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

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