File:Patterns Figure4.jpg

figure 4 - part of Patterns in seismology and palaeoseismology, and their application in long-term hazard assessments - the Swedish case in view of nuclear waste management.

Figure 4. Cumulative distribution over time of the 59 events in the Swedish Paleoseismic-logical Catalogue (Appendix A; Mörner, 2003, 2011). There is a distinct peak in the period 11 000–9000 BP, which is the time of the peak rate of glacial isostatic uplift (left curve).

Original source: Scientific paper provided by N.-A. Mörner. Published originally on July 24, 2013 in Pattern Recognition in Physics (PRP)