Drainage Basin Geomorphology

Drainage Basin Geomorphology:

Drainage Basin:

A drainage basin is a naturally arising extent of land that functions as a funnel to channel precipitation and excess water to a nearby stream or river. They are also termed as catchment basins, catchments, water basins, or watersheds. Drainage basins are divided through geographical boundaries like: hills, mounds, mountains, or ridges, which are termed as water or drainage divides. The divides aid along with finding the direction of the flow of the water, while landscape, soil type, weather and life of plant will initiate the content and function of the flow.

While first formed, a drainage basin can adopt one of several various patterns that are simply identifiable on a map or by an aerial view. While draining precipitation, also termed as runoff, basins flow in a hierarchical pattern. Minor sub-drainage basins merge to form larger basins. Typically, minor basins supply to streams, while larger basins supply to rivers. Patterns formed through these drainage basins oftentimes give insight regarding to the landscape on that they flow.

Radial drainage basin patterns arise around a central, high point like: a mound or a hill. The streams flow downward by the highest point. Very similar to the radial pattern is the parallel pattern, which forms in rocky regions, here the water flows similarly in the one direction. While there are fractures in the massive rock on that the water flows, like: fault joints or lines, the drainage patterns suppose right angles and by a rectangular pattern.


It is explained as the science of landforms along with an emphasis on their basis, form, evolution and distribution across the physical landscape. The knowing of geomorphology and its processes is thus necessary to the understanding of physical geography.

History of Geomorphology:

Though the study of geomorphology has been approximately as ancient times, the initial official geomorphologic model was proposed in between 1884 and 1899 from the American geographer, William Morris Davis. His geomorphic cycle model was stimulated by theories of uniformitarians and attempted to theorize the improvement of several landform features.

Davis's geomorphic cycle model states that a landscape undergoes a preliminary uplift which is paired along with erosion as the wearing down or removal of materials in such uplifted landscape. Inside the similar landscape, precipitation purposes streams to flow extreme quickly. Like they develop their power after that cuts into the ground's surface both at the start of the stream and lower down the stream. It makes the stream channels exhibits in several landscapes.

This model also states that the slope angle of the land is gradually decreased and the ridges and divides present in specific landscapes become rounded over time due to erosion. The purpose of this erosion is not though restricted to water as in the stream illustration. At last, as per to Davis's model, over time that erosion arises in cycles and a landscape finally morphs into an old erosion surface.

Davis's theory was significant in launching the field of geomorphology and was new at its time as this was an innovative attempt to illustrate physical landform features. Today conversely, this is not generally utilized as a model since the processes he illustrated are not more systematic in the real world and this failed to acquire in account the processes being viewed in later geomorphic studies.

As Davis's model, many option attempts have been created to illustrate landform processes. Walther Penck, an Austrian geographer, urbanized a model in the 1920s for instance, that seem at ratios of uplift and erosion. This did not acquire hold although since this could not illustrates each landform feature.

Geomorphological Drainage system:

Within geomorphology, a drainage system is the pattern formed through the lakes, streams, and rivers in an exact drainage basin. They are governed through the topography of the land, whether an exact region is dominated through hard or soft rocks, and the gradient of the land. Hydrologists and Geomorphologists often visualize streams as to be part of drainage basins. A drainage basin is the topographic region from that a stream receives runoff, groundwater flow and through flow. Drainage basins are divided from each other by topographic barriers termed a watershed. A watershed exhibits each of the stream tributaries which flow to several locations along the stream channel. The shape, size, and number of the drainage basins determined in a region vary and the larger the topographic map, the additional information on the drainage basin is accessible.

Drainage patterns:

As per to the configuration of the channels, drainage systems can reduce into one of many categories termed as drainage patterns. Drainage patterns depend upon the geology  and topography of the land.

Dendritic drainage pattern:

These systems are the most general form of drainage system. Within a dendritic system, there are several contributing streams (analogous to the twigs of a tree), that are after that joined together in the tributaries of the particular river (the trunk and the branches of the tree, respectively). They extend where the river channel obeys the slope of the terrain. Dendritic systems form in V-shaped valleys; as a consequence, the rock types should be non-porous and imperviouss.

Parallel drainage pattern:

A parallel drainage system is a pattern of rivers caused through steep slopes along with several reliefs. Due to the steep slopes, the streams are straight and swift, along with very little tributaries, and each flow in the similar direction. This system forms on evenly sloping surfaces, for instance, rivers flowing southeast in Kenya through the Aberdare Mountains.

Trellis drainage pattern:

The geometry of a trellis drainage system is the same to that of a general garden trellis utilized to grow vines. Like the river flows along a strike valley, minor tributaries feed into it from the steep slopes on the sides of mountains. These tributaries enter the particular river at around 90 degree angles, causing a trellis-like form of the drainage system. Trellis drainage is feature of folded mountains, like: in North America, the Appalachian Mountains.

Rectangular drainage pattern:

Rectangular drainage extends on rocks which are of around uniform resistance to erosion, but that have two directions of jointing at around right angles. The joints are generally less resistant to erosion than the bulk rock more erosion tends to preferentially open the streams and joints eventually develop beside the joints. The consequence is a stream system in which streams comprise mainly straight line segments along with right angle bends and tributaries join larger streams at right angles.

Radial drainage pattern:

Within a radial drainage system, the streams radiate outwards by a central high point. Volcano generally displays outstanding radial drainage. The other geological characteristics on that radial drainage usually develops are laccoliths and domes. On these characteristics the drainage may present a combination of annular and radial patterns.

Deranged drainage pattern:

This system is a drainage system in drainage basins where there is no coherent pattern to the lakes and rivers. This arises in regions where there has been much geological disruption. The classic illustration is the Canadian Shield. Throughout the last ice age, the top soil was scraped off, leaving mainly bare rock. The melting of the glaciers left land along with several irregularities of elevation, and a huge deal of water to collect in the low points, illustrating the large number of lakes that are determined in Canada. The watersheds are new and are now sorting themselves out. Eventually the system will stabilize.

Annular drainage pattern:

In this pattern streams follow an approximate circular or concentric path along a belt of weak rock, similar to plan a ring like model. This is best displayed through streams draining a maturely dissected structural basin or dome where erosion has exposed rimming sedimentary strata of very much varying degrees of hardness, like in the Red Valley that nearly encircles the domal structure of the South Dakota’s Black Hills.

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