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The MARGINS Program “To understand the complex interplay of processes that govern the evolution of continental margins”
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MARGINS has four themes: Rupturing Continental Lithosphere, Seismogenic Zone, Subduction Factory, and SOURCE TO SINK
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Writing Earth history with continental- margin sedimentary processes WRITING EARTH HISTORY WITH CONTINENTAL-MARGIN SEDIMENTARY PROCESSES
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Jantang, Sumatra Courtesy of H. Higman
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Photo: Brian Atwater Courtesy of Brian Atwater
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41 o 00’ 40 o 50’ 40 o 40’ 124 o 40’ 124 o 30’ 7 0 0 6 0 0 5 0 0 4 0 0 3 5 0 3 0 0 2 5 0 2 0 0 1 5 0 1 0 0 9 0 8 0 7 0 6 0 5 0 4 0 3 0 2 0 1 0 Eel River Drainage Basin ~9000 km 2 Study Area 0 m 350 1400 Elevation California Eel margin
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Courtesy of Jeff Borgeld
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Wheatcroft and Borgeld, 2000
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Fingerprint of Flood Sedimentation on the Eel Shelf (Sommerfield et al., 1999)
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Sommerfield et al., 2007
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S 60 Location of observations in Eel Canyon
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Eel Canyon Morphology Complex channel shape makes placement of sediment cores difficult
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( Mullenbach and Nittrouer, in 2004) Sedimentary fingerprints indicates that flood sediments are entering submarine canyon
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Southeast Alaska Coast Sediment supplied from glacier-fed rivers Courtesy of John Jaeger
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Surge events from Bering Glacier recorded on adjacent shelf Courtesy of John Jaeger
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Courtesy of Peter Harris
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Modern Coastal Rivers Courtesy of Bill Dietrich Obo
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From Lui et al. (2003)
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NORTHERN ADRIATIC SEA Po River ITALY CROATIA Ancona Promontory Gargano Peninsula Apennine Mountains Venice Lagoon
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abandonment of Po di Primaro 1152 AD a major natural avulsion northward shifting of distributary channels Venice Republic is threatened by the potential infilling of the lagoon 1604 AD digging of a diversionary canal (Taglio di porto Viro) The artificial form of the modern delta
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NORTHERN ADRIATIC SEA Po River ITALY CROATIA Ancona Promontory Gargano Peninsula Apennine Mountains Venice Lagoon
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History of Apennine sediment discharge Excess 210 Pb Activity (dpm/g) 0 50 100 150 200 250 1.010.0 Supported = 0.7 0.1 11.2 mm/y R 2 = 0.72 15.0 mm/y R 2 = 0.97 7.80 mm/y R 2 = 0.89 Tronto River 9.7 mm/y 3.2 mm/y Eel RiverSangro River 0 50 100 150 200 250 1.010.0 Excess 210 Pb Activity (dpm/g) 0.1 10.2 mm/y R 2 = 0.68 15.4 mm/y R 2 = 0.96 6.58 mm/y R 2 = 0.97 (KS02-30)(KS02-355) Dams reduce sediment accumulation in Adriatic Sea
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Clearcutting increases sediment load Dams reduce sediment load DAMS WIN
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Sediment source for southern WA coast beaches Dams placed on Columbia River during 20 th century likely trapped much sediment Greatest impact reached the coast in ~1980, after lower river was flushed
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Ocean waves and currents transport sediment northward, distributing it along beach and continental shelf Coast of Washington State Southwest Washington Erosion Study
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Changes in Wave Climate (Allan and Komar, 2001)
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Coastal erosion has caused loss of structures and roads And has led to hardening of the shoreline in some places
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Mississippi Delta Historically has provided coastal protection to New Orleans Bird-foot delta Sedimentation extends to shelf break
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List of some things we did Dammed river – reduced sediment supply, 400 million t/y to 200 t/y Built artificial levees – reduced nourishment of flood plain Prevented lobe switching – reduced sediment supply to other parts of delta plain (30% to Atchafalaya) Constrained flow to modern delta – caused delta to build to shelf break, and lose sediment to continental slope Removed water and natural gas – accelerated consolidation of deltaic sediment and subsidence of land surface Dredged channels – created depressions that act as sediment traps and water conduits
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Writing Earth history with continental- margin sedimentary processes IF WE DON’T LEARN FROM HISTORY, WE’RE DOOMED TO RELIVE IT
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Trees are ripped out of hills to an elevation of >30 m by the tsunami in Sumatra (just south of Lho Nga) Courtesy of H. Higman
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Tsunami transported bridge at Jantang, Aceh (Sumatra)
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2/27/99
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