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.
| Original language | English |
|---|---|
| Pages (from-to) | 201-205 |
| Number of pages | 5 |
| Journal | Proceedings of the International Association of Hydrological Sciences |
| Volume | 382 |
| DOIs | |
| Publication status | Published - 22 Apr 2020 |
| Event | 10th International Symposium on Land Subsidence, TISOLS 2020 - Delft, Netherlands Duration: 17 May 2021 → 21 May 2021 |
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