TYPES OF RIVER DRAINAGE PATTERNS
Dendritic drainage pattern
dendritic drainage pattern require the following condition to be formed:
rock should be uniformly resistant to erosion
this pattern is not dependent on geology
characteristics of dendritic drainage pattern
the pattern is tree shaped
the tributaries join the main stream at acute angles
example of rivers with dendritic pattern include tigela, mooi and umgeni in the south Africa
Radial drainage pattern
radial drainage pattern is formed on dome shaped hill, conical hill, mesa or butte
characteristic of radial drainage pattern
streams radiate outwards from the central high point.
example of areas with radial drainage pattern includekoffiebus and teebus in south africa
Trellis drainage pattern
requirement for trellis drainage pattern to be formed
parallell ranges of fold mountains or alternate layers of hard and soft rock
a strong main stream
the pattern is dependent on the relief and the geology of the area
characteristics of the trellised drainage pattern
tributaries meet the main stream at the right angles
the main stream cut gaps through the mountains
example of areas with trellis drainage pattern include beffels river at laingsburg in south africa
Centripetal drainage pattern
this type of drainage pattern is formed on a central basin or a low lying area such as a lake or a marsh
characteristics of centripetal drainage pattern include:
streams radiate inward from a sorrounding higher area
it is opposite of radial drainage pattern
example of centripetal drainage pattern is flatter parts of namaqualand in south africa
parallel drainage pattern
parallel drainage patterns occur in the recently uplifted sloping plain and require a rock type that is uniformly resistant to erosion
characteristics of parallel drainage pattern
the main streams flows parallel (or nearly) to each other
the tributaries enters the main stream at very small angles
An example of an area with a parallel drainage pattern is tributaries of the steelport river in Limpopo
rectangular drainage pattern
this occurs in a well-jointed rock with joints exposed at the surface
characteristics of rectangular drainage pattern
rivers flows in exposed joints
rivers and tributaries have right angled bends
An example of areas with rectangular drainage pattern is rivers in Waterberg (Limpopo)
deranged drainage pattern
this type of drainage pattern occur in geologically young areas
characteristics of deranged drainage pattern
haphazard pattern
numerous lakes and swamps
streams enters and leaves swamps and lakes randomly
example of areas with deranged drainage patterns are recently glaciated areas such as the Canadian shield
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