SaltationBouncing ofrocks alongthe bed ofthe riverTransportmovementin riversPlungepoolforms atthe baseof awaterfallMouthEnd ofriverEstuaryThenavigablemouth ofa riverFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercourseMeanderthebend ina riverLeveeFlood defenceon banks ofriver can benatural ormanmandeNWEngland ,CumbriaLocationof thefloodingcase studyVshapedvalleyIn the uppercourse andshaped byverticalerosionwaterfallFormedbecause of aband of hardrock in thecourse of ariverHydraulicactionErosionusing thesheer forceof the waterAttritionRocks aremade smootherand rounder bybashingtogetherChannelthe bitthe waterflows inDepositiondroppingstuffAbrasionSand papereffect of therivertransportsedimentStormDesmondOurfloodingcasestudySourceStart ofa riverRiverTeesOur casestudyriverDeltafan shapeddepositis atthe mouthof a riverTruncatedspurCreated when ariver erodesround area ofharder rocks inthe uppercourseNEEnglandLocationof riverTeesErosionwearingaway (withmovement)of the bedand banksOxbowlakeformed whena meander iscut off leavinga marshy lakeareaSaltationBouncing ofrocks alongthe bed ofthe riverTransportmovementin riversPlungepoolforms atthe baseof awaterfallMouthEnd ofriverEstuaryThenavigablemouth ofa riverFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercourseMeanderthebend ina riverLeveeFlood defenceon banks ofriver can benatural ormanmandeNWEngland ,CumbriaLocationof thefloodingcase studyVshapedvalleyIn the uppercourse andshaped byverticalerosionwaterfallFormedbecause of aband of hardrock in thecourse of ariverHydraulicactionErosionusing thesheer forceof the waterAttritionRocks aremade smootherand rounder bybashingtogetherChannelthe bitthe waterflows inDepositiondroppingstuffAbrasionSand papereffect of therivertransportsedimentStormDesmondOurfloodingcasestudySourceStart ofa riverRiverTeesOur casestudyriverDeltafan shapeddepositis atthe mouthof a riverTruncatedspurCreated when ariver erodesround area ofharder rocks inthe uppercourseNEEnglandLocationof riverTeesErosionwearingaway (withmovement)of the bedand banksOxbowlakeformed whena meander iscut off leavinga marshy lakearea

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