Hence, the spatial distribution of landforms is often scale-dependent as is the case for soils and geological strata. V-shaped Valleys, Interlocking Spurs, Gorges & Waterfalls, V-shaped Valleys, Interlocking Spurs, Gorges & Waterfalls. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. TASK: Draw labelled diagrams describing and explaining the creation of different river landforms: Watch the video above and note the names of the landforms referenced. They form when a band of hard resistant rock (cap rock) lies over softer, less resistant rock. Processes of erosion, transport and deposition work together to create river landforms. [1] Until recently, compiling the data found in such data sets required time consuming and expensive techniques involving many man-hours. River landforms A resource identifying the different river landforms created by processes of erosion and deposition. River landforms can be divided into upper, middle and lower course features. Steep-sided V-shaped valleys, interlocking spurs, rapids, waterfalls and gorges. Springer. In the upper course of a river the altitude is high and the gradient is steep. The processes of erosion and deposition create different river landforms. Read about our approach to external linking. River landscapes change as you go downstream from the source to the mouth. Watch the video below and note the names of the landforms mentioned. It erodes soft rock more quickly than hard rock and this may lead to the creation of a waterfall. Meanders are bends in a rivers course. Formed when a river runs over alternating layers of hard and soft rock and the river undercuts the harder rock leaving an overhang. Meanders often migrate downstream and become wider and larger over time. Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure, and soil type. As a river moves along its course, it creates several landforms by fluvial processes. Formed as the river breaks through a meander, possibly from a flood when the river has a higher discharge and more energy, and the ends join, the loop is cut-off from the main channel. Found at the mouth of large rivers - for example, the Mississippi. Meanders and oxbow lakes use erosional and depositional processes in their creation. Some generic landform elements including: pits, peaks, channels, ridges, passes, pools and plains. River landscapes change as you go downstream from the source to the mouth. Read about our approach to external linking. Drainage Basin Watch the video below and note the names of the landforms mentioned. In the middle course, the river. Landforms in the upper course V-shaped valley When a river is near its source, it often develops a V-shaped valley as the river erodes down (this is called vertical erosion ).
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