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

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