How easilywater or aircan passthrough soilor rock.Large soilparticles thatfeel gritty anddrain waterquickly.The solidrock layerbeneath soiland looserocks.Characteristicsof soil liketexture, color,and moisture.Material fromdead plantsand animals inthe soil thathelps plantsgrow.Naturalresources thatcan be replacedor grownagain,like sunlight,wind, and trees.The amount ofempty space insoil or rockthat can holdair or water.A very fine soilparticle thatfeels stickywhen wet andhard when dry.Fine soilparticles thatare smallerthan sand butbigger thanclay.Non-livingmaterials in soillike mineralsand tiny rockpieces.Fuels like coal,oil, and naturalgas formedfrom ancientplants andanimals.The color ofsoil, which canshow what it’smade of or howhealthy it is.Rock that hasbeen brokendown intosmaller piecesby weather.The processof fixingdamaged landso it can beused again.Materials fromnature thatpeople use, likewater, wood,and minerals.Resourcesthat cannot bereplaced onceused, like coaland oil.Dark, richorganicmaterial in soilmade fromdecayed plantsand animals.A type of soilmade up of amix of sand,silt, and claythat is good forgrowing plants.What soil ismade of,includingminerals,organic matter,air, and water.The uppermostsoil layer rich inorganic matterwhere mostplants grow.The layer ofsoil below thetopsoil that hasless organicmatter.A layer of soilthat has differentcolor or texturefrom the layersabove or belowit.The processwhere soil orrock is wornaway by wind,water, or ice.The breakingdown of rocksand mineralsby wind, water,or chemicals.The feel of thesoil based onthe size of itsparticles, likesandy, silty, orclayey.The processof diggingminerals orores out ofthe earth.The speedat whichwater soaksinto the soil.A type of rockthat containsenoughminerals to bemined for profit.How easilywater or aircan passthrough soilor rock.Large soilparticles thatfeel gritty anddrain waterquickly.The solidrock layerbeneath soiland looserocks.Characteristicsof soil liketexture, color,and moisture.Material fromdead plantsand animals inthe soil thathelps plantsgrow.Naturalresources thatcan be replacedor grownagain,like sunlight,wind, and trees.The amount ofempty space insoil or rockthat can holdair or water.A very fine soilparticle thatfeels stickywhen wet andhard when dry.Fine soilparticles thatare smallerthan sand butbigger thanclay.Non-livingmaterials in soillike mineralsand tiny rockpieces.Fuels like coal,oil, and naturalgas formedfrom ancientplants andanimals.The color ofsoil, which canshow what it’smade of or howhealthy it is.Rock that hasbeen brokendown intosmaller piecesby weather.The processof fixingdamaged landso it can beused again.Materials fromnature thatpeople use, likewater, wood,and minerals.Resourcesthat cannot bereplaced onceused, like coaland oil.Dark, richorganicmaterial in soilmade fromdecayed plantsand animals.A type of soilmade up of amix of sand,silt, and claythat is good forgrowing plants.What soil ismade of,includingminerals,organic matter,air, and water.The uppermostsoil layer rich inorganic matterwhere mostplants grow.The layer ofsoil below thetopsoil that hasless organicmatter.A layer of soilthat has differentcolor or texturefrom the layersabove or belowit.The processwhere soil orrock is wornaway by wind,water, or ice.The breakingdown of rocksand mineralsby wind, water,or chemicals.The feel of thesoil based onthe size of itsparticles, likesandy, silty, orclayey.The processof diggingminerals orores out ofthe earth.The speedat whichwater soaksinto the soil.A type of rockthat containsenoughminerals to bemined for profit.

Soils Terminology Bingo - 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. How easily water or air can pass through soil or rock.
  2. Large soil particles that feel gritty and drain water quickly.
  5. The solid rock layer beneath soil and loose rocks.
  6. Characteristics of soil like texture, color, and moisture.
  7. Material from dead plants and animals in the soil that helps plants grow.
  9. Natural resources that can be replaced or grownagain, like sunlight, wind, and trees.
  10. The amount of empty space in soil or rock that can hold air or water.
  11. A very fine soil particle that feels sticky when wet and hard when dry.
  12. Fine soil particles that are smaller than sand but bigger than clay.
  13. Non-living materials in soil like minerals and tiny rock pieces.
  14. Fuels like coal, oil, and natural gas formed from ancient plants and animals.
  15. The color of soil, which can show what it’s made of or how healthy it is.
  16. Rock that has been broken down into smaller pieces by weather.
  17. The process of fixing damaged land so it can be used again.
  18. Materials from nature that people use, like water, wood, and minerals.
  19. Resources that cannot be replaced once used, like coal and oil.
  20. Dark, rich organic material in soil made from decayed plants and animals.
  21. A type of soil made up of a mix of sand, silt, and clay that is good for growing plants.
  23. What soil is made of, including minerals, organic matter, air, and water.
  25. The uppermost soil layer rich in organic matter where most plants grow.
  28. The layer of soil below the topsoil that has less organic matter.
  29. A layer of soil that has different color or texture from the layers above or below it.
  30. The process where soil or rock is worn away by wind, water, or ice.
  31. The breaking down of rocks and minerals by wind, water, or chemicals.
  32. The feel of the soil based on the size of its particles, like sandy, silty, or clayey.
  33. The process of digging minerals or ores out of the earth.
  35. The speed at which water soaks into the soil.
  36. A type of rock that contains enough minerals to be mined for profit.