Deltafan shapeddepositis atthe mouthof a riverChannelthe bitthe waterflows inFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercoursePlungepoolforms atthe baseof awaterfallMeanderthebend ina riverVshapedvalleyIn the uppercourse andshaped byverticalerosionSourceStart ofa riverAbrasionSand papereffect of therivertransportsedimentOxbowlakeformed whena meander iscut off leavinga marshy lakeareaAttritionRocks aremade smootherand rounder bybashingtogetherwaterfallFormedbecause of aband of hardrock in thecourse of ariverHydraulicactionErosionusing thesheer forceof the waterTransportmovementin riversNWEngland ,CumbriaLocationof thefloodingcase studyRiverTeesOur casestudyriverSaltationBouncing ofrocks alongthe bed ofthe riverLeveeFlood defenceon banks ofriver can benatural ormanmandeErosionwearingaway (withmovement)of the bedand banksDepositiondroppingstuffStormDesmondOurfloodingcasestudyMouthEnd ofriverNEEnglandLocationof riverTeesEstuaryThenavigablemouth ofa riverTruncatedspurCreated when ariver erodesround area ofharder rocks inthe uppercourseDeltafan shapeddepositis atthe mouthof a riverChannelthe bitthe waterflows inFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercoursePlungepoolforms atthe baseof awaterfallMeanderthebend ina riverVshapedvalleyIn the uppercourse andshaped byverticalerosionSourceStart ofa riverAbrasionSand papereffect of therivertransportsedimentOxbowlakeformed whena meander iscut off leavinga marshy lakeareaAttritionRocks aremade smootherand rounder bybashingtogetherwaterfallFormedbecause of aband of hardrock in thecourse of ariverHydraulicactionErosionusing thesheer forceof the waterTransportmovementin riversNWEngland ,CumbriaLocationof thefloodingcase studyRiverTeesOur casestudyriverSaltationBouncing ofrocks alongthe bed ofthe riverLeveeFlood defenceon banks ofriver can benatural ormanmandeErosionwearingaway (withmovement)of the bedand banksDepositiondroppingstuffStormDesmondOurfloodingcasestudyMouthEnd ofriverNEEnglandLocationof riverTeesEstuaryThenavigablemouth ofa riverTruncatedspurCreated when ariver erodesround area ofharder rocks inthe uppercourse

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