RiverTeesOur casestudyriverFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercourseVshapedvalleyIn the uppercourse andshaped byverticalerosionAttritionRocks aremade smootherand rounder bybashingtogetherNWEngland ,CumbriaLocationof thefloodingcase studyDeltafan shapeddepositis atthe mouthof a riverwaterfallFormedbecause of aband of hardrock in thecourse of ariverEstuaryThenavigablemouth ofa riverStormDesmondOurfloodingcasestudySourceStart ofa riverHydraulicactionErosionusing thesheer forceof the waterSaltationBouncing ofrocks alongthe bed ofthe riverMouthEnd ofriverChannelthe bitthe waterflows inLeveeFlood defenceon banks ofriver can benatural ormanmandeTransportmovementin riversPlungepoolforms atthe baseof awaterfallOxbowlakeformed whena meander iscut off leavinga marshy lakeareaErosionwearingaway (withmovement)of the bedand banksTruncatedspurCreated when ariver erodesround area ofharder rocks inthe uppercourseAbrasionSand papereffect of therivertransportsedimentMeanderthebend ina riverDepositiondroppingstuffNEEnglandLocationof riverTeesRiverTeesOur casestudyriverFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercourseVshapedvalleyIn the uppercourse andshaped byverticalerosionAttritionRocks aremade smootherand rounder bybashingtogetherNWEngland ,CumbriaLocationof thefloodingcase studyDeltafan shapeddepositis atthe mouthof a riverwaterfallFormedbecause of aband of hardrock in thecourse of ariverEstuaryThenavigablemouth ofa riverStormDesmondOurfloodingcasestudySourceStart ofa riverHydraulicactionErosionusing thesheer forceof the waterSaltationBouncing ofrocks alongthe bed ofthe riverMouthEnd ofriverChannelthe bitthe waterflows inLeveeFlood defenceon banks ofriver can benatural ormanmandeTransportmovementin riversPlungepoolforms atthe baseof awaterfallOxbowlakeformed whena meander iscut off leavinga marshy lakeareaErosionwearingaway (withmovement)of the bedand banksTruncatedspurCreated when ariver erodesround area ofharder rocks inthe uppercourseAbrasionSand papereffect of therivertransportsedimentMeanderthebend ina riverDepositiondroppingstuffNEEnglandLocationof riverTees

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