Presentation is loading. Please wait.

Presentation is loading. Please wait.

YehliuTaiwan-HoneycombWeathering

Similar presentations


Presentation on theme: "YehliuTaiwan-HoneycombWeathering"— Presentation transcript:

1 YehliuTaiwan-HoneycombWeathering
Weathering The process of breaking down of rocks into smaller and smaller pieces of rock. These small pieces are known as sediment. Sediment breaks down further and becomes soil. YehliuTaiwan-HoneycombWeathering 180px-GeologicalExfoliationOfGraniteRock

2 Types of Weathering Mechanical/ Physical Weathering
Chemical Weathering

3 Types of Mechanical Weathering
Ice Wedging- Water in the cracks of rocks freeze Abrasion- Particles of sand are carried by the wind and water Plant Action – roots from plants grow in the cracks of rocks Release pressure – when pressure is removed from rocks

4 Chemical Weathering The process in which the chemical makeup of a rock is changed by a chemical reaction.

5 Types of Chemical Weathering
Oxidation – a chemical change that occurs when oxygen and iron form. Acids – natural acids break down rock.

6 Erosion Erosion takes rocks and other particles from one location and puts them in another. Weathering is breaking up rocks erosion is carrying them away.

7 The Agents of Erosion Wind Water Glaciers Gravity / Mass Movement

8 Wind Erosion Wind can carry sand, silt, and clay from one place and deposit it in another. This type of erosion is most frequent in dry areas with little or no vegetation.

9 Wind Erosion

10 Water Erosion The most important agent of erosion is running water.
Water runs down hill and form a gully by taking away sediment. Water continues to flow in the gully and eventually forming a valley. Water can cause erosion of the shore line can be from waves in the ocean.

11 Water Erosion

12 Water Erosion

13 Glaciers Erosion Glacier Erosion is sometimes referred to as Ice Erosion Glaciers move slowly across land picking up large rocks and even larger boulders. Glaciers can cause deep valleys to form as they move across the land.

14 Glaciers Erosion

15 Gravity/Mass Movement Erosion
Gravity is the force behind Water and Glacier Erosion Gravity alone can cause Erosion

16 Gravity/Mass Movement Erosion

17 Types of Gravity/Mass Movement Erosion
Slump Creep Rockfalls Rockslides Mudflows Landslides

18 Slump A slump occurs when a mass of land slips and moves down a slope.
A slump occurs when the slope becomes too steep and the material under it can not support the ground above it.

19 Creep Sediment slowly moves down hill.
Leaning trees and fence post are clues that creeping is occurring

20

21 Rockfalls Occur when parts of a rock break off a tumble through the air.

22 Rockslides Large and small rock slide down a slope.

23 Mudflows Happen after heavy rains.
More likely to occur when there is a lack of vegetation. Gravity pulls on the heavy water saturated sediment and causes it to flow down hill.

24 Landslides A movement of land down a slope.

25 Deposition Process by which sediments, soil and rocks are added to a landform or land mass (the end of erosion).


Download ppt "YehliuTaiwan-HoneycombWeathering"

Similar presentations


Ads by Google