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Virginia Geology 2011

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Virginia Geology. 2011. Basic Landforms. Mountains : Natural elevation of the land. Hill : Small natural elevation of the land. Plains : A large area of flat land free from forests and mountains. Plateaus : Large, flat area of land that is higher than the surrounding land. - PowerPoint PPT Presentation

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Page 1: Virginia Geology

Virginia Geology

2011

Page 2: Virginia Geology

Basic Landforms• Mountains: Natural elevation of the land.• Hill: Small natural elevation of the land.• Plains: A large area of flat land free from

forests and mountains.• Plateaus: Large, flat area of land that is

higher than the surrounding land.• Watershed: Ridge or crest dividing two

drainage areas.• River Basin: A round, low area of land

surrounded by higher land.

Page 3: Virginia Geology
Page 4: Virginia Geology

There are 5 provinces in Virginia.

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Page 5: Virginia Geology

Each province has unique features.

Coastal Plain – Land is relatively flat and gently slopes to the

ocean– Ground is made mostly of sedimentary rocks.

There is also lots of sand, clay and gravel (sediments). This comes from the erosion of the Appalachian Mountains.

– Mining of the sand, clay and gravel is an important resource.

– Youngest land of all the provinces– Large tidal rivers: James, Potomac,

Rappahannock and James

Page 6: Virginia Geology

Piedmont– The largest of all the provinces.– Ground is made mostly of Metamorphic rocks.

These rocks formed as the Appalachian Mountains were created by the rifting (splitting apart) of Pangaea.

– Contains the Fall Line on the Eastern border. The fall line is rapid drop in elevation. There are many rapids and waterfalls along the fall line.

– Major rivers: Anna, James, Rappahannock and Roanoke.

Page 7: Virginia Geology

Blue Ridge– The Blue Ridge Mountains contain some rocks

that are over 1 billion years old.– Ground is made mostly of Igneous rocks.– The Blue Ridge Mountains formed as Pangaea

(where North America and Africa are today) smashed together (lots of volcanic activity). This action caused the rocks to be pushed up and on top of the Valley and Ridge Province.

– Major Rivers: Roanoke, James, Anna and Rappahannock.

Page 8: Virginia Geology

Valley and Ridge– Made of long parallel ridges and valleys that

were created by the folding and faulting of rock (during Appalachian Mountains formation).

– Ground is made mainly of sedimentary rock, some of which have carbonates (limestone's) on top.

– Many caves and sinkholes are found in the limestone regions of the Valley and Ridge province. Natural bridge and Luray Caverns are examples.

– Major Rivers: Jackson (turns into James) and New River.

Page 9: Virginia Geology

Appalachian Plateau– The smallest province located to the far west of

the state.– Valleys and Ridges become smaller so the land

is still rugged and hilly. There are many streams and valleys.

– The ground is made up of sedimentary rocks (much like the valley and ridge province).

– Many mineral deposits of coal, petroleum and natural gas are mined from this province.

– Major Rivers: None

Page 10: Virginia Geology
Page 11: Virginia Geology

Chesapeake Bay Formation

Virginia has 5 physiographic provinces produced by past tectonic and geologic activity. Each province has unique physical characteristics resulting from its geologic past. Virginia has a billion year long tectonic and geologic history. Provinces extend from Georgia to New York. Chesapeake Bay formed from the flooding of the Susquehanna river and was impacted by a meteorite.

Page 12: Virginia Geology

Watersheds– A watershed is an area that is separated by a ridge

or crest (divide) allowing the water to drain.

– Land can be divided into major and minor watersheds (there can be a watershed in another watershed).

Page 13: Virginia Geology

– The US is divided into 3 major watersheds: The Atlantic, Mississippi and Pacific.

Page 14: Virginia Geology

VA Watersheds

Page 15: Virginia Geology

Local Watersheds