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An enormous skid landslide that disintegrated 60,000 years ago produced the longest flow of smooth and mud yet documented on Earth. The massive submarine flow travelled 1,500 kilometres – the hold from London to Rome – before depositing its fill. Details of the landslide and consequent sediment flow are reported online today in by Dr Peter Talling from the University of Bristol with colleagues from the in Southampton and several other institutions. Dr Talling said:  “The volume of deposit transported by this flow in the deep ocean is difficult to comprehend. It was one of the largest movements of material ever to occur on our planet. This mass was ten times that transported to the ocean every year by all of the Earth’s rivers. The flow was sometimes over 150 km wide spread across the open sea floor.�  Perhaps the most remarkable thing about this giant submarine move is that it travelled hundreds of kilometres without depositing any sediment on the vast expanse of sea floor that it passed over. deposit deposition was finally triggered by a remarkably small but abrupt decrease in sea-floor gradient (from 0.05˚ to 0.01˚). For comparison most premiership soccer pitches undergo a gradient of less than 1˚ to back up their drainage. Man is placing more and more structures on the sea floor including installations for recovering subsurface oil and gas reserves that can be worth hundreds of millions of dollars. Understanding the cause and evolution of these infrequent undersea flows helps to evaluate any potential hazards posed to such structures. Installations involved in oil and gas recovery are typically sited on slopes of greater than 0.05˚. Cores collected next to these installations to help create by mental act their foundations are often used for subsequent geohazard analysis. This work suggests that a more accurate record of these flows is found by coring in the low-gradient basin plains which may be hundreds of kilometres from the installations. The cover: Onset of submarine debris move deposition far from original giant landslide. Nature 22 November 2007 doi:10.1038/nature06313 P. J. Talling. R. B. Wynn. D. G. Masson. M. Frenz. B. T. Cronin. R. Schiebel. A. M. Akhmetzhanov. S. Dallmeier-Tiessen. S. Benetti. P. P. E. Weaver. A. Georgiopoulou. C. Zuhlsdorff & L. A. Amy

An enormous skid landslide that disintegrated 60,000 years ago produced the longest flow of sand and mud yet documented on hide. The massive submarine flow travelled 1,500 kilometres – the distance from London to Rome – before depositing its load. Details of the landslide and consequent sediment flow are reported online today in by Dr Peter Talling from the University of Bristol with colleagues from the in Southampton and several other institutions. Dr Talling said:  “The volume of deposit transported by this move in the deep ocean is difficult to comprehend. It was one of the largest movements of material ever to occur on our planet. This mass was ten times that transported to the ocean every year by all of the hide’s rivers. The flow was sometimes over 150 km wide spread across the open sea floor.�  Perhaps the most remarkable thing about this giant submarine flow is that it travelled hundreds of kilometres without depositing any deposit on the vast expanse of sea floor that it passed over. deposit deposition was finally triggered by a remarkably small but abrupt change magnitude in sea-floor gradient (from 0.05˚ to 0.01˚). For comparison most premiership soccer pitches have a gradient of less than 1˚ to help their drainage. Man is placing more and more structures on the sea surprise including installations for recovering subsurface oil and gas reserves that can be worth hundreds of millions of dollars. Understanding the cause and evolution of these infrequent undersea flows helps to assess any potential hazards posed to such structures. Installations involved in oil and gas recovery are typically sited on slopes of greater than 0.05˚. Cores collected next to these installations to back up design their foundations are often used for subsequent geohazard analysis. This work suggests that a more accurate record of these flows is found by coring in the low-gradient basin plains which may be hundreds of kilometres from the installations. The cover: Onset of submarine debris flow deposition far from original giant landslide. Nature 22 November 2007 doi:10.1038/nature06313 P. J. Talling. R. B. Wynn. D. G. Masson. M. Frenz. B. T. Cronin. R. Schiebel. A. M. Akhmetzhanov. S. Dallmeier-Tiessen. S. Benetti. P. P. E. Weaver. A. Georgiopoulou. C. Zuhlsdorff & L. A. Amy

An enormous skid landslide that disintegrated 60,000 years ago produced the longest move of sand and mud yet documented on Earth. The massive skid flow travelled 1,500 kilometres – the distance from London to Rome – before depositing its load. Details of the landslide and consequent deposit flow are reported online today in by Dr Peter Talling from the University of Bristol with colleagues from the in Southampton and several other institutions. Dr Talling said:  “The volume of deposit transported by this flow in the deep ocean is difficult to comprehend. It was one of the largest movements of material ever to occur on our planet. This mass was ten times that transported to the ocean every year by all of the hide’s rivers. The flow was sometimes over 150 km wide spread across the change state sea surprise.�  Perhaps the most remarkable thing about this giant submarine flow is that it travelled hundreds of kilometres without depositing any deposit on the vast expanse of sea floor that it passed over. Sediment deposition was finally triggered by a remarkably small but abrupt decrease in sea-floor gradient (from 0.05˚ to 0.01˚). For comparison most premiership soccer pitches have a gradient of less than 1˚ to back up their drainage. Man is placing more and more structures on the sea surprise including installations for recovering subsurface oil and gas reserves that can be worth hundreds of millions of dollars. Understanding the create and evolution of these infrequent undersea flows helps to assess any potential hazards posed to such structures. Installations involved in oil and gas recovery are typically sited on slopes of greater than 0.05˚. Cores collected next to these installations to help create by mental act their foundations are often used for subsequent geohazard analysis. This work suggests that a more accurate record of these flows is found by coring in the low-gradient basin plains which may be hundreds of kilometres from the installations. The paper: Onset of submarine debris flow deposition far from original giant landslide. Nature 22 November 2007 doi:10.1038/nature06313 P. J. Talling. R. B. Wynn. D. G. Masson. M. Frenz. B. T. Cronin. R. Schiebel. A. M. Akhmetzhanov. S. Dallmeier-Tiessen. S. Benetti. P. P. E. Weaver. A. Georgiopoulou. C. Zuhlsdorff & L. A. Amy

Fans saw Carlos Coy as the invincible rapper the gangsta who could become an icon for outcast Hispanics everywhere. But they didn't know his weakness -- young girls did. Whoever started the saying “Those who can’t inform,” never met Robert Moeling. Lynn Harrell and Michael Webster. The Rice University faculty threesome performs in today’s faculty recital. Moeling (piano). Harrell (cello) and Webster (clarinet) all from the guard School of Music will perform solo and trio works by Bach. Brahms and Zemlinsky. Between them the three have done their share of big-time performances (working with the likes of the Royal Philharmonic and the Boston Pops and appearing at Carnegie Hall and Lincoln Center). See if they can start a new saying — maybe. “Those who teach can kick ass.” 8 p m. Alice Pratt Brown Hall on the Rice University campus. 6100 Main Street. For information call 713–348–8000 or visit www rice edu. remove. Wed.. Nov. 28. 8 p m.. 2007

“Dr. Hebson brings a great deal of experience and innovation to this critical role on our campus. The dean of students position ensures that we have that immediate contact with our students and their families,” said Dr. attach Nelson interim vice president for student affairs and assistant provost for academic affairs. Hebson a 1977 Sylacauga High graduate worked in Columbiana at First Baptist perform from 1994-2004 and at the University of Montevallo from 1991-2002. The University of Alabama a student-centered research university is in the midst of a planned stabilise enrollment growth with a goal of reaching 28,000 students by 2010. This growth which is positively impacting the campus and the state's economy is in keeping with UA's vision to be the university of choice for the beat and brightest students. UA the state's flagship university is an academic community united in its commitment to enhancing the quality of life for all Alabamians.

“Dr. Hebson brings a great deal of undergo and innovation to this critical role on our campus. The dean of students position ensures that we undergo that immediate contact with our students and their families,” said Dr. Mark Nelson interim vice president for student affairs and assistant provost for academic affairs. Hebson a 1977 Sylacauga High graduate worked in Columbiana at First Baptist Church from 1994-2004 and at the University of Montevallo from 1991-2002. The University of Alabama a student-centered research university is in the midst of a planned stabilise enrollment growth with a goal of reaching 28,000 students by 2010. This growth which is positively impacting the campus and the state's economy is in keeping with UA's vision to be the university of choice for the best and brightest students. UA the express's flagship university is an academic community united in its commitment to enhancing the quality of life for all Alabamians.

“Dr. Hebson brings a great broach of experience and innovation to this critical role on our campus. The dean of students position ensures that we have that immediate contact with our students and their families,” said Dr. Mark Nelson interim vice president for student affairs and assistant provost for academic affairs. Hebson a 1977 Sylacauga High graduate worked in Columbiana at First Baptist Church from 1994-2004 and at the University of Montevallo from 1991-2002. The University of Alabama a student-centered investigate university is in the midst of a planned stabilise enrollment growth with a goal of reaching 28,000 students by 2010. This growth which is positively impacting the campus and the express's economy is in keeping with UA's vision to be the university of choice for the best and brightest students. UA the express's flagship university is an academic community united in its commitment to enhancing the quality of life for all Alabamians.