yosemite - university of colorado boulder

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YOSEMITE VALLEY

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Page 1: Yosemite - University of Colorado Boulder

YOSEMITE VALLEY

Page 2: Yosemite - University of Colorado Boulder

GENERALCHARACTERISTICS

• Yosemite means ‘grizzly bear’• 7 miles in length• 1-2 miles in width• Elevation almost exactly 4,000’

Page 3: Yosemite - University of Colorado Boulder

50-10 million yrs ago - a broad valley

Merced river meanders along

Page 4: Yosemite - University of Colorado Boulder

Valley Stage: 50-10 My

• The land destined to become YosemiteNational Park was made up of gentle,rolling hills and streams.

• The Merced River was a slow-moving,sluggish stream.

• Hardwood forests flourish

Page 5: Yosemite - University of Colorado Boulder

The land rises- the valley becomes a canyon10-3 million years ago, tilting of Sierras

Page 6: Yosemite - University of Colorado Boulder

10-3 Ma Canyon Stage

• 10-3 million years ago, the Sierra Nevada,California's "backbone", rose.

• The Sierran block uplifted, tilting westward,increasing the Merced Rivers flow so itcarved the valley into a canyon.

• Redwood forests flourished.• 3 Ma ago the Merced River is a steep, V-

shaped, riverine canyon.

Page 7: Yosemite - University of Colorado Boulder

The Ice Age begins, glaciers carve the valleyEl Portal/Sherwin glacial stage: 1 My

40-60 milesin length

Page 8: Yosemite - University of Colorado Boulder

Major Glaciation

• Probably lasted about 300,000 years• Glaciers filled the V-shaped Yosemite

Valley, widening, deepening and carving itinto a "U" shape, forming hanging valleysfrom which waterfalls now cascade.

• Gouged out basin that lies more than 1,000’below present valley floor

• Half dome a nunatak

Page 9: Yosemite - University of Colorado Boulder

The last glacier surge- 30,000 yrs ago

Page 10: Yosemite - University of Colorado Boulder

Tioga Glacial Stage

• Yosemite Glacier entered the valley but did littleto alter the landscape. Older glaciers had alreadyexcavated 2,000 feet into the bedrock.

• Only advanced as far as Bridalveil Falls.• At this location the forward movement of the

glacier was balanced by the melting of ice at itsfront, producing a large terminal moraine.

Page 11: Yosemite - University of Colorado Boulder

The ice age ends: Lake Yosemite

Page 12: Yosemite - University of Colorado Boulder

14,000-10,000 years ago

• Temperatures warmed and the last valleyglacier melted. Its terminal moraine (rockdebris) dammed the valley 14,000 to 15,000years ago, creating Lake Yosemite.Sediment eventually filled the lake, whichbecame the flat valley floor we see today.

Page 13: Yosemite - University of Colorado Boulder

Following pictures from the USGS site at:http://geology.wr.usgs.gov/docs/usgsnps/yos/topobk.html

Page 14: Yosemite - University of Colorado Boulder

El Capitan on left

Page 15: Yosemite - University of Colorado Boulder

Cathedral Spires

Page 16: Yosemite - University of Colorado Boulder

Bridal Veil Falls, Leaning Tower

Page 17: Yosemite - University of Colorado Boulder

Sentinel Rock

Page 18: Yosemite - University of Colorado Boulder

Yosemite Falls

Page 19: Yosemite - University of Colorado Boulder

Royal Arches, Washington’s column

Page 20: Yosemite - University of Colorado Boulder

Half Dome

Page 21: Yosemite - University of Colorado Boulder

Hetch Hetchy Canyon, next to Yosemite ValleyNow Hetch Hetchy Reservoir, San Fran water supply

Page 22: Yosemite - University of Colorado Boulder

Protestors had put in a simulated "crack" on the face of the dam, and inscribed the text, "Free the Rivers! - J. Muir."

O'Shaugnessy Dam at Hetch Hetchy Reservoir

David Cross, July 1987

Page 23: Yosemite - University of Colorado Boulder

SUMMARY

• Broad-valley stage (50-10 My)• Canyon stage (10-3 My)• Pleistocene glaciation begins (2 My)• Last glacial stage 30,000 years ago

(Wisconsin/Tioga)• Lake Yosemite formed by recessional

moraine about 10,00 years ago• El Capitan and Half Dome nunataks