worksheet 6 Flashcards

1
Q

what happened during the caledonian orogeny

A

the iapetus ocean closed

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2
Q

what happened during the variscan orogeny

A

the rheic ocean closed

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3
Q

what were the principle continents before pangea formed

A

gondwana, siberia, baltica, laurentia
- avalonia was a microcontinent

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4
Q

what were the principle oceans before pangea formed

A

panthalassic ocean, rheic ocean, iapetus ocean

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5
Q

what was in gondwana

A

present-day south america, africa, antarctica, new zealand, southeastern USA, arabia, southern europe, india

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6
Q

what was in siberia

A

siberia and kazakhstan

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7
Q

what was in baltica

A

scandinavia, eastern russia, north europe

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8
Q

what was in laurentia

A

most of present day north america

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9
Q

where was ireland and uk before pangea

A

southern ireland, england and wales are in avalonia
northern ireland and scotland were part of laurentia

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10
Q

what happens during the late cambrian to early silurian period

A

the iapetus closes (between avalonia and laurentia) and rheic opens

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11
Q

when did avalonia form and how

A

in the cambrian by rifting away from gondwana

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12
Q

what is rifting

A

when crust pulls apart and thins which decompresses the mantle so magma rises

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13
Q

how do avalonia and laurentia move during the late cambrian/early silurian

A

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

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14
Q

what happened to the island arc in the iapetus during middle ordovician

A

it collided with laurentia and oceanic material was over thrusted onto the continental crust. this is part of the grampian phase

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15
Q

what happens in the late silurian period

A

the iapetus ocean closes due to subduction and collision between avalonia, laurentia and baltica

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16
Q

what is the acadian phase

A

the final period of the caledonian orogeny in which the mountain belt is formed between canada –> ireland –> scotland –> greenland –> noway

17
Q

where did subduction occur for the caledonia orogeny

A

oceanic crust subducted towards the north in the oceanic trench on the northern laurentian margin

18
Q

what type of collision was the one between avalonia and laurentia

A

bleak, non head on collision. there was some sliding past one another

19
Q

what is geological evidence of the avalonian and laurentian blocks colliding in ireland

A

distinction sections of precambrian rocks align with laurentian margin in the north and avalonian margin in the south

20
Q

what is an accretionary wedge/prism? where can they be found?

A

deformed sediments created as iapetus seafloor sediments were scraped off the oceanic crust during subduction. the younger sediments are further south of the laurentian margin

21
Q

what accompanied the closure of the iapetus and how old are the rocks

A

granite emplacement which is 360-480 myo (from late devonian to early ordovician)

22
Q

what happened to the mountains that were created by the caledonia orogeny and what did they form

A

they were eroded and weathered down which formed an angular unconformity

23
Q

how did the continents move to close the rheic

A

gondwana drifted northwards to form with the laurentia-avalonia-baltica continent

24
Q

when was the rheic closed

A

by the late devonian (360-380 mya)

25
Q

what was the last step of all of the continents combining? what is the evidence for this?

A

baltica came together with siberia (the ural mountains were formed as baltica collided with kazakhstan during caroniferous)

26
Q

when was pangea formed by

A

335 mya

27
Q

what are the appalachian mountains proof of

A

the rheic ocean closing