Q.Radial and Centripetal drainage pattern

Think of a city after heavy rain. Water doesn't just vanish — it finds the path of least resistance, carving little streams along road edges, pooling in low spots, and eventually joining bigger channels. Now scale that up to a mountain range or a plateau. Rivers do exactly the same thing, but over thousands of years. The pattern they etch into the land is not random. It is a direct response to the slope, the hardness of the rocks, and the fractures or folds hidden beneath the soil.

That etched arrangement is what we call a drainage pattern. It is the spatial layout of a river system and its tributaries, seen from above. For a humanities student, the key shift is this: you are not memorising river names. You are reading a landscape's autobiography. A drainage pattern tells you what kind of terrain you are standing on — whether the rocks are uniform, whether the land has been tilted, whether it was once a dome or a plain.

The most common pattern, and the easiest to recognise, is the dendritic pattern. The name comes from the Greek word for tree, and that is exactly what it looks like — a trunk with branches splitting into smaller twigs. This happens where the underlying rock is uniform and the slope is gentle, so the river has no structural reason to turn sharply. It just wanders, branching naturally. Think of the rivers of the northern Indian plains — they spread out like a tree because the ground is flat and the soil is consistent.

Now imagine the opposite. Suppose the land is a series of parallel ridges and valleys, like corrugated cardboard. A river flowing down the slope will follow the troughs, and its tributaries will join it at sharp, almost right angles. This is the trellis pattern, named after a garden trellis. It forms where hard and soft rocks alternate in bands. The main river cuts through the hard ridge, but the tributaries are forced to run along the softer valleys. You see this in the folded mountains of the Himalayas' outer ranges.

Then there is the rectangular pattern. It looks similar to trellis at first, but the bends are even sharper — nearly 90 degrees, and the tributaries join in a way that makes the whole system look like a grid. This happens when the rocks are criss-crossed by joints and faults, natural cracks that give the river a ready-made path. The river follows the cracks, turns, follows another crack, turns again. It is not obeying a slope; it is obeying a fracture map.

A more dramatic one is the radial pattern. Picture a dome or a volcanic cone. Rivers start at the summit and flow outward in all directions, like the spokes of a wheel or the rays of the sun. This is common around hills and mountains that stand alone. The Amarkantak range in central India gives rise to rivers flowing in several directions — that is a radial pattern in action.

Finally, there is the centripetal pattern, which is the reverse of radial. Here, rivers flow inward toward a central low point, usually a lake or a depression. This happens in basins and inland drainage areas. The rivers do not reach the sea; they end in a lake or simply dry up. The Rann of Kutch and parts of Rajasthan show this kind of inward drainage.