SlideShare une entreprise Scribd logo
1  sur  24
What’s this?
Himalaya / Tibetan Plateau formation – key words starter ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Learning objectives ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Can you remember how Tibet / The Himalayas were formed?
Amazing Earth – Himalaya Rising
(130 Mya)
 
 
 
 
 
 
On these two pictures, think about what happens to the sediment in the bottom of the disappearing ocean  (can you predict?) So, what  has  happened to it? Truth is,  some  has gone down here (subducted), and… … some has been squashed right up here, to the top of the highest mountains
Click for animation video
Both of these things are important in understanding plate tectonics. The subducted sediment (and water) is what causes the melting (and so the volcanoes), by adding impurities to the mantle (like adding salt to ice) The sediments being squashed to the top result in the amazing truth that the highest mountains are made from material from the bottom of the ocean.
What is this fossil called? Ammonites like this are found in the Himalayas. This is how they lived when they were alive. They lived in the oceans. So how come they are found in the highest mountains?
 
After Collision
You can see on this slide that the continental rocks get ‘squashed’ when they are put under great pressure (and buried, so they heat up). Geology teachers often say it behaves like plasticine. This is an important thing to understand about continental rocks: when heated and pressurised, they behave  plastically  (i.e. they squash not snap – unlike the oceanic crust, which does not squash – i.e. it is  rigid .)
Indian plate Eurasian plate This is getting ‘squished’ sideways! Where is the Indian plate? What is the name of the other plate? Which direction are they moving?
 
1 1 2 6 8 3 9 10 5 4 The formation of Himalaya / Tibet  ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],NAME: ........................................ 7
1 1 2 6 8 3 7 9 10 5 4 The formation of Himalaya / Tibet  ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],8 3 1 2 9 10 7 6 5 4 8 3 1 3 1 8 3 1 2 9 1 2 9 3 1 2 9 8 3 1 8 3 2 1 8 3 9 2 1 8 3 10 9 2 1 8 3 7 10 9 2 1 8 3 6 7 10 9 2 1 8 3 5 4 6 7 10 9 2 1 8 3
Learning objectives ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]

Contenu connexe

En vedette

Coasts Intro Homework
Coasts Intro HomeworkCoasts Intro Homework
Coasts Intro Homework
Kevin Cooper
 
Weathering and erosion
Weathering and erosionWeathering and erosion
Weathering and erosion
Kevin Cooper
 
Coasts Intro Lesson
Coasts Intro LessonCoasts Intro Lesson
Coasts Intro Lesson
Kevin Cooper
 

En vedette (16)

mindsets quiz KC (fixed v growth mindsets - student questionnaire)
mindsets quiz KC (fixed v growth mindsets - student questionnaire)mindsets quiz KC (fixed v growth mindsets - student questionnaire)
mindsets quiz KC (fixed v growth mindsets - student questionnaire)
 
AS geography grey areas and key concepts
AS geography grey areas and key conceptsAS geography grey areas and key concepts
AS geography grey areas and key concepts
 
Arid Spain uses and management KC AQA AS level Geography
Arid Spain uses and management KC AQA AS level GeographyArid Spain uses and management KC AQA AS level Geography
Arid Spain uses and management KC AQA AS level Geography
 
Coasts Intro Test
Coasts Intro TestCoasts Intro Test
Coasts Intro Test
 
Coasts Intro Homework
Coasts Intro HomeworkCoasts Intro Homework
Coasts Intro Homework
 
Tectonic Plates names test
Tectonic Plates names testTectonic Plates names test
Tectonic Plates names test
 
Y8 air pressure weather march 2013
Y8 air pressure weather march 2013Y8 air pressure weather march 2013
Y8 air pressure weather march 2013
 
Tsunamis
TsunamisTsunamis
Tsunamis
 
0008 Talking Essay Kc Adjusted Nicola Gamble
0008 Talking Essay Kc Adjusted Nicola Gamble0008 Talking Essay Kc Adjusted Nicola Gamble
0008 Talking Essay Kc Adjusted Nicola Gamble
 
TRF Sustainable Roles
TRF Sustainable RolesTRF Sustainable Roles
TRF Sustainable Roles
 
A level glaciation millionaire print quiz
A level glaciation millionaire print quizA level glaciation millionaire print quiz
A level glaciation millionaire print quiz
 
Geology OCR A-level igneous rocks terms revision interactive - need to downlo...
Geology OCR A-level igneous rocks terms revision interactive - need to downlo...Geology OCR A-level igneous rocks terms revision interactive - need to downlo...
Geology OCR A-level igneous rocks terms revision interactive - need to downlo...
 
Sustainable Development Of Tropical Rainforests
Sustainable Development Of Tropical RainforestsSustainable Development Of Tropical Rainforests
Sustainable Development Of Tropical Rainforests
 
Rock identification igneous kc
Rock identification igneous kcRock identification igneous kc
Rock identification igneous kc
 
Weathering and erosion
Weathering and erosionWeathering and erosion
Weathering and erosion
 
Coasts Intro Lesson
Coasts Intro LessonCoasts Intro Lesson
Coasts Intro Lesson
 

Similaire à Tibet 4 Continental Collision K Co

Mountain Building
Mountain BuildingMountain Building
Mountain Building
John Barlow
 
Plate Boundaries
Plate BoundariesPlate Boundaries
Plate Boundaries
whiskeyhj
 
Earth Science. Geopshere ppt
Earth Science. Geopshere pptEarth Science. Geopshere ppt
Earth Science. Geopshere ppt
Mrs. Henley
 
Chapter 14new Notes
Chapter 14new NotesChapter 14new Notes
Chapter 14new Notes
basdsci
 
Petrologi 3-difinisi
Petrologi 3-difinisiPetrologi 3-difinisi
Petrologi 3-difinisi
Ovan Geovano
 

Similaire à Tibet 4 Continental Collision K Co (20)

Himalaya Formation Millionaire
Himalaya Formation MillionaireHimalaya Formation Millionaire
Himalaya Formation Millionaire
 
Everest Vs Himalaya
Everest Vs HimalayaEverest Vs Himalaya
Everest Vs Himalaya
 
Mountain Building
Mountain BuildingMountain Building
Mountain Building
 
science 10 ppt.pptx
science 10 ppt.pptxscience 10 ppt.pptx
science 10 ppt.pptx
 
Rocks
RocksRocks
Rocks
 
Types of rocks metamorphic
Types of rocks   metamorphicTypes of rocks   metamorphic
Types of rocks metamorphic
 
Rocks.powerpoint.jocelyn cabling
Rocks.powerpoint.jocelyn cablingRocks.powerpoint.jocelyn cabling
Rocks.powerpoint.jocelyn cabling
 
Plate Boundaries
Plate BoundariesPlate Boundaries
Plate Boundaries
 
The dynamic crust
The dynamic crustThe dynamic crust
The dynamic crust
 
Inside our earth.
Inside our earth.Inside our earth.
Inside our earth.
 
Rock cycle
Rock cycleRock cycle
Rock cycle
 
Rock cycle
Rock cycleRock cycle
Rock cycle
 
Earth Science. Geopshere ppt
Earth Science. Geopshere pptEarth Science. Geopshere ppt
Earth Science. Geopshere ppt
 
The Rock Cycle - Science
The Rock Cycle - ScienceThe Rock Cycle - Science
The Rock Cycle - Science
 
Strata and rocks 2
Strata and rocks 2Strata and rocks 2
Strata and rocks 2
 
Geography 7 cg ch 2 (1)
Geography 7 cg ch 2 (1)Geography 7 cg ch 2 (1)
Geography 7 cg ch 2 (1)
 
Chapter 14new Notes
Chapter 14new NotesChapter 14new Notes
Chapter 14new Notes
 
Petrologi 3-difinisi
Petrologi 3-difinisiPetrologi 3-difinisi
Petrologi 3-difinisi
 
COT PLATE TECTONIC.pptx
COT PLATE TECTONIC.pptxCOT PLATE TECTONIC.pptx
COT PLATE TECTONIC.pptx
 
Types of rocks - the quiz
Types of rocks - the quizTypes of rocks - the quiz
Types of rocks - the quiz
 

Plus de Kevin Cooper (6)

A level glaciation millionaire
A level glaciation millionaireA level glaciation millionaire
A level glaciation millionaire
 
Sustainable development in Masoala / Madagascar
Sustainable development in Masoala / MadagascarSustainable development in Masoala / Madagascar
Sustainable development in Masoala / Madagascar
 
Detroit
DetroitDetroit
Detroit
 
Korea quiz
Korea quizKorea quiz
Korea quiz
 
Anglo chinese glossary for_geography
Anglo chinese glossary for_geographyAnglo chinese glossary for_geography
Anglo chinese glossary for_geography
 
Rio Favelas Etc
Rio Favelas EtcRio Favelas Etc
Rio Favelas Etc
 

Dernier

Activity 01 - Artificial Culture (1).pdf
Activity 01 - Artificial Culture (1).pdfActivity 01 - Artificial Culture (1).pdf
Activity 01 - Artificial Culture (1).pdf
ciinovamais
 
1029 - Danh muc Sach Giao Khoa 10 . pdf
1029 -  Danh muc Sach Giao Khoa 10 . pdf1029 -  Danh muc Sach Giao Khoa 10 . pdf
1029 - Danh muc Sach Giao Khoa 10 . pdf
QucHHunhnh
 

Dernier (20)

Measures of Dispersion and Variability: Range, QD, AD and SD
Measures of Dispersion and Variability: Range, QD, AD and SDMeasures of Dispersion and Variability: Range, QD, AD and SD
Measures of Dispersion and Variability: Range, QD, AD and SD
 
Sports & Fitness Value Added Course FY..
Sports & Fitness Value Added Course FY..Sports & Fitness Value Added Course FY..
Sports & Fitness Value Added Course FY..
 
Advance Mobile Application Development class 07
Advance Mobile Application Development class 07Advance Mobile Application Development class 07
Advance Mobile Application Development class 07
 
Key note speaker Neum_Admir Softic_ENG.pdf
Key note speaker Neum_Admir Softic_ENG.pdfKey note speaker Neum_Admir Softic_ENG.pdf
Key note speaker Neum_Admir Softic_ENG.pdf
 
INDIA QUIZ 2024 RLAC DELHI UNIVERSITY.pptx
INDIA QUIZ 2024 RLAC DELHI UNIVERSITY.pptxINDIA QUIZ 2024 RLAC DELHI UNIVERSITY.pptx
INDIA QUIZ 2024 RLAC DELHI UNIVERSITY.pptx
 
social pharmacy d-pharm 1st year by Pragati K. Mahajan
social pharmacy d-pharm 1st year by Pragati K. Mahajansocial pharmacy d-pharm 1st year by Pragati K. Mahajan
social pharmacy d-pharm 1st year by Pragati K. Mahajan
 
Nutritional Needs Presentation - HLTH 104
Nutritional Needs Presentation - HLTH 104Nutritional Needs Presentation - HLTH 104
Nutritional Needs Presentation - HLTH 104
 
Arihant handbook biology for class 11 .pdf
Arihant handbook biology for class 11 .pdfArihant handbook biology for class 11 .pdf
Arihant handbook biology for class 11 .pdf
 
Class 11th Physics NEET formula sheet pdf
Class 11th Physics NEET formula sheet pdfClass 11th Physics NEET formula sheet pdf
Class 11th Physics NEET formula sheet pdf
 
Holdier Curriculum Vitae (April 2024).pdf
Holdier Curriculum Vitae (April 2024).pdfHoldier Curriculum Vitae (April 2024).pdf
Holdier Curriculum Vitae (April 2024).pdf
 
Call Girls in Dwarka Mor Delhi Contact Us 9654467111
Call Girls in Dwarka Mor Delhi Contact Us 9654467111Call Girls in Dwarka Mor Delhi Contact Us 9654467111
Call Girls in Dwarka Mor Delhi Contact Us 9654467111
 
Measures of Central Tendency: Mean, Median and Mode
Measures of Central Tendency: Mean, Median and ModeMeasures of Central Tendency: Mean, Median and Mode
Measures of Central Tendency: Mean, Median and Mode
 
Activity 01 - Artificial Culture (1).pdf
Activity 01 - Artificial Culture (1).pdfActivity 01 - Artificial Culture (1).pdf
Activity 01 - Artificial Culture (1).pdf
 
1029 - Danh muc Sach Giao Khoa 10 . pdf
1029 -  Danh muc Sach Giao Khoa 10 . pdf1029 -  Danh muc Sach Giao Khoa 10 . pdf
1029 - Danh muc Sach Giao Khoa 10 . pdf
 
Mattingly "AI & Prompt Design: Structured Data, Assistants, & RAG"
Mattingly "AI & Prompt Design: Structured Data, Assistants, & RAG"Mattingly "AI & Prompt Design: Structured Data, Assistants, & RAG"
Mattingly "AI & Prompt Design: Structured Data, Assistants, & RAG"
 
Grant Readiness 101 TechSoup and Remy Consulting
Grant Readiness 101 TechSoup and Remy ConsultingGrant Readiness 101 TechSoup and Remy Consulting
Grant Readiness 101 TechSoup and Remy Consulting
 
Unit-IV- Pharma. Marketing Channels.pptx
Unit-IV- Pharma. Marketing Channels.pptxUnit-IV- Pharma. Marketing Channels.pptx
Unit-IV- Pharma. Marketing Channels.pptx
 
SOCIAL AND HISTORICAL CONTEXT - LFTVD.pptx
SOCIAL AND HISTORICAL CONTEXT - LFTVD.pptxSOCIAL AND HISTORICAL CONTEXT - LFTVD.pptx
SOCIAL AND HISTORICAL CONTEXT - LFTVD.pptx
 
microwave assisted reaction. General introduction
microwave assisted reaction. General introductionmicrowave assisted reaction. General introduction
microwave assisted reaction. General introduction
 
Accessible design: Minimum effort, maximum impact
Accessible design: Minimum effort, maximum impactAccessible design: Minimum effort, maximum impact
Accessible design: Minimum effort, maximum impact
 

Tibet 4 Continental Collision K Co

  • 2.
  • 3.
  • 4. Can you remember how Tibet / The Himalayas were formed?
  • 5. Amazing Earth – Himalaya Rising
  • 7.  
  • 8.  
  • 9.  
  • 10.  
  • 11.  
  • 12.  
  • 13. On these two pictures, think about what happens to the sediment in the bottom of the disappearing ocean (can you predict?) So, what has happened to it? Truth is, some has gone down here (subducted), and… … some has been squashed right up here, to the top of the highest mountains
  • 15. Both of these things are important in understanding plate tectonics. The subducted sediment (and water) is what causes the melting (and so the volcanoes), by adding impurities to the mantle (like adding salt to ice) The sediments being squashed to the top result in the amazing truth that the highest mountains are made from material from the bottom of the ocean.
  • 16. What is this fossil called? Ammonites like this are found in the Himalayas. This is how they lived when they were alive. They lived in the oceans. So how come they are found in the highest mountains?
  • 17.  
  • 19. You can see on this slide that the continental rocks get ‘squashed’ when they are put under great pressure (and buried, so they heat up). Geology teachers often say it behaves like plasticine. This is an important thing to understand about continental rocks: when heated and pressurised, they behave plastically (i.e. they squash not snap – unlike the oceanic crust, which does not squash – i.e. it is rigid .)
  • 20. Indian plate Eurasian plate This is getting ‘squished’ sideways! Where is the Indian plate? What is the name of the other plate? Which direction are they moving?
  • 21.  
  • 22.
  • 23.
  • 24.