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When large chunks of mountains or volcanoes slide into the ocean that is a Mega-tsunami that will be very very huge and there are many places around the world where this will happen eventually. Temperature or sea-level has little to no impact on the rock buried within the mountain.
Recent numerical modeling studies, forecasting mega tsunami generation from postulated, massive slope failures of Cumbre Vieja in La Palma, Canary Islands, and Kilauea, in Hawaii, have been based on incorrect assumptions of volcanic island slope instability, source dimensions, speed of failure and tsunami coupling mechanisms. Incorrect input parameters and treatment of wave energy propagation and dispersion, have led to overestimates of tsunami far field effects. Inappropriate media attention and publicity to such probabilistic results have created unnecessary anxiety that mega tsunamis may be imminent and may devastate densely populated coastlines at locations distant from the source - in both the Atlantic and Pacific Oceans.
Similarly, there is evidence that major landslides have occurred in the Hawaiian islands in the past. The Kilauea volcano on the island of Hawaii was identified as another site where a major flank collapse would generate a mega tsunami (Ward, 2001). Although no specific time frame for these postulated collapses has been provided, it was inferred that they could be induced by the next volcanic eruption of Cumbre Vieja on La Palma, or by the next major earthquake near the Kilauea volcano in Hawaii.
And here is another link, this one describes how Massive flank failures of island stratovolcanoes are extremely rare phenomena and none have occurred within recorded history.
On November 29, 1975, a 37 mile (60 km) wide section of the Hilina Slump plunged 11 feet (3 m) into the ocean, widening the crack by 26 feet (7.9 m). This movement caused a 7.2 magnitude earthquake and a 48 foot (15 m) high tsunami. Oceanfront properties were washed off their foundations in Punaluu. Two deaths were reported at Halape, and 19 other persons were injured.
On April 2, 1868, an earthquake in this area with a magnitude estimated between 7.25 and 7.75 rocked the southeast coast of Hawaii. It triggered a landslide on the slopes of the Mauna Loa volcano, five miles (8 km) north of Pahala, killing 31 persons. A tsunami claimed 46 additional lives.
Originally posted by flyingfish
reply to post by kro32
There are indeed, however this slump could devastate the entire U.S. pacific coast and no one seems to know about it.
It just doesn’t seem like a reasonable response... a tsunami of that size from a small slither of land.. comparatively speaking. The amount of land that moved for the Indonesian quake, or Japanese quake feels like it would dwarf that Hawaiian slither.. both quakes were large plates tilting, where as this is just land sliding into the ocean... ... i mean if you drop a rock in a bucket you get a fast splash and small ripples.. . if you tip the bucket sideways you get massive amounts of water shifting.
Originally posted by sdebunker
And its number 5 on the most dangerous volcano decade list"
Avachinsky-Koryaksky, Kamchatka
Colima Volcano, Mexico
Mount Etna, Italy
Galeras Volcano, Colombia
Mauna Loa, Hawaii
Merapi Volcano, Indonesia
Niragongo Volcano, Democratic Republic of the Congo
Mount Rainier, Washington
Sakurajima Volcano, Japan
Santa Maria/Santiaguito Volcano, Guatemala
Santorini Volcano, Greece
Taal Volcano, Philippines
Teide Volcano, Canary Islands, Spain
Ulawun Volcano, Papua New Guinea
Unzen Volcano, Japan
Vesuvius Volcano, Italy
USGS
Originally posted by flyingfish
reply to post by kro32
Derek Elsworth has done some interesting research on the role of interior fluid pressures in triggering collapse.
link
link
His research proves that water pressure in volcano's causes instability for landslides.
Introduction: Introduction There is a remote possibility that Kilauea volcano’s south flank will slump into the ocean and trigger a massive tsunami that would devastate coastlines around the Pacific. While there are no tsunamis of that magnitude on record, there is scientific evidence that supports these massive landslides and subsequent gigantic tsunamis in the Pacific within the past 100,000 to 200,000 years
The photos above were taken months apart and are a great example of the instability of the volcanic land. The photo on the left was taken in May of 2007 shortly after a small chunk of bench collapsed and it also shows the “shattering ring” that has developed. The photo on the right was taken August 17, 2007. Note that it is unclear why the shelf fell but it is believed that the M5.4 earthquake or high surf from hurricane Flossie could have been contributing factors. Photos courtesy of USGS East Lae'apuki Bench Collapse