FloodplainThe area eitherside of a riverthat floodsespecially inthe lowercourseSourceStart ofa riverStormDesmondOurfloodingcasestudyAttritionRocks aremade smootherand rounder bybashingtogetherRiverTeesOur casestudyriverSaltationBouncing ofrocks alongthe bed ofthe riverEstuaryThenavigablemouth ofa riverOxbowlakeformed whena meander iscut off leavinga marshy lakeareaVshapedvalleyIn the uppercourse andshaped byverticalerosionErosionwearingaway (withmovement)of the bedand banksLeveeFlood defenceon banks ofriver can benatural ormanmandeTransportmovementin riversMouthEnd ofriverMeanderthebend ina riverDepositiondroppingstuffNEEnglandLocationof riverTeesHydraulicactionErosionusing thesheer forceof the waterNWEngland ,CumbriaLocationof thefloodingcase studyChannelthe bitthe waterflows inPlungepoolforms atthe baseof awaterfallAbrasionSand papereffect of therivertransportsedimentDeltafan shapeddepositis atthe mouthof a riverTruncatedspurCreated when ariver erodesround area ofharder rocks inthe uppercoursewaterfallFormedbecause of aband of hardrock in thecourse of ariverFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercourseSourceStart ofa riverStormDesmondOurfloodingcasestudyAttritionRocks aremade smootherand rounder bybashingtogetherRiverTeesOur casestudyriverSaltationBouncing ofrocks alongthe bed ofthe riverEstuaryThenavigablemouth ofa riverOxbowlakeformed whena meander iscut off leavinga marshy lakeareaVshapedvalleyIn the uppercourse andshaped byverticalerosionErosionwearingaway (withmovement)of the bedand banksLeveeFlood defenceon banks ofriver can benatural ormanmandeTransportmovementin riversMouthEnd ofriverMeanderthebend ina riverDepositiondroppingstuffNEEnglandLocationof riverTeesHydraulicactionErosionusing thesheer forceof the waterNWEngland ,CumbriaLocationof thefloodingcase studyChannelthe bitthe waterflows inPlungepoolforms atthe baseof awaterfallAbrasionSand papereffect of therivertransportsedimentDeltafan shapeddepositis atthe mouthof a riverTruncatedspurCreated when ariver erodesround area ofharder rocks inthe uppercoursewaterfallFormedbecause of aband of hardrock in thecourse of ariver

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