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Massive earthquakes are no more likely today than they were a century ago, despite an apparent rise of the devastating temblors in recent years, US researchers said on Monday.
The deadly 9.0 earthquake this year in Japan, an 8.8 quake in Chile last year and the 2004 Sumatra-Andaman earthquake that registered 9.0 on the moment magnitude scale have raised alarm in some science and media circles that such events may be linked.
But researchers at the University of California went back over the world’s earthquake records dating back to 1900 and found over time there was no statistically significant rise in the number of big quakes 7.0 and higher.
Originally posted by TrueAmerican
It just appears to go through cycles of increased activity, then diminished activity.
If we are on the upside of increased activity, then wouldn't that technically mean earthquakes are increasing?
If they only went back to 1900, then how do we know the cycle does not increase activity far more, say every 300 years?
We know from the earths landscape that there has been some very extreme sudden earth movements. Could they be cyclic, thousands, if not millions of years apart?
Does this study really rule out peoples fears?
The ice is melting so fast in Greenland that the giant island is rising noticeably as the weight is lifted. In some spots, the land is rising 1 inch per year. A vast ice cap covers much of Greenland, in some places up to 1.2 miles (2 km) thick. The ice, in place for eons, presses down the land, making the elevation at any given point lower than it would be sans ice. Scientists have documented on Greenland and elsewhere that when longstanding ice melts away, the land rebounds. Even the European Alps are rising as glaciers melt. Now, scientists at the University of Miami say Greenland's ice is melting so quickly that the land underneath is rising at an accelerated pace.
According to the theory of plate tectonics, plate-plate interaction results in earthquakes near plate boundaries. However, large earthquakes are found in intraplate environment like eastern Canada (up to M7) and northern Europe (up to M5) which are far away from present-day plate boundaries. An important intraplate earthquake was the magnitude 8 New Madrid earthquake that occurred in mid-continental USA in the year 1811. Glacial loads have provided more than 30 MPa of vertical stress in northern Canada and more than 20 MPa in northern Europe during glacial maximum. This vertical stress is supported by the mantle and the flexure of the lithosphere. Since the mantle and the lithosphere continuously respond to the changing ice and water loads, the state of stress at any location continuously changes in time. The changes in the orientation of the state of stress is recorded in the postglacial faults in southeastern Canada.[18] When the postglacial faults formed at the end of deglaciation 9000 years ago, the horizontal principal stress orientation was almost perpendicular to the former ice margin, but today the orientation is in the northeast-southwest, along the direction of seafloor spreading at the Mid-Atlantic Ridge. This shows that the stress due to postglacial rebound had played an important role at deglacial time, but has gradually relaxed so that tectonic stress has become more dominant today. According to the Mohr–Coulomb theory of rock failure, large glacial loads generally suppress earthquakes, but rapid deglaciation promotes earthquakes. According to Wu & Hasagawa, the rebound stress that is available to trigger earthquakes today is of the order of 1 MPa.[19] This stress level is not large enough to rupture intact rocks but is large enough to reactivate pre-existing faults that are close to failure. Thus, both postglacial rebound and past tectonics play important roles in today's intraplate earthquakes in eastern Canada and southeast USA. Generally postglacial rebound stress could have triggered the intraplate earthquakes in eastern Canada and may have played some role in triggering earthquakes in eastern USA including the New Madrid earthquakes of 1811.[5] The situation in northern Europe today is complicated by the current tectonic activities nearby and by coastal loading and weakening.
Originally posted by TrueAmerican
reply to post by kdog1982
@PM: You're welcome.
kdog, that's a very interesting theory, but how are they going to prove the New Madrid quakes were caused by this rebound stress? Everything I've read is about the known fault there. And so they mention the land rebound, but are they documenting more quakes because of it than usual in Greenland?
But if so, maybe the Yellowstone quake of 1959 could have been same? And what about Alaska 1964? I dunno man. An awful lot of big quakes have happened on interplate faults- some might be due to it, but most are likely just faulting and stress releases from plate movements.
To understand how glacial isostatic adjustment affects Earth's rotation rate, we note that the movement of mass on and beneath the Earth's surface affects the moment of inertia of the Earth; by the conservation of angular momentum, the rotational motion must also change. This is illustrated by a rotating ice skater: as she extends her arms above her head, her moment of inertia decreases, and she spins faster. On the other hand, as she extends her arms horizontally, her moment of inertia increases and her spin slows.
According to the Mohr–Coulomb theory of rock failure, large glacial loads generally suppress earthquakes, but rapid deglaciation promotes earthquakes. According to Wu & Hasagawa, the rebound stress that is available to trigger earthquakes today is of the order of 1 MPa.[19] This stress level is not large enough to rupture intact rocks but is large enough to reactivate pre-existing faults that are close to failure. Thus, both postglacial rebound and past tectonics play important roles in today's intraplate earthquakes in eastern Canada and southeast USA. Generally postglacial rebound stress could have triggered the intraplate earthquakes in eastern Canada and may have played some role in triggering earthquakes in eastern USA including the New Madrid earthquakes of 1811.[5] The situation in northern Europe today is complicated by the current tectonic activities nearby and by coastal loading and weakening.
Originally posted by PuterMan
Second, it is my firm belief that the 'increase' peaked with Japan and we are going down the down slope.
Originally posted by ANOK
Originally posted by PuterMan
Second, it is my firm belief that the 'increase' peaked with Japan and we are going down the down slope.
I hope you are right. Thanx for the reply.
Whatever happens it's a waste of energy worrying about it I guess, not much we can do. It's just one of many ways to hasten our demise.
The estimated global rate of very large (M >9) earthquakes is still very uncertain because only five such events have occurred since 1900. The recent elevated rate of large earthquakes has increased estimates of large earthquake danger: The empirical rate of such events is higher than before. However, there is no evidence that the rate of the underlying process has changed. In other words, there is no evidence that the risk has changed, but our estimates of the risk have changed.