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British Isles
Lower Palaeozoic
 i) Lower Palaeozoic -
 Britain was south of the
  equator: evidence for
  plate collision
 from Caledonian orogenic
  belt.
 turbidites
 granites, regional
  metamorphism, thrusts,
  folds
Lower Palaeozoic
 i) Lower Palaeozoic -
 Britain was south of the
  equator: evidence for
  plate collision
 from Caledonian orogenic
  belt.
 turbidites
 granites, regional
  metamorphism, thrusts,
  folds
Lower Palaeozoic             Ordovician


 i) Lower Palaeozoic -
 Britain was south of the
  equator: evidence for
  plate collision
 from Caledonian orogenic
  belt.
 turbidites
 granites, regional
  metamorphism, thrusts, f
  olds
Lower Palaeozoic             Silurian
 i) Lower Palaeozoic -
 Britain was south of the
  equator: evidence for
  plate collision
 from Caledonian orogenic
  belt.
 turbidites
 granites, regional
  metamorphism, thrusts,
  folds
Upper Palaeozoic
 (ii) Upper Palaeozoic -
    Britain drifts across the
    equator.
    tropical seas [limestone]
    swamp forest [deltas, coal
    formation]
    desert conditions 15oN
    [wind-formed dune-bedded
    sandstone, evaporites,
   breccia]

                                  Devonian
Upper Palaeozoic
 (ii) Upper Palaeozoic -
    Britain drifts across the
    equator.
    tropical seas [limestone]
    swamp forest [deltas, coal
    formation]
    desert conditions 15oN
    [wind-formed dune-bedded
    sandstone, evaporites,
   breccia]

                                  Carboniferous
Upper Palaeozoic
 (ii) Upper Palaeozoic -
    Britain drifts across the
    equator.
    tropical seas [limestone]
    swamp forest [deltas, coal
    formation]
    desert conditions 15oN
    [wind-formed dune-bedded
    sandstone, evaporites,
   breccia]



              Carboniferous
Upper Palaeozoic
 (ii) Upper Palaeozoic -
    Britain drifts across the
    equator.
    tropical seas [limestone]
    swamp forest [deltas, coal
    formation]
    desert conditions 15oN
    [wind-formed dune-bedded
    sandstone, evaporites,
   breccia]

                                  Permian
Mesozoic
 Britain at 30o - 40oN;
  separation of Africa
  from America
 extensive warm seas
  [limestone]




        Jurassic
Mesozoic
 Britain at 30o - 40oN;
  separation of Africa
  from America
 extensive warm seas
  [limestone]




        Cretaceous
Cenozoic
 opening of north
  Atlantic; Britain at 50o
  - 60oN; diverging plate
 volcanism in NW
  Britain; glaciation
 volcanism (flood
  basalts)
 glaciation (glacial till)




                        Tertiary
Cenozoic
 opening of north
  Atlantic; Britain at 50o
  - 60oN; diverging plate
 volcanism in NW
  Britain; glaciation
 volcanism (flood
  basalts)
 glaciation (glacial till)




                        Quaternary

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Palaeo geography

  • 2. Lower Palaeozoic  i) Lower Palaeozoic -  Britain was south of the equator: evidence for plate collision  from Caledonian orogenic belt.  turbidites  granites, regional metamorphism, thrusts, folds
  • 3. Lower Palaeozoic  i) Lower Palaeozoic -  Britain was south of the equator: evidence for plate collision  from Caledonian orogenic belt.  turbidites  granites, regional metamorphism, thrusts, folds
  • 4. Lower Palaeozoic Ordovician  i) Lower Palaeozoic -  Britain was south of the equator: evidence for plate collision  from Caledonian orogenic belt.  turbidites  granites, regional metamorphism, thrusts, f olds
  • 5. Lower Palaeozoic Silurian  i) Lower Palaeozoic -  Britain was south of the equator: evidence for plate collision  from Caledonian orogenic belt.  turbidites  granites, regional metamorphism, thrusts, folds
  • 6. Upper Palaeozoic  (ii) Upper Palaeozoic - Britain drifts across the equator.  tropical seas [limestone]  swamp forest [deltas, coal formation]  desert conditions 15oN [wind-formed dune-bedded sandstone, evaporites,  breccia] Devonian
  • 7. Upper Palaeozoic  (ii) Upper Palaeozoic - Britain drifts across the equator.  tropical seas [limestone]  swamp forest [deltas, coal formation]  desert conditions 15oN [wind-formed dune-bedded sandstone, evaporites,  breccia] Carboniferous
  • 8. Upper Palaeozoic  (ii) Upper Palaeozoic - Britain drifts across the equator.  tropical seas [limestone]  swamp forest [deltas, coal formation]  desert conditions 15oN [wind-formed dune-bedded sandstone, evaporites,  breccia] Carboniferous
  • 9. Upper Palaeozoic  (ii) Upper Palaeozoic - Britain drifts across the equator.  tropical seas [limestone]  swamp forest [deltas, coal formation]  desert conditions 15oN [wind-formed dune-bedded sandstone, evaporites,  breccia] Permian
  • 10. Mesozoic  Britain at 30o - 40oN; separation of Africa from America  extensive warm seas [limestone] Jurassic
  • 11. Mesozoic  Britain at 30o - 40oN; separation of Africa from America  extensive warm seas [limestone] Cretaceous
  • 12. Cenozoic  opening of north Atlantic; Britain at 50o - 60oN; diverging plate  volcanism in NW Britain; glaciation  volcanism (flood basalts)  glaciation (glacial till) Tertiary
  • 13. Cenozoic  opening of north Atlantic; Britain at 50o - 60oN; diverging plate  volcanism in NW Britain; glaciation  volcanism (flood basalts)  glaciation (glacial till) Quaternary