The listed tsunami source earthquake and landslide models are developed for hazard assessments of at-risk coastal communities throughout Alaska and indexed by the community names and the publications in which they are utilized.
The comprehensive publication of all models can be found here.
| Publication | Community Name(s) | Scenario Number/Model Name | Case ID |
|---|---|---|---|
| RI 2014-3 | Chenega Bay, Sawmill Bay | Scenario 1: Earthquake in the Gulf of Alaska region, repeat of the 1964 event, PDM (Plafker, 1969) | Sawmill/PDM |
| RI 2014-3 | Chenega Bay, Sawmill Bay | Scenario 2: Repeat of the 1964 Great Alaska earthquake, JDM(Johnson et al., 1996) | Sawmill/JDM |
| RI 2014-3 | Chenega Bay, Sawmill Bay | Scenario 3: Repeat of the 1964 Great Alaska earthquake, SDM(Suito and Freymueller, 2009, in review) | Sawmill/SDM |
| RI 2014-3 | Chenega Bay, Sawmill Bay | Scenario 4: Multi-segment event based on the repeat of the 1964 Great Alaska earthquake, JDM(Johnson et al., 1996) | Sawmill/JDMY |
| RI 2014-3 | Chenega Bay, Sawmill Bay | Scenario 5: Repeat of the 1964 Great Alaska earthquake, SDM(Suito and Freymueller, 2009) | Sawmill/SDMY |
| RI 2014-3 | Chenega Bay, Sawmill Bay | Scenario 6: Rupture of the Yakutat-Yakataga segment of the Aleutian megathrust(hypothetical event) | Sawmill/YY |
| RI 2014-3 | Chenega Bay, Sawmill Bay | Scenario 7: Rupture of the Kodiak Island asperity of the repeat of the 1964 Great Alaska earthquake, JDM(Johnson et al., 1996) | Sawmill/JDMK |
| RI 2014-3 | Chenega Bay, Sawmill Bay | Scenario 8: Rupture of the Kodiak Island asperity of the repeat of the 1964 Great Alaska earthquake, SDM(Suito and Freymueller, 2009, in review) | Sawmill/SDMK |
| RI 2014-3 | Chenega Bay, Sawmill Bay | Scenario 9: Earthquake in the Cascadia subduction zone along the British Columbia, Washington, Oregon and northern California shore(Geological Survey of Canada, K. Wang, written commun., 2010) | Sawmill/CAS1200 |
| RI 2014-3 | Chenega Bay, Sawmill Bay | Scenario 10: Mw9.0 earthquake in the Gulf of Alaska region: 4-18 km depth, variable slip along strike, Tohoku-type event | Sawmill/Toh |
