In the upper course of a river gradients are steep and river channels are narrow. Vertical erosion is greatest in the upper course of a river. As the result of this typical features include steep valley sides, interlocking spurs, rapids, gorges and waterfalls.
When a river runs over alternating layers of hard and soft rock, rapids and waterfalls may form.
Waterfalls commonly form where water rushes down steep hillsides in upland areas and quickly erodes the rocks. The height and number of waterfalls along a stream or river depends upon the type of rocks that are being eroded by the water. Some types of rocks (shale, for example) wear away more easily than others (such as sandstone or limestone).
As the river or stream wears away the weak rocks, they travel across the surface of stronger rocks. These more resistant rocks become the capstones to waterfalls. The number and thickness of these stronger rock units in a vertical sequence of rocks controls how many water falls there are and how much vertical drop there is on each waterfall.
The diagram above shows the formation of a waterfall. Soft rock is undercut (1). This leaves a layer of hard rock which overhangs the layer of soft rock (2). The water flows over the overhang and creates a plunge pool in the soft rock below (3). Eventually the overhang will collapse due to the erosion of the soft rock beneath it. The waterfall then retreats up stream (4). This creates a steep, gorge-like valley.
An example of a water fall is High Force in Northumberland. It is located on the River Tees, near Middleton in Teesdale, Tees Valley, England. The waterfall is 20m in height.
High Force Waterfall
High Force was formed where the River Tees crosses the Whin Sill - a hard layer of rock. The waterfall itself consists of two different types of rock. The upper band is made up of whinstone, a hard rock which the waterfall takes a lot of time to erode. Underlying the whin sill is a layer of of Carboniferous Limestone, a softer rock which is easily worn away by the waterfall. This creates a plunge pool beneath the waterfall. As the limestone is eroded the whin sill is left over hanging the waterfall. Eventually the overhang collapses. This process of erosion means that the waterfall is slowly moving upstream, leaving a narrow, deep gorge in front of it. The length of the gorge is currently about 700 metres. The bed load (rocks that the river is carrying) is mainly composed of large boulders, which are rolled along the river bed. Upstream of the waterfall, the river is narrow; downstream, it widens and meanders.
The video below shows the view from the top of High Force waterfall.
You can view more videos of High Force in our video area.
The 3D model below shows Low Force waterfall on the River Tees.