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Kenai Fjords National Park DMoutoux & Earth Science Class of 2015

Kenai Fjords National Park

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Kenai Fjords National Park. DMoutoux & Earth Science Class of 2015. Where is Kenai Fjords National Park?. Why Visit Kenai Fjords National Park?. View arctic marine wildlife Visit fjords and glaciers Sea kayak, hike, backpack Find solitude – most of the park is inaccessible by car. - PowerPoint PPT Presentation

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Page 1: Kenai Fjords National Park

Kenai Fjords National Park

DMoutoux & Earth ScienceClass of 2015

Page 2: Kenai Fjords National Park

Where is Kenai Fjords National Park?

Page 3: Kenai Fjords National Park

Why Visit Kenai Fjords National Park?

• View arctic marine wildlife

• Visit fjords and glaciers

• Sea kayak, hike, backpack

• Find solitude – most of the park is inaccessible by car

Page 4: Kenai Fjords National Park

4 Active Volcanoes on the Kenai Peninsula

Large & frequent earthquakes One of the largest

recorded earthquakes, MR 9.2 struck nearby in 1964

How Plate Tectonics Affect the Park …

Southern coast of Alaska lies along a convergent plate boundaryo Pacific Plate subducting beneath NA Plate

Page 5: Kenai Fjords National Park

Pillow Basalts from VolcanoesPlate Tectonics Affects Rock Type …

Page 6: Kenai Fjords National Park

Batholith Magma that cools Underground Granodiorite (like granite, but darker)

Plate Tectonics Affects Rock Type …

Page 7: Kenai Fjords National Park

Accreted Terranes Foreign land transported by the Pacific Plate and

scraped off on the coast Chert & Basalt from the ocean floor Limestone (old coral reef)

Plate Tectonics Affects Rock Type …

Page 8: Kenai Fjords National Park

Produces Fractures Injected with superheated water carrying

minerals Iron, silica (quartz), arsenic, and gold

Plate Tectonics Affects Rock Type …

Page 9: Kenai Fjords National Park

Half the park covered in ice Glaciers originate in the Harding Ice Field

Kenai Fjord National Park Today …

Page 10: Kenai Fjords National Park

About 30,000 year ago, the entire Kenai Peninsula was covered by an ice sheet, much like Greendland or Antarctica

Kenai Fjord’s Past …

West AntarcticIce Sheet

Page 11: Kenai Fjords National Park

Elevation was higher Tectonic action is causing subsidence

(slow sinking) Diagram shows subsidence following the 1964

earthquake

Kenai Fjord’s Past …

Page 12: Kenai Fjords National Park

Glaciers

Mechanical Weathering & Erosion by …

Waves

Page 13: Kenai Fjords National Park

Abundant snowfall Harding Icefield receives 60 feet of snow per

year. Cool summers

More snow accumulates than melts Air squeezed out as snow accumulates Becomes glacial ice in 4-10 years.

Vertical relief To allow flow downhill Tremendous weight of glacier crushes and

abrades rock Flow transport debris downhill.

How Glaciers Form

Page 14: Kenai Fjords National Park

U-Shaped Valleys

Glacier-carved Features

Page 15: Kenai Fjords National Park

Morraines – Piles of eroded rock left by retreating glaciers

Glacier-carved Features

Page 16: Kenai Fjords National Park

Glacial Marks

Glacier-carved Features

Page 17: Kenai Fjords National Park

Fjords – a long, narrow, deep glacier-carved valley filled by ocean water Found only in Norway, Greenland, New Zealand,

Chile, and Alaska

Glacier-carved Features

Page 18: Kenai Fjords National Park

During an ice age, ocean water levels are much lower, so valleys can be longer

After the ice age, water level rises and fills the long, narrow, and deep u-shaped valley.

How Does a Glacier Carve a Fjord? Glaciers carve deep u-shaped valleys, but stop

at the edge of the ocean

Page 19: Kenai Fjords National Park

Wave-carved Features Pounding surf erodes the coast Softer rock (limestone) far more susceptible

than basalts and granodiorite

Page 20: Kenai Fjords National Park

Near Future - Embattled glaciers 3% decrease in area of Harding Ice Field in the last

16 years Estimated 40 cubic miles of glacial loss in Alaska

annually 1000’s of Years Gradual filling of fjords

Sediments accumulate at rates of up to a foot a year.

Fjords that are 600 to 1000 feet deep could be filled within the next couple thousand years.

Long Term - Continued subsidence The ocean will slowly encroach on the park.

Kenai Fjord’s Future

Page 21: Kenai Fjords National Park

More, Inventory And Monitoring Network Learn about the various projects being studied. Read. National Parks Service. 19 Jan. 2013. National Parks Service. 12 Feb. 2013 <http://www.nps.gov/kefj/naturescience/index.htm>.

"Geomorphology." Geomorphology. 12 Feb. 2013 <http://svp.soic.indiana.edu/svp/4970813/FID1/html/ecosys/physical/geomorph.htm>.

"Moraine on Pederson Glacier, Aialik Bay, Kenai Fjords NP, Alaska." Panoramio. 12 Feb. 2013 <http://www.panoramio.com/photo/1268828>.

"McCarty Fjord and glacier, Kenai Fjords National Park, Alaska - aerial photograph (aat)."Panoramio. 12 Feb. 2013 <http://www.panoramio.com/photo/76217421>.

"Glaciers: Earthâs Rivers of Ice â Icebergs and Glaciers â Beyond �� �� ��Penguins and Polar Bears."Beyond Penguins and Polar Bears Glaciers Earths Rivers of Ice Comments. 12 Feb. 2013 <http://beyondpenguins.ehe.osu.edu/issue/icebergs-and-glaciers/glaciers-earths-rivers-of-ice>.

Bibliography

Page 22: Kenai Fjords National Park

"West Antarctic Ice Sheet Science Traverse." : The Ice. 12 Feb. 2013 <http://waisdividetraverse.blogspot.com/2010/12/ice.html>.

"Harding Icefield." Photo Blog Photography Blog for Niebrugge Images Harding Icefield Comments. 12 Feb. 2013 <http://www.my-photo-blog.com/harding-icefield>.

"LARRY'S RAMBLE." : 2011-02-13. 12 Feb. 2013 <http://larrysramble.blogspot.com/2011_02_13_archive.html>.

"Kurt Friehauf - Alaska 2011 project description - Kenai FjordsNational Park." Kurt Friehauf - Alaska 2011 project description - Kenai FjordsNational Park. 12 Feb. 2013 <http://faculty.kutztown.edu/friehauf/alaska_2011/kenai_fjords/>.

Bibliography