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Types of Drainage

Centripetal
Centripetal

Centripetal patterns are produced where drainage converges on a single outlet or sink, as in some craters, eroded structural domes with weak cores, parts of some limestone country, and enclosed desert depressions.

Dendritic
Dendritic

A dendritic drainage pattern is the most common form and looks like the branching pattern of tree roots. It develops in regions underlain by homogeneous material. That is, the subsurface geology has a similar resistance to weathering so there is no apparent control over the direction the tributaries take.

Deranged
Deranged

A drainage pattern has to do with rivers and tributaries, draining rainwater and snowmelt from a land mass. Tributaries flowing into bigger tributaries and then into rivers often follow a pattern, when viewed from above, or on a topo map.

source: quora.com
Trellised
Trellised

Quick Answer. A trellis drainage pattern occurs when tributaries join a river and erode a valley at right angles in a pattern that resembles a garden trellis. Drainage patterns occur most often where rock or other soil formations can erode easily along weak areas in the rock.

source: reference.com