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What factors affect the rates of landform change?

Factors that affect the rate of landform change in a river are:

  • Geology – such as hard and soft rocks in the formation of a waterfall.
  • Climate – in the UK this varies with seasons, and affects the discharge amounts in a river and the level of energy it has to erode and deposit.
  • Human activity – intended and unintended consequences, such as building a dam which traps sediment and controls the flow of a river.

The River Severn

The of the River Severn is located in the Cambrian Mountains of Mid Wales, and it flows east and south to its where the river joins the Bristol Channel underneath the Severn Bridges.

The River Severn runs from Plynlimon to the Bristol Channel, along the Welsh-English border.

The area receives excessive rainfall due to depressions from the Atlantic. The Severn swiftly grows and forms a V-shaped valley. The river transports a large load, which allows rapid erosion to take place. Waterfalls and gorges have been formed in the upper course. As the gradient decreases, meanders can be found. As the river nears the lower course, flooding is a threat.

Upper course

  • The has hard impermeable rocks. Here, has formed a V-shaped valley.
  • The River Severn has many waterfalls in its upper course.

Middle course

As the River Severn starts to erode sideways (), it forms . These can be identified in the near Kempsey in Worcestershire.

Lower course

Near Tewkesbury in Gloucestershire, the meanders in the are much larger. In this area there are also which have formed when the river has flooded.

The River Severn has a very large mouth with mudflats and sandbanks which support wildlife in the area. Many of the sites are protected areas.

Aerial view of the Severn Bridge