River processes and the hydrological cycle Abrasion The movement of water after a storm across the surface of the ground. It is the fastest way in which water reaches a river. Throughflow Graph showing how the discharge of a river varies with time. Attrition The process by which material too heavy to be carried in suspension is transported by bouncing along the riverbed. Run-off (overland run-off) Water that falls to the earth from the atmosphere as part of the hydrological cycle. This will include rain, snow, sleet, hail, dew, and frost etc. Evapotranspiration The movement of water through rock. Evaporation The combined loss of water by evaporation and transpiration. © www.teachitgeography.co.uk 2012 17507 Page 1 of 6 River processes and the hydrological cycle Transpiration Small sized materials, such as clay and silt, which are suspended in the turbulent flow of a river. Discharge The movement of water into the soil. Precipitation The erosive force exerted by the pressure of the water. This erodes river banks, particularly on the outer curve of meanders and at waterfalls. Groundwater flow A type of erosion in which rock fragments carried by a river erode the river’s bed and sides. Interception The loss of water from plants by evaporation. Saltation The process where large sized materials are transported by a rolling or sliding action along the riverbed. © www.teachitgeography.co.uk 2012 17507 Page 2 of 6 River processes and the hydrological cycle Suspension The water which travels through the soil towards a river or the sea. Hydrograph The volume of water passing a certain point per unit of time. It is usually measured in cubic metres per second (cumecs). Hydraulic action The process where precipitation does not reach the soil, but is stopped by impermeable surfaces e.g. tarmac roads, the leaves and branches of trees and plants and by leaf litter on the forest floor etc. Traction The process by which liquid water becomes water vapour. Solution The process by which transported particles of rock become rounded and smaller by being knocked against one another. Infiltration The process by which the minerals in a rock, especially calcium ions, are dissolved in acidic water. It is a type of erosion and weathering. © www.teachitgeography.co.uk 2012 17507 Page 3 of 6 River processes and the hydrological cycle Teaching notes This resource could be used in a variety of ways depending on the ability of the class. If the cards are laminated, they could then be reused many times. Possible approaches could be: Separate the cards into 36 individual cards and then match the shaded key word(s) to the correct definition. Separate the cards into 18 paired cards. Use these cards as a dominoes game. Separate the cards into 18 paired cards. Use these as a loop game around the class. The loop game could be repeated against the clock after reissuing the cards, to measure progress. Answers Abrasion A type of erosion in which rock fragments carried by a river erode the river’s bed and sides. Attrition The process by which transported particles of rock become rounded and smaller by being knocked against one another. Discharge The volume of water passing a certain point per unit of time. It is usually measured in cubic metres per second (cumecs). Evaporation The process by which liquid water becomes water vapour. Evapotranspiration The combined loss of water by evaporation and transpiration. © www.teachitgeography.co.uk 2012 17507 Page 4 of 6 River processes and the hydrological cycle Groundwater flow The movement of water through rock. Hydraulic action The erosive force exerted by the pressure of the water. This erodes river banks, particularly on the outer curve of meanders and at waterfalls. Hydrograph Graph showing how the discharge of a river varies with time. Infiltration The movement of water into the soil. Interception The process where precipitation does not reach the soil, but is stopped by impermeable surfaces e.g. tarmac roads, the leaves and branches of trees and plants and by leaf litter on the forest floor etc. Precipitation Water that falls to the earth from the atmosphere as part of the hydrological cycle. This will include rain, snow, sleet, hail, dew, and frost etc. Run-off (overland or surface run-off) The movement of water after a storm across the surface of the ground. It is the fastest way in which water reaches a river. Saltation The process by which material too heavy to be carried in suspension is transported by bouncing along the riverbed. Solution The process by which the minerals in a rock, especially calcium ions, are dissolved in acidic water. It is a type of erosion and weathering. © www.teachitgeography.co.uk 2012 17507 Page 5 of 6 River processes and the hydrological cycle Suspension Small sized materials, such as clay and silt, which are suspended in the turbulent flow of a river Traction The process where large sized materials are transported by a rolling or sliding action along the riverbed. Transpiration The loss of water from plants by evaporation. Throughflow The water which travels through the soil towards a river or the sea. © www.teachitgeography.co.uk 2012 17507 Page 6 of 6
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