STATE OF OREGON DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES Tsunami Inundation Map Linc-09 www.OregonGeology.org Local Source (Cascadia Subduction Zone) Tsunami Inundation Map Tsunami Inundation Maps for Yaquina River, W. Lawrence Givens, Governing Board Chair Lincoln County, Oregon Vicki S. McConnell, Director and State Geologist Andree V. Pollock, Assistant Director, Geologic Survey and Services Yaquina River, Oregon Plate 1

Rachel L. Smith, Project Operations Manager S C H L E C H T R D

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g 200 Ian P. Madin, Chief Scientist 100 u 2013

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Introduction B S U N N Y R I D G E R D 25

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200 100 100 C 200 25 I T Y The Oregon Department of Geology and Mineral Industries (DOGAMI) Oregon. DOGAMI has also incorporated physical evidence that suggests R 25 100 eek D C R I T E S E R L P C r has been identifying and mapping the tsunami inundation hazard along that portions of the coast may drop 4 to 10 feet during the earthquake; 25 Babcock the Oregon coast since 1994. In Oregon, DOGAMI manages the National this effect is known as subsidence. Detailed information on fault Tsunami Hazard Mitigation Program, which has been administered by geometries, subsidence, computer models, and the methodology used to 100

N B B' the National Oceanic and Atmospheric Administration (NOAA) since create the tsunami scenarios presented on this map can be found in u t e D R Yaquina River 1995. DOGAMI’s work is designed to help cities, counties, and other sites DOGAMI Special Papers 41 (Priest and others, 2009) and 43 (Witter and S Y

l A o B111 B in coastal areas reduce the potential for disastrous tsunami-related others, 2011). u g H h T M IL L C R E E K R D consequences by understanding and mitigating this geologic hazard. U O 200 Using federal funding awarded by NOAA, DOGAMI has developed a new S Map Explanation o o B n e S l 100 generation of tsunami inundation maps to help residents and visitors o u g h 25 along the entire Oregon coast prepare for the next Cascadia Subduction This tsunami inundation map displays the output of computer models Zone (CSZ) earthquake and tsunami. representing five selected tsunami scenarios, all of which include the earthquake-produced subsidence and the tsunami-amplifying effects of r e Slack Creek The CSZ is the tectonic plate boundary between the North American the splay fault. Each scenario assumes that a tsunami occurs at Mean iv Plate and the Juan de Fuca Plate (Figure 1). These plates are converging Higher High Water (MHHW) tide; MHHW is defined as the average R

a 1 at a rate of about 1.5 inches per year, but the movement is not smooth height of the higher high tides observed over an 18-year period at the n 0 i 0

200 0 and continuous. Rather, the plates lock in place, and unreleased energy Yaquina Bay (Central Coast Model) tide gauge. To make it easier to u 200 100 q L

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builds over time. At intervals, this accumulated energy is violently understand this scientific material and to enhance the educational E 25

25 R D released in the form of a megathrust earthquake rupture, where the aspects of hazard mitigation and response, the five scenarios are labeled 200

100 North American Plate suddenly slips westward over the Juan de Fuca as “T-shirt sizes” ranging from Small, Medium, Large, Extra Large, to 25

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Plate. This rupture causes a vertical displacement of water that creates a Extra Extra Large (S, M, L, XL, XXL). The map legend depicts the 100 tsunami (Figure 2). Similar rupture processes and tsunamis have respective amounts of slip, the frequency of occurrence, and the 25 occurred elsewhere on the planet where subduction zones exist: for earthquake magnitude for these five scenarios. Figure 4 shows the 200 example, offshore Chile in 1960 and 2010, offshore Alaska in 1964, near cumulative number of buildings inundated within the map area. 100 Sumatra in 2004, and offshore Japan in March 2011.

The computer simulation model output is provided to DOGAMI as 200 CSZ Frequency: Comprehensive research of the offshore geologic record millions of points with values that indicate whether the location of each

25 h 100 100 indicates that at least 19 major ruptures of the full length of the CSZ have point is wet or dry. These points are converted to wet and dry contour ug Slo 200 n 25 occurred off the Oregon coast over the past 10,000 years (Figure 3). All lines that form the extent of inundation. The transition area between the o s n 200 19 of these full-rupture CSZ events were likely magnitude 8.9 to 9.2 wet and dry contour lines is termed the Wet/Dry Zone, which equates to h o J Y earthquakes (Witter and others, 2011). The most recent CSZ event the amount of error in the model when determining the maximum A Q 100 U 200

inundation for each scenario. Only the XXL Wet/Dry Zone is shown on I N happened approximately 300 years ago on January 26, 1700. Sand 25 BA 100

200 100 A 200 deposits carried onshore and left by the 1700 event have been found 1.2 this map. Y R miles inland; older tsunami sand deposits have also been discovered in D

25 estuaries 6 miles inland. As shown in Figure 3, the range in time This map also shows the regulatory tsunami inundation line (Oregon D

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100 between these 19 events varies from 110 to 1,150 years, with a median Revised Statutes 455.446 and 455.447), commonly known as the Senate Y 100 A B time interval of 490 years. In 2008 the United States Geological Survey Bill 379 line. Senate Bill 379 (1995) instructed DOGAMI to establish the A N I 25 U (USGS) released the results of a study announcing that the probability of area of expected tsunami inundation based on scientific evidence and Q A a magnitude 8-9 CSZ earthquake occurring over the next 30 years is tsunami modeling in order to prohibit the construction of new essential Y A A' 10% and that such earthquakes occur about every 500 years (WGCEP, and special occupancy structures in this tsunami inundation zone 2008). (Priest, 1995). Y

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a 200 O 100 U Time Series Graphs and Wave Elevation Profiles: In addition to the T q CSZ Model Specifications: The sizes of the earthquake and its resultant H B A u tsunami are primarily driven by the amount and geometry of the slip tsunami scenarios, the computer model produces time series data for Y R D i that takes place when the North American Plate snaps westward over “gauge” locations in the area. These points are simulated gauge stations n a R D A Y the Juan de Fuca Plate during a CSZ event. DOGAMI has modeled a wide that record the time, in seconds, of the tsunami wave arrival and the H B

U T 100 R 200 S O range of earthquake and tsunami sizes that take into account different wave height observed. It is especially noteworthy that the greatest wave i I L L C R E E K v M R D fault geometries that could amplify the amount of seawater height and velocity observed are not necessarily associated with the first e r displacement and increase tsunami inundation. Seismic geophysical tsunami wave to arrive onshore. Therefore evacuees should not assume profiles show that there may be a steep splay fault running nearly that the tsunami event is over until the proper authorities have sounded B107 parallel to the CSZ but closer to the Oregon coastline (Figure 1). The the all-clear signal at the end of the evacuation. Figure 5 depicts the effect of this splay fault moving during a full-rupture CSZ event would be tsunami waves as they arrive at a simulated gauge station. Figure 6 an increase in the amount of vertical displacement of the Pacific depicts the overall wave height and inundation extent for all five Re eek se r rv Ocean, resulting in an increase of the tsunami inundation onshore in scenarios at the profile locations shown on this map. C o D l l ir R i

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Cascadia Subduction Zone Setting 200 l o 200 u g

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Figure 1: This block diagram depicts the tectonic setting of the region. See Figure 2 for the sequence of events that occur during a Cascadia Subduction Zone megathrust earthquake and tsunami. 200 200

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How Tsunamis Occur 25 25 200 100

Poole Slough

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Figure 2: The North American Plate rides Because the two plates are stuck in place at Eventually the locked zone ruptures and 100

over the descending Juan de Fuca Plate at a the “locked zone,” strain builds up over time causes a great earthquake. The sudden slip of 25

200 100 rate of approximately 1.5 inches per year. and the North American Plate bulges up. the two plates displaces Pacific Ocean water 200 upward and creates a tsunami.

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D E Displaced and uplifted Pacific Ocean water Along the Oregon coast, tsunami waves run rushes in all directions. up onto the land for several hours.

Occurrence and Relative Size of Cascadia Subduction Zone Megathrust Earthquakes

Figure 3: This chart depicts the timing, frequency, and magnitude of the last 19 great Cascadia Subduction Zone events over the past 10,000 years. The most recent event

occurred on January 26, 1700. The 1700 D R E N I L 0 0 0 1 event is considered to be a “medium sized” event. The data used to create this chart came from research that examined the many submarine landslides, known as “turbidites,” that are triggered only by these great earthquakes (Witter and others, 2011). The loose correlation is “the bigger the turbidite, the bigger the earthquake.”

Buildings within Tsunami Inundation Zones

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Estimated Tsunami Wave Height through Time for Simulated Gauge Station Maximum Wave Elevation Profiles Legend Tsunami Inundation Map Index Data References

Source Data: References: Average Slip Maximum Slip Time to Earthquake Tillamook This map is based on hydrodynamic tsunami modeling by 2007 Working Group on California Earthquake Earthquake Size Range (ft) Range (ft) Accumulate Slip (yrs) Magnitude 01 Lincoln Joseph Zhang, Oregon Health and Science University, Probabilities (WGCEP), 2008, The Uniform California Portland, Oregon. Model data input were created by John Earthquake Rupture Forecast, Version 2 (UCERF 2): U.S. T. English and George R. Priest, Department of Geology Geological Survey Open-File Report 2007-1437 and XXL 59 to 72 118 to 144 1,200 ~9.1 and Mineral Industries (DOGAMI), Portland, Oregon. California Geological Survey Special Report 203 02 [http://pubs.usgs.gov/of/2007/1437/].

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l Hydrology data, contours, critical facilities, and building

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o l footprints were created by DOGAMI. Senate Bill 379 line Priest, G. R., 1995, Explanation of mapping methods and XL 56 to 72 115 to 144 1,050 to 1,200 ~9.1 c o

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P data were redigitized by Rachel L. Smith and Sean G. use of the tsunami hazard maps of the Oregon coast, 03 i

L Pickner, DOGAMI, in 2011 (GIS file set, in press, 2012). Oregon Department of Geology and Mineral Industries L 36 to 49 72 to 98 650 to 800 ~9.0 Open-File Report O-95-67, 95 p. 04 Urban growth boundaries (2011) were provided by the Oregon Department of Land Conservation and Priest, G.R., Goldfinger, C., Wang, K., Witter, R.C., Zhang, Y., 05 Development (DLCD). and Baptista, A.M., 2009, Tsunami hazard assessment of M 23 to 30 46 to 62 425 to 525 ~8.9 the northern Oregon coast: a multi-deterministic Polk Transportation data (2007) provided by Lincoln County approach tested at Cannon Beach, Clatsop County, B were edited by DOGAMI to improve the spatial accuracy Oregon: Oregon Department of Geology and Mineral S 13 to 16 30 to 36 300 ~8.7 enton 06 of the features or to add newly constructed roads not Industries Special Paper 41, 87 p. present in the original data layer. 08 Witter, R.C., Zhang, Y., Wang, K., Priest, G.R., Goldfinger, C., XXL Wet/Dry Zone Lidar data are from DOGAMI Lidar Data Quadrangles Stimely, L.L., English, J.T., and Ferro, P.A., 2011, Simulating 07 LDQ-2011-44123-E7-Elk City, LDQ-2011-44123-E8- tsunami inundation at Bandon, Coos County, Oregon, 09 OREGON Toledo South, and LDQ-2011-44124-E1-Newport South; using hypothetical Cascadia and Alaska earthquake additional unpublished lidar data flown 2011. scenarios: Oregon Department of Geology and Mineral 10 Industries Special Paper 43, 57 p. Urban Growth Boundary Fire Station Coordinate System: Oregon Statewide Lambert 11 Conformal Conic, Unit: International Feet, Horizontal Datum: NAD 1983 HARN, Vertical Datum: NAVD 1988. Graticule shown with geographic coordinates Police Station 12 Building Footprint 13 (latitude/longitude).

14 A1 School Simulated Gauge Station Software: Esri ArcGIS® 10.1, Microsoft® Excel®, and 15 Lincoln Adobe® Illustrator® Figure 6: These profiles depict the expected maximum tsunami wave elevation for the five “tsunami T-shirt scenarios” along lines A-A' and B-B'. The tsunami scenarios are modeled to occur at high tide and to account for local subsidence or uplift of the ground surface. Benton Lane Profile Location Hospital/Urgent Care Clinic Lane Funding: This map was funded under award #NA09NW54670014 by the National Oceanic and Senate Bill 379 Line Atmospheric Administration (NOAA) through the 101 National Tsunami Hazard Mitigation Program. U.S. Highway Linc-01 Lincoln City North Linc-09 Yaquina River Linc-02 Lincoln City South Linc-10 Seal Rock Map Data Creation/Development: State Park Figure 5: This chart depicts the tsunami waves as they arrive at the selected reference point (simulated gauge station). It shows the change in wave heights for Linc-03 Gleneden Beach - Siletz River Linc-11 Driftwood Beach Tsunami Inundation Scenarios: George R. Priest, 241 Laura L. Stimely, Daniel E. Coe, Paul A. Ferro, all five tsunami scenarios over an 8-hour period. The starting water elevation (0.0 hour) takes into account the local land subsidence or uplift caused by the State Highway Linc-04 Depoe Bay Linc-12 Waldport Linc-05 Otter Rock - Beverly Beach Linc-13 Tidewater Sean G. Pickner, Rachel L. Smith earthquake. Wave heights vary through time, and the first wave will not necessarily be the largest as waves interfere and reflect off local topography and Basemap Data: Kaleena L.B. Hughes, Sean G. Pickner bathymetry. Any absence of data indicates periods for which tsunami inundation has not yet reached or has receded from the station location and dry land is Elevation Contour Linc-06 Newport North Linc-14 Ocean Shores exposed. (25 ft intervals up to 200 ft) Improved Road Linc-07 Newport South Linc-15 Yachats Map Production: Linc-08 Toledo Cartography: Kaleena L.B. Hughes, Sean G. Pickner, Taylore E. Wille For copies of this publication contact: Nature of the Northwest Information Center 0 0.25 0.5 Mile Text: Don W.T. Lewis, Rachel L. Smith Figure 4: The table and chart show the number of buildings inundated for each “tsunami T-shirt scenario” for cities and Editing: Don W.T. Lewis, Rachel L. Smith 800 NE Oregon Street, #28, Ste. 965 unincorporated portions of the map. Portland, Oregon 97232 Publication: Deborah A. Schueller telephone (971) 673-2331 Scale 1:10,000 0 0.25 0.5 1 Kilometer Map Date: 02/08/2013 http://www.naturenw.org