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This upheaval may result in sediment transfers and soil production.
Both examples illustrate the importance of variable sediment sources; the seasonality, frequency, and magnitude of sediment transfers; and the profound influence of ice cover over contemporary, neoglacial and Pleistocene time scales.
The results were compared to some pertinent observations made on the Namibian margin such as the vertical displacements, the sediment transfers, the denudation and the stratigraphic architecture in the marginal basin.
Laterally contiguous units, therefore, may vary greatly in age and sediment character, suggesting that current facies models inadequately characterize sediment transfers when the ice front is decoupled from its sandur.
Headspace C2H2 concentrations decreased slowly in bottles containing mixed culture enrichments derived from sediment transfers.
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Sediment transfer is thus frequently associated with sporadic flash floods that may include mudflows.
Debris flows strongly control sediment transfer patterns in mountainous catchments.
These phases of high sediment transfer occurred at ∼1 2, ∼4 5, and ∼7 8 ka.
The climate significantly influenced the mode of sediment transfer from the feeder system to the basin.
Sediment transfer is additionally slowed down by the presence of numerous anthropogenic barriers within slope and valley-floor domains.
We quantify sediment transfer at the Illgraben, Switzerland, where debris flows are frequent and geomorphic change is rapid.
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