1. TODAY Get out your ESRT and a piece of paper The following questions are from your ESRT. You’ll have a minute per question…

2. Question 1 What are 2 examples of weathering?

3. Question 2 What is the difference between soil and dirt?

4. Question 3 What is the P-wave travel time for 4000 km?

5. Question 4 What layer of the earth has a greater temperature than melting point?

6. Answers Two examples –Abrasion, Frost action Soil and Dirt? –Darker, particle size P-wave travel time for 4000 km? –00:07:00 What layer of the earth has a greater temperature than melting point? –Outer Core

7. Erosion Movement of weathered particles

8. Vocab Agents of erosion Suspension Saltation Creep Angle of repose Mass wasting

9. Weathering Vs Erosion Weathering –Breaking down of rocks and other particles into smaller pieces Erosion –Transport of the weathered particles. TALUS ?

10. Agents of Erosion 1)Gravity 2)Water 3)Wind 4)Ice

11. Water Water when driven by gravity can be very powerful. Think of the drainage ditch after it rains – does the water flow fast? Is it clean?

12. Wind 3 things to know. 1.Suspension – Stuff in the air 2.Saltation – Bouncing 3.Creep – Rolling on the ground Dust bowl, Causes???

13. Ice Glaciers move ice down a slope picking up sediments along the way. Long Island is simply glacial Poop!

14. Gravity Gravity drives all erosion, but one form more important to know is mass movements. This is when the soil fails and falls or slides down a slope. Angle Of Repose –Angle where material stays on surface!

15. Mass movements Slump –This is when the land slides down equally. Slide –This is when the land slides down not equally. Fall- avalanche –The land falls Flow –The land is liquefied and flows down.

16. Things that will increase mass movements 1.Change water content 2.Change slope 3.Change mass 4.Change vegetation 5.Change human activity

17. Tully Landslide ‘91 http://pubs.usgs.gov/of/1994/ofr-94-0615/tvstudy.htm ¼ mile

18. Tully Landslide April 30, 1993. After a long winter full of rain and snow. The saturated land gave away and began to flow down the hill.

19. Deposition What is this? What controls this?

20. Deposition This is like going to the bank geologically. Weathering breaks the rocks up Erosion moves the particles. Deposition leaves the particles on the ground.

21. Factors Particle Size –How big the sediments are. Shape –Round or flat Density –Weight and composition Settling rates –How fast things settle

22. Sorting Vs Unsorted ESRT page How to find sediment size. How to find Speed.

23. Ways to deposit Glaciers –Sorted or Unsorted Streams (Water) –Sorted or Unsorted Wind –Sorted or Unsorted Mass movements (gravity) –Sorted or Unsorted

24. Gravity Gravity alone does not sort sediment Landslides are the main form of gravity deposition. Why are sediments unsorted?

25. Glaciers Glaciers leave sediment unsorted. Like gravity Land slides What moves the glacier?

26. Water Streams, Rivers deposit sediment in sorted layers. Why are sediments sorted?

27. Wind Wind like water sorts sediments. Why are sediments sorted?

28. Wind Wind like water sorts sediments. Why are sediments sorted?