![Spreading on land - Rift valleys ,[object Object],[object Object]](https://image.slidesharecdn.com/thelithosphere-110907140154-phpapp02/75/the-lithosphere-14-2048.jpg?cb=1668210711)
![Convergent (destructive) boundaries ,[object Object],[object Object],[object Object]](https://image.slidesharecdn.com/thelithosphere-110907140154-phpapp02/75/the-lithosphere-20-2048.jpg?cb=1668210711)
![So, how come we have volcanoes away from plate boundaries? ,[object Object],[object Object]](https://image.slidesharecdn.com/thelithosphere-110907140154-phpapp02/75/the-lithosphere-25-2048.jpg?cb=1668210711)
![[object Object],[object Object]](https://image.slidesharecdn.com/thelithosphere-110907140154-phpapp02/75/the-lithosphere-31-2048.jpg?cb=1668210711)
![There are 3 types of weathering ,[object Object],[object Object],[object Object],[object Object]](https://image.slidesharecdn.com/thelithosphere-110907140154-phpapp02/75/the-lithosphere-35-2048.jpg?cb=1668210711)
![Mechanical weathering ,[object Object],[object Object]](https://image.slidesharecdn.com/thelithosphere-110907140154-phpapp02/75/the-lithosphere-36-2048.jpg?cb=1668210711)
![Factors that influence rates of weathering ,[object Object],[object Object],[object Object],[object Object]](https://image.slidesharecdn.com/thelithosphere-110907140154-phpapp02/75/the-lithosphere-39-2048.jpg?cb=1668210711)
![[object Object]](https://image.slidesharecdn.com/thelithosphere-110907140154-phpapp02/75/the-lithosphere-40-2048.jpg?cb=1668210711)
![Chalk scenery ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]](https://image.slidesharecdn.com/thelithosphere-110907140154-phpapp02/75/the-lithosphere-47-2048.jpg?cb=1668210711)
![Granite scenery ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]](https://image.slidesharecdn.com/thelithosphere-110907140154-phpapp02/75/the-lithosphere-49-2048.jpg?cb=1668210711)
![Types of mass movement ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]](https://image.slidesharecdn.com/thelithosphere-110907140154-phpapp02/75/the-lithosphere-57-2048.jpg?cb=1668210711)
![Heaves ,[object Object]](https://image.slidesharecdn.com/thelithosphere-110907140154-phpapp02/75/the-lithosphere-59-2048.jpg?cb=1668210711)
![Flows ,[object Object],[object Object],[object Object],[object Object],[object Object]](https://image.slidesharecdn.com/thelithosphere-110907140154-phpapp02/75/the-lithosphere-60-2048.jpg?cb=1668210711)
![Soil creep ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]](https://image.slidesharecdn.com/thelithosphere-110907140154-phpapp02/75/the-lithosphere-62-2048.jpg?cb=1668210711)
![Solifluction ,[object Object],[object Object],[object Object],Solifluction lobes](https://image.slidesharecdn.com/thelithosphere-110907140154-phpapp02/75/the-lithosphere-65-2048.jpg?cb=1668210711)
![Earthflow (debris flow) ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]](https://image.slidesharecdn.com/thelithosphere-110907140154-phpapp02/75/the-lithosphere-67-2048.jpg?cb=1668210711)
![Aberfan ,[object Object],[object Object],[object Object]](https://image.slidesharecdn.com/thelithosphere-110907140154-phpapp02/75/the-lithosphere-69-2048.jpg?cb=1668210711)
![Mudflow (mudslide) ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]](https://image.slidesharecdn.com/thelithosphere-110907140154-phpapp02/75/the-lithosphere-70-2048.jpg?cb=1668210711)
![Slides/Falls ,[object Object],[object Object],[object Object],[object Object],[object Object]](https://image.slidesharecdn.com/thelithosphere-110907140154-phpapp02/75/the-lithosphere-73-2048.jpg?cb=1668210711)
![Landslide ,[object Object],[object Object],[object Object]](https://image.slidesharecdn.com/thelithosphere-110907140154-phpapp02/75/the-lithosphere-75-2048.jpg?cb=1668210711)
![Rotational slump (slip) ,[object Object],[object Object],[object Object]](https://image.slidesharecdn.com/thelithosphere-110907140154-phpapp02/75/the-lithosphere-82-2048.jpg?cb=1668210711)
![Debris/rock avalanche ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]](https://image.slidesharecdn.com/thelithosphere-110907140154-phpapp02/75/the-lithosphere-84-2048.jpg?cb=1668210711)
![Huascaran avalanche – Peru, 1970 ,[object Object],[object Object],[object Object]](https://image.slidesharecdn.com/thelithosphere-110907140154-phpapp02/75/the-lithosphere-85-2048.jpg?cb=1668210711)
![[object Object],[object Object]](https://image.slidesharecdn.com/thelithosphere-110907140154-phpapp02/75/the-lithosphere-86-2048.jpg?cb=1668210711)
The lithosphere
•1 gostou•3,094 visualizações
Denunciar
Compartilhar
Baixar para ler offline
Mais conteúdo relacionado
Mais procurados
Mais procurados(20)
Destaque
Destaque(10)
Similar a The lithosphere
Similar a The lithosphere(20)
Último
Último(20)
The lithosphere
- 4. Why do the plates move?
- 5. Why do the plates move?
- 6. Plate names African Indo-Australian Plate North American South American Eurasian Pacific Nazca Antarctic Pacific
- 7. Plate names
- 10. Divergent (extensional) plate boundary (you might know it as a constructive boundary – don’t use this term)
- 13. How do we know the sea floor is spreading?
- 16. East Africa: The Great Rift Valley
- 17. East Africa: The Great Rift Valley
- 21. Convergent (destructive) plate boundary (1) Subduction zone
- 22. Convergent (destructive) plate boundary (2)
- 23. Convergent (destructive) plate boundary (3)
- 28. This measures how much damage is caused by the earthquake based on observations. It is measured on a scale between I and XII. Mercalli Scale Mercalli Scale
- 34. Weathering What is the difference between weathering & erosion? Weathering is the breakdown of material caused by climactic conditions and weather action upon the rock. Erosion is the wearing away by constant forces related to, but not directly caused by temperature change or climactic conditions. Weathering creates the process we know of as Denudation.
- 42. Pothole Grike Clint Sinkhole Limestone pavement
- 64. Examples of soil creep