The drainage pattern in Haryana is mostly dendritic. A dendritic drainage pattern is a branching pattern of streams that resembles the branches of a tree. It is the most common type of drainage pattern in the world. Dendritic drainage patterns are formed when streams flow downhill and erode the land in a uniform manner. The streams then join together to form larger streams, which eventually join together to form rivers. The dendritic drainage pattern is found in a variety of landscapes, including mountains, hills, and plains.
Radial drainage patterns are formed when streams flow away from a central point, such as a mountain peak. Rectangular drainage patterns are formed when streams flow in a straight line, often due to the presence of a fault line. Trellis drainage patterns are formed when streams flow in a series of parallel lines, often due to the presence of a cuesta.
The dendritic drainage pattern is the most common type of drainage pattern in Haryana because the state is located in a relatively flat area. The streams in Haryana flow downhill and erode the land in a uniform manner, which creates a branching pattern. The dendritic drainage pattern is also found in other parts of India, such as the Ganges River basin.