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Reih 2:
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
Se kumme zoshtand, wann en de [[Ääd (Planeet)|Ääd]] ier [[Äädkruß|Kruß]] [[Spannong (Meschanik)|Spannonge]] optredde, weil de [[Äädplaat]]e sesch bewääje wolle. Dat don se dann öff met enem kleijne odder jrůůße Růck, wann de Spannung rick. Dobei entshtonn sujenannte [[seißmesche Well]]e, di loufe dorsch, un öm de janze Ääd. Do, woh se her kumme, sen se am shtärkßte. Dat kann ööhnßwo [[deef]] unge en de Ääd sin. Mir merke se am shtärkßte jrad jenou do drövver, woh se de op de Ääd ier Bovverkant op der Boddem treffe, wo mir drop shtonn. För dä Plaz säät mer och „et [[Eppizäntrom]]“ fum Äädbevve. Met [[Seismomeeter]]e un [[Seismojraaf]]e donn de Weßßschaffler di Welle [[messe (Donn)|messe]] un [[opzeichne]]. Do han se sesch verschiidene [[Skala|Skale]] un [[Mohß]]e ußjedaach, öm dänne ier [[Shtärk (Äädbevve)|Shtärk]] en [[Zahl]]e ußdrökke ze künne.
Reih 27:
===Earthquakes away from plate boundaries===
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
All tectonic plates have internal stress fields caused by their interactions with neighbouring plates and sedimentary loading or unloading (e.g. deglaciation). These stresses may be sufficient to cause failure along existing fault planes, giving rise to [[intraplate earthquake]]s.<ref>{{Cite book|last=Noson, Qamar, and Thorsen|date=1988|title=Washington State Earthquake Hazards: Washington State Department of Natural Resources|publisher=Washington Division of Geology and Earth Resources Information Circular 85}}</ref>
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