2480 CSZ PDF

2480 CSZ PDF

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Just before midnight on January 27, a tsunami struck the coasts of Japan without warning since no one in Japan felt the earthquake that must have caused it. This map shows where the cores are located. They learned that this geologically active region, the Cascadia Subduction Zone, not only hosts erupting volcanoes but also produces megathrust earthquakes capable of generating devastating, ocean-crossing tsunamis.

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YT link for the embedded video below. Sites where evidence of past earthquakes paleoseismology are denoted by white dots. The faults are from Chaytor et al. These turbidites are thought to have been deposited as a result of strong ground shaking from large magnitude earthquakes. More importantly, the model also shows what happens when these cxz waves strike land, the very information that PTWC needs to issue tsunami hazard guidance for impacted coastlines.

This figure, also from Wang et al. New post about The M9 Project and 3-D computer simulations on our blog! Now plants that can survive in this environment start growing again.

I here commemorate this birthday with some figures 2408 are 24800 two USGS open source professional papers. Back to top Proudly powered by WordPress. This correlation figure demonstrates how well these turbidites have been correlated. Geology Student Colloquium Rotary Silverton: Here is a version of the CSZ cross section alone Plafker, The correlations are the basis for the interpretation that these submarine landslides were triggered by Cascadia subduction zone earthquakes. These cores contain submarine landslide deposits called turbidites.


I include a yt link and embedded video and an mp4 embedded video and download […].

Contours are in meters. Brian Atwater and his colleagues have updated the Orphan Tsunami and produced a second edition available here for download and here for hard copy purchase I have a hard copy. From the beginning the animation shows all coastlines covered by colored points. This debate has resulted in a renewed interest in becoming more resilient.

Patton “earthjay” is currently living in Arcata, CA.

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This shows how a tsunami deposit may be preserved in the sediment stratigraphy following a subduction zone earthquake, like in Cascadia. This sediment has organisms within it that reflect the tidal environment. Eventually, the sediment builds up and the crust deforms interseismically until the ground surface is again above sea level. Here is the Chaytor et al. Your email address will not be published. Here is a photo I took in Alaska, where there was a subduction zone earthquake in I combined the plot above into another figure that includes all the recurrence intervals and segment lengths in a single figure.

Here is a graphic showing the sediment-stratigraphic evidence of earthquakes in Cascadia. This is modified from Goldfinger et al. There are stumps and tree snags that were rooted in the pre-earthquake soil that can be used to estimate the age of the earthquake using radiocarbon age determinations.

There are 3 panels on the left, showing times of 1 prior to earthquake, 2 several years following the earthquake, and 3 cszz after the earthquake. There are some animations on this web page showing seismicity with time along the BFZ, over the past 15 years. The Blanco fracture zone is also an active transform plate boundary. Such an earthquake would have ruptured the earth along the entire length of the km mi -long fault of the Cascadia Subduction Zone and severe shaking could have lasted for 5 minutes or longer.


This shows how the CSZ is deforming vertically today Wang et al. Here is a map from Rollins and Stein, showing their interpretations of different historic earthquakes cwz the region. This figure shows how a subduction zone deforms between interseismic and during coseismic earthquakes.

Cascadia subduction zone: years ago tonight! | Jay Patton online

Before the earthquake, the ground is sufficiently above sea level that trees can grow without fear of being inundated with salt water.

We also can see how a subduction zone generates a tsunami. Some submarine paleoseismology core sites are also shown as grey dots.

This is the timeline of prehistoric earthquakes as preserved in sediment stratigraphy in Grays Harbor and Willapa Bay, Washington. This animation shows these values through the simulated motion of the waves and as they race around the globe one can also see the distance between successive wave crests wavelength as well as their height half-amplitude indicated by their color.

I have several posts about that earthquake here and here. This map shows the various possible prehistoric earthquake rupture regions patches for the past 10, years. A 6, year earthquake history in the region of the Sumatra-Andaman Earthquake Paper 2: Is this a reasonable statement: He was most recently teaching classes at Humboldt State University, Dept. The first article summarized what we might expect from a CSZ earthquake and tsunami and the follow-up article discussed how to best prepare for this series of devastating events.

Here is an animation produced by the folks at Cal Tech following the Sumatra-Andaman subduction zone earthquake. Sometimes plants that were growing prior to the earthquake get entombed within the tsunami deposit.