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The same topography that leads to the heavy tidal currents at the entrance also created the highest wave from a tsunami ever recorded anywhere in the world. An earthquake caused a landslide in the Gilbert Inlet at the head of the bay on July 9, 1958, generating a massive mega-tsunami measuring 1,720 feet high. The wave stripped trees and soil from the opposite headland and consumed the entire bay. There were three fishing boats anchored near the entrance of Lituya Bay on the day the giant waves occurred. One boat sank and the two people on board lost their lives. The other two boats were able to ride the waves. When the wave reached the open sea it dissipated quickly.
The giant wave run-up of 1720 feet at the head of the Bay and the subsequent huge wave along the main body of Lituya Bay were caused primarily by an enormous rockfall into Gilbert Inlet at the head of Lituya Bay, triggered by an earthquake. The large mass of rock impacted the bottom of the inlet with great force. The displaced water and the folding of sediments broke and uplifted 1300 feet of ice along the entire front of the Lituya Glacier and the impact resulted in water splashing action that reached the 1720 foot elevation on the other side of the inlet.
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Artist's view of 1958 earthquake triggered rock slide into Gilbert Inlet Heller,V, Hager, W,: Impulse product parameter in landslide generated impulse waves, J. Waterw. Port C-ASCE 2010. |
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Photo of Lituya Bay the day after the wave. This and below photos were captured by USFS Officer Miller. |
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Denuded peninsula forming west wall of Gilbert Inlet and rock slide that filled most of the Inlet. |
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View looking northeast across Lituya Bay towards Gilbert Inlet. |
A recent geologic study has determined that slides and tsunamis have been rather frequent in Lituya Bay. Approximately every 30 years since about 1860 a slide, and possibly a tsunami, has occurred. This pattern stopped after the 1958 slide, so many believe another slide, and tsunami are overdue. So with those facts in hand, we decided to anchor on the east side of Centotaph Island last night, the anchorage of one of the surviving boats form the 1958 slide.
But today's cruise sort of explains why a recent slide may not cause another tsunami. The head of Lituya Bay has filled in with slide material. There is no water or ice to displace anymore, and thus no tsunami. Thankyou Dr. Benson, nice work.
But today's cruise sort of explains why a recent slide may not cause another tsunami. The head of Lituya Bay has filled in with slide material. There is no water or ice to displace anymore, and thus no tsunami. Thankyou Dr. Benson, nice work.
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More research is needed so an expedition party is organized and managed by Ground Captain Gerard. Four crew take the tender ashore for the assault of the Cascade Glacier, or it's waterfall. It's a rough 2-hour, uphill trek but the expedition succeeds and photographs record their findings.
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At last it's dinner time. Let's see what should we have with our halibut. How about fresh prawns? We cook them for just four minutes only as per the Karen Almas recipe. What an awesome sweet flavor!
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Interesting idea re: why there haven't been any giant waves in Lituya since '58, even though we're supposedly long overdue for one by the historical record. The satellite photos of Lituya on Google Maps support that the inlets have been filled beyond what the charts show. On the other hand, Don Miller's USGS study of the '58 wave suggested that the areas prone to landslides in Lituya Bay extend beyond just the inlets; see http://www.uwsp.edu/geo/projects/geoweb/participants/Dutch/LituyaBay/Lituya8.HTM
ReplyDeleteMy amateur guess would be there's still the possibility of future waves, but its much reduced from what it was before '58.
Great photos, thanks again for sharing them!