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The Annamese Cordillera forms a drainage divide, with rivers to the east flowing to the South China Sea and those to the west to the Mekong River.
The top of Lee Mountain forms a drainage divide between the creek's watershed and another watershed.
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The land rises from west to east, the eastern boundary forming a drainage divide.
The network of drainage channels and tributaries forms a particular drainage pattern as determined by local topography and subsurface geology (lithology and structures).
The occurrence of sand in the northern part develops a good drainage conditions by virtue of its high hydraulic conductivity, while in the southern part the content of clay increases gradually from the northern part, which forms a sluggish drainage condition due to its low hydraulic conductivity.
During the third stage a series of marine terraces formed and a drainage system developed creating both bland valleys and well-defined channels and gorges.
Analytical and numerical models of landscape evolution in general either assume steady state hydrology or use empirically based functions in the form of a drainage area power law to model runoff.
The northwestern region is arid and eroded by the wind; it forms an inland drainage basin.
Water continuously seeps from the base of the intact rip-rap dam that forms Lost Lake, forming a small drainage that continues for 75-100 m before joining with surface water flowing over the concrete spillway.
In addition to this, the presence of rocks in the southern part has low hydraulic conductivity, because of limited weathered and fractured portions, which form a poor drainage conditions.
Seven different trapezoidal drainage sections were designed to form an integrated drainage network which is 'self-healing' to a certain extent.
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CEO of Professional Science Editing for Scientists @ prosciediting.com