1. Erosion An Examination of the Erosional Agents That Shape Our Land

2. Main Erosional Agents This slideshow explores the transportation variances and depositional features of the four main erosional agents. Rivers Glaciers Wind Ocean Waves Click on the agent to go directly to that section

3. The ‘Jobs’ of the Agents Each erosional agent will be examined in 4 ways: General information Erosion Transportation Deposition

5. River Basics – Energy and Velocity How much stream erosion and how much sediment is transported depends on the energy of the river. The energy of a river depends on The gradient (slope) The rivers discharge Channel characteristics A braided river

6. River Features Meanders form as the stream gradient lowers. The river travels laterally across the flood plain forming large bends. Bends may become cut off (oxbow lakes) during flooding. Edge of flood plain Meanders Oxbow lakes

7. Erosional Features Rivers are one of the most pervasive erosional agents, creating dramatic structures through stream abrasion.

8. River Transportation Rivers transport sediment in three different ways: Solution – dissolved particles Suspension – ‘floating’ particles Bed Load – bouncing & sliding particles

9. Depositional Features Deltas form at the end of rivers/streams as energy drops and sediment settles out. Sediment plumes Back to Table of Contents

11. Glacial Basics A Glacier is a thick ice sheet (min. 50 m) that is always moving. Glaciers cover almost 10% of the Earth’s land surface, however they are located mostly in Antarctica and Greenland. Glaciers move about 2-5 m/day, but can move 10’s of m/day

12. Glacial Features Crevasses are large crack in the ice that can extend down 50 m. Icebergs form at the edge of the ice as the glacier meets the ocean – called calving.

13. 2 Main Glacier Types Continental – Found covering Greenland and Antarctica. Unconfined and large Alpine – Found in mountain ranges and confined to mountain valleys

14. Erosional Features As the glacier moves, sediment in the ice scrapes against the bedrock forming striations or groves. Striations

15. Transportation Glaciers transport sediment in two ways – by rivers in the ice and by material being carried or pushed by the glacier. Rock flour gives the river a green milky appearance

16. Depositional Features Sediment pushed to the edges of the glacier are called moraines. Terminal – at the end Lateral – to the side Medial – in the middle Medial moraine Lateral moraine

17. Depositional Features Drumlins form as the glacier carves out the land. Back to Table of Contents Direction of ice flow

19. Wind Basics Wind is the least powerful of the erosional agents. In order for wind to be most effective, the area must be dry and lacking in vegetation. Deserts are excellent examples of such areas. Dust storms

20. Desert Features While most individuals think of deserts as areas of sand dunes – only about 20% of deserts consist of sand. Most deserts are composed of desert pavement - a rocky, hard packed surface.

21. Deflation – forming Desert Pavement deflation--removal of fine-grained material by the wind--has exposed loose gravels mostly pebbles and cobbles. This makes up the majority of the desert surface.

22. Transportation Most sediment is moved in the form of sand dunes. Sand dunes migrate through the transportation of sand up the gentle upwind side and deposition on the steeper slipface, thus sand is constantly recycled.

23. Deposition Formation of Sand Dunes Dunes are created when loose sand gathers together due to an obstruction The type of dune that forms depends on Amount of wind Amount of sand Amount of vegetation

24. Sand Dunes in the Rx Record The slipface of the sand dune can be preserved in the layers of rock From this To this

25. Back to Table of Contents Types of Dunes

27. Wave Basics Energy from waves is generated by the wind. How much energy depends on Strength of wind Time of blowing Fetch – area the wind blows over

28. Wave Erosion Oceans erode the coastline through abrasion and wave impact.

29. Sediment Transportation Longshore drift allows sediment to move down the coast line. As material is eroded from headlands, it can then be redistributed down the shore.

30. Wave Depositional Features Waves transport material forming barrier bars and sandspits Back to Table of Contents Sandspit Barrier bar

31. Excellent Erosional Resources http://tvl1.geo.uc.edu/ice/Image/imageref.html http://nsidc.org/glaciers/index.html http://pubs.usgs.gov/gip/deserts/

32. The End