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originally posted by: tigertatzen
a reply to: TrueAmerican
You know...when I read your OP, the first thing I thought of was that NZ quake. Forgive my ignorance on the subject, but when it comes to chain reactions, could a fault like that cause a chain that spreads/branches out over the whole planet, like a big crack in a piece of glass? And if yes, and it happened rapidly, would multiple tsunamis occur all over the world too?
originally posted by: TrueAmerican
Now I can speculate that if this did indeed happen all at once, the sheer size alone of that abyss is more than scary in implication. It's flat out biblical. The scale of that tsunami would be rivaled perhaps only by the one in my book, or maybe what happened in Latuya Bay in Alaska back in the 50's. Except this would dwarf that one. And considering the mega tsunami in Alaska was like some 1,200 feet high or higher, to dwarf that means a major cataclysm.
The 1958 Lituya Bay megatsunami occurred on July 9 at 22:15:58, following an earthquake with a moment magnitude of 7.8 and a maximum Mercalli Intensity of XI (Extreme). The earthquake took place on the Fairweather Fault and triggered a rockslide of 30 million cubic metres (40 million cubic yards, and about 90 million tons) to fall from several hundred metres into the narrow inlet of Lituya Bay, Alaska. The impact was heard 50 miles (80 km) away,[6] and the sudden displacement of water resulted in a megatsunami that destroyed vegetation up to 1,722 feet (525 m) above the height of the bay and a wave that traveled across the bay with a crest reported by witnesses to be on the order of 98 feet (30 m) in height.[citation needed] This is the most significant megatsunami and the largest known in modern times. The event forced a re-evaluation of large wave events, and recognition of impact, rockfall and landslide events as a previously unknown cause of very large waves.
As measured with a seismometer, an earthquake that registers 5.0 on the Richter scale has a shaking amplitude 10 times greater than an earthquake that registered 4.0 at the same distance. As energy release is generally proportional to the shaking amplitude raised to the 3/2 power, an increase of 1 magnitude corresponds to a release of energy 31.6 times that released by the lesser earthquake.[1] This means that, for instance, an earthquake of magnitude 5 releases 31.6 times as much energy as an earthquake of magnitude 4.
Magnitude 3 = 2 gigajoules
Magnitude 4 = 63 gigajoules
Magnitude 5 = 2,000 gigajoules
Magnitude 6 = 63,000 gigajoules
Magnitude 7 = 2,000,000 gigajoules
The Richter scale built on the previous, more subjective Mercalli scale by offering a quantifiable measure of an earthquake's size.[2]
originally posted by: Newt22
a reply to: crazyewok
or a water planet/Moon... I am still working on our earth getting struck by a large ball of water... Everything I see seems to point that way.
originally posted by: TrueAmerican
Now I can speculate that if this did indeed happen all at once, the sheer size alone of that abyss is more than scary in implication. It's flat out biblical. The scale of that tsunami would be rivaled perhaps only by the one in my book, or maybe what happened in Latuya Bay in Alaska back in the 50's. Except this would dwarf that one. And considering the mega tsunami in Alaska was like some 1,200 feet high or higher, to dwarf that means a major cataclysm.
Ocean Sci., 9, 147-169, 2013
www.ocean-sci.net...
doi:10.5194/os-9-147-2013
© Author(s) 2013. This work is distributed
under the Creative Commons Attribution 3.0 License.
Research article
19 Feb 2013
Observations of water masses and circulation with focus on the Eurasian Basin of the Arctic Ocean from the 1990s to the late 2000s
B. Rudels1,2, U. Schauer3, G. Björk4, M. Korhonen1,2, S. Pisarev5, B. Rabe3, and A. Wisotzki3 1Department of Physics, University of Helsinki, P.O. Box 64, 00014, Helsinki, Finland
2Finnish Meteorological Institute, Erik Palmenin aukio 1, P.O. Box 503, 00101 Helsinki, Finland
3Alfred Wegener Institute for Polar and Marine Research, P.O. Box 120161, 27515 Bremerhaven, Germany
4Department of Earth Sciences, University of Gothenburg, Box 460, 40530 Gothenburg, Sweden
5Shirshov Institute of Oceanology, 36 Nakhimovsky Prospect, Moscow 117997, Russia
Received: 05 Jul 2012 – Published in Ocean Sci. Discuss.: 08 Aug 2012
Revised: 15 Jan 2013 – Accepted: 28 Jan 2013 – Published: 19 Feb 2013
Abstract. The circulation and water mass properties in the Eurasian Basin are discussed based on a review of previous research and an examination of observations made in recent years within, or parallel to, DAMOCLES (Developing Arctic Modeling and Observational Capabilities for Long-term Environmental Studies). The discussion is strongly biased towards observations made from icebreakers and particularly from the cruise with R/V Polarstern 2007 during the International Polar Year (IPY). Focus is on the Barents Sea inflow branch and its mixing with the Fram Strait inflow branch. It is proposed that the Barents Sea branch contributes not just intermediate water but also most of the water to the Atlantic layer in the Amundsen Basin and also in the Makarov and Canada basins. Only occasionally would high temperature pulses originating from the Fram Strait branch penetrate along the Laptev Sea slope across the Gakkel Ridge into the Amundsen Basin. Interactions between the Barents Sea and the Fram Strait branches lead to formation of intrusive layers, in the Atlantic layer and in the intermediate waters. The intrusion characteristics found downstream, north of the Laptev Sea are similar to those observed in the northern Nansen Basin and over the Gakkel Ridge, suggesting a flow from the Laptev Sea towards Fram Strait. The formation mechanisms for the intrusions at the continental slope, or in the interior of the basins if they are reformed there, have not been identified. The temperature of the deep water of the Eurasian Basin has increased in the last 10 yr rather more than expected from geothermal heating. That geothermal heating does influence the deep water column was obvious from 2007 Polarstern observations made close to a hydrothermal vent in the Gakkel Ridge, where the temperature minimum usually found above the 600–800 m thick homogenous bottom layer was absent. However, heat entrained from the Atlantic water into descending, saline boundary plumes may also contribute to the warming of the deeper layers.
Citation: Rudels, B., Schauer, U., Björk, G., Korhonen, M., Pisarev, S., Rabe, B., and Wisotzki, A.: Observations of water masses and circulation with focus on the Eurasian Basin of the Arctic Ocean from the 1990s to the late 2000s, Ocean Sci., 9, 147-169, doi:10.5194/os-9-147-2013, 2013.
SCIENTISTS DISCOVER GIANT VOLCANIC ERUPTION IN ARCTIC OCEAN
By Climatologist Cliff Harris
An international team of researchers was able to provide evidence of explosive volcanism in the depths of the ice-covered Arctic Ocean for the first time. Researchers from an expedition to the Gakkel Ridge, led by the American Woods Hole Oceanographic Institution (WHOI), report in the current issue of the journal Nature that they discovered, with a specially developed camera, extensive layers of volcanic ash on the seafloor, which indicates a gigantic volcanic eruption.
"Explosive volcanic eruptions on land are nothing unusual and pose a great threat for whole areas," explains Dr Vera Schlindwein of the Alfred Wegener Institute for Polar and Marine Research in the Helmholtz Association. She participated in the expedition as a geophysicist and has been, together with her team, examining the earthquake activity of the Arctic Ocean for many years. "Mount Vesuvius in Italy erupted in 79 AD and buried thriving Pompeii under a thick layer of ash and pumice. Far away in the Arctic Ocean, at 85 degrees North and 85 degrees East, a similarly violent volcanic eruption happened, almost undetected, in 1999. In this case, however, under a water layer of 4,000 meters thickness." So far, researchers have assumed that explosive volcanism cannot happen in water depths exceeding 3 kilometers because of high ambient pressure. "These are the first pyroclastic deposits we've ever found in such deep water, at oppressive pressures that inhibit the formation of steam, and many people thought this was not possible," says Robert Reves-Sohn, staff member of the WHOI and lead scientist of the expedition carried out on the Swedish icebreaker Oden in 2007. This 1999 eruption occurred right after the peak of "global warming" in 1998.
...
Bottom water warming in the North Pacific Ocean
Masao Fukasawa1, Howard Freeland2, Ron Perkin2, Tomowo Watanabe3,5, Hiroshi Uchida1 & Ayako Nishina4
Ocean Observation and Research Department, Japan Marine Science and Technology Centre, Yokosuka, 237-0061, Japan
The Institute of Ocean Sciences, Sidney, British Columbia, V8L 4B2, Canada
Far-fisheries Laboratory, Japan Fisheries Agency, Shimizu, 424-8633, Japan
Faculty of Fisheries, Kagoshima University, Kagoshima, 890-0056, Japan
Present address: Central Fisheries Laboratory, Japan Fisheries Agency, Japan
Correspondence to: Masao Fukasawa1Howard Freeland2 Email: [email protected]
Email: [email protected]
Top of page
Abstract
Observations of changes in the properties of ocean waters have been restricted to surface1 or intermediate-depth waters2, 3, because the detection of change in bottom water is extremely difficult owing to the small magnitude of the expected signals. Nevertheless, temporal changes in the properties of such deep waters across an ocean basin are of particular interest, as they can be used to constrain the transport of water at the bottom of the ocean and to detect changes in the global thermohaline circulation. Here we present a comparison of a trans-Pacific survey completed in 1985 (refs 4, 5) and its repetition in 1999 (ref. 6). We find that the deepest waters of the North Pacific Ocean have warmed significantly across the entire width of the ocean basin. Our observations imply that changes in water properties are now detectable in water masses that have long been insulated from heat exchange with the atmosphere.
So now the question is if this happened all at once, or if it ripped apart over thousands of years. And from the sounds of it, it seems it happened at once.
Now I can speculate that if this did indeed happen all at once, the sheer size alone of that abyss is more than scary in implication. It's flat out biblical.
originally posted by: ElectricUniverse
...
In 1999 there was a powerful volcanic explosion, similar to the Vesuvious explosion, which occurred at 4,000 km underwater on the Gakkel ridge, Arctic Ocean. This was previously thought to be impossible, and they are thought to be rare.
...