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• W2018207908 abstract "Geomorphologic analysis of submarine and subaerial surface features using a combined topographic/bathymetric digital elevation model coupled with onshore geological and geophysical data constrain the age and geometry of giant landslides affecting the north flank of Tenerife. Shaded relief and contour maps, and topographic profiles of the submarine north flank, permit the identification of two generations of post-shield landslides. Older landslide materials accumulated near the shore (<40-km) and comprise ∼700 km3 of debris. Thickening towards a prominent axis suggests one major landslide deposit. Younger landslide materials accumulated 40–70 km offshore and comprise the products of three major landslides: the La Orotava landslide complex, the Icod landslide and the East Dorsal landslide complex, each with an onshore scar, a proximal submarine trough, and a distal deposit lobe. Estimated lobe volumes are 80, 80 and 100 km3, respectively. The old post-shield landslide scar is an amphitheatre, 20–25 km wide, partly submarine, now completely filled with younger materials. Age–width relationships for Tenerife's coastal platform plus onshore geological constraints suggest an age of ca. 3 Ma for the old collapse. Young landslides are all less than 560 ka old. The La Orotava and Icod slides involved failures of slabs of subaerial flank to form the subaerial La Orotava and Icod valleys. Offshore, they excavated troughs by sudden loading and basal erosion of older slide debris. The onshore East Dorsal slide also triggered secondary failure of older debris offshore. The slab-like geometry of young failures was controlled by weak layers, deep drainage channels and flank truncation by marine erosion. The (partly) submarine geometry of the older amphitheatre reflects the absence of these features. Relatively low H/L ratios for the young slides are attributed to filling of the slope break at the base of the submarine edifice by old landslide materials, low aspect ratios of the failed slabs and channelling within troughs. Post-shield landslides on Tenerife correlate with major falls in sea level, reflecting increased rates of volcanism and coastal erosion, and reduced support for the flank. Landslide head zones have strongly influenced the pattern of volcanism on Tenerife, providing sites for major volcanic centres." @default.
• W2018207908 created "2016-06-24" @default.
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• W2018207908 date "2000-12-01" @default.
• W2018207908 modified "2023-10-06" @default.
• W2018207908 title "Evolution of the north flank of Tenerife by recurrent giant landslides" @default.
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• W2018207908 cites W1984458293 @default.
• W2018207908 cites W1985011582 @default.
• W2018207908 cites W1985693541 @default.
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• W2018207908 cites W1994977293 @default.
• W2018207908 cites W1995440282 @default.
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• W2018207908 cites W2007289985 @default.
• W2018207908 cites W2011564699 @default.
• W2018207908 cites W2016020657 @default.
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• W2018207908 cites W2024466496 @default.
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• W2018207908 cites W2069724782 @default.
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• W2018207908 cites W2076176221 @default.
• W2018207908 cites W2077906973 @default.
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• W2018207908 doi "https://doi.org/10.1016/s0377-0273(00)00220-1" @default.
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