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

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