File:Patterns Figure4.jpg

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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)

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current15:29, 29 November 2013Thumbnail for version as of 15:29, 29 November 20131,033x641 (62 KB)Falk (Talk | contribs)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...

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