Ongerscheide zwesche Versione vun dä Sigg „Äädbevve“

En '''Äädbevve''' hät mer, wann der [[Boddem]] unger unsere [[Fööß]] enne [[Rock (Bewääjung)|Rock]] määt odder et [[Rappelle]] aanfängk. Dobei künne [[Bersch|Bërje]], [[Hüüser]], un [[Bröck (Bouwerrək)|Bröcke]] en et [[Wangke]] kůmme un sůjaa zesamme falle. Et jitt janz höösche Äädbevve, di mer koum merrk, ävver se künne och [[Katastof]]e un schwer [[Onjlöck]]e sin, met http://www.youtube.com/watch?v=vEy90qy8wJs dousende [[Duude (Minsch)|Duude]], [[Obdachloos]]e un schlemme [[Schade|Schäde]].

Where plate boundaries occur within continental lithosphere, deformation is spread out a over a much larger area than the plate boundary itself. In the case of the [[San Andreas fault]] continental transform, many earthquakes occur away from the plate boundary and are related to strains developed within the broader zone of deformation caused by major irregularities in the fault trace (e.g. the “Big bend” region). The [[Northridge earthquake]] was associated with movement on a blind thrust within such a zone. Another example is the strongly oblique convergent plate boundary betweenbetweenhttp://www.youtube.com/watch?v=vEy90qy8wJs the [[Arabian plate|Arabian]] and [[Eurasian plate]]s where it runs through the northwestern part of the [[Zagros]] mountains. The deformation associated with this plate boundary is partitioned into nearly pure thrust sense movements perpendicular to the boundary over a wide zone to the southwest and nearly pure strike-slip motion along the Main Recent Fault close to the actual plate boundary itself. This is demonstrated by earthquake [[focal mechanism]]s. <ref> Talebian, M. Jackson, J. 2004. A reappraisal of earthquake focal mechanisms and active shortening in the Zagros mountains of Iran. Geophysical Journal International, 156, pages 506-526</ref>