Suspension is material carried along in the rivers channel, usually fine particles.
Traction is heavy material usually big boulders that are rolled along the river bed.
Transportation is when the river moves material as bedload, suspended load or dissolved load (in solution).
Bedload can be moved by saltation or traction.
Tributary is a small river that joins a larger one.
Upper course is the highest stage of a river near to its source, characterised by large boulders and turbulent water.
V shaped valley is usually found in the upper course of the river where the water has considerable erosive power.
Vertical erosion leads to the bed getting deeper.
The valley sides become unstable and weakened by weathering and eventually collapse creating this.
Waterfalls form where the river meets a band of softer rock after flowing over an area of more resistant material.
Waterfalls progressively cut back, leaving a gorge.
Watershed is the high land marking the boundary between two drainage basins.
Weathering is the breaking down of rock by chemical, biological, freeze thaw or onion skin processes.
Hydrological Cycle is the movement of water around the water system.
Evaporation is when water is heated by the sun, it turns to vapour (gas) and rises (because it is lighter than the surrounding air as molecules spread out through heating).
Transpiration is when water is lost through the leaves (stomata) of plants into the atmosphere.
Condensation occurs when water vapour cools and changes from gas to liquid.
Precipitation is the ways in which water moves from the atmosphere to the ground.
Infiltration is when water passes down into the ground.
Percolation is when water moves down through soil.
Surface runoff, also called overland flow, occurs when water cannot sink into the ground.
Interception is when water is prevented from reaching the ground by vegetation.
Ground water flow is when water passes through rocks in the ground.
Groundwater storage is when water is held in rocks underground.
Surface Storage puddles, ponds and lakes are all examples of this store.
Channel flow is water that is moving in the river.
Store is when water is stationary in the water cycle e.g. clouds, groundwater storage, surface storage etc.
Flow is when water is moving in the water cycle.
Lag time is the time between peak rainfall and peak discharge.
Peak Discharge is the maximum amount of water held by a river after a storm.
Base flow is the normal discharge of a river.
Hydraulic Action is when the force of the water washes away rocks, a bit like when you wash the car with a hose.
Delta is a land form made of sediment that is deposited where a river flows into an ocean or lake, usually when waves are not strong enough to take it out to sea.
Catchment is an area from which a river system or lake derives its water.
Prevailing wind is the direction in which the wind most often blows.
Water cycle is the continuous flow of water between the Earth's surface and the atmosphere.
Porous is a rock, such as chalk and sandstone, which has many tiny gaps (pores) within it, which allow it to store water.
Soft engineering is an alternative method of reducing floods by, for example, planting trees, creating areas along river banks to flood naturally or importing beach material along coasts.
Undercutting is a type of erosion at the base of a river cliff, sea cliff or waterfall.
Transpiration is water loss from plants through pores in the leaves.