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Section3  From Bedrock to Soil Chapter 7 The Source of Soil ,[object Object]
Not all soils are the same. Because soils are made from weathered rock fragments, the types of soil that forms depends on the type of rock that weathers.
The rock formation that is the source of mineral fragments in the soil is called parent rock.,[object Object]
Sometimes, the bedrock is the parent rock if the soil above it formed from the bedrock below. Soil that remains above its parent rock is called residual soil.
Soil that is blown or washed away from its parent rock is called transported soil.,[object Object]
Waves usually play a major role in building up and breaking down the shoreline. A shoreline is the boundary between land and a body of water.,[object Object]
The wind that results from summer hurricanes and severe winter storms produces large waves that cause dramatic shoreline erosion.,[object Object]
The upper part of the wave moves more rapidly and grows taller, and begins to curl and break. These breaking waves are known as surf.
The time interval between breaking waves is called the wave period.,[object Object]
Section1  Shoreline Erosion and Deposition Chapter 17 Wave Energy, continued ,[object Object]
Breaking waves also wash away fine grains of sand, which are picked up by the waves and wear down and polish coastal rock.
The process continues until rock is broken down in  smaller and smaller pieces that eventually become sand.,[object Object]
Sea cliffs are formed when waves erode and undercut rock to produce steep slopes.
The next two slides show some of the major features that result from wave erosion.,[object Object]
Section1  Shoreline Erosion and Deposition Chapter 17
Section1  Shoreline Erosion and Deposition Chapter 17 Wave Deposits ,[object Object]
Waves carry a variety of materials, including sand, rock fragments, dead coral, and shells.
The colors and textures of beaches vary because the type of material found on a beach depends on its source.,[object Object]
Longshore currents move sand in a zigzag pattern along the beach.,[object Object]
A sandbar is an underwater or exposed ridge of sand, gravel, or shell material.
A barrier spit is an exposed sandbar connected to the shoreline.,[object Object]
Glaciers form in areas so cold that snow stays on the ground year-round. Because glaciers are so massive, the pull of gravity causes them to flow slowly, like “rivers of ice.”,[object Object]
Valley glaciers form in valleys originally created by stream erosion. As these glaciers slowly flow downhill, they widen and straighten the valleys into broad U shapes.,[object Object]
The largest continental glacier in the world covers almost all of Antarctica. This ice sheet is approximately one and a half times the size of the United States, and is more than 4,000 m thick in some places.,[object Object]
Glaciers move in two ways: sliding and flowing. A glacier slides when its weight causes the ice at the bottom to melt. A glacier flows as ice crystals within the glacier slip over each other.,[object Object]

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Unit 3 pp #4 6th grade

  • 1.
  • 2. Not all soils are the same. Because soils are made from weathered rock fragments, the types of soil that forms depends on the type of rock that weathers.
  • 3.
  • 4. Sometimes, the bedrock is the parent rock if the soil above it formed from the bedrock below. Soil that remains above its parent rock is called residual soil.
  • 5.
  • 6.
  • 7.
  • 8. The upper part of the wave moves more rapidly and grows taller, and begins to curl and break. These breaking waves are known as surf.
  • 9.
  • 10.
  • 11. Breaking waves also wash away fine grains of sand, which are picked up by the waves and wear down and polish coastal rock.
  • 12.
  • 13. Sea cliffs are formed when waves erode and undercut rock to produce steep slopes.
  • 14.
  • 15. Section1 Shoreline Erosion and Deposition Chapter 17
  • 16.
  • 17. Waves carry a variety of materials, including sand, rock fragments, dead coral, and shells.
  • 18.
  • 19.
  • 20. A sandbar is an underwater or exposed ridge of sand, gravel, or shell material.
  • 21.
  • 22.
  • 23.
  • 24.
  • 25.
  • 26.
  • 27. Continental glaciers smooth the landscape by scraping and eroding features that existed before the ice appeared.
  • 28.
  • 29.
  • 30.
  • 31.
  • 32. Streams carry sorted material and deposit it in front of the glacier in a broad area called an outwash plain.
  • 33.