AbrasionSand papereffect of therivertransportsedimentEstuaryThenavigablemouth ofa riverLeveeFlood defenceon banks ofriver can benatural ormanmandeSaltationBouncing ofrocks alongthe bed ofthe riverAttritionRocks aremade smootherand rounder bybashingtogetherNEEnglandLocationof riverTeesSourceStart ofa riverDepositiondroppingstuffTruncatedspurCreated when ariver erodesround area ofharder rocks inthe uppercourseMeanderthebend ina riverDeltafan shapeddepositis atthe mouthof a riverwaterfallFormedbecause of aband of hardrock in thecourse of ariverFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercoursePlungepoolforms atthe baseof awaterfallRiverTeesOur casestudyriverStormDesmondOurfloodingcasestudyMouthEnd ofriverChannelthe bitthe waterflows inVshapedvalleyIn the uppercourse andshaped byverticalerosionHydraulicactionErosionusing thesheer forceof the waterTransportmovementin riversErosionwearingaway (withmovement)of the bedand banksOxbowlakeformed whena meander iscut off leavinga marshy lakeareaNWEngland ,CumbriaLocationof thefloodingcase studyAbrasionSand papereffect of therivertransportsedimentEstuaryThenavigablemouth ofa riverLeveeFlood defenceon banks ofriver can benatural ormanmandeSaltationBouncing ofrocks alongthe bed ofthe riverAttritionRocks aremade smootherand rounder bybashingtogetherNEEnglandLocationof riverTeesSourceStart ofa riverDepositiondroppingstuffTruncatedspurCreated when ariver erodesround area ofharder rocks inthe uppercourseMeanderthebend ina riverDeltafan shapeddepositis atthe mouthof a riverwaterfallFormedbecause of aband of hardrock in thecourse of ariverFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercoursePlungepoolforms atthe baseof awaterfallRiverTeesOur casestudyriverStormDesmondOurfloodingcasestudyMouthEnd ofriverChannelthe bitthe waterflows inVshapedvalleyIn the uppercourse andshaped byverticalerosionHydraulicactionErosionusing thesheer forceof the waterTransportmovementin riversErosionwearingaway (withmovement)of the bedand banksOxbowlakeformed whena meander iscut off leavinga marshy lakeareaNWEngland ,CumbriaLocationof thefloodingcase study

River Landforms and processes - Call List

(Print) Use this randomly generated list as your call list when playing the game. There is no need to say the BINGO column name. Place some kind of mark (like an X, a checkmark, a dot, tally mark, etc) on each cell as you announce it, to keep track. You can also cut out each item, place them in a bag and pull words from the bag.


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  1. Sand paper effect of the river transport sediment
    Abrasion
  2. The navigable mouth of a river
    Estuary
  3. Flood defence on banks of river can be natural or manmande
    Levee
  4. Bouncing of rocks along the bed of the river
    Saltation
  5. Rocks are made smoother and rounder by bashing together
    Attrition
  6. Location of river Tees
    NE England
  7. Start of a river
    Source
  8. dropping stuff
    Deposition
  9. Created when a river erodes round area of harder rocks in the upper course
    Truncated spur
  10. the bend in a river
    Meander
  11. fan shaped depositis at the mouth of a river
    Delta
  12. Formed because of a band of hard rock in the course of a river
    waterfall
  13. The area either side of a river that floods especially in the lower course
    Flood plain
  14. forms at the base of a waterfall
    Plunge pool
  15. Our case study river
    River Tees
  16. Our flooding case study
    Storm Desmond
  17. End of river
    Mouth
  18. the bit the water flows in
    Channel
  19. In the upper course and shaped by vertical erosion
    V shaped valley
  20. Erosion using the sheer force of the water
    Hydraulic action
  21. movement in rivers
    Transport
  22. wearing away (with movement) of the bed and banks
    Erosion
  23. formed when a meander is cut off leaving a marshy lake area
    Ox bow lake
  24. Location of the flooding case study
    NW England , Cumbria