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Showing 1 to 4 of 4 for “"hyperconcentrated flow"”.
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The sedimentology of coarse grained hyperconcentrated flow deposits within modern and ancient volcaniclastic and alluvial fan sequences
… A. in 1984, triggered the formation of a debris flow in the headwaters of the North Fork Toutle River. As the debris flow progressed downstream it transformed through the incorporation of water and the loss of sediment and within 34 kilometres became a muddy flood. The deposits produced by the …
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Ephemeral river systems at the Skeleton Coast, NW-Namibia - Sedimentological and geomorphological studies on the braided river dominated Koigab Fan, the Cenozoic succession in the Uniabmond area and comparative studies on fluvio-aeolian interaction between ephemeral rivers and the Skeleton Coast Erg
… comprising several ephemeral rivers, which flow west-southwest towards the Atlantic Ocean. The area is hyper-arid with less than 50 mm average annual rainfall and a rainfall variability of 72%. Therefore, the major catchment areas of the rivers are about 100-200 km further inland in regions …
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The Effective Viscosity of Ash-Laden Flows
<p>Debris flows can drastically alter ecosystems and damage infrastructure, and there is an increased risk of debris flows following a wildfire. In general, runoff and erosion drastically increase following a wildfire as a result of many processes, one of them being debris flows. Large debris flows …
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The Effective Viscosity of Ash-Laden Flows
<p>Debris flows can drastically alter ecosystems and damage infrastructure, and there is an increased risk of debris flows following a wildfire. In general, runoff and erosion drastically increase following a wildfire as a result of many processes, one of them being debris flows. Large debris flows …