worksheet 6 Flashcards
what happened during the caledonian orogeny
the iapetus ocean closed
what happened during the variscan orogeny
the rheic ocean closed
what were the principle continents before pangea formed
gondwana, siberia, baltica, laurentia
- avalonia was a microcontinent
what were the principle oceans before pangea formed
panthalassic ocean, rheic ocean, iapetus ocean
what was in gondwana
present-day south america, africa, antarctica, new zealand, southeastern USA, arabia, southern europe, india
what was in siberia
siberia and kazakhstan
what was in baltica
scandinavia, eastern russia, north europe
what was in laurentia
most of present day north america
where was ireland and uk before pangea
southern ireland, england and wales are in avalonia
northern ireland and scotland were part of laurentia
what happens during the late cambrian to early silurian period
the iapetus closes (between avalonia and laurentia) and rheic opens
when did avalonia form and how
in the cambrian by rifting away from gondwana
what is rifting
when crust pulls apart and thins which decompresses the mantle so magma rises
how do avalonia and laurentia move during the late cambrian/early silurian
avalonia drifts up from 80S to 35 while laurentia moves east and north. avalonia is moving at a faster rate and catching up with laurentia
what happened to the island arc in the iapetus during middle ordovician
it collided with laurentia and oceanic material was over thrusted onto the continental crust. this is part of the grampian phase
what happens in the late silurian period
the iapetus ocean closes due to subduction and collision between avalonia, laurentia and baltica