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MAIN IDEA: LANDFORMS CAUSED BY THE CHEMICAL WEATHERING OF LIMESTONE ARE CALLED KARST TOPOGRAPHY. Chp 10.2 Notes Groundwater Erosion & Deposition
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Chp 10.2 Notes Groundwater Erosion & Deposition

Feb 22, 2016

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Chp 10.2 Notes Groundwater Erosion & Deposition. Main Idea: Landforms caused by the chemical weathering of limestone are called karst topography . Two Requirements for Karst Topography!. ACIDIC WATER IS FORMED BY a CARBONATION PROCESS: Describe: - PowerPoint PPT Presentation
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Page 1: Chp  10.2 Notes Groundwater  Erosion & Deposition

MAIN IDEA: LANDFORMS CAUSED BY THE CHEMICAL

WEATHERING OF LIMESTONE ARE CALLED

KARST TOPOGRAPHY.

Chp 10.2 NotesGroundwater

Erosion & Deposition

Page 2: Chp  10.2 Notes Groundwater  Erosion & Deposition

Two Requirements for Karst Topography!

ACIDIC WATER IS FORMED BY a CARBONATION PROCESS:

Describe: Water drips down through soil and reacts with carbon dioxide. This creates carbonic acid, a relatively weak acid.

ACIDIC RAIN WATER

Limestone (Rock) +

Page 3: Chp  10.2 Notes Groundwater  Erosion & Deposition

When the two meet

Action:Carbonic acid dissolves limestone slowly, over a long period of time.

Page 4: Chp  10.2 Notes Groundwater  Erosion & Deposition

The Structures formed

LIMESTONE PAVEMENTDescribe:An area of limestone that has been chiseled away and is exposed at earth surface

Page 5: Chp  10.2 Notes Groundwater  Erosion & Deposition

Shallow hole

Describe:A hole that forms and “swallows” a stream as underground limestone is dissolved

Page 6: Chp  10.2 Notes Groundwater  Erosion & Deposition

Sinkhole (hint: Avoid Limestone regions!!)

Describe:Rainfall in the soil absorbs carbon dioxide & reacts with decaying vegetation, creating acidic water. Acidic water moves through spaces underground, SLOWLY dissolving limestone, creating cavities. Cavities gradually get enlarged & carry even more acidic water. Sinkholes formed when the land surface above finally collapses by gravity & then sinks into the cavities.

Page 7: Chp  10.2 Notes Groundwater  Erosion & Deposition

Caves/caverns

Page 8: Chp  10.2 Notes Groundwater  Erosion & Deposition

Stalactites (“don’t fall, hang on tite!”)

Describe: Hollow, elongated forms of various

minerals deposited from solution by slowly dripping water. They hang from a cave ceiling.

Page 9: Chp  10.2 Notes Groundwater  Erosion & Deposition

Stalagmites

Describe: Cones or massive mounds of calcite deposits that grow up from a cave floor due

to dripping water.

Page 10: Chp  10.2 Notes Groundwater  Erosion & Deposition

Speleothems

Describe: Known as “decorative cave formations”. Threads of deposited minerals that hang from a cave ceiling and sprout from a cave floor as a result of dripping water.