Soils, Weathering and Groundwater Landscape Evolution

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Erosion and Landscape Evolution

Anatomy of a

Drainage

System

The

Continental

Divide,

Colorado

The Ideal Stream Cycle (W.M.

Davis, 1880)

Not a Literal Time Sequence

• Youth

• Maturity

• Old Age

• Rejuvenation

The Ideal Stream Cycle

Youthful Landscape, Utah

Young-Mature Landscape, California

Mature Landscape, Pennsylvania

Monadnock, Colorado

Monadnocks, Maine

Old Age Landscape, South America

Rejuvenation

• Some change causes stream to speed up and cut deeper.

– Uplift of Land

– Lowering of Sea Level

– Greater stream flow

• Stream valley takes on youthful characteristics but retains features of older stages as well.

• Can happen at any point in the cycle.

Rejuvenation

Rejuvenation, San Juan River,

Utah

Machu Picchu, Peru

Machu Picchu, Peru

The Onset of Old Age? Indiana

Why the Stream Cycle Doesn't

Explain Everything

• Changes in sea level during the ice ages

• Most landscapes have been repeatedly rejuvenated

• Seems to work best in stable interiors of

Africa, Australia and South America.

Superposed (Antecedent) Drainage

Streams Cut Right Through High Topography

• Crustal Uplift Across River

• Rejuvenation

• Buried Ridge

The

Ultimate

Antecedent

Drainage,

India-Nepal-

Tibet

Rejuvenated Peneplain

Devil’s Gap, Wyoming

The Huang

He: “China’s

Sorrow”

• 1887: 2,000,000 dead

• 1931: 3,700,000 dead

• 1938: The Chinese dynamite levees to slow the Japanese; half a million Chinese died.

River Diversions in the Caspian

Region

Why is the Danube Blue?

Arid and Humid Weathering

Compared

• Rain: Rare, May Be Seasonal, Often

Violent

• Soil: Thin or Absent

• Vegetation: Sparse-no Continuous Cover

• Chemical Weathering: Weak

• Episodic Processes Dominate

Arid Erosion Cycle

• Alluvial Fans

• Playa Lakes

• Pediments

Alluvial Fans, Utah

Old Arid Landscape

Deltas

Deltas, Greece

Yosemite Falls, California

Niagara Falls

Evolution of Niagara Falls

Lakes

Limited Lifetime

Thousands - Millions of

Yr.

How They Form:

• Grabens (Faulting)

– Tahoe 1600'

– Baikal 5600'

– Tanganyika 4000'

Scour

– Great Lakes to 1300'

– Great Slave L. 2000'

– Lake Winnipeg

Damming: Crustal movement, Landslide, etc.

Volcanic Collapse -

Crater Lake

Sinkholes

Kettle Ponds

How Lakes Die

• Eutrophication

• Infilling - Only Way to Destroy Very Deep

Lakes

• Drainage at Outlet

• Climate Change

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