Rivers and river valleys Flashcards
precipitation
Moisture falling from clouds as rain, snow, or hail.
Interception
Vegetation prevents water from reaching the ground
Surface Runoff
Water flowing over the surface of the land into rivers
Infiltration
Water absorbed into the soil from the ground.
Transpiration
Water lost through the leaves of plants.
Upper Course of a River
Near the source, the river flows over a steep gradient from the hill/mountains. This gives the river a lot of energy, so it will erode the riverbed vertically to form narrow valleys
Lower Course of a River
Near the river’s mouth, the river widens further and
becomes flatter. Material transported is deposited
River Discharge
River discharge is the volume of water that flows in a river.
Hydrographs that discharge at a certain point in a river changes over time in relation to rainfall
Peak discharge
the discharge in a period of time
. Lag time
the delay between peak rainfall and peak discharge
Rising limb
the increase in river discharge.
Falling limb
the decrease in river discharge to normal level
Geomorphic Processes Upper
– Features include V-Shaped valleys, rapids, and waterfalls.
High force Waterfall located close to Forest-in Teesdale drops 21m
and is made from harder Whinstone and softer limestone rocks.
Gradually a gorge has been formed.
geomorphic processes middle
– Features include meanders and ox-bow lakes. The
meander near Yarm encloses the town.
geomorphic processes lower
– Greater lateral erosion creates features such as floodplains & levees near Darlington. Mudflats at the river’s estuary.