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Introduction to Virginia’s Karst

Date post: 22-Feb-2016
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Introduction to Virginia’s Karst . Caves, Sinkholes, and Carbonates, Oh My!. Karst-Develops in Carbonate Rocks. Carbonic Acid= CO2 + H2O. Caves and Caverns. Formed from the chemical weathering of limestone and dolomite through carbonic acid. Cracks open and eventually widen to make a cave. - PowerPoint PPT Presentation
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INTRODUCTION TO VIRGINIA’S KARST Caves, Sinkholes, and Carbonates, Oh My!
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Page 1: Introduction to Virginia’s Karst

INTRODUCTION TO VIRGINIA’S KARST Caves, Sinkholes, and Carbonates, Oh My!

Page 2: Introduction to Virginia’s Karst

Karst-Develops in Carbonate Rocks

Page 3: Introduction to Virginia’s Karst

Carbonic Acid= CO2 + H2O

Page 4: Introduction to Virginia’s Karst
Page 5: Introduction to Virginia’s Karst
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Caves and Caverns• Formed from the chemical weathering of limestone and

dolomite through carbonic acid. Cracks open and eventually widen to make a cave.

• Dripstone: Calcium carbonate deposited from solution as water enters a cave. Stalactites, Stalagmites, and Columns are all dripstones.

• Stalactites: Hang “tight” to the ceiling.• Stalagmites: Push (mightily) hard through the ground.• Column: Formed when stalactites and stalagmites meet.

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Stalactites and Stalagmites

Page 8: Introduction to Virginia’s Karst

Columns

Page 9: Introduction to Virginia’s Karst

Sinkholes• Caused by the collapse of cave or cavern roof. Usually

from pumping more groundwater than can be recharged.•

Page 10: Introduction to Virginia’s Karst

Sinking Streams• Where a river or stream enters a cave system and

appears to “sink” into the ground.


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