What are the different types of drainage patterns for streams?
Drainage patterns
- Dendritic drainage pattern.
- Parallel drainage pattern.
- Trellis drainage pattern.
- Rectangular drainage pattern.
- Radial drainage pattern.
- Centripetal drainage pattern.
- Deranged drainage pattern.
- Annular drainage pattern.
What are some drainage patterns for rivers?
Drainage Patterns
- A dendritic drainage pattern is the most common form and looks like the branching pattern of tree roots.
- Parallel drainage patterns form where there is a pronounced slope to the surface.
- Trellis drainage patterns look similar to their namesake, the common garden trellis.
What is river pattern?
River pattern are patterns formed by the streams, rivers. Drainage systems are also known as river pattern. The four river patterns are dendritic, trellis, radial & rectangular.
How many types of drainage patterns are there?
The drainage patterns are divided into the following ten types: Trellised Drainage Pattern. Dendritic Drainage Pattern. Rectangular Drainage Pattern.
What is the most common drainage pattern?
dendritic drainage pattern
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.
What is main drainage pattern?
The drainage pattern marked by right-angled bends and right-angled junctions between tributaries and the main stream is known as rectangular drainage. It differs from the trellis pattern in so far as it is more irregular and its tributary streams are neither as long, nor parallel as in trellis drainage.
Which is the most common drainage pattern?
What is drainage pattern?
Drainage Pattern is the pattern formed by the streams, rivers, and lakes in a particular drainage basin. The pattern created by stream erosion over time reveals characteristics of the kind of rocks and geologic structures in a landscape region drained by streams.
What is centripetal drainage pattern?
river systems In river: Drainage patterns. 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.