A type of rockthat containsenoughminerals to bemined for profit.The uppermostsoil layer rich inorganic matterwhere mostplants grow.The amount ofempty space insoil or rockthat can holdair or water.The processwhere soil orrock is wornaway by wind,water, or ice.Large soilparticles thatfeel gritty anddrain waterquickly.Dark, richorganicmaterial in soilmade fromdecayed plantsand animals.The solidrock layerbeneath soiland looserocks.Rock that hasbeen brokendown intosmaller piecesby weather.A very fine soilparticle thatfeels stickywhen wet andhard when dry.The processof diggingminerals orores out ofthe earth.The feel of thesoil based onthe size of itsparticles, likesandy, silty, orclayey.The speedat whichwater soaksinto the soil.A type of soilmade up of amix of sand,silt, and claythat is good forgrowing plants.Characteristicsof soil liketexture, color,and moisture.The layer ofsoil below thetopsoil that hasless organicmatter.The breakingdown of rocksand mineralsby wind, water,or chemicals.The processof fixingdamaged landso it can beused again.Materials fromnature thatpeople use, likewater, wood,and minerals.The color ofsoil, which canshow what it’smade of or howhealthy it is.A layer of soilthat has differentcolor or texturefrom the layersabove or belowit.Resourcesthat cannot bereplaced onceused, like coaland oil.Naturalresources thatcan be replacedor grownagain,like sunlight,wind, and trees.Material fromdead plantsand animals inthe soil thathelps plantsgrow.Non-livingmaterials in soillike mineralsand tiny rockpieces.What soil ismade of,includingminerals,organic matter,air, and water.How easilywater or aircan passthrough soilor rock.Fuels like coal,oil, and naturalgas formedfrom ancientplants andanimals.Fine soilparticles thatare smallerthan sand butbigger thanclay.A type of rockthat containsenoughminerals to bemined for profit.The uppermostsoil layer rich inorganic matterwhere mostplants grow.The amount ofempty space insoil or rockthat can holdair or water.The processwhere soil orrock is wornaway by wind,water, or ice.Large soilparticles thatfeel gritty anddrain waterquickly.Dark, richorganicmaterial in soilmade fromdecayed plantsand animals.The solidrock layerbeneath soiland looserocks.Rock that hasbeen brokendown intosmaller piecesby weather.A very fine soilparticle thatfeels stickywhen wet andhard when dry.The processof diggingminerals orores out ofthe earth.The feel of thesoil based onthe size of itsparticles, likesandy, silty, orclayey.The speedat whichwater soaksinto the soil.A type of soilmade up of amix of sand,silt, and claythat is good forgrowing plants.Characteristicsof soil liketexture, color,and moisture.The layer ofsoil below thetopsoil that hasless organicmatter.The breakingdown of rocksand mineralsby wind, water,or chemicals.The processof fixingdamaged landso it can beused again.Materials fromnature thatpeople use, likewater, wood,and minerals.The color ofsoil, which canshow what it’smade of or howhealthy it is.A layer of soilthat has differentcolor or texturefrom the layersabove or belowit.Resourcesthat cannot bereplaced onceused, like coaland oil.Naturalresources thatcan be replacedor grownagain,like sunlight,wind, and trees.Material fromdead plantsand animals inthe soil thathelps plantsgrow.Non-livingmaterials in soillike mineralsand tiny rockpieces.What soil ismade of,includingminerals,organic matter,air, and water.How easilywater or aircan passthrough soilor rock.Fuels like coal,oil, and naturalgas formedfrom ancientplants andanimals.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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  1. A type of rock that contains enough minerals to be mined for profit.
  3. The uppermost soil layer rich in organic matter where most plants grow.
  4. The amount of empty space in soil or rock that can hold air or water.
  5. The process where soil or rock is worn away by wind, water, or ice.
  6. Large soil particles that feel gritty and drain water quickly.
  7. Dark, rich organic material in soil made from decayed plants and animals.
  8. The solid rock layer beneath soil and loose rocks.
  9. Rock that has been broken down into smaller pieces by weather.
  10. A very fine soil particle that feels sticky when wet and hard when dry.
  12. The process of digging minerals or ores out of the earth.
  13. The feel of the soil based on the size of its particles, like sandy, silty, or clayey.
  14. The speed at which water soaks into the soil.
  15. A type of soil made up of a mix of sand, silt, and clay that is good for growing plants.
  16. Characteristics of soil like texture, color, and moisture.
  17. The layer of soil below the topsoil that has less organic matter.
  18. The breaking down of rocks and minerals by wind, water, or chemicals.
  22. The process of fixing damaged land so it can be used again.
  23. Materials from nature that people use, like water, wood, and minerals.
  24. The color of soil, which can show what it’s made of or how healthy it is.
  25. A layer of soil that has different color or texture from the layers above or below it.
  26. Resources that cannot be replaced once used, like coal and oil.
  27. Natural resources that can be replaced or grownagain, like sunlight, wind, and trees.
  28. Material from dead plants and animals in the soil that helps plants grow.
  30. Non-living materials in soil like minerals and tiny rock pieces.
  31. What soil is made of, including minerals, organic matter, air, and water.
  33. How easily water or air can pass through soil or rock.
  34. Fuels like coal, oil, and natural gas formed from ancient plants and animals.
  36. Fine soil particles that are smaller than sand but bigger than clay.