during the prehistoric and historical period. The MSS method can be used to detect iron spherules in alluvia in other river catchments, confirming the presence of yet-undiscovered bloomery sites.

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Section: Discussionsupporting

confidence: 64%

Section: Introductionmentioning

confidence: 99%

Sedimentological and geochemical traces of metallurgical activity in the Świślina River valley (central Poland) at the Doły Biskupie site

Przepióra,

Kalicki

2024

Quat. res.

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“…173-194 and second half of the 15th century -17th century) (Gębica et al, 2013a). Both flood subphases, in addition to the anthropogenic component associated with the beginning of the Wallachian settlements in the Eastern Carpathians (Kukulak, 2004(Kukulak, , 2014Alexandrowicz et al, 2005;Gębica et al, 2013b) coincide with the climate wetting and cooling at the beginning of the Little Ice Age (Steinhilber & Beer, 2011). In the last 2000 years a clear increase (peaks) in the frequency of floods in the following periods: 1400-1100 BP, 800-500 BP and 300-0 BP, was recorded in the lakes of the central Alps (Wirth et al, 2013) and in the Romanian Carpathian river valleys (Radoane et al, 2019).…”

Section: Discussionmentioning

confidence: 99%

Evolution of the Holocene alluvial fan of the River Stryi in the foreland of the Eastern Carpathians (Western Ukraine)

Gębica¹,

Jacyšyn²,

Szczepanek

2023

Geogr. Pol.

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The research reconstructs the development of the alluvial fan of the River Stryi in the Holocene and dates the phases of increased river activity and their correlation with other valleys in the upper Dniester and Vistula river basins. The age of the palaeochannels and the stratigraphy of alluvial fills are based on radiocarbon dating supported by the results of palynological analyses. The oldest (fossil) palaeochannel of the Stryi was dated to the Younger Dryas. The large-radius meander was abandoned at the end of the Boreal Phase during the period of flood intensification at about 8700 BP. The uneven top of the gravels (cut by palaeotroughs of a depth ranging from 2 to 4 m) indicates that during periods of increased discharges (Younger Dryas, end of the Boreal Phase, late Atlantic and beginning of the Subboreal) the troughs were cut and filled with channel sands. From the beginning of the Subboreal Phase (5400-5300 BP), aggradation of the valley bottom has been predominant, which is manifested not only by the overbuilding of the floodplain but also by the gradual elevation of the channel. The accumulation of sandy-silty overbank sediments dated to about 8300, 5400 and 2800 BP correlates well with the beginning of humid phases and floods in the upper Vistula and upper Dniester basins as well as floods recorded in lakes in the northern foreland of the Alps.

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“…W efekcie oddziaływań antropogenicznych koryta rzek i potoków w wielu odcinkach zostały zmienione ze żwirodennych w skalne oraz z roztokowych w błądzące lub kręte, docięte do litego podłoża (Wyżga 1993, Starkel, Łajczak 2008, Bucała 2012, Kukulak 2015, Witkowski, Wysmołek 2015, Zawiejska i in. 2015, Gorczyca i in.…”

Section: Rola Regulacji Koryt W Zmianach Ich Morfologii I Bilansie Transportu Rumowiskaunclassified

Współczesna ewolucja rzeźby Karpat Zewnętrznych i Podhala

Święchowicz¹,

Margielewski²,

Starkel³

et al. 2021

Współczesne Przemiany Rzeźby Polski

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Terasy Wetliny w Bieszczadach (Karpaty Wschodnie) – próba porównania ich hipsometrii, budowy i wieku z doliną górnego Sanu

Cited by 4 publications

References 7 publications

Sedimentological and geochemical traces of metallurgical activity in the Świślina River valley (central Poland) at the Doły Biskupie site

Sedimentological and geochemical traces of metallurgical activity in the Świślina River valley (central Poland) at the Doły Biskupie site

Evolution of the Holocene alluvial fan of the River Stryi in the foreland of the Eastern Carpathians (Western Ukraine)

Współczesna ewolucja rzeźby Karpat Zewnętrznych i Podhala

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