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

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