G. Vis, Erik van Linden, R. V. van Balen, K. Cohen
{"title":"Depressions caused by localized subsidence in the Netherlands, Belgium and Germany: a link with coal mining?","authors":"G. Vis, Erik van Linden, R. V. van Balen, K. Cohen","doi":"10.5194/piahs-382-201-2020","DOIUrl":null,"url":null,"abstract":"Abstract. In the coal mining districts of the Netherlands, Belgium and\nGermany, we identified 662 previously unidentified depressions at the land\nsurface using LIDAR data. Their density decreases westwards along with\ndeepening of the Carboniferous coal layers, while not changing in\ndimensions. The timing of their formation based on historical maps and\nlandowner reports, suggests that they mostly formed during the period\n1920–1970, the peak of mining activity. Based on their position, density and\nage, we link the formation of depressions to the coal-mining activities in\nSouth Limburg, Germany and Belgium. Our working hypothesis tentatively\nexplains the origin, mechanism of formation and timing of these local\nsubsidence features.\n","PeriodicalId":53381,"journal":{"name":"Proceedings of the International Association of Hydrological Sciences","volume":null,"pages":null},"PeriodicalIF":0.0000,"publicationDate":"2020-04-22","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Proceedings of the International Association of Hydrological Sciences","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.5194/piahs-382-201-2020","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"Earth and Planetary Sciences","Score":null,"Total":0}
引用次数: 1
Abstract
Abstract. In the coal mining districts of the Netherlands, Belgium and
Germany, we identified 662 previously unidentified depressions at the land
surface using LIDAR data. Their density decreases westwards along with
deepening of the Carboniferous coal layers, while not changing in
dimensions. The timing of their formation based on historical maps and
landowner reports, suggests that they mostly formed during the period
1920–1970, the peak of mining activity. Based on their position, density and
age, we link the formation of depressions to the coal-mining activities in
South Limburg, Germany and Belgium. Our working hypothesis tentatively
explains the origin, mechanism of formation and timing of these local
subsidence features.