Development Environments and Factors of Subsidence Dolines
This study describes the development environments of subsidence dolines based on literary data (development environments create favorable conditions for the local denudation of superficial deposit and thus, for the development of depressions). Development environments are the inclination of the bear...
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2021
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Online Access: | https://doi.org/10.3390/geosciences11120513 https://doaj.org/article/fd3c836fd9ce4212b6fd8a123282df6b |
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ftdoajarticles:oai:doaj.org/article:fd3c836fd9ce4212b6fd8a123282df6b 2023-05-15T17:57:50+02:00 Development Environments and Factors of Subsidence Dolines Márton Veress 2021-12-01T00:00:00Z https://doi.org/10.3390/geosciences11120513 https://doaj.org/article/fd3c836fd9ce4212b6fd8a123282df6b EN eng MDPI AG https://www.mdpi.com/2076-3263/11/12/513 https://doaj.org/toc/2076-3263 doi:10.3390/geosciences11120513 2076-3263 https://doaj.org/article/fd3c836fd9ce4212b6fd8a123282df6b Geosciences, Vol 11, Iss 513, p 513 (2021) subsidence doline karst development environment interval geohazard Geology QE1-996.5 article 2021 ftdoajarticles https://doi.org/10.3390/geosciences11120513 2022-12-31T15:17:49Z This study describes the development environments of subsidence dolines based on literary data (development environments create favorable conditions for the local denudation of superficial deposit and thus, for the development of depressions). Development environments are the inclination of the bearing surface, the secondary porosity of the bedrock, the characteristics of the cover, water influx into the cover, karstwater and groundwater, melting permafrost, and anthropogenic activity. These may become optimal when controlled by various geological, geomorphological, and climatic factors. Development environments may be qualitative (there is doline development in case of its presence) and quantitative (doline development occurs in case of suitable quantitative values). The development environment groups of subsidence dolines are environment groups independent of water level, environment groups dependent on water level, and anthropogenic environment groups. In the case of an environment group independent of water level, surface morphology, cover characteristics, geomorphic evolution, and water supply are determining, while in case of an environment group dependent of water level, subsurface water level and its fluctuations and the characteristics of rainfalls interrupting dry seasons are crucial. Anthropogenic impacts mainly affect doline development through water balance. Article in Journal/Newspaper permafrost Directory of Open Access Journals: DOAJ Articles Geosciences 11 12 513 |
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Open Polar |
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Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
subsidence doline karst development environment interval geohazard Geology QE1-996.5 |
spellingShingle |
subsidence doline karst development environment interval geohazard Geology QE1-996.5 Márton Veress Development Environments and Factors of Subsidence Dolines |
topic_facet |
subsidence doline karst development environment interval geohazard Geology QE1-996.5 |
description |
This study describes the development environments of subsidence dolines based on literary data (development environments create favorable conditions for the local denudation of superficial deposit and thus, for the development of depressions). Development environments are the inclination of the bearing surface, the secondary porosity of the bedrock, the characteristics of the cover, water influx into the cover, karstwater and groundwater, melting permafrost, and anthropogenic activity. These may become optimal when controlled by various geological, geomorphological, and climatic factors. Development environments may be qualitative (there is doline development in case of its presence) and quantitative (doline development occurs in case of suitable quantitative values). The development environment groups of subsidence dolines are environment groups independent of water level, environment groups dependent on water level, and anthropogenic environment groups. In the case of an environment group independent of water level, surface morphology, cover characteristics, geomorphic evolution, and water supply are determining, while in case of an environment group dependent of water level, subsurface water level and its fluctuations and the characteristics of rainfalls interrupting dry seasons are crucial. Anthropogenic impacts mainly affect doline development through water balance. |
format |
Article in Journal/Newspaper |
author |
Márton Veress |
author_facet |
Márton Veress |
author_sort |
Márton Veress |
title |
Development Environments and Factors of Subsidence Dolines |
title_short |
Development Environments and Factors of Subsidence Dolines |
title_full |
Development Environments and Factors of Subsidence Dolines |
title_fullStr |
Development Environments and Factors of Subsidence Dolines |
title_full_unstemmed |
Development Environments and Factors of Subsidence Dolines |
title_sort |
development environments and factors of subsidence dolines |
publisher |
MDPI AG |
publishDate |
2021 |
url |
https://doi.org/10.3390/geosciences11120513 https://doaj.org/article/fd3c836fd9ce4212b6fd8a123282df6b |
genre |
permafrost |
genre_facet |
permafrost |
op_source |
Geosciences, Vol 11, Iss 513, p 513 (2021) |
op_relation |
https://www.mdpi.com/2076-3263/11/12/513 https://doaj.org/toc/2076-3263 doi:10.3390/geosciences11120513 2076-3263 https://doaj.org/article/fd3c836fd9ce4212b6fd8a123282df6b |
op_doi |
https://doi.org/10.3390/geosciences11120513 |
container_title |
Geosciences |
container_volume |
11 |
container_issue |
12 |
container_start_page |
513 |
_version_ |
1766166331618492416 |