The evaporitic layers in the molasse deposits of the NE Carpathian forelands have been mined for potassium salt mainly in the 1970s and 1980s. Collapse of mining-induced cavities is the most likely cause for the rapid formation of this sinkhole in 2017, 300 m in diameter and 50 m deep. The ground in this area is unstable, with a dynamic system of evolving cracks and frequent small landslides.
- Location
- View on OpenStreetMap
- Created
- on Wednesday 19 June 2019 by Martin Mergili
- Keywords
- cultural landscape, hazard impact, lake, landslide, mining, mirror of the past, subsidence, Zonobiome VI
- Visits and license
- 5152 visits, CC BY-NC-SA 4.0 DEED license