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BOUNDARIES WORK TOGETHER?

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Presentation on theme: "BOUNDARIES WORK TOGETHER?"— Presentation transcript:

1 BOUNDARIES WORK TOGETHER?
HOW DO ALL THESE BOUNDARIES WORK TOGETHER? PACIFIC NORTHWEST AND SOUTHWEST BRITISH COLUMBIA

2 BOUNDARIES WORK TOGETHER?
HOW DO ALL THESE BOUNDARIES WORK TOGETHER? PACIFIC NORTHWEST AND SOUTHWEST BRITISH COLUMBIA North American Plate Movement

3 BOUNDARIES WORK TOGETHER?
HOW DO ALL THESE BOUNDARIES WORK TOGETHER? PACIFIC NORTHWEST AND SOUTHWEST BRITISH COLUMBIA Pacific Plate Movement And Mendico Fault (San Andreas extension)

4 BOUNDARIES WORK TOGETHER?
HOW DO ALL THESE BOUNDARIES WORK TOGETHER? PACIFIC NORTHWEST AND SOUTHWEST BRITISH COLUMBIA SMALL “MID-OCEAN” RIDGES DIVERGENT GORDA RIDGE

5 BOUNDARIES WORK TOGETHER?
HOW DO ALL THESE BOUNDARIES WORK TOGETHER? PACIFIC NORTHWEST AND SOUTHWEST BRITISH COLUMBIA SMALL “MID-OCEAN” RIDGES DIVERGENT JUAN DE FUCA RIDGE

6 BOUNDARIES WORK TOGETHER?
HOW DO ALL THESE BOUNDARIES WORK TOGETHER? PACIFIC NORTHWEST AND SOUTHWEST BRITISH COLUMBIA SMALL “MID-OCEAN” RIDGES DIVERGENT EXPLORER RIDGE

7 BOUNDARIES WORK TOGETHER?
HOW DO ALL THESE BOUNDARIES WORK TOGETHER? PACIFIC NORTHWEST AND SOUTHWEST BRITISH COLUMBIA SEAFLOOR SPREADING AND TRANSFORM FAULT

8 BOUNDARIES WORK TOGETHER?
HOW DO ALL THESE BOUNDARIES WORK TOGETHER? PACIFIC NORTHWEST AND SOUTHWEST BRITISH COLUMBIA SEAFLOOR SPREADING AND TRANSFORM FAULT

9 BOUNDARIES WORK TOGETHER?
HOW DO ALL THESE BOUNDARIES WORK TOGETHER? PACIFIC NORTHWEST AND SOUTHWEST BRITISH COLUMBIA SEAFLOOR SPREADING AND TRANSFORM FAULT

10 BOUNDARIES WORK TOGETHER?
HOW DO ALL THESE BOUNDARIES WORK TOGETHER? PACIFIC NORTHWEST AND SOUTHWEST BRITISH COLUMBIA North American Plate (black and white) CONVERGING (white dashes) with Juan de Fuca Plate (blue and yellow).

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12 PACIFIC NORTHWEST JUAN DE FUCA NORTH AMERICAN PLATE MOUNTAINS
CASCADE MOUNTAIN MOUNTAINS PUGET- WILLAMETTE LOWLANDS OLYMPIC MOUNTAINS COAST RANGE NORTH AMERICAN PLATE JUAN DE FUCA PACIFIC OCEAN

13 PLATES LOCK IN PLACE JUAN DE FUCA PLATE NORTH AMERICAN PLATE

14 BETWEEN EARTHQUAKES CONVERGENCE CAUSES UPWARD BUCKLING OF
COASTAL AREAS Energy stored as in a bent cane. JUAN DE FUCA PLATE NORTH AMERICAN PLATE

15 DURING ERTHQUAKES PLATES Coastline UNLOCK subsides
Energy in earthquake and tsunami JUAN DE FUCA PLATE NORTH AMERICAN PLATE

16 Plates lock back together After release of energy by
BETWEEN EARTHQUAKES Plates lock back together After release of energy by earthquake Coastline slowly Re-emerges. JUAN DE FUCA PLATE NORTH AMERICAN PLATE

17 Tsunami Deposits, Southern
Chile. Dark bands are organic soils, lighter greys are marine sands deposited by tsunamis. Source: Rhodes, Tuttle, Horton, Doner, Kelsey, Nelson and Cisternas, EOS, 87, May 2006.

18 TSUNAMI MARCH 2011

19 Displacement during Earthquake March 2011. Source: Simons et al., 2011
Science Express

20 PUEGET SOUND 3,500BP Tidal Marsh

21 PUEGET SOUND 3,300BP Earthquake

22 PUEGET SOUND 3,200 BP Emergence

23 PUEGET SOUND 3,000 BP Forested Upland

24 PUEGET SOUND 3,000 BP Earthquake Submersion

25 PUEGET SOUND 2,700 BP Earthquake Submergence

26 PUEGET SOUND 400 Emergence Forest

27 PUEGET SOUND 400 Earthquake Submersion

28 PUEGET SOUND 700 Emergence

29 PUEGET SOUND 700 Earthquake Submersion

30 PUEGET SOUND 900 Emergence

31 PUEGET SOUND 900 Earthquake

32 PUEGET SOUND 1700 Emergence Forested Uplands

33 PUEGET SOUND 1700 Earthquake Submersion

34 Simulation of 1700 Earthquake and Tsunami

35 PUEGET SOUND 2000 Emergence

36 PUEGET SOUND AVERAGE LENGTH OF TIME BETWEEN EARTHQUAKES 300 yrs

37 PUEGET SOUND AVERAGE LENGTH OF TIME BETWEEN EARTHQUAKES 300 yrs ? 1700

38 SUBSTUTUTE DEPTH FOR TIME
1700 900 700 3300BP 3000BP Present Geologists’ Principle of Superposition


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