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Chapter 4 Georgia’s Features

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Chapter 4. Georgia’s Features. Regions of Georgia. Appalachian Plateau Valley and Ridge region Blue Ridge region Piedmont region Coastal Plain http://georgiamagazine.com/default.asp. Regions of Georgia. - PowerPoint PPT Presentation

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Page 1: Chapter 4

Chapter 4

Georgia’s Features

Page 2: Chapter 4

Regions of Georgia

• Appalachian Plateau• Valley and Ridge region• Blue Ridge region• Piedmont region• Coastal Plain

• http://georgiamagazine.com/default.asp

Page 3: Chapter 4

Regions of Georgia

• The Appalachian plateau region of Georgia is the northwest corner of Georgia. This region contains flat-topped mountains.

• The Cumberland Plateau marks the gradual change from flat lands in the north to the faults and folds of the Valley and Ridge Plateau of Sand and Lookout Mountain.

Page 4: Chapter 4

Differences

Cumberland PlateauLarge, flat-topped

Lookout MountainSteep, rising more to a point

Page 5: Chapter 4

Differences

http://www.nps.gov/cuga/index.htmhttp://www.lookoutmountain.com/

Page 6: Chapter 4

Differences

http://www.nps.gov/blri/index.htmBlue Ridge, Mountains in the clouds

Piedmont areaFlat, low hills

Page 7: Chapter 4

Differences

Coastal Plains

Page 8: Chapter 4

Appalachian Mountains

• Landforms were formed over millions of years.

• During that time multiple tectonic plates collided to build mountains and caused volcanic eruptions.

• At certain times, much of what is now Georgia was covered by shallow seas

Page 9: Chapter 4

Appalachian Mountains

• Sediments were deposited in these waters, which would later form the sedimentary rock found in the Valley and Ridge and Appalachian Plateau regions.

• A total of three collisions involving North America occurred.

• The last formed the Appalachian Mountains, as well as the folds and faults of the Valley and Ridge regions.

Page 10: Chapter 4

Appalachian Mountains

• Separating the Valley and Ridge region from the Piedmont region is the Cartersville Fault.

• This fault, actually runs from Alabama to Pennsylvania.

Page 11: Chapter 4

Blue Ridge and Piedmont region

• This area was affected by the same geologic activities as the Valley and Ridge, but with different results.

• Many of the rocks found in the Blue Ridge are metamorphic, which is rock that changes in form.

• These rocks formed from the heat and pressure caused by plate tectonics.

Page 12: Chapter 4

Blue Ridge and Piedmont region

• The Blue Ridge is also made up of igneous rocks-rocks that were once liquid.

• When Pangaea broke up about 220 million years ago, the Appalachians were torn apart.

• The rolling hills of the Piedmont region are the remains of heavily eroded mountain peaks.

Page 13: Chapter 4

Stone Mountain

• Stone mountain, the world’s largest mass of granite, was uncovered as the softer rock that covered it was eroded.

Page 14: Chapter 4

What is the Coastal Plain

• During the breakup, the Coastal Plains region was formed.

• The coastal plain is generally wet, including many rivers, marsh, and swampland.