aggradationalの例文

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Aggradational channels commonly form where the slope is below grade.
Typical aggradational environments include lowland alluvial rivers, river deltas, and alluvial fans.
Aggradational environments are often undergoing slow subsidence which balances the increase in land surface elevation due to aggradation.
Hypothetical valley cross-section illustrating a complex sequence of aggradational ( fill ) and degradational ( cut and strath ) terraces.
After millions of years, an aggradational environment will become a sedimentary basin, which contains the deposited sediment, including paleochannels and ancient floodplains.
The aggradational Great Plains cover about 72.4mha area with the Ganga and the Brahmaputra forming the main drainage axes in the major portion.
Whatever the process this stacking plays an important role in aggradational systems and potentially is one of the leading controls in the formation of levee confined complexes.
Hypothetical valley cross-section illustrating a complex sequence of aggradational ( fill ) and degradational ( cut and strath ) terraces and deposits ( upland gravels ).
The approximate elevation of the area around the present site is 1010m MSL . The existing slope angle of 42?suggests a localised aggradational environment dominated by the continuous erosion and sometime the occurrences of destructive land-slides towards an eastern direction.