The report reviews ancient geological processes that created Oregon's coast, then uses previous research to provide context for the most recent data gathered about earthquakes, tsunamis, tides, erosion, wave runup, overtopping, and floods. Wonderful color graphics - photographs (including aerials), charts, diagrams and maps - help explain the detailed analysis. Much of it is still beyond my understanding, but I didn't see anything that conflicts with Pre-historic Geomorphology of Bayocean Peninsula and Changes in Bayocean Beaches Studied by DOGAMI; most likely because the study's lead author, Jonathan Allan, was kind enough to give me feedback while writing them.
The jetty built on the north side of Tillamook Bay's inlet is blamed for Bayocean's eventual destruction. The report provides specific distances and rates of erosion post starting on page 36. After the south jetty was finished in 1979, the shoreline started to grow. These two maps depict shoreline changes across the last century. Other diagrams depicting these changes in different ways are at Bayocean Shoreline Changes Over Time and Oregon Coastal Atlas.
|Shoreline changes at north end of Bayocean Spit (page 37)|
|Shoreline changes at south end of Bayocean Spit (page 39)|
The report listed 128' as the height of the highest dune measured on Bayocean. This concerned me because I'd reported hiking to 152' back in January. So I contacted Allan. He clarified that they measured the dune closest to each transect, not older ones farther from the beach. His Lidar map showed the highest point on Bayocean to be approximately 153'. Close enough.