About terraces on the shore of the Teriberskaya Bay of the Barents Sea (the Kola Peninsula)
The paper considers the results of the study of modern terraces on the coast of the Lodeyny Peninsula in the Barents Sea. According to field observations, decoding of space and geodetic maps and volumetric modeling, signs of three terraces have been identified. Two terraces having a rear seam, a cli...
Main Authors: | , , , |
---|---|
Format: | Other Non-Article Part of Journal/Newspaper |
Language: | Russian |
Published: |
2022
|
Subjects: | |
Online Access: | http://hdl.handle.net/1834/41970 |
id |
ftoceandocs:oai:aquadocs.org:1834/41970 |
---|---|
record_format |
openpolar |
spelling |
ftoceandocs:oai:aquadocs.org:1834/41970 2023-05-15T14:59:44+02:00 About terraces on the shore of the Teriberskaya Bay of the Barents Sea (the Kola Peninsula) О террасах на берегу Териберской губы Баренцева моря (Кольский полуостров) Neradovsky, Yu. N. Miroshnikova, Ya. A. Companchenko, A. A. Chernyavsky, A. V. Russia Barents Sea Murmansk region Kola Peninsula Teriberskaya Bay Lodeyny Peninsula Россия Баренцево море Мурманская область Кольский полуостров Териберская губа Полуостров Лодейный 2022 pp.38-49 http://hdl.handle.net/1834/41970 ru rus http://vestnik.mstu.edu.ru/show-eng.shtml?art=2126 http://vestnik.mstu.edu.ru/show.shtml?art=2126 http://hdl.handle.net/1834/41970 Attribution-NonCommercial-NoDerivatives 4.0 International http://creativecommons.org/licenses/by-nc-nd/4.0/ Arctic coast Transformation of the shores Арктическое побережье Tрансформация берегов ASFA_2015::T::Terraces ASFA_2015::A::Arctic zone ASFA_2015::A::Arctic waters ASFA_2015::B::Bays ASFA_2015::B::Beach cusps ASFA_2015::B::Beach features Journal Contribution 2022 ftoceandocs 2023-04-06T17:07:05Z The paper considers the results of the study of modern terraces on the coast of the Lodeyny Peninsula in the Barents Sea. According to field observations, decoding of space and geodetic maps and volumetric modeling, signs of three terraces have been identified. Two terraces having a rear seam, a cliff, a brow and horizontal platforms have been studied in more detail. The rear seams are located at 7 and 30 m, and the edges at 10 and 40 m above the sea level. The third terrace is confined to the level of 40–60 m, and has not been studied in detail. According to estimates, the first two terraces were formed about 3,300 and 6,000 years ago respectively. The 1st terrace characterizes the period of slow land rise by 10 m, at the speed up to 3 mm/year, which began about 3,300 years ago and continues to the present. It is characterized by a uniform sea retreat of about 15 mm/year. The erosion products of this terrace are common in the lateral zone and represent modern marine sediments, including beaches forming a new terrace. The 2nd terrace characterizes to the dynamics of rapid land rise by 30 m at a speed of about 11 mm/year, which occurred in the period from 6,000 to 3,300 years ago. The erosion products of this terrace are most common on the coast and are found at a distance of 100 m to 2–3 km from the shore. It is assumed that the speed of movement of the coastline during the retreat of the sea was different and reached up to 900 mm/year. According to the authors, preliminary data indicate the instability of the territory and the manifestation of block movements, which may have a negative impact on the development of infrastructure. В статье рассмотрены результаты изучения современных террас на побережье Баренцева моря в районе п-ва Лодейный. По данным натурных наблюдений, дешифрирования космических и геодезических карт и объемного моделирования выявлены признаки трех террас. Более детально изучены две террасы, у которых присутствуют тыловой шов, обрыв, бровка и горизонтальные площадки. Тыловые швы располагаются ... Other Non-Article Part of Journal/Newspaper Arctic Barents Sea kola peninsula Teriberskaya IODE-UNESCO: OceanDocs - E-Repository of Ocean Publications Arctic Barents Sea Kola Peninsula Murmansk |
institution |
Open Polar |
collection |
IODE-UNESCO: OceanDocs - E-Repository of Ocean Publications |
op_collection_id |
ftoceandocs |
language |
Russian |
topic |
Arctic coast Transformation of the shores Арктическое побережье Tрансформация берегов ASFA_2015::T::Terraces ASFA_2015::A::Arctic zone ASFA_2015::A::Arctic waters ASFA_2015::B::Bays ASFA_2015::B::Beach cusps ASFA_2015::B::Beach features |
spellingShingle |
Arctic coast Transformation of the shores Арктическое побережье Tрансформация берегов ASFA_2015::T::Terraces ASFA_2015::A::Arctic zone ASFA_2015::A::Arctic waters ASFA_2015::B::Bays ASFA_2015::B::Beach cusps ASFA_2015::B::Beach features Neradovsky, Yu. N. Miroshnikova, Ya. A. Companchenko, A. A. Chernyavsky, A. V. About terraces on the shore of the Teriberskaya Bay of the Barents Sea (the Kola Peninsula) |
topic_facet |
Arctic coast Transformation of the shores Арктическое побережье Tрансформация берегов ASFA_2015::T::Terraces ASFA_2015::A::Arctic zone ASFA_2015::A::Arctic waters ASFA_2015::B::Bays ASFA_2015::B::Beach cusps ASFA_2015::B::Beach features |
description |
The paper considers the results of the study of modern terraces on the coast of the Lodeyny Peninsula in the Barents Sea. According to field observations, decoding of space and geodetic maps and volumetric modeling, signs of three terraces have been identified. Two terraces having a rear seam, a cliff, a brow and horizontal platforms have been studied in more detail. The rear seams are located at 7 and 30 m, and the edges at 10 and 40 m above the sea level. The third terrace is confined to the level of 40–60 m, and has not been studied in detail. According to estimates, the first two terraces were formed about 3,300 and 6,000 years ago respectively. The 1st terrace characterizes the period of slow land rise by 10 m, at the speed up to 3 mm/year, which began about 3,300 years ago and continues to the present. It is characterized by a uniform sea retreat of about 15 mm/year. The erosion products of this terrace are common in the lateral zone and represent modern marine sediments, including beaches forming a new terrace. The 2nd terrace characterizes to the dynamics of rapid land rise by 30 m at a speed of about 11 mm/year, which occurred in the period from 6,000 to 3,300 years ago. The erosion products of this terrace are most common on the coast and are found at a distance of 100 m to 2–3 km from the shore. It is assumed that the speed of movement of the coastline during the retreat of the sea was different and reached up to 900 mm/year. According to the authors, preliminary data indicate the instability of the territory and the manifestation of block movements, which may have a negative impact on the development of infrastructure. В статье рассмотрены результаты изучения современных террас на побережье Баренцева моря в районе п-ва Лодейный. По данным натурных наблюдений, дешифрирования космических и геодезических карт и объемного моделирования выявлены признаки трех террас. Более детально изучены две террасы, у которых присутствуют тыловой шов, обрыв, бровка и горизонтальные площадки. Тыловые швы располагаются ... |
format |
Other Non-Article Part of Journal/Newspaper |
author |
Neradovsky, Yu. N. Miroshnikova, Ya. A. Companchenko, A. A. Chernyavsky, A. V. |
author_facet |
Neradovsky, Yu. N. Miroshnikova, Ya. A. Companchenko, A. A. Chernyavsky, A. V. |
author_sort |
Neradovsky, Yu. N. |
title |
About terraces on the shore of the Teriberskaya Bay of the Barents Sea (the Kola Peninsula) |
title_short |
About terraces on the shore of the Teriberskaya Bay of the Barents Sea (the Kola Peninsula) |
title_full |
About terraces on the shore of the Teriberskaya Bay of the Barents Sea (the Kola Peninsula) |
title_fullStr |
About terraces on the shore of the Teriberskaya Bay of the Barents Sea (the Kola Peninsula) |
title_full_unstemmed |
About terraces on the shore of the Teriberskaya Bay of the Barents Sea (the Kola Peninsula) |
title_sort |
about terraces on the shore of the teriberskaya bay of the barents sea (the kola peninsula) |
publishDate |
2022 |
url |
http://hdl.handle.net/1834/41970 |
op_coverage |
Russia Barents Sea Murmansk region Kola Peninsula Teriberskaya Bay Lodeyny Peninsula Россия Баренцево море Мурманская область Кольский полуостров Териберская губа Полуостров Лодейный |
geographic |
Arctic Barents Sea Kola Peninsula Murmansk |
geographic_facet |
Arctic Barents Sea Kola Peninsula Murmansk |
genre |
Arctic Barents Sea kola peninsula Teriberskaya |
genre_facet |
Arctic Barents Sea kola peninsula Teriberskaya |
op_relation |
http://vestnik.mstu.edu.ru/show-eng.shtml?art=2126 http://vestnik.mstu.edu.ru/show.shtml?art=2126 http://hdl.handle.net/1834/41970 |
op_rights |
Attribution-NonCommercial-NoDerivatives 4.0 International http://creativecommons.org/licenses/by-nc-nd/4.0/ |
_version_ |
1766331858720653312 |