GGR 2A10/GGR02A2

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Across
  1. 3. Physical, chemical and minerological characteristics of surficial material
  2. 4. The weathered material lying above the unaltered fresh bedrock.
  3. 5. The repeated cycle of ice formation and ice melt in the pore spaces and fractures of rocks causing disintegration of the rock.
  4. 10. the chemical weathering of chalk and limestone rocks by rain Fall
  5. 11. are depositional contacts that overlie rocks distinctly older than they are.
  6. 12. weathering causes the rocks to decompose.
  7. 13. This means the rocks fall apart into smaller pieces.
  8. 14. the process when ice turns to water.
  9. 15. refers to particle size or the range of particle sizes
  10. 16. sequence of layers in which individual layers are not horizontal but incline down stream
  11. 17. refers to layers (if any) or bending within surficial material
  12. 18. Many pedons together in one area make up a ____
  13. 19. weathering causes the rocks to disintegrate.
Down
  1. 1. The chemical reaction between some minerals in rocks and the oxygen in the air.
  2. 2. Rock formed by magma or lava cooling.
  3. 6. is when pieces of the outer layer of rock break away.
  4. 7. The weathering _____ is the boundary between fresh and weathered rock.
  5. 8. the isolate rock hills created by long term weathering and erosion
  6. 9. the rock formed by layers of sediment under water.
  7. 17. (ψ) describes how closely a rock particle resembles a sphere.