VshapedvalleyIn the uppercourse andshaped byverticalerosionSourceStart ofa riverOxbowlakeformed whena meander iscut off leavinga marshy lakeareaMeanderthebend ina riverCondensationLocationof riverTeesHydraulicactionErosionusing thesheer forceof the waterSpurCreated when ariver erodesround area ofharder rocks inthe uppercoursePrecipitationRocks aremade smootherand rounder bybashingtogetherwaterfallFormedbecause of aband of hardrock in thecourse of ariverEstuaryThenavigablemouth ofa riverBoggygroundLocationof thefloodingcase studyPlungepoolforms atthe baseof awaterfallAbrasionSand papereffect of therivertransportsedimentLeveeFlood defenceon banks ofriver can benatural ormanmandeDeltafan shapeddepositis atthe mouthof a riverFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercourseStormsOurfloodingcasestudyDepositiondroppingstuffTransportmovementin riversErosionwearingaway (withmovement)of the bedand banksMouthEnd ofriverSpringBouncing ofrocks alongthe bed ofthe riverChannelthe bitthe waterflows inRiverBrunOur casestudyriverVshapedvalleyIn the uppercourse andshaped byverticalerosionSourceStart ofa riverOxbowlakeformed whena meander iscut off leavinga marshy lakeareaMeanderthebend ina riverCondensationLocationof riverTeesHydraulicactionErosionusing thesheer forceof the waterSpurCreated when ariver erodesround area ofharder rocks inthe uppercoursePrecipitationRocks aremade smootherand rounder bybashingtogetherwaterfallFormedbecause of aband of hardrock in thecourse of ariverEstuaryThenavigablemouth ofa riverBoggygroundLocationof thefloodingcase studyPlungepoolforms atthe baseof awaterfallAbrasionSand papereffect of therivertransportsedimentLeveeFlood defenceon banks ofriver can benatural ormanmandeDeltafan shapeddepositis atthe mouthof a riverFloodplainThe area eitherside of a riverthat floodsespecially inthe lowercourseStormsOurfloodingcasestudyDepositiondroppingstuffTransportmovementin riversErosionwearingaway (withmovement)of the bedand banksMouthEnd ofriverSpringBouncing ofrocks alongthe bed ofthe riverChannelthe bitthe waterflows inRiverBrunOur casestudyriver

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