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True or False: The Earths surface has stayed the same for thousands of years.

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Presentation on theme: "True or False: The Earths surface has stayed the same for thousands of years."— Presentation transcript:

1 True or False: The Earths surface has stayed the same for thousands of years

2 The Earths surface is always changing!

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8 Weathering The breakdown do the materials of Earths crust into smaller pieces.

9 Water causes weathering What evidence of weathering do you see in this picture?

10 Wind causes weathering What evidence of weathering do you see in this picture? Why wasnt this mass of land weathered away?

11 Ice causes weathering Describe how ice causes weathering?

12 Erosion The process by which water, ice, wind or gravity moves fragments of rock and soil. What evidence of erosion do you see in this picture?

13 Erosion is Movement of Sediment ! This process, known as Erosion, is gradually wearing down the surface of the earth. Erosion is the process by which weathered rock and soil (sediment) are moved from one place to another. Erosion carves the Earth's surface creating canyons, gorges, and even beaches. What do you think has caused this rock to look this way?

14 Wind Erosion As the wind blows it picks up small particles of sand/sediment and blasts large rocks with the abrasive particles, cutting and shaping the rock. The intensity of wind erosion is determined by: Sum (amount) Speed Slope Surface

15 Wind Erosion

16 Water Causes Erosion runoff, rivers and, streams

17 Water causes Erosion When rain falls to the Earth it can evaporate, sink into the ground, or flow over the land as Runoff. When it flows over land, erosion occurs. Runoff picks up pieces of rock and "runs" downhill cutting tiny grooves (called rills) into the land. rills

18 Water causes Erosion How much erosion takes place is determined by the: Sum (amount) Slope Speed Surface Can you act increasing and decreasing the four Ss?

19 Ice Causes Erosion Glaciers wear down the landscape; by picking up and carrying debris that moves across the land along with the ice.

20 Ice Causes Erosion Glaciers can pick up and carry sediment that ranges in size from sand grains to boulders bigger than houses. Moving like a conveyor belt and a bulldozer, a single glacier can move millions of tons of material!

21 Ice Causes Erosion How much erosion takes place is determined by the: **Sum (Glaciers are massive!) Slope Speed Surface

22 Gravity causes erosion landslide clip.mpeg Creep, Slump, Landslides, Mudslides, and Avalanches. These are examples of mass movement (or called mass wasting) SlowerFaster

23 Gravity causes Erosion How much erosion takes place is determined by the: Sum **Slope Speed **Surface

24 Plants CAN CAUSE weathering

25 Plants CAN PREVENT erosion

26 Deposition Rock particles that are picked up and transported during erosion will ultimately be deposited somewhere else Deposition is the process by which sediments (small particles of rock) are laid down in new locations. Together, Erosion and Deposition build new landforms. Deltas Canyons Meanders Floodplains

27 Delta Where rivers meet the ocean is called the mouth of the river. Soil and dirt carried by these rivers is deposited at the mouth, and new land is formed. The new, soil-rich land is known as a Delta

28 Canyons This simple animation provides you with a visualization of how the Colorado River has "downcut" into the rock layers of the Grand Canyon. How long it took to carve the Grand Canyon is debated by geologists. Some estimates are between 6 and 8 million years, which is very recent by comparison. Canyons are large valleys created by a river or stream.

29 Meanders Meandering streams wander side to side as they constantly seek out the lowest elevation. This constant motion creates a series of S-shaped loops.

30 Meanders Stream Velocity varies from one side to the other side of the S, resulting in erosion in some places and deposition of sediments in others.

31 Floodplains Floodplains form along the banks of mid-order streams and larger rivers. These are low-lying areas along the sides of a river channel that have regular times of heavy waterflow to cause the river to spill over and flood the land.

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