TIM Maps Factsheet
TIM Maps Factsheet
TIM Maps Factsheet
Fact Sheet
In summer 2013 DOGAMI completed mapping for modeled tsunami inundation along the entire Oregon coast. This 4-year,
NOAA-funded project brought together the latest science, new mapping techniques, and lessons learned from earthquakes and
tsunamis around the globe.
Why should we get ready for How do tsunami inundation and evacuation maps work?
tsunamis in Oregon? These maps show safe areas so you can For distant-source earthquakes,
Oregon sits on the Pacific Rim “ring of locate your home, school, or business, DOGAMI scientists modeled two
fire,” a zone of very active plate tectonics. find your safe area, and practice your inundation scenarios: one simulates the
If plates move suddenly (“slip”) in an area route to the safe area. 1964 Alaska magnitude 9.2 earthquake
where they usually stick, an earthquake To create the inundation maps, and tsunami; the other simulates a
happens. When a plate descends, or “sub- DOGAMI scientists modeled tsunami hypothetical maximum considered
ducts,” under an adjacent plate, a subduc- scenarios for local-source (Cascadia Alaska tsunami from a magnitude ~9.2
tion zone exists. Subduction Zone, or CSZ) and for event with more seafloor uplift and
distant-source (Gulf of Alaska subduction positioned to focus tsunamis at the
zone) tsunamis. CSZ scenarios can show Oregon coast.
a wide range of inundation in the same To make the evacuation maps,
area. To make it easier to understand the Cascadia XXL scenario and the
CSZ inundation scenarios for different hypothetical maximum Alaska scenario
earthquake sizes, the sizes are labeled like inundation zones are put on one map.
T-shirts: small (magnitude ~8.7), medium Green on the evacuation map shows
Tsunami diagram: http://pubs.usgs.gov/circ/c1187/ (magnitude ~8.9), large (magnitude ~9.0), typically higher elevation areas that
When earthquakes occur in a subduction extra-large (magnitude ~9.1), and extra- lie outside the tsunami hazard zones.
zone, they can generate large tsunamis. extra-large (magnitude ~9.1). XL and The evacuation map also shows safe
Tsunamis can come from local or distant XXL scenarios simulate tsunamis similar evacuation routes and assembly areas, as
sources. to the 2011 Tōhoku, Japan, tsunami. developed by local emergency authorities.
A local tsunami, caused by a big Cas-
cadia Subduction Zone (CSZ) earthquake The maximum tsunami scenarios from each inundation map are combined... ... to create the tsunami evacuation map
just off our coast, can come on shore maximum distant source (orange) + maximum local source (yellow) distant source local source
within 15–20 minutes, before there’s time Distant-source (Alaska-Aleutian Island
Subduction Zone) tsunami inundation map
Local-source (Cascadia Subduction Zone)
tsunami inundation map
Tsunami evacuation map
for an official warning. Ground shaking Alaska 1964 (M 9.2) XXL extra extra large Distant Tsunami Inundation Zone
L large
M medium
to a safe area.
Recent work by the U.S. Geological
Survey (Professional Paper 1661–F) sug-
LOCAL TSUNAMI
INUNDATION ZONE
won’t feel an earthquake, and there will OUTSIDE HAZARD AREA: Evacuate to this
area for all tsunami warnings or if you feel an
ation to a safe area. Your loved ones are LOCAL CASCADIA EARTHQUAKE AND
TSUNAMI: Evacuation zone for a local tsu-
nami from an earthquake at the Oregon coast.
IN
arrive.
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Oregon Department of Geology and Mineral Industries 800 NE Oregon St., #28, Suite 965 Portland, OR 97232 971-673-1555 OregonGeology.org
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Oregon Department of Geology and Mineral Industries 800 NE Oregon St., #28, Suite 965 Portland, OR 97232 971-673-1555 OregonGeology.org
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