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- W2014914154 abstract "The mean size of particles mantling quartz monzonite debris slopes in the Mojave Desert is found to be correlated with slope gradient 5, but the relation is shown to vary from one debris slope to another as a result of differences in joint spacing and mode of weathering of the underlying quartz monzonite. Unlike debris slopes developed on closely jointed and/or mechanically weak rocks, which we have previously shown to be adjusted to present-day hydraulic processes, those developed on quartz monzonite are only partly adjusted. The degree of adjustment of any part of a debris slope varies inversely with gradient and joint spacing. The correlations between S and are due to decreasing as debris slopes become better adjusted and to debris slopes becoming better adjusted at lower gradients." @default.
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- W2014914154 date "1987-05-01" @default.
- W2014914154 modified "2023-09-23" @default.
- W2014914154 title "Gradient-Particle Size Relations on Quartz Monzonite Debris Slopes in the Mojave Desert" @default.
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- W2014914154 doi "https://doi.org/10.1086/629139" @default.
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