2. How Is Soil Formed?  Have you ever squished your toes in a muddy garden?

3. How Is Soil Formed?  Have you ever squished your toes in a muddy garden?  What did if feel like?

4. How Is Soil Formed?  Have you ever squished your toes in a muddy garden?  What did if feel like?  What materials combine to make mud?

5. How Is Soil Formed?  Have you ever squished your toes in a muddy garden?  What did if feel like?  What materials combine to make mud?  Is all mud the same? Why or why not?

6. Soil Formation  Over time, materials are deposited and eventually mix with air, water, and decayed organic matter, or humus, to form soil.

7. Soil Formation  Over time, materials are deposited and eventually mix with air, water, and decayed organic matter, or humus, to form soil.  Soil forms from the surface downward and also from the bottom up.

8. Soil Formation  Over time, materials are deposited and eventually mix with air, water, and decayed organic matter, or humus, to form soil.  Soil forms from the surface downward and also from the bottom up.  Soil forms as the result of weathering.

9. Soil Formation  Humus and other decaying materials in the top layer of soil continue to decompose and move lower into the soil profile.

10. Soil Formation  Humus and other decaying materials in the top layer of soil continue to decompose and move lower into the soil profile.  Rock particles from weathered rock lower down in the soil profile move higher up toward the surface.

11. Soil Formation  Humus and other decaying materials in the top layer of soil continue to decompose and move lower into the soil profile.  Rock particles from weathered rock lower down in the soil profile move higher up toward the surface.  The two meet and mix to form the topsoil layer.

12. Soil Formation  Silty soil has much smaller particles than sandy soil, so its is smooth to the touch and retains water longer, and is fairly fertile.

13. Soil Formation  Many of the same factors that control weathering also affect soil development:  Climate  Vegetation  Type of rocks  Time  Topography  Biotic activity

14. Soil Formation  A thicker layer of soil takes more time to form than a thinner layer of soil.

15. Soil Formation  A thicker layer of soil takes more time to form than a thinner layer of soil.  Soils are thinner on steeper slopes than on level land.

16. Soil Formation  A thicker layer of soil takes more time to form than a thinner layer of soil.  Soils are thinner on steeper slopes than on level land.  Soil develops and matures in areas where animals and other organisms burrow into the ground.

17. Soil Formation  A thicker layer of soil takes more time to form than a thinner layer of soil.  Soils are thinner on steeper slopes than on level land.  Soil develops and matures in areas where animals and other organisms burrow into the ground.  Soil also develops more easily in places where plant roots are abundant.

18. Soil Formation In autumn, leaves fall from the trees onto the ground.

19. Soil Formation In autumn, leaves fall from the trees onto the ground. What happens to the leaf litter that falls on the ground?

20. Soil Formation In autumn, leaves fall from the trees onto the ground. What happens to the leaf litter that falls on the ground? The organic matter in the leaf litter is broken down and turned into organic particles that make up the topsoil

21. Soil Formation  While many factors affect soil formation, most soils form distinct layers called soil horizons.

22. Soil Formation  While many factors affect soil formation, most soils form distinct layers called soil horizons.  These layers make up what is called a soil profile.

23. Soil Formation  While many factors affect soil formation, most soils form distinct layers called soil horizons.  These layers make up what is called a soil profile.  A soil profile ends where the unweathered rock, or bedrock, meets the lowermost soil horizon.

24. Soil Formation 0 Horizon  The 0 horizon includes leaf litter, humus, and animal parts.

25. Soil Formation 0 Horizon  The 0 horizon includes leaf litter, humus, and animal parts.  Although this layer contains the most organic matter, it is often the thinnest horizon in nay soil profile.

26. Soil Formation A Horizon  The A horizon is a crumbly mixture of weathered rock and organic material.

27. Soil Formation A Horizon  The A horizon is a crumbly mixture of weathered rock and organic material.  It is often called topsoil.

28. Soil Formation A Horizon  The A horizon is a crumbly mixture of weathered rock and organic material.  It is often called topsoil.  Water moving down through the A horizon leaches, or removes, certain minerals from this soil layer

29. Soil Formation B Horizon  The B horizon is subsoil mostly made up of very fine sediment.

30. Soil Formation B Horizon  The B horizon is subsoil mostly made up of very fine sediment.  Some B horizons are rich in calcium or iron minerals due to the type of underlying rock.

31. Soil Formation B Horizon  The B horizon is subsoil mostly made up of very fine sediment.  Some B horizons are rich in calcium or iron minerals due to the type of underlying rock.  These minerals often form hard pans that do not allow good drainage.

32. Soil Formation C Horizon  The C horizon contains weathered materials as well as some bedrock.

33. Soil Formation C Horizon  The C horizon contains weathered materials as well as some bedrock.  The C horizon usually does not contain any organic matter.

34. Soil Formation  Soils form all over the world.

35. Soil Formation  Soils form all over the world.  Their composition is based on the bedrock in the area.

36. Soil Formation  Soils form all over the world.  Their composition is based on the bedrock in the area.  The climate of the region also contributes to how rapidly the soils form.

37. Soil Formation  Soils form all over the world.  Their composition is based on the bedrock in the area.  The climate of the region also contributes to how rapidly the soils form.  Other factors that help soils form included organisms in the soil, like earthworms.

38. Types of Soil  There are five basic soil types.

39. Types of Soil  There are five basic soil types.  All five are combination of just three types of weathered rock particles that make up the soil:

40. Types of Soil  There are five basic soil types.  All five are combination of just three types of weathered rock particles that make up the soil:  Sand  Silt  Clay

41. Types of Soil  Sandy soil has the largest particles among the different soil types.

42. Types of Soil  Sandy soil has the largest particles among the different soil types.  It is dry and gritty to the touch.

43. Types of Soil  Sandy soil has the largest particles among the different soil types.  It is dry and gritty to the touch.  Because the particles have huge spaces between them, water drains rapidly.

44. Types of Soil  Silty soil has much smaller particles than sandy soil, so it is smooth to the touch.

45. Types of Soil  Silty soil has much smaller particles than sandy soil, so it is smooth to the touch.  Silty soil retains water longer, and is fairly fertile.

46. Types of Soil  Clay soil has the smallest particles, so it has good water-storage qualities.

47. Types of Soil  Clay soil has the smallest particles, so it has good water-storage qualities.  It is sticky to the touch when wet, but smooth when dry.

48. Types of Soil  Peaty soil is dark brown or black in color, soft, easily compressed due to its high water content, and rich in organic matter.

49. Types of Soil  Peaty soil is dark brown or black in color, soft, easily compressed due to its high water content, and rich in organic matter.  Saline soil in extremely dry arid regions is usually brackish because of its high salt content and has poor plant growth potential.