Presentation is loading. Please wait.

Presentation is loading. Please wait.

ALABAMA GEOLOGY.

Similar presentations


Presentation on theme: "ALABAMA GEOLOGY."— Presentation transcript:

1 ALABAMA GEOLOGY

2 North American can be divided into 8 distinct physiographic regions based on landscape features, which are mostly controlled by the geology of the regions.

3 Physiographic Hierarchy
Physiographic Regions are the largest landscape divisions recognized on a continent.  They are based on rock type and age, geologic structure and history and generally parallel major geologic units.   They can be thought of as the landscape divisions that can be seen from space: plains, mountain ranges, etc.  Physiographic Provinces are components of Physiographic Regions and represent an area within a region whose pattern of relief features or landforms differs significantly from that of adjacent provinces. Physiographic Sections are components of Physiographic Provinces based on geographic distribution.   physiographic districts are components of Physiographic Sections based on local landforms

4 Physiographic Sections in Alabama
There are five sections in Alabama: three belongs to the Appalachian Highlands region; one to the Inland Plains and one to the Coastal Plain regions.  Region: Atlantic Plain Province: Coastal Plain  Section: East Gulf Coastal Plain Region: Appalachian Highlands Province: Piedmont  Section: Piedmont Upland Province: Valley and Ridge Section: Tennessee Province: Appalachian Plateaus  Section: Cumberland Plateau Region: Interior Plains Province: Interior Low Plateaus Section: Highland Rim

5 Physiographic sections of Alabama.

6 Piedmont Districts Northern Piedmont Upland Southern Piedmont Upland

7 Piedmont Upland Section Deep soil horizon and saprolite,

8 Valley and Ridge “Tennessee Section”
Image of the Valley and Ridge showing zigzag ridges in bottom right.  Birmingham is top left.

9 Cumberland Plateau

10 Highland Rim Section

11 East Gulf Coastal Plain

12 ALABAMA’S GEOLOGIC HISTORY

13

14

15 Cambrian (505-542 mya) Early Cambrian Late Cambrian
No sedimentary rocks: Suggests land above Sea Level Late Cambrian Progressive rise in sea level Alabama lay beneath warm shallow ocean Rock Formations: Dolomite Chilhowee, Shady, Knox Group, Copper Ridge

16 Ordovician (438-505 mya) Taconomic Orogeny
Alabama lay to the south or orogenic activity Volcanic Eruptions Covered millions of square miles, 1 to 2 meters thick Alabama covered in shallow marine. Rocks limestone: Chickamauga, Knox Group Bentonite clay: from volcanic eruption

17

18 Silurian (396-438 mya) Red Mountain Formation – Most Important
Iron Ore Shale, Siltstone, Sandstone, Limestone, Hematite Shallow seas still covered area

19 Devonian (350-396 mya) Marine Deposits Frog mountain sandstone
Chattanooga Shale

20 Mississippian (320-350 mya) Marine Deposits
Rocks responsible for cave formation Rocks Fort Payne Chert Tuscumbia Limestone Pride Mountain Formation Hartselle Sandstone Bangor Limestone

21

22 Pennsylvanian (286-320 mya) Coal Age Tropical Forests
Assemblage of Pangea Birth of Southern Appalachians “Alleghany Orogeny” Rocks Pennington, Parkwood, Pottsville Formations

23 Coal Cyclothem

24

25 Unconformity (286 – 144 mya missing)
Missing Formations Permian, Triassic, Jurasic Possible Cause Alabama experiencing period of uplift, which lacked sedimentary deposits.

26 Cretacious (65-144 mya) Pangea Break-up Gulf of Mexico Forming
Warm Global Climate Known for Chalk Deposits – Selma Chalk Emile Landfill 3 sets of rocks Tuscaloosa Group: Freshwater Deposits Eutaw Formation: Marine sands and muds Selma Chalk: Chalk & Marls Cocoliths & Foraminifera Wetumpka Impact

27 Emile Alabama

28 Emile Alabama

29

30 Paleogene/Neogene (65-Present)
Alabama Coastal Plains

31 ALABAMA’S POINTS OF INTEREST

32 Alabama State Parks

33

34

35

36

37

38

39

40

41

42

43

44 Wetumpka Impact Crater

45 Wetumpka Impact Crater

46 Wetumpka Impact Crater

47 Wetumpka Impact Crater
Location: East of Wetumpka When: Cretaceous, 83 MYA Size: Five mile wide crater created by object 1000 feet in diameter. Evidence: 1) Sharply bent rocks pointing toward the center of the impact and 2) Shocked quartz History 1891: State Geologist Eugene Allen Smith described area as structurally disturbed. 1972: Geological Survey of Alabama Geologist Tony Neathery noted a catastrophe had occurred, but source unknown. 1998: 2 well drilled by a research team from Auburn and Found shocked quartz. ·       

48 ALABAMA CAVES

49 Alabama Caves Desoto Caverns Manitou Cave Rickwood Caverns
Russell Cave Sequoyah Caverns Cathedral Caverns

50 AL/MS BARRIER ISLANDS

51 AL/MS Barrier Islands

52

53 Dauphin Island

54 Dauphin Island

55 Land-Loss Trends

56 Mobile Bay

57 Evolution of Mobile Bay

58 THE END


Download ppt "ALABAMA GEOLOGY."

Similar presentations


Ads by Google