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First, we discuss the general properties of deformation related to different collapse scenarios in the Grenzland. In each of the scenarios, deformation within the entire subsurface is clearly visible over the top of the cavities. Whereas cavities and steep slopes cause the strongest deformation, the shallowest areas have lower maximum values, delineating roughly the transition from swell to subsidence ground. In scenario S1, maximum subsidence is about 5 cm. The peak values are located at the top sides of both cavities. Sinkholes appear as peaks (or maxima) of the deformation field and are composed of several cavities. Whereas the slopes in between the cavities are maxima of subsidence, cavities are peaks of peak subsidence. The maximum subsidence, related to the first cavity it is intersecting, is more pronounced than the maximum subsidence related to the second cavity. In scenario S2 of the complete collapse of both cavities, maximum subsidence values of up to approximately 225 cm are observed. Deformations occur in all directions; however, while the maximal subsidence may be located close to one of the main cavities or at the crater tops and slopes, the maximum subsidence is located close to the two main cavities. Here, subsidence values greater than 75 cm are concentrated in areas close to the main cavities and reach values up to approximately 115 cm at the elevations of the two main cavities. In scenario S3, the deformation is similar to S2, including peaks of highest values in the cavities and slopes. However, in the interior areas of the main cavities, the deformation is reduced. Thus, this scenario is similar to scenario S2, with minor changes at the craters and with the location of the maximum subsidence close to the main cavities.
In scenarios S4 and S5, subsidence is opposite to the directions of the deformation in the other scenarios. In the scenario of a complete collapses of both craters, the greatest maximum subsidence values of up to approximately 100 cm occurred in areas related to the main cavities. In addition, subsidence values of up to approximately 55 cm are located at the top sides of the craters and slopes and on the causative craters. d2c66b5586
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