SourceStart ofa riverDeltafan shapeddepositis atthe mouthof a riverPlungepoolforms atthe baseof awaterfallNEEnglandLocationof riverTeesOxbowlakeformed whena meander iscut off leavinga marshy lakeareaMeanderthebend ina riverTransportmovementin riversAbrasionSand papereffect of therivertransportsedimentRiverTeesOur casestudyriverStormDesmondOurfloodingcasestudyErosionwearingaway (withmovement)of the bedand banksAttritionRocks aremade smootherand rounder bybashingtogetherTruncatedspurCreated when ariver erodesround area ofharder rocks inthe uppercourseChannelthe bitthe waterflows inHydraulicactionErosionusing thesheer forceof the waterLeveeFlood defenceon banks ofriver can benatural ormanmandeDepositiondroppingstuffFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercoursewaterfallFormedbecause of aband of hardrock in thecourse of ariverEstuaryThenavigablemouth ofa riverNWEngland ,CumbriaLocationof thefloodingcase studyVshapedvalleyIn the uppercourse andshaped byverticalerosionSaltationBouncing ofrocks alongthe bed ofthe riverMouthEnd ofriverSourceStart ofa riverDeltafan shapeddepositis atthe mouthof a riverPlungepoolforms atthe baseof awaterfallNEEnglandLocationof riverTeesOxbowlakeformed whena meander iscut off leavinga marshy lakeareaMeanderthebend ina riverTransportmovementin riversAbrasionSand papereffect of therivertransportsedimentRiverTeesOur casestudyriverStormDesmondOurfloodingcasestudyErosionwearingaway (withmovement)of the bedand banksAttritionRocks aremade smootherand rounder bybashingtogetherTruncatedspurCreated when ariver erodesround area ofharder rocks inthe uppercourseChannelthe bitthe waterflows inHydraulicactionErosionusing thesheer forceof the waterLeveeFlood defenceon banks ofriver can benatural ormanmandeDepositiondroppingstuffFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercoursewaterfallFormedbecause of aband of hardrock in thecourse of ariverEstuaryThenavigablemouth ofa riverNWEngland ,CumbriaLocationof thefloodingcase studyVshapedvalleyIn the uppercourse andshaped byverticalerosionSaltationBouncing ofrocks alongthe bed ofthe riverMouthEnd ofriver

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.


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