2480 CSZ PDF


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These cores contain submarine landslide deposits called turbidites. There are some animations on this web page showing seismicity with time along the BFZ, over the past 15 years. The two main spreading ridges are not labeled, but the northern one is the Juan de Fuca ridge where oceanic crust is formed for the Juan de Fuca plate and the southern one is the Gorda rise where the oceanic crust is formed for the Gorda plate.

I combined the plot above into another figure that includes all the recurrence intervals and segment lengths in a single figure. A 6, year earthquake history in the region of the Sumatra-Andaman Earthquake Paper 2: The Atwater et al.

Leave a Reply Cancel reply Your email address will not be published. This figure shows how a subduction zone deforms between interseismic and during coseismic earthquakes. Here is a graphic showing the sediment-stratigraphic evidence of earthquakes in Cascadia.

These turbidites are thought to have been deposited as a result of strong ground shaking from large magnitude earthquakes. Some submarine paleoseismology core sites are also shown as grey dots.

Black dots on the map show sites where evidence for coseismic subsidence has been found in coastal marshes, lakes, and estuaries. This debate has resulted in a renewed interest in becoming cwz resilient.

Here is a map from Rollins and Stein, showing their interpretations of different historic earthquakes in the region. 24880 should have said locally… there are extensive uplifted dunes in oregon….

He was most recently teaching classes at Humboldt State University, Dept.


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

How do we know about Cascadia ‘s ancient earthquakes? By comparing the tree rings of dead trees with those still living they could tell when the last of 248 great earthquakes struck the region. Following the earthquake, tidal sediment is deposited above the tsunami transported sediment. That much motion over such a large area requires a very large earthquake to explain it—perhaps as large as 9. New post about The M9 Project and 3-D computer simulations on our blog! The Blanco fracture zone is also an active transform cxz boundary.

During the earthquake, the ground subsides lowers so that the area is now inundated during high tides.

This animation shows these values through the simulated motion of the waves and as they race around the 280 one can also see the distance between successive wave crests wavelength as well as their height half-amplitude indicated by their color. From the beginning the animation cz all coastlines covered by colored points. We also can see how a subduction zone generates a tsunami. Before the earthquake, the ground is sufficiently above sea level that trees can grow without fear of being inundated with salt water.

Here is a map of the Cascadia subduction zone, modified from Nelson et al. Patton “earthjay” is currently living in Arcata, CA. These paleoseismology sites are labeled e.


Most notably was a pair of articles that were published in the New Yorker magazine, xsz by Kathryn Shulz. This sediment has organisms within it that reflect the tidal environment.

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. Eventually, the sediment builds up and the crust deforms interseismically until the ground surface is again above sea level. The Cdz Tsunami Warning Center PTWC can create an animation of a historical tsunami like this one using the same csa that they use for determining tsunami hazard in real time for any tsunami today: On this evening, years ago, the Cascadia subduction zone fault ruptured as a margin wide earthquake.


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Here is an animation produced by the folks at Cal Tech following the Sumatra-Andaman subduction zone earthquake. Now plants that can survive in this environment start growing again. Tidal sediment like mud starts to be deposited above the pre-earthquake ground surface. I summarized the regional tectonics of the Cascadia subduction zone recently here.

These are initially a blue color like the undisturbed ocean to indicate normal sea level, but as the tsunami waves reach them they will change color to represent the height of the waves coming ashore, and often these values are higher than they were in the deeper waters offshore. Back to top Proudly powered by WordPress. I have several posts about that earthquake here and here.

This site uses Akismet to reduce spam. Here is a photo I took cwz Alaska, where there was a subduction zone earthquake cszz This was published in response to the Januray Gorda plate earthquake. This figure shows the regions that participate in this interseismic and coseismic deformation at Cascadia.

If there 2408 a source of sediment to be transported by a tsunami, it will come along for the ride and possibly be deposited upon the pre-earthquake ground surface. This shows how a tsunami vsz may be preserved in the sediment stratigraphy following a subduction zone earthquake, like in Cascadia. Your email address will not be published.

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I include a yt link and embedded video and an mp4 embedded video and download […]. Is this a reasonable statement: Since last years commemoration, there have been a few additions.

YT link for the embedded video below.

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