Presentation is loading. Please wait.

Presentation is loading. Please wait.

PALEOZOIC Ch 10 & 11.

Similar presentations


Presentation on theme: "PALEOZOIC Ch 10 & 11."— Presentation transcript:

1 PALEOZOIC Ch 10 & 11

2 AGENDA Geologic Time (7 Periods) Plate Tectonics – “Driving Force”
Geography/Landforms Mountains, Rock Formations Appalachian Mountains Climate Change Sea Level Changes Ice Ages Animal/Plant Evolution Animal/Plant Extinction

3

4 Geologic Time

5

6 Plate Tectonics

7 Geological Supercontinents
Vaalbara: Oldest, Formed 3.6 bya Ur: Formed 3.0 bya Nena: Formed 1.8 bya Kenorland: Formed 2.7 bya Columbia: Formed 2.1 bya Rodinia: Formed 1.1 bya Pannotia: Formed 0.6 bya, broke up 0.54 bya Pangea: Formed bya

8 Rodinia Breakup Rodinia Breakup (Neoproterozoic) producing 6 large continents: Laurentia (N. America, Greenland, NW Ireland & Scotland) Baltica (Russia & N. Europe) Kazakhstania (Bet. Caspian Sea & China) Siberia (Russia) China (China, Indochina, & Malay) Gondwana (S. America, Africa, India, Australia, & Antarctica) Movements/interactions of these continents responsible for creation of landforms and evolution of lifeforms.

9 NEOPROTEROZOIC Laurentia (N. America, Greenland, NW Ireland & Scotland) Baltica (Russia & N. Europe) Kazakhstania (Bet. Caspian Sea & China) Siberia (Russia) China (China, Indochina, & Malay) Gondwana (S. America, Africa, India, Australia, & Antarctica)

10 CAMBRIAN f10_04_pg271 f10_04_pg271.jpg f10_04_pg271

11 ORDOVICIAN f10_25_pg287 f10_25_pg287.jpg f10_25_pg287

12 SILURIAN f10_28_pg289 f10_28_pg289.jpg f10_28_pg289

13 DEVONIAN f11_04_pg299 f11_04_pg299.jpg f11_04_pg299

14 MISSISSIPPIAN f11_08_pg302 f11_08_pg302.jpg f11_08_pg302

15 Mississippian/Pennsylvanian Periods
f11_38_pg321 f11_38_pg321.jpg f11_38_pg321

16 PENNSYLVANIAN f11_10_pg304 f11_10_pg304.jpg f11_10_pg304

17 PERMIAN f11_17_pg307 f11_17_pg307.jpg f11_17_pg307

18 Consequence of Plate Tectonics

19 Mountain Building Episodes

20 f11_32_pg318 f11_32_pg318.jpg f11_32_pg318

21 Review Craton: The stable interior of a continent.
2 components of a Craton: Shield: Large area of exposed crystalline rocks. Platforms: Areas surrounding the shields containing flat-lying sedimentary layers.

22 Four Orogenic Belts West – Cordilleran North – Franklinian
Northeast – Caledonian/Acadian East - Appalachian

23 f10_07_pg273 f10_07_pg273.jpg f10_07_pg273

24 Mountain Building (Orogenic) Episodes
Break-up of Rodinia (Proterozoic) 7 Continents Iapetus Ocean Formation (Cambrian) Taconic Orogeny (Ordovician) Iapetus Ocean Narrowing, 1st Appalachian Episode Cordilleran Orogeny (Ordovician – Silurian) Rocky Mtns Caledonian Orogeny (Mid Sil. Mid Dev.) Laurasia Formed (N. America/Europe) Acadian (Mid Sil. Mid Dev.) Closing of Iapetus Ocean, 2nd Appalachian Episode Alleghenian Orogeny (MS – Perm) Final Appalachian Episode Ouachita Orogeny (Early Dev – Late MS)

25 Appalachian Mountains

26 f11_19_pg310 f11_19_pg310.jpg f11_19_pg310

27 U.S. PHYSIOGRAPHIC REGIONS

28 United States Physiographic Regions
Physiographic regions are based on landscape features, which are mostly controlled by the geology of the regions.

29 Alabama Physiographic Regions

30 Sea Level Changes Epicontinental Seas “Transgressive/Regressive Sequences”

31 f11_19_pg310 f11_19_pg310.jpg f11_19_pg310

32 Transgressive/Regressive Sequences
Sauk (Cambrian – Ordovician) Tippecanoe (Ordovician – Silurian) Kaskaskia (Silurian – Mississippian) Absaroka (Pennsylvanian – Triassic)

33 Causes of Sea Level Changes

34

35

36 Evidence of Sea Level Changes

37

38 Paleozoic Summary

39 t10_01_pg274 t10_01_pg274.jpg t10_01_pg274

40 THE END


Download ppt "PALEOZOIC Ch 10 & 11."

Similar presentations


Ads by Google