The sedimentary environment in the Ljubljansko barje basin during the pile-dwelling period

Geological processes on the Ljubljansko barje basin after the Last Glacial Maximum are known merely on a general level. At few points more detailed circumstances are known, but this information is fragmented spatially and temporally. While artefacts from the archaeological sites were studied in deta...

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Main Author: Verbič, Tomaž
Format: Article in Journal/Newspaper
Language:Slovenian
Published: ZRC SAZU, Založba ZRC 2011
Subjects:
Online Access:https://ojs.zrc-sazu.si/av/article/view/7918/7417
https://ojs.zrc-sazu.si/av/article/view/7918
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spelling ftslacadscienart:oai:ojs.zrc-sazu.si:article/7918 2023-05-15T18:12:21+02:00 The sedimentary environment in the Ljubljansko barje basin during the pile-dwelling period Sedimentacijsko okolje na Ljubljanskem barju v času kolišč Verbič, Tomaž 2011-01-01 application/pdf https://ojs.zrc-sazu.si/av/article/view/7918/7417 https://ojs.zrc-sazu.si/av/article/view/7918 slv slv ZRC SAZU, Založba ZRC https://ojs.zrc-sazu.si/av/article/view/7918 https://creativecommons.org/licenses/by-nc-sa/4.0 CC-BY-NC-SA Arheološki vestnik; Vol. 62 (2011): ARHEOLOŠKI VESTNIK Arheološki vestnik; Letn. 62 (2011): ARHEOLOŠKI VESTNIK 0570-8966 1581-1204 Ljubljansko barje geological processes Quaternary and Holocene environments Seekreide gyttja organic sediments pile-dwellings geološki procesi kvartarno in holocensko okolje jezerska kreda organski sedimenti kolišča info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2011 ftslacadscienart 2022-08-11T20:10:23Z Geological processes on the Ljubljansko barje basin after the Last Glacial Maximum are known merely on a general level. At few points more detailed circumstances are known, but this information is fragmented spatially and temporally. While artefacts from the archaeological sites were studied in detail, the sediments were mostly only imperfectly described. Better understanding of the evolution of the environment requires accurate study of these sediments and buried soils, and detection of evident stratigraphical hiatuses. Geološki procesi na Ljubljanskem barju po zadnjem glacialnem višku so le splošno poznani. Izjemoma sicer poznamo detajlne razmere, vendar so te prostorsko in časovno fragmentarne. Artefakti iz arheoloških najdišč so bili v preteklosti deležni natančnega proučevanja, sami sedimenti s kulturno vsebino, njihova talnina in krovnina pa bistveno manj. Pot do boljšega razumevanja okoljskih razmer v času kolišč verjetno vodi prav preko natančnega poznavanja sedimentov in pokopanih tal ter razumevanja evidentiranih stratigrafskih hiatusov. Article in Journal/Newspaper sami ZRC SAZU Publishing (Znanstvenoraziskovalni center - Slovenske akademije znanosti in umetnosti)
institution Open Polar
collection ZRC SAZU Publishing (Znanstvenoraziskovalni center - Slovenske akademije znanosti in umetnosti)
op_collection_id ftslacadscienart
language Slovenian
topic Ljubljansko barje
geological processes
Quaternary and Holocene environments
Seekreide
gyttja
organic sediments
pile-dwellings
geološki procesi
kvartarno in holocensko okolje
jezerska kreda
organski sedimenti
kolišča
spellingShingle Ljubljansko barje
geological processes
Quaternary and Holocene environments
Seekreide
gyttja
organic sediments
pile-dwellings
geološki procesi
kvartarno in holocensko okolje
jezerska kreda
organski sedimenti
kolišča
Verbič, Tomaž
The sedimentary environment in the Ljubljansko barje basin during the pile-dwelling period
topic_facet Ljubljansko barje
geological processes
Quaternary and Holocene environments
Seekreide
gyttja
organic sediments
pile-dwellings
geološki procesi
kvartarno in holocensko okolje
jezerska kreda
organski sedimenti
kolišča
description Geological processes on the Ljubljansko barje basin after the Last Glacial Maximum are known merely on a general level. At few points more detailed circumstances are known, but this information is fragmented spatially and temporally. While artefacts from the archaeological sites were studied in detail, the sediments were mostly only imperfectly described. Better understanding of the evolution of the environment requires accurate study of these sediments and buried soils, and detection of evident stratigraphical hiatuses. Geološki procesi na Ljubljanskem barju po zadnjem glacialnem višku so le splošno poznani. Izjemoma sicer poznamo detajlne razmere, vendar so te prostorsko in časovno fragmentarne. Artefakti iz arheoloških najdišč so bili v preteklosti deležni natančnega proučevanja, sami sedimenti s kulturno vsebino, njihova talnina in krovnina pa bistveno manj. Pot do boljšega razumevanja okoljskih razmer v času kolišč verjetno vodi prav preko natančnega poznavanja sedimentov in pokopanih tal ter razumevanja evidentiranih stratigrafskih hiatusov.
format Article in Journal/Newspaper
author Verbič, Tomaž
author_facet Verbič, Tomaž
author_sort Verbič, Tomaž
title The sedimentary environment in the Ljubljansko barje basin during the pile-dwelling period
title_short The sedimentary environment in the Ljubljansko barje basin during the pile-dwelling period
title_full The sedimentary environment in the Ljubljansko barje basin during the pile-dwelling period
title_fullStr The sedimentary environment in the Ljubljansko barje basin during the pile-dwelling period
title_full_unstemmed The sedimentary environment in the Ljubljansko barje basin during the pile-dwelling period
title_sort sedimentary environment in the ljubljansko barje basin during the pile-dwelling period
publisher ZRC SAZU, Založba ZRC
publishDate 2011
url https://ojs.zrc-sazu.si/av/article/view/7918/7417
https://ojs.zrc-sazu.si/av/article/view/7918
genre sami
genre_facet sami
op_source Arheološki vestnik; Vol. 62 (2011): ARHEOLOŠKI VESTNIK
Arheološki vestnik; Letn. 62 (2011): ARHEOLOŠKI VESTNIK
0570-8966
1581-1204
op_relation https://ojs.zrc-sazu.si/av/article/view/7918
op_rights https://creativecommons.org/licenses/by-nc-sa/4.0
op_rightsnorm CC-BY-NC-SA
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