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Tsunami Hazards in Cascadia :
                  by
           Timothy J. Walsh
   Washington Department of Natural
             Resources
Division of Geology and Earth Resources
      Partners in Emergency
          Preparedness
             April 27, 2011
•On April 1, 1946, a
magnitude 8.0 (Mw)
earthquake with the
source in the
Aleutian Islands to
the south of Unimak
Island generated a
tsunami that
destroyed this five-
story lighthouse,
located 9.8 m above
sea level.
•Only the
foundation and
part of the
concrete sea wall
remained. All five
occupants were
killed. The waves
deposited debris
as high as 35 m
above the sea.
Although little
damage occurred
in Alaska, except
at Scotch Cap, the
tsunami was one
of the most
destructive ever to
occur in the
Hawaiian Islands.
Photo credit: U.S.
The school children noted that the water had receded
•Many went down to the shore to watch
Across what had
been the playing
fields is the
monument to the
victims
•At least 24 people were killed here, many of whom were children
playing by the waterfront. The tragedy of the 1946 tsunami
prompted the U.S. Coast and Geodetic Survey to establish the
Tsunami Warning System
Abridged from
Seismicity of the
United States,
1568-1989
(Revised), by
Carl W. Stover
and Jerry L.
Coffman, U.S.
Geological
Survey
Professional
Paper 1527,
United States
Government
Printing Office,
Washington:
1993.




                    Prince William Sound, Alaska
                    1964 March 28 03:36:14 UTC (March 27
                    local) Magnitude 9.2
Valdez sits on the edge of an outwash delta 150 km from the epicenter. During
the shaking, the unstable, saturated material failed. A slice of the delta, 1,220
m long and 183 m wide, slid into the sea, carrying the docks and part of the
town with it. The slide generated a wave which slammed the waterfront 2 to 3
minutes after the onset of the quake. The wave demolished the rest of the
waterfront, destroyed the fishing fleet, and reached 2 blocks into town, killing 30
people
Tsunami damage from the
      Highway 109 bridge over   1964 Alaska earthquake
           Copalis River

                                The wave here was about
                                10-12 feet.




                                 Highway 109 bridge
House torn apart                 over Joe Creek
at Pacific Beach
This earthquake also generated a Pacific Ocean-wide tsunami that killed 110
people, 8 here in Crescent City, CA. Note fire in background. This event led to
the opening of a second tsunami warning center in Palmer, Alaska.
1993
Okushiri
Island




A view of tsunami and related fire damage on southeast Okushiri
Island in the community of Aonae. Photo orientation is looking
northeast. Numerous fires broke out following the tsunami, adding
to the property loss and misery. More than 120 people were killed
in Japan (Okushiri and Hokkaido Islands) by the tsunami.
On the west side of Okushiri Island many locations experienced a maximum runup of
over 20 m. This small valley leading to the ocean experienced a spectacular runup of 31
m. Note the debris in the foreground, including a broken steel reinforced concrete utility
pole. Discolored and dead plants and grasses are evident on the hillside. This well-
studied earthquake and tsunami led to significant advances in modeling tsunamis.
Placer
                                                     River Silt




                                                                  Earthquake-induced
                                                                  ground crack
Drowned forest in Girdwood, Alaska, killed in 1964


                                                           A.D. 1700
                                                           Ground
                                                           surface



                                                          1,100 year
                                                          old ground
                                                          surface
                             from Brian Atwater
Drowned forest along the Copalis River,
Washington, killed in A.D. 1700
Right, subsided marsh
along the Niawiakum River,
                             Tsunami sands
southwest Washington.
Below, note pitfalls of
working in tidal marshes.




                                 A.D. 1700 ground
                                 surface
The realization that Cascadia was active was instrumental to the creation of
the National Tsunami Hazard Mitigation Program, which develops tsunami
inundation maps for vulnerable coastlines. These are based on a combination
of numerical modeling, and , where possible, paleoseismology.
The model
calculates
the water
surface
elevation
and velocity
at each grid
point
Tsunami parade at Hiro.




                                                Storm surge trace



                            REMEMBER
                             THE PAST

Tsunami monument
                             from Nobuo Shuto
A TRAGEDY OF FOREIGN TOURIST WHO
 COULD NOT UNDERSTAND WARNING
                Her last position




                  from Nobuo Shuto
Washington has a limited historical record, so we rely on
modeling to establish tsunami hazard zones
A tsunami generated by a Cascadia
subduction zone earthquake will
arrive in less than 45 minutes. For
these events, as was the case in
Banda Aceh, the earthquake must be
the warning. Citizens must know
where to evacuate from and where to
evacuate to, and must do so quickly
and on foot.

Note the long peninsulas or spits of
low-lying ground. Ocean Shores
peninsula is 7 miles long and Long
Beach peninsula is 20 miles long with
little or no high ground over those
distances. For these areas, tsunami
defenses are appropriate.
After

  TWO BUILDINGS
    IN AONAE,
       1993



                  During




Before            (北海道新聞社)

                    from Nobuo Shuto
THE TWO
     BUILDINGS
   THAT REMAINED.


                                           Tsunami trace




This building stopped a house and boats.
Those two buildings
and other Japanese
tsunami defense
structures formed
the basis of a study
of buildings that
survived
devastating
tsunamis when
everything else in
the area was
destroyed.
DEFENCE
     STRUCTURES

SEA WALLS

TSUNAMI BREAKWATERS

TSUNAMI GATE

HIGHTENING OF RIVER DIKES

               from Nobuo Shuto
ARTIFICIALLY-ELEVATED GROUND




                      from Nobuo Shuto
SEA-WALLS
  WORKED
The 1968 tsunami reflected by
sea-walls.




                from Nobuo Shuto
from Nobuo Shuto




     SEA-WALLS
   DID NOT WORK.
The 1993 tsunami was higher than
the sea-walls by 5 m.
from Nobuo Shuto



SHELTER TOWER
  4th & 5th: Shelter
  3rd: Tsunami museum
  2nd: Meeting room
  1st: Ware house          Tsunami level




  Wat Ban Nyan, Khao Lak
Expected
                                        tsunami


                                        Past tsunami




AN ELEVATED SHELTER AT SHIRAHAMA SEA-
BATHING RESORT, TOKUSHIMA PREF.
                                            from
                                            Nobuo
                                            Shuto
© 2010      Extent of debris
German                                                           Tagajo Castle
Aerospace
Center
(DLR).




 Tsunami Catalogue for the Sanriku District near the Sendai Area, mostly based upon
 Miyagi Showa Shinsho-Shi (Record of the Showa Earthquake and Tsunami in Miyagi
 Prefecture) and partially on Shuto’s memory
   In 869. Giant earthquake in the Tohoku District. Tsunami flooded up to the
   Tagajo castle near Sendai. Over 1,000 drowned.
At Minami-
Sanriku town,
an apartment
building was
situated right
next to the
coast and
designated as
an evacuation
building as
shown by
evacuation
signs, but there
were traces
that tsunami
also had
reached the 4th
floor.
This three-story
building (below) was
the disaster
management center
of the town which
was also designed
to function as a
tsunami evacuation
building. At the time
of tsunami, about
thirty municipal
officials evacuated
to the rooftop but
only ten of them
survived. A young
female official who
kept delivering
evacuation message
to the villagers until
the last moment has
not been found yet.
We formed a partnership
with FEMA and the
Applied Technology
Council to provide
building code style
guidance for building
facilities to withstand a
magnitude 9 earthquake
and be suitable for
vertical evacuation.
Planning for the right size
earthquake is critical.
Project Safe Haven:
     Tsunami Vertical
       Evacuation
Long Beach Peninsula/Pacific County
Safe Haven Options (from FEMA 646):
Towers –
• Limited Space
• Blocks Views
• Few Options for Shelter


Buildings –
• Expensive
     • Better get it right the first time!
• Very Large, Likely to Block Views
• May require Private Development
     • Incentives for Height?

Berms –
• Least Expensive Option
• Can be Multi-Purpose
• May be Placed to Limit View Blocking
Vertical Evacuation Safe
    Haven Project
 • Community-based,
   ‘bottom-up’ approach

 • All options (buildings,
  towers, berms, etc.) are on
  the table for consideration

 Common Themes:
 • School Safety
 • Seniors and special needs
   populations
 • More conservative travel
  times
Safe Haven Berms
Safe Haven Berms
Safe Haven Towers
Safe Haven Buildings
Civilization exists by
geological consent—
subject to change without
notice


Will Durant
National Tsunami Hazard
      Mitigation Program
      nthmp.tsunami.gov
      Division of Geology
 dnr.wa.gov/ResearchScience/
     GeologyEarthSciences
Emergency Management Division
          emd.wa.gov

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Tsunami Hazards in Cascadia

  • 1. Tsunami Hazards in Cascadia : by Timothy J. Walsh Washington Department of Natural Resources Division of Geology and Earth Resources Partners in Emergency Preparedness April 27, 2011
  • 2. •On April 1, 1946, a magnitude 8.0 (Mw) earthquake with the source in the Aleutian Islands to the south of Unimak Island generated a tsunami that destroyed this five- story lighthouse, located 9.8 m above sea level.
  • 3. •Only the foundation and part of the concrete sea wall remained. All five occupants were killed. The waves deposited debris as high as 35 m above the sea. Although little damage occurred in Alaska, except at Scotch Cap, the tsunami was one of the most destructive ever to occur in the Hawaiian Islands. Photo credit: U.S.
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  • 5. The school children noted that the water had receded
  • 6. •Many went down to the shore to watch
  • 7. Across what had been the playing fields is the monument to the victims
  • 8. •At least 24 people were killed here, many of whom were children playing by the waterfront. The tragedy of the 1946 tsunami prompted the U.S. Coast and Geodetic Survey to establish the Tsunami Warning System
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  • 10. Abridged from Seismicity of the United States, 1568-1989 (Revised), by Carl W. Stover and Jerry L. Coffman, U.S. Geological Survey Professional Paper 1527, United States Government Printing Office, Washington: 1993. Prince William Sound, Alaska 1964 March 28 03:36:14 UTC (March 27 local) Magnitude 9.2
  • 11. Valdez sits on the edge of an outwash delta 150 km from the epicenter. During the shaking, the unstable, saturated material failed. A slice of the delta, 1,220 m long and 183 m wide, slid into the sea, carrying the docks and part of the town with it. The slide generated a wave which slammed the waterfront 2 to 3 minutes after the onset of the quake. The wave demolished the rest of the waterfront, destroyed the fishing fleet, and reached 2 blocks into town, killing 30 people
  • 12. Tsunami damage from the Highway 109 bridge over 1964 Alaska earthquake Copalis River The wave here was about 10-12 feet. Highway 109 bridge House torn apart over Joe Creek at Pacific Beach
  • 13. This earthquake also generated a Pacific Ocean-wide tsunami that killed 110 people, 8 here in Crescent City, CA. Note fire in background. This event led to the opening of a second tsunami warning center in Palmer, Alaska.
  • 14. 1993 Okushiri Island A view of tsunami and related fire damage on southeast Okushiri Island in the community of Aonae. Photo orientation is looking northeast. Numerous fires broke out following the tsunami, adding to the property loss and misery. More than 120 people were killed in Japan (Okushiri and Hokkaido Islands) by the tsunami.
  • 15. On the west side of Okushiri Island many locations experienced a maximum runup of over 20 m. This small valley leading to the ocean experienced a spectacular runup of 31 m. Note the debris in the foreground, including a broken steel reinforced concrete utility pole. Discolored and dead plants and grasses are evident on the hillside. This well- studied earthquake and tsunami led to significant advances in modeling tsunamis.
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  • 17. Placer River Silt Earthquake-induced ground crack Drowned forest in Girdwood, Alaska, killed in 1964 A.D. 1700 Ground surface 1,100 year old ground surface from Brian Atwater Drowned forest along the Copalis River, Washington, killed in A.D. 1700
  • 18. Right, subsided marsh along the Niawiakum River, Tsunami sands southwest Washington. Below, note pitfalls of working in tidal marshes. A.D. 1700 ground surface
  • 19. The realization that Cascadia was active was instrumental to the creation of the National Tsunami Hazard Mitigation Program, which develops tsunami inundation maps for vulnerable coastlines. These are based on a combination of numerical modeling, and , where possible, paleoseismology.
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  • 23. Tsunami parade at Hiro. Storm surge trace REMEMBER THE PAST Tsunami monument from Nobuo Shuto
  • 24. A TRAGEDY OF FOREIGN TOURIST WHO COULD NOT UNDERSTAND WARNING Her last position from Nobuo Shuto
  • 25. Washington has a limited historical record, so we rely on modeling to establish tsunami hazard zones
  • 26. A tsunami generated by a Cascadia subduction zone earthquake will arrive in less than 45 minutes. For these events, as was the case in Banda Aceh, the earthquake must be the warning. Citizens must know where to evacuate from and where to evacuate to, and must do so quickly and on foot. Note the long peninsulas or spits of low-lying ground. Ocean Shores peninsula is 7 miles long and Long Beach peninsula is 20 miles long with little or no high ground over those distances. For these areas, tsunami defenses are appropriate.
  • 27. After TWO BUILDINGS IN AONAE, 1993 During Before (北海道新聞社) from Nobuo Shuto
  • 28. THE TWO BUILDINGS THAT REMAINED. Tsunami trace This building stopped a house and boats.
  • 29. Those two buildings and other Japanese tsunami defense structures formed the basis of a study of buildings that survived devastating tsunamis when everything else in the area was destroyed.
  • 30. DEFENCE STRUCTURES SEA WALLS TSUNAMI BREAKWATERS TSUNAMI GATE HIGHTENING OF RIVER DIKES from Nobuo Shuto
  • 31. ARTIFICIALLY-ELEVATED GROUND from Nobuo Shuto
  • 32. SEA-WALLS WORKED The 1968 tsunami reflected by sea-walls. from Nobuo Shuto
  • 33. from Nobuo Shuto SEA-WALLS DID NOT WORK. The 1993 tsunami was higher than the sea-walls by 5 m.
  • 34. from Nobuo Shuto SHELTER TOWER 4th & 5th: Shelter 3rd: Tsunami museum 2nd: Meeting room 1st: Ware house Tsunami level Wat Ban Nyan, Khao Lak
  • 35. Expected tsunami Past tsunami AN ELEVATED SHELTER AT SHIRAHAMA SEA- BATHING RESORT, TOKUSHIMA PREF. from Nobuo Shuto
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  • 37. © 2010 Extent of debris German Tagajo Castle Aerospace Center (DLR). Tsunami Catalogue for the Sanriku District near the Sendai Area, mostly based upon Miyagi Showa Shinsho-Shi (Record of the Showa Earthquake and Tsunami in Miyagi Prefecture) and partially on Shuto’s memory In 869. Giant earthquake in the Tohoku District. Tsunami flooded up to the Tagajo castle near Sendai. Over 1,000 drowned.
  • 38. At Minami- Sanriku town, an apartment building was situated right next to the coast and designated as an evacuation building as shown by evacuation signs, but there were traces that tsunami also had reached the 4th floor.
  • 39. This three-story building (below) was the disaster management center of the town which was also designed to function as a tsunami evacuation building. At the time of tsunami, about thirty municipal officials evacuated to the rooftop but only ten of them survived. A young female official who kept delivering evacuation message to the villagers until the last moment has not been found yet.
  • 40. We formed a partnership with FEMA and the Applied Technology Council to provide building code style guidance for building facilities to withstand a magnitude 9 earthquake and be suitable for vertical evacuation. Planning for the right size earthquake is critical.
  • 41. Project Safe Haven: Tsunami Vertical Evacuation Long Beach Peninsula/Pacific County
  • 42. Safe Haven Options (from FEMA 646): Towers – • Limited Space • Blocks Views • Few Options for Shelter Buildings – • Expensive • Better get it right the first time! • Very Large, Likely to Block Views • May require Private Development • Incentives for Height? Berms – • Least Expensive Option • Can be Multi-Purpose • May be Placed to Limit View Blocking
  • 43. Vertical Evacuation Safe Haven Project • Community-based, ‘bottom-up’ approach • All options (buildings, towers, berms, etc.) are on the table for consideration Common Themes: • School Safety • Seniors and special needs populations • More conservative travel times
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  • 49. Civilization exists by geological consent— subject to change without notice Will Durant
  • 50. National Tsunami Hazard Mitigation Program nthmp.tsunami.gov Division of Geology dnr.wa.gov/ResearchScience/ GeologyEarthSciences Emergency Management Division emd.wa.gov