2020
Raně středověké říční koryto v blízkosti fortifikačního systému velkomoravského hradiska Pohansko u Břeclavi
NEHYBA, Slavomír, Petr DRESLER, Nela DOLÁKOVÁ, František KUDA, Michaela PRIŠŤÁKOVÁ et. al.Základní údaje
Originální název
Raně středověké říční koryto v blízkosti fortifikačního systému velkomoravského hradiska Pohansko u Břeclavi
Název česky
Raně středověké říční koryto v blízkosti fortifikačního systému velkomoravského hradiska Pohansko u Břeclavi
Název anglicky
The Early Medieval fluvial channel within the defence system of the Great Moravia Empire agglomeration Pohansko near Břeclav
Autoři
NEHYBA, Slavomír (203 Česká republika, garant, domácí), Petr DRESLER (203 Česká republika, domácí), Nela DOLÁKOVÁ (203 Česká republika, domácí), František KUDA (203 Česká republika), Michaela PRIŠŤÁKOVÁ (703 Slovensko, domácí), Jakub ŠIMÍK (203 Česká republika), Jaroslav ŠKOJEC (203 Česká republika) a Karel KIRCHNER (203 Česká republika)
Vydání
Geologické výzkumy na Moravě a ve Slezsku, Brno, Masarykova univerzita, 2020, 1212-6209
Další údaje
Jazyk
čeština
Typ výsledku
Článek v odborném periodiku
Obor
10505 Geology
Stát vydavatele
Česká republika
Utajení
není předmětem státního či obchodního tajemství
Odkazy
Kód RIV
RIV/00216224:14310/20:00114409
Organizační jednotka
Přírodovědecká fakulta
Klíčová slova anglicky
fluvial channel; absolute-age dating techniques; medieval fortification; paleogeographic reconstruction
Štítky
Příznaky
Mezinárodní význam, Recenzováno
Změněno: 27. 1. 2021 16:43, Mgr. Marie Šípková, DiS.
V originále
Geophysical, sedimentological, palynological, absolute-age dating and archeological techniques were used to study the deposits of the Early Medieval fluvial channel in the area of the Great Moravia Empire agglomeration Pohansko near Břeclav. Artificial profile situated on the base of ERT profiles and the archeological results led to opening of the fluvial channel. Newly documented fluvial channel erosively cut the complex of flood loams. Gravel lag covers the bottom of the channel and grade upwards into sandy channel infill with fining upward trend. Fluvial sandy dunes forming the most characteristic architectural element of the infill are represented mostly by trough cross-stratified medium-grained sands. These sands were penetrated by the piece of oak wood. Both the OSL dating of the sandy deposits and the dating of the oak wood (C14 and dendrochronology) point to the 9th century A.D. when the Great Moravia Empire was on its peak expansion. Active fluvial channel was probably used as a part of the fortification system and a possible wood bridge existed here in the front of the proposed Western Gate of the Pohansko agglomeration. Palynological studies reveal some fragmentation of the landscape and agricultural activities in the close surroundings. Deposits of the studied fluvial channel were covered by the beds of the younger flood loams.
Anglicky
Geophysical, sedimentological, palynological, absolute-age dating and archeological techniques were used to study the deposits of the Early Medieval fluvial channel in the area of the Great Moravia Empire agglomeration Pohansko near Břeclav. Artificial profile situated on the base of ERT profiles and the archeological results led to opening of the fluvial channel. Newly documented fluvial channel erosively cut the complex of flood loams. Gravel lag covers the bottom of the channel and grade upwards into sandy channel infill with fining upward trend. Fluvial sandy dunes forming the most characteristic architectural element of the infill are represented mostly by trough cross-stratified medium-grained sands. These sands were penetrated by the piece of oak wood. Both the OSL dating of the sandy deposits and the dating of the oak wood (C14 and dendrochronology) point to the 9th century A.D. when the Great Moravia Empire was on its peak expansion. Active fluvial channel was probably used as a part of the fortification system and a possible wood bridge existed here in the front of the proposed Western Gate of the Pohansko agglomeration. Palynological studies reveal some fragmentation of the landscape and agricultural activities in the close surroundings. Deposits of the studied fluvial channel were covered by the beds of the younger flood loams.
Návaznosti
| GA20-18929S, projekt VaV |
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