Explanation:

The dendritic pattern develops where the river channel follows the slope of the terrain. The stream with its tributaries resembles the branches of a tree, thus the name dendritic
Dendritic or tree-shaped drainage pattern is the most common and widespread pattern to be found on the earth’s surface. The pattern is called dendritic on the ground that the network of tributaries of various orders and magnitudes of the trunk or master stream resembles the branches and roots and rootlets of a tree.
This pattern develops in a variety of structural and lithological environments such as in the mountainous and hilly areas (e.g., dendritic pattern is one of the dominant patterns in the Himalayas), on extensive plateau surfaces (e.g., Deccan plateau), on peneplain surfaces (e.g., the Peninsular peneplains of India, mostly in the basins of the Mahanadi, the Godavari, the Krishna, the Cauvery, the Domodar etc.), in the alleviated plains (e.g., Great Plains of North India), in the desert plains (e.g., Rajasthan desert), in the glaciated lowland regions (e.g., North European plains and northern lowlands of North America) etc.
Do you know?
Hazaribagh plateau, Parasnath hill, Panchet hill and Dalma lava upland (all in Jharkhand) have issued radial drainage pattern.
THINK!
Centripetal drainage pattern.