A stream that takes its course down the slope of an initial landform such as a newly emerged coastal plain or a volcano is a/an:

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A consequent stream is one that takes its course down the slope of an initial landform, such as a newly emerged coastal plain or a volcano. It develops in response to the initial slope of the land and is influenced by the underlying geology. It is different from a subsequent stream, which develops after the landform has been eroded and is influenced by the existing topography. Braided streams are characterized by multiple channels that divide and rejoin, while graded streams have a slope that is in equilibrium with the energy of the flowing water. Alluvial streams are those that deposit sediment along their banks and floodplains.

A Stream That Takes Its Course Down the Slope of an Initial