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The Olympic Mountains A Wedge of Fun. Olympic Mountains, Wilapa Hills & Oregon Coast Range E-1.

Dec 21, 2015

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Page 1: The Olympic Mountains A Wedge of Fun. Olympic Mountains, Wilapa Hills & Oregon Coast Range E-1.

The Olympic Mountains

A Wedge of Fun

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Page 2: The Olympic Mountains A Wedge of Fun. Olympic Mountains, Wilapa Hills & Oregon Coast Range E-1.

Olympic Mountains, Wilapa Hills & Oregon Coast Range

E-1

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Page 3: The Olympic Mountains A Wedge of Fun. Olympic Mountains, Wilapa Hills & Oregon Coast Range E-1.

Geology Map

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Page 4: The Olympic Mountains A Wedge of Fun. Olympic Mountains, Wilapa Hills & Oregon Coast Range E-1.

Major Rock Units

E-4

1. Peripheral Rocks

2. Core Rocks

Separated by reverse faults

Page 5: The Olympic Mountains A Wedge of Fun. Olympic Mountains, Wilapa Hills & Oregon Coast Range E-1.

Peripheral Rocks: Mostly the Crescent Fm

E-4

Age:Mostly Eocene (60-50 Myrs)

RocksPillow BasaltsSome Vesicular Basalts15-30 km thick

Limestone(Red)w/deep water forams

Page 6: The Olympic Mountains A Wedge of Fun. Olympic Mountains, Wilapa Hills & Oregon Coast Range E-1.

Crescent Formation

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Basalt of the Crescent Formation on Klahhane Ridge above Port Angeles (USGS).

Page 7: The Olympic Mountains A Wedge of Fun. Olympic Mountains, Wilapa Hills & Oregon Coast Range E-1.

Core Rocks

E-4

Age:Eocene-Miocene (40-20 Myrs)Metamorphosed 14-12 Myrs

RocksSandstones

w/graded bedsShale

MetamorphismEast - Low Grade

(11 km burial)West - Not Met.

Youngest Oldest

Page 8: The Olympic Mountains A Wedge of Fun. Olympic Mountains, Wilapa Hills & Oregon Coast Range E-1.

Core Rocks

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Sandstone beds with thin shale interbeds on Windfall Peak. (USGS)

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Complexly disrupted sandstone and shale beds of Olympic Core on north ridge of Mount Fitzhenry. (USGS)

Page 9: The Olympic Mountains A Wedge of Fun. Olympic Mountains, Wilapa Hills & Oregon Coast Range E-1.

Olympic Structures

E-3

Peripheral RocksCore Rocks

Note faults place older rock over younger rock

Page 10: The Olympic Mountains A Wedge of Fun. Olympic Mountains, Wilapa Hills & Oregon Coast Range E-1.

Interpretation: Peripheral Rocks

E-4

Hot Spot Island

Terrane (fault bounded)

Basalt Chemistry = Hot Spot & Divergent Zone

Page 11: The Olympic Mountains A Wedge of Fun. Olympic Mountains, Wilapa Hills & Oregon Coast Range E-1.

Modern Analogy - Iceland

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Page 12: The Olympic Mountains A Wedge of Fun. Olympic Mountains, Wilapa Hills & Oregon Coast Range E-1.

Possible Eocene ReconstructionE-1

55 Myrs

35 Myrs

Page 13: The Olympic Mountains A Wedge of Fun. Olympic Mountains, Wilapa Hills & Oregon Coast Range E-1.

Plate Reconstruction: 55 Myrs

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D-2

Page 14: The Olympic Mountains A Wedge of Fun. Olympic Mountains, Wilapa Hills & Oregon Coast Range E-1.

Supporting Evidence: Rock Age

E-3

Page 15: The Olympic Mountains A Wedge of Fun. Olympic Mountains, Wilapa Hills & Oregon Coast Range E-1.

Interpretation: Core Rocks

E-4

Trench Sediments

Accretionary Wedge

Page 16: The Olympic Mountains A Wedge of Fun. Olympic Mountains, Wilapa Hills & Oregon Coast Range E-1.

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What is an Accretionary

Wedge?

Page 17: The Olympic Mountains A Wedge of Fun. Olympic Mountains, Wilapa Hills & Oregon Coast Range E-1.

Olympic Accretionary Wedge

Page 18: The Olympic Mountains A Wedge of Fun. Olympic Mountains, Wilapa Hills & Oregon Coast Range E-1.

Olympic History

E-4

Western Core rocks accreted first & were buried deepest

(explains why they are oldest and most metamorphosed)

Page 19: The Olympic Mountains A Wedge of Fun. Olympic Mountains, Wilapa Hills & Oregon Coast Range E-1.

But Why is the North “Wedge” (Olympics) so much larger than the

South “Wedge” (Wilipa Hills/Oregan Coast Range)?

1. Shoved in the Corner

Insular ST

WashingtonOlympics

CoastRange Oregon

Page 20: The Olympic Mountains A Wedge of Fun. Olympic Mountains, Wilapa Hills & Oregon Coast Range E-1.

But Why is the North “Wedge” (Olympics) so much larger than the

South “Wedge” (Wilipa Hills/Oregan Coast Range)?

2. There is a bend in the Juan de Fuca Plate under the Olympics

N. America

Cross SectionNorth ------ South

Juan de Fuca

Olympics

Page 21: The Olympic Mountains A Wedge of Fun. Olympic Mountains, Wilapa Hills & Oregon Coast Range E-1.

Evidence for the Bend1. NW Volcanoes

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100 Depth

Steep Subduction Shallow Subduction

Page 22: The Olympic Mountains A Wedge of Fun. Olympic Mountains, Wilapa Hills & Oregon Coast Range E-1.

Evidence for the Bend2. NW Earthquakes

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Quakes occur in the subducting plate

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Page 23: The Olympic Mountains A Wedge of Fun. Olympic Mountains, Wilapa Hills & Oregon Coast Range E-1.

Why is there a Bend at all?Basin & Range Extention to the South

Page 24: The Olympic Mountains A Wedge of Fun. Olympic Mountains, Wilapa Hills & Oregon Coast Range E-1.

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