DOGAMI Open-File Report Series

[Go back] | Publications Center | DOGAMI Home

Publication Preview

Open-File Report O-21-03, Local tsunami evacuation analysis of Gold Beach and nearby unincorporated communities, Curry County, Oregon,
by Laura L. S. Gabel, Fletcher E. O’Brien, and Jonathan C. Allan; 71 p. report, one Esri® geodatabase with internal metadata, external metadata in .xml and .html formats.

Learn more about Beat the Wave series maps.

 

PUBLICATION DOWNLOADS

ABSTRACT
Pedestrian evacuation routes were evaluated for a local tsunami generated by an earthquake on the Cascadia Subduction Zone (CSZ) in the City of Gold Beach and nearby unincorporated communities of Curry County, Oregon. Our analyses focused on a maximum-considered CSZ tsunami event, termed XXL, that could be produced by a locally generated magnitude (Mw) 9.1 earthquake and covers 100 percent of potential variability. We also analyzed evacuation for a slightly smaller local tsunami event covering 95% of potential variability, termed Large (sometimes referred to as L1 in other DOGAMI reports), and generated by a magnitude 8.9 earthquake. Evacuation paths were limited to established roads, trails, and pedestrian pathways designated by local government reviewers as the most likely routes.

To assist in pedestrian tsunami evacuation, we produced maps and digital data that include the following:

The BTW maps depict the minimum evacuation speed required to stay ahead of the tsunami wave for each scenario. For planning purposes, we present a variety of scenarios that increase and decrease evacuation difficulty (due to additional complications and mitigation options, respectively). Model assumptions include:

In addition to the assumptions listed above, the current conditions scenario also assumes the failure of non-retrofitted bridges. In all cases, the identified minimum speeds must be maintained for the entire time it takes to evacuate from the inundation zone.

Given the model assumptions defined in the Methods section and summarized above, results show that evacuation for most of the region examined is only achievable at relatively fast walking speeds (6 fps, or 4.1 mph) or greater. Those people who find themselves especially far from high ground, such as the beach and the Rogue Shores neighborhood, have the greatest challenge. It will be difficult for evacuees from these locations to reach safety prior to the arrival of the tsunami. Liquefaction and landslides could present additional challenges to evacuation across the region.

In this report, tsunami mitigation refers to actions used to improve the survivability of a local community population. This project is about evaluating ways to help move people out of the tsunami zone in the shortest amount of time possible between the start of earthquake shaking and the arrival of the tsunami. Mitigation options may include adding new evacuation routes, constructing earthquake-hardened roads and trails (that is, built or remodeled to withstand shaking from a major earthquake and liquefaction), enhancing tsunami wayfinding signage along core routes, and/or installing a tsunami refuge, otherwise known as a vertical evacuation structure.


GEOGRAPHIC INFORMATION SYSTEM (GIS) DATA

Geodatabase is Esri® version 10.6 format.
Metadata is embedded in the geodatabase and is also provided as separate .xml and .html formatted files.

Port_Orford_Evacuation_Modeling.gdb (GIS data bundle zip file)
Raster_Flow_Depth_XXL1 This raster layer shows maximum flow depths (over the course of the entire simulation) in meters relative to the NAVD88 vertical datum. Flow depth reflects the maximum tsunami water level minus the ground elevation. This layer was created based on the Extra-extra-large1 (XXL1) tsunami scenario, which is a Local Cascadia Subduction Zone (CSZ) tsunami scenario generated by a magnitude 9.1 earthquake. The XXL1 event has an estimated recurrence rate of at least 10,000 years. .xml
.html
Raster_Wave_Arrival_XXL1 This raster layer shows estimated wave arrival times, in minutes, for a maximum-considered XXL1 tsunami caused by a magnitude 9.1 Cascadia Subduction Zone (CSZ) earthquake. This layer was created based on the Extra-extra-large1 (XXL1) tsunami scenario, which is a Local Cascadia Subduction Zone (CSZ) tsunami scenario generated by a magnitude 9.1 earthquake. The XXL1 event has an estimated recurrence rate of at least 10,000 years. .xml
.html
 
L1_BridgesOut_EvacuationFlowZones This polygon feature class shows the nearest safety destination for every point in the inundation zone (on the road and trail network) assuming all non-retrofitted bridges within the inundation zone fail due to earthquake shaking. This layer was created based on the Large1 (L1) tsunami scenario, which is a Local Cascadia Subduction Zone (CSZ) tsunami scenario generated by a magnitude 9.0 earthquake. The L1 event has an estimated recurrence rate of 2,500 to 3,333 years. .xml
.html
L1_BridgesOut_EvacuationRoutes This line feature class shows the most efficient routes to safety for every point in the inundation zone (on the road and trail network) assuming all non-retrofitted bridges within the inundation zone fail due to earthquake shaking. Symbolize with arrow at end, using the right arrow symbology, to see direction of line segments. This layer was created based on the Large1 (L1) tsunami scenario, which is a Local Cascadia Subduction Zone (CSZ) tsunami scenario generated by a magnitude 9.0 earthquake. The L1 event has an estimated recurrence rate of 2,500 to 3,333 years. .xml
.html
L1_BridgesOut_WalkingSpeeds_Roads This polygon feature class shows minimum evacuation speeds, in feet per second, needed to stay ahead of the wave assuming all non-retrofitted bridges within the inundation zone fail due to earthquake shaking. This feature class contains data on paved roads. A separate feature class contains data for trails and beach networks. This layer was created based on the Large1 (L1) tsunami scenario, which is a Local Cascadia Subduction Zone (CSZ) tsunami scenario generated by a magnitude 9.0 earthquake. The L1 event has an estimated recurrence rate of 2,500 to 3,333 years. .xml
.html
L1_BridgesOut_WalkingSpeeds_Trails This line feature class shows minimum evacuation speeds, in feet per second, needed to stay ahead of the wave assuming all non-retrofitted bridges within the inundation zone fail due to earthquake shaking. This feature class contains data on trails and beach networks. A separate feature class contains data for paved roads. This layer was created based on the Large1 (L1) tsunami scenario, which is a Local Cascadia Subduction Zone (CSZ) tsunami scenario generated by a magnitude 9.0 earthquake. The L1 event has an estimated recurrence rate of 2,500 to 3,333 years. .xml
.html
 
XXL1_EvacuationFlowZones This polygon feature class shows the nearest safety destination for every point in the inundation zone (on the road and trail network) assuming all non-retrofitted bridges within the inundation zone fail due to earthquake shaking. This layer was created based on the Extra-extra-large1 (XXL1) tsunami scenario, which is a Local Cascadia Subduction Zone (CSZ) tsunami scenario generated by a magnitude 9.1 earthquake. The XXL1 event has an estimated recurrence rate of at least 10,000 years. .xml
.html
XXL1_EvacuationRoutes This line feature class shows the most efficient routes to safety for every point in the inundation zone (on the road and trail network) assuming all non-retrofitted bridges within the inundation zone fail due to earthquake shaking. Symbolize with arrow at end, using the right arrow symbology, to see direction of line segments. This layer was created based on the Extra-extra-large1 (XXL1) tsunami scenario, which is a Local Cascadia Subduction Zone (CSZ) tsunami scenario generated by a magnitude 9.1 earthquake. The XXL1 event has an estimated recurrence rate of at least 10,000 years. .xml
.html
XXL1_WalkingSpeeds_Roads This polygon feature class shows minimum evacuation speeds, in feet per second, needed to stay ahead of the wave assuming all non-retrofitted bridges within the inundation zone fail due to earthquake shaking. This feature class contains data on paved roads. A separate feature class contains data for trails and beach networks. This layer was created based on the Extra-extra-large1 (XXL1) tsunami scenario, which is a Local Cascadia Subduction Zone (CSZ) tsunami scenario generated by a magnitude 9.1 earthquake. The XXL1 event has an estimated recurrence rate of at least 10,000 years. .xml
.html
XXL1_WalkingSpeeds_Trails This line feature class shows minimum evacuation speeds, in feet per second, needed to stay ahead of the wave assuming all non-retrofitted bridges within the inundation zone fail due to earthquake shaking. This feature class contains data on trails and beach networks. A separate feature class contains data for paved roads. This layer was created based on the Extra-extra-large1 (XXL1) tsunami scenario, which is a Local Cascadia Subduction Zone (CSZ) tsunami scenario generated by a magnitude 9.1 earthquake. The XXL1 event has an estimated recurrence rate of at least 10,000 years. .xml
.html