Medieval accumulation in the Upper Dnister river valley and its connection with colonization of the Eastern Carpathians Foreland (Western Ukraine)
Study of the Holocene terraces and alluvia filling the Dnister river valley and its tributary Strwiąż river, between the Carpathians’ margin and graben of the Upper Dnister Basin and covered by the extensive peat-bogs, has been performed for slightly more than last ten years. Within the Dnister vall...
Main Authors: | , , , |
---|---|
Format: | Article |
Language: | English |
Published: |
„Ștefan cel Mare” University Press
2011-06-01
|
Series: | GEOREVIEW: Scientific Annals of Stefan cel Mare University of Suceava. Geography Series |
Subjects: | |
Online Access: | http://georeview.ro/ojs/index.php/revista/article/view/260 |
id |
doaj-d94c3ed9b52048e0b337cc17d1215b83 |
---|---|
record_format |
Article |
spelling |
doaj-d94c3ed9b52048e0b337cc17d1215b832021-06-02T12:56:43Zeng„Ștefan cel Mare” University PressGEOREVIEW: Scientific Annals of Stefan cel Mare University of Suceava. Geography Series1583-14692011-06-01202303Medieval accumulation in the Upper Dnister river valley and its connection with colonization of the Eastern Carpathians Foreland (Western Ukraine)Piotr GEBICAAndrij JACYSYNLeszek STARKELMarek KRAPIECStudy of the Holocene terraces and alluvia filling the Dnister river valley and its tributary Strwiąż river, between the Carpathians’ margin and graben of the Upper Dnister Basin and covered by the extensive peat-bogs, has been performed for slightly more than last ten years. Within the Dnister valley, below the gravel terrace-fan 10-11 m high, the terrace 5-7 m high occurs. They are formed of channel sediments of various age (from the Late Glacial to the Neo-Holocene) and overbank sediments which top parts, often separated by peat layers are dated at the last millenium. In the outlet of the Upper Dnister Basin these sediments are usually youngerhttp://georeview.ro/ojs/index.php/revista/article/view/260geoarcheology |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Piotr GEBICA Andrij JACYSYN Leszek STARKEL Marek KRAPIEC |
spellingShingle |
Piotr GEBICA Andrij JACYSYN Leszek STARKEL Marek KRAPIEC Medieval accumulation in the Upper Dnister river valley and its connection with colonization of the Eastern Carpathians Foreland (Western Ukraine) GEOREVIEW: Scientific Annals of Stefan cel Mare University of Suceava. Geography Series geoarcheology |
author_facet |
Piotr GEBICA Andrij JACYSYN Leszek STARKEL Marek KRAPIEC |
author_sort |
Piotr GEBICA |
title |
Medieval accumulation in the Upper Dnister river valley and its connection with colonization of the Eastern Carpathians Foreland (Western Ukraine) |
title_short |
Medieval accumulation in the Upper Dnister river valley and its connection with colonization of the Eastern Carpathians Foreland (Western Ukraine) |
title_full |
Medieval accumulation in the Upper Dnister river valley and its connection with colonization of the Eastern Carpathians Foreland (Western Ukraine) |
title_fullStr |
Medieval accumulation in the Upper Dnister river valley and its connection with colonization of the Eastern Carpathians Foreland (Western Ukraine) |
title_full_unstemmed |
Medieval accumulation in the Upper Dnister river valley and its connection with colonization of the Eastern Carpathians Foreland (Western Ukraine) |
title_sort |
medieval accumulation in the upper dnister river valley and its connection with colonization of the eastern carpathians foreland (western ukraine) |
publisher |
„Ștefan cel Mare” University Press |
series |
GEOREVIEW: Scientific Annals of Stefan cel Mare University of Suceava. Geography Series |
issn |
1583-1469 |
publishDate |
2011-06-01 |
description |
Study of the Holocene terraces and alluvia filling the Dnister river valley and its tributary Strwiąż river, between the Carpathians’ margin and graben of the Upper Dnister Basin and covered by the extensive peat-bogs, has been performed for slightly more than last ten years. Within the Dnister valley, below the gravel terrace-fan 10-11 m high, the terrace 5-7 m high occurs. They are formed of channel sediments of various age (from the Late Glacial to the Neo-Holocene) and overbank sediments which top parts, often separated by peat layers are dated at the last millenium. In the outlet of the Upper Dnister Basin these sediments are usually younger |
topic |
geoarcheology |
url |
http://georeview.ro/ojs/index.php/revista/article/view/260 |
work_keys_str_mv |
AT piotrgebica medievalaccumulationintheupperdnisterrivervalleyanditsconnectionwithcolonizationoftheeasterncarpathiansforelandwesternukraine AT andrijjacysyn medievalaccumulationintheupperdnisterrivervalleyanditsconnectionwithcolonizationoftheeasterncarpathiansforelandwesternukraine AT leszekstarkel medievalaccumulationintheupperdnisterrivervalleyanditsconnectionwithcolonizationoftheeasterncarpathiansforelandwesternukraine AT marekkrapiec medievalaccumulationintheupperdnisterrivervalleyanditsconnectionwithcolonizationoftheeasterncarpathiansforelandwesternukraine |
_version_ |
1721404235192467456 |