SlideShare une entreprise Scribd logo
1  sur  38
P.
SANDHYASHREE
SHETTY
WORLD MAP LOCATING THE PLATES
MOVEMEMENT OF THE EARTH
THE MOVEMENT OF
THESE PLATES
CAUSES CHANGES ON
SURFACE ON THEOF
THE EARTH.
THE EARTH
MOVEMENTARE
DIVIDED ONTHE BASIS
OFTHE FORCESWHICH
CAUSETHEM.
THEY ARE:-
ENDOGENIC FORCES
EXOGENIC FORCES
ENDOGENIC FORCES
CONSISTS OF:-
EARTHQUAKE
VOLCANO
LANDSLIDES
HOW DOES EARTHQUAKE OCCUR
DUE TO THE PLATES
VOLCANO
 A volcano is an opening, or rupture, in a
planet's surface or crust, which allows
hot magma, volcanic ash and gases to escape
from the magma chamber below the surface.
 Deep below the Earth's crust, the
temperatures and
pressures are great enough to melt rock.
When this molten
rock blasts to the surface, the result is a
volcano - and for
the inhabitants of the place, it's as if Hell
has been let loose.
 Why doVolcanoes occur?
 Volcanoes occur when the Earth's plates pull apart causing
magma to rise to the surface.Volcanoes can also occur over
hotspots and where one plate dives beneath another,
forcing magma to rise to the surface. Plates diving under
one another is known as subduction.
 Where doVolcanoes occur?
 Volcanoes usually occur on the edges of plates, similar to
where earthquakes occur. A lot of volcanoes occur in the
area around the edge of the Pacific ocean called the Pacific
Ring of Fire.Volcanoes can also occur in the middle of
plates, in hotspots. One such hotspot has formed the
Hawaiian islands chain. As the earth rotated, it passed over
the hotspot and new islands were formed.
LANDSLIDES
 What are landslides and how do they occur?
 Landslides have always existed on our planet.
Generally classified as mass movements of rock,
debris, and soil down a slope of land. While
landslides are a naturally occurring
environmental hazard they have recently
increased in frequency in certain areas due to
human activity. Although there are many
different causes of landslides, they all have two
things in common.They are the results of the
failure of the soil and rock materials that make
up the hill-slope and they are driven by gravity."
EXOGENIC FORCES
• glaciers• wind
• River
and
Seawaves
WORK OF A RIVER
WEATHERING
 Weathering is the breaking down
of rocks, soils and minerals as well as artificial
materials through contact with the Earth's
atmosphere, biota and waters.Weathering
occurs in situ, or "with no movement", and
thus should not be confused with erosion,
which involves the movement of rocks and
minerals by agents such as water, ice, snow,
wind, waves and gravity.
Erosion
The removal of solids like sediments,
soil rocks and other particles in the
natural environment.
THE ERODED
MATERIALS GETS SET
DOWN INTHE EARTH
SURFACE.
 DUETOTHESE PROCESS DIFFERENT
LANDFORMSONTHE SURFACE OFTHE
EARTH .
LANDFORMS FORMED BYTHE RIVER
WATERFALL
 AWATERFALL IS A PLACE WHERE FLOWING
WATER RAPIDLY DRROPS IN ELEVATION AS IT
FLOWS OVER A STEEP REGION OR A CLIFF.
MEANDERS
A meander, in general, is a bend in
a sinuous watercourse or river.A meander is
formed when the moving water in a stream
erodes the outer banks and widens its valley
and the inner part of the river has less energy
and deposits what it is carrying.
OX BOW LAKE
An oxbow is a crescent-shaped lake
lying alongside a winding river.
The oxbow lake is created over
time as erosion and deposits of
soil change the river's course.
FLOODPLAIN
A floodplain or flood plain is an area of land
adjacent to a stream or river that stretches
from the banks of its channel to the base of
the enclosing valley walls and
experiences flooding during periods of high
discharge.
LEVEES
 Naturally formed raised bank along the side of a
river channel are called natural environment .
The river approaches the sea the river begins to
break up into many streams called distributaries
LANDFORMS FORMED BYTHE SEA
WAVES
Dueto continuous strikesof sea wavesat the
rocks,cracks appear in therocks.Changes
appear in the rocks.
LANDFORMS FORMED BY THE
GLACIERS
 THE DEPOSITSOF MATERIAL CARRIED BY
THE GLACIER IS CALLED GLACIAL
MORAINES.
LANDFORMS FORMED BY WIND
SAND DUNES
LOESS
THANKYOU!

Contenu connexe

Tendances

Endogenic processes(Michelle Domingo)
Endogenic processes(Michelle Domingo)Endogenic processes(Michelle Domingo)
Endogenic processes(Michelle Domingo)ericsongwapo2
 
Endogenic influences on geomorphic landscapes
Endogenic influences on geomorphic landscapesEndogenic influences on geomorphic landscapes
Endogenic influences on geomorphic landscapesEsha Aabi
 
Ppt 4 eso the internal processes in the earth (1)
Ppt 4 eso the internal processes in the earth (1)Ppt 4 eso the internal processes in the earth (1)
Ppt 4 eso the internal processes in the earth (1)mmiro
 
2.3 - Internal Forces
2.3 - Internal Forces2.3 - Internal Forces
2.3 - Internal ForcesDan Ewert
 
Ii. c. endogenic processes
Ii. c. endogenic processesIi. c. endogenic processes
Ii. c. endogenic processesMarian Santos
 
GEOG 100--Lecture 13--Earthquakes
GEOG 100--Lecture 13--EarthquakesGEOG 100--Lecture 13--Earthquakes
GEOG 100--Lecture 13--Earthquakesangelaorr
 
Chapter 2 principle of geology 1 meeting
Chapter 2 principle of geology 1 meetingChapter 2 principle of geology 1 meeting
Chapter 2 principle of geology 1 meetingHary Death
 
Chapter 2 section 3
Chapter 2 section 3Chapter 2 section 3
Chapter 2 section 3Jason Hauck
 
Module 2 Week 1 Geologic Cycles
Module 2 Week 1 Geologic CyclesModule 2 Week 1 Geologic Cycles
Module 2 Week 1 Geologic CyclesStuart Kirkham
 
Chapter 6 (other related geological hazard)
Chapter 6 (other related geological hazard)Chapter 6 (other related geological hazard)
Chapter 6 (other related geological hazard)carminajoysibayan1
 
Chapter 12 Volcanoes
Chapter 12 VolcanoesChapter 12 Volcanoes
Chapter 12 Volcanoesllaub
 
Earth Materials and Processes : ENDOGENIC PROCESS
Earth Materials and Processes : ENDOGENIC PROCESSEarth Materials and Processes : ENDOGENIC PROCESS
Earth Materials and Processes : ENDOGENIC PROCESSSimple ABbieC
 
Geology 1: Notes on Earth's geologic forces that shape the crust with video ...
Geology 1:  Notes on Earth's geologic forces that shape the crust with video ...Geology 1:  Notes on Earth's geologic forces that shape the crust with video ...
Geology 1: Notes on Earth's geologic forces that shape the crust with video ...Robin Seamon
 
geography earthquakes ppt
geography  earthquakes pptgeography  earthquakes ppt
geography earthquakes pptvinu74
 
Slides on our changing earth
Slides on our changing earthSlides on our changing earth
Slides on our changing earthvijaybh3
 

Tendances (20)

Endogenic processe sppt
Endogenic processe spptEndogenic processe sppt
Endogenic processe sppt
 
glacier
glacierglacier
glacier
 
Endogenic processes(Michelle Domingo)
Endogenic processes(Michelle Domingo)Endogenic processes(Michelle Domingo)
Endogenic processes(Michelle Domingo)
 
Our earth
Our earthOur earth
Our earth
 
Endogenic influences on geomorphic landscapes
Endogenic influences on geomorphic landscapesEndogenic influences on geomorphic landscapes
Endogenic influences on geomorphic landscapes
 
Ppt 4 eso the internal processes in the earth (1)
Ppt 4 eso the internal processes in the earth (1)Ppt 4 eso the internal processes in the earth (1)
Ppt 4 eso the internal processes in the earth (1)
 
14
1414
14
 
2.3 - Internal Forces
2.3 - Internal Forces2.3 - Internal Forces
2.3 - Internal Forces
 
Nota sains t1 b9
Nota sains t1 b9Nota sains t1 b9
Nota sains t1 b9
 
Ii. c. endogenic processes
Ii. c. endogenic processesIi. c. endogenic processes
Ii. c. endogenic processes
 
GEOG 100--Lecture 13--Earthquakes
GEOG 100--Lecture 13--EarthquakesGEOG 100--Lecture 13--Earthquakes
GEOG 100--Lecture 13--Earthquakes
 
Chapter 2 principle of geology 1 meeting
Chapter 2 principle of geology 1 meetingChapter 2 principle of geology 1 meeting
Chapter 2 principle of geology 1 meeting
 
Chapter 2 section 3
Chapter 2 section 3Chapter 2 section 3
Chapter 2 section 3
 
Module 2 Week 1 Geologic Cycles
Module 2 Week 1 Geologic CyclesModule 2 Week 1 Geologic Cycles
Module 2 Week 1 Geologic Cycles
 
Chapter 6 (other related geological hazard)
Chapter 6 (other related geological hazard)Chapter 6 (other related geological hazard)
Chapter 6 (other related geological hazard)
 
Chapter 12 Volcanoes
Chapter 12 VolcanoesChapter 12 Volcanoes
Chapter 12 Volcanoes
 
Earth Materials and Processes : ENDOGENIC PROCESS
Earth Materials and Processes : ENDOGENIC PROCESSEarth Materials and Processes : ENDOGENIC PROCESS
Earth Materials and Processes : ENDOGENIC PROCESS
 
Geology 1: Notes on Earth's geologic forces that shape the crust with video ...
Geology 1:  Notes on Earth's geologic forces that shape the crust with video ...Geology 1:  Notes on Earth's geologic forces that shape the crust with video ...
Geology 1: Notes on Earth's geologic forces that shape the crust with video ...
 
geography earthquakes ppt
geography  earthquakes pptgeography  earthquakes ppt
geography earthquakes ppt
 
Slides on our changing earth
Slides on our changing earthSlides on our changing earth
Slides on our changing earth
 

En vedette

Earth Processes
Earth ProcessesEarth Processes
Earth Processessstoffre
 
Weathering and Erosion
Weathering and ErosionWeathering and Erosion
Weathering and ErosionDaniyal Ahmad
 
earth movements Endogenic forces
 earth movements Endogenic forces earth movements Endogenic forces
earth movements Endogenic forcesMandeep Kaur
 
Drainage basin hydrological cycle smy
Drainage basin hydrological cycle smyDrainage basin hydrological cycle smy
Drainage basin hydrological cycle smytonybattista
 
Rivers Drainage Basin
Rivers Drainage BasinRivers Drainage Basin
Rivers Drainage BasinMrs Coles
 
Drainage system
Drainage systemDrainage system
Drainage systemNikhil Jp
 

En vedette (10)

Earth Processes
Earth ProcessesEarth Processes
Earth Processes
 
Weathering and Erosion
Weathering and ErosionWeathering and Erosion
Weathering and Erosion
 
River Profiles
River ProfilesRiver Profiles
River Profiles
 
Drainage Basins
Drainage BasinsDrainage Basins
Drainage Basins
 
Plate tectonics
Plate tectonicsPlate tectonics
Plate tectonics
 
Exogenic Processes
Exogenic Processes Exogenic Processes
Exogenic Processes
 
earth movements Endogenic forces
 earth movements Endogenic forces earth movements Endogenic forces
earth movements Endogenic forces
 
Drainage basin hydrological cycle smy
Drainage basin hydrological cycle smyDrainage basin hydrological cycle smy
Drainage basin hydrological cycle smy
 
Rivers Drainage Basin
Rivers Drainage BasinRivers Drainage Basin
Rivers Drainage Basin
 
Drainage system
Drainage systemDrainage system
Drainage system
 

Similaire à Plates of the earth

Intorduction to Volcanology, Weathering, Erotion, Dispertion and Soil.
Intorduction to Volcanology, Weathering, Erotion, Dispertion and Soil.Intorduction to Volcanology, Weathering, Erotion, Dispertion and Soil.
Intorduction to Volcanology, Weathering, Erotion, Dispertion and Soil.Mark Barbero
 
Constructive and deconstructive
Constructive and deconstructiveConstructive and deconstructive
Constructive and deconstructivecalee1182
 
Geological History of New Zealand
Geological History of New ZealandGeological History of New Zealand
Geological History of New ZealandAlexOCNZ
 
Ch 3 Our Changing Earth 2.pptx
Ch 3 Our Changing Earth 2.pptxCh 3 Our Changing Earth 2.pptx
Ch 3 Our Changing Earth 2.pptxMayankChanne
 
Geography our changing earth notes class 7. Nityant Singhal
Geography our changing earth notes class 7. Nityant SinghalGeography our changing earth notes class 7. Nityant Singhal
Geography our changing earth notes class 7. Nityant SinghalNityant Singhal
 
Works Of The Sea And Development Of The Related Landforms For Presentation
Works Of The Sea And Development Of The Related Landforms   For PresentationWorks Of The Sea And Development Of The Related Landforms   For Presentation
Works Of The Sea And Development Of The Related Landforms For Presentationparinshah
 
Our Changing Earth (Grade 7)
Our Changing Earth (Grade 7)Our Changing Earth (Grade 7)
Our Changing Earth (Grade 7)Sandeep Patnaik
 
Class 7 chapter 3 part 2 pdf
Class 7 chapter 3 part 2 pdfClass 7 chapter 3 part 2 pdf
Class 7 chapter 3 part 2 pdfPoonamMudaliar
 
Chapter 2 lesson 2 sci
Chapter 2 lesson 2 sciChapter 2 lesson 2 sci
Chapter 2 lesson 2 sciirschonberg
 
Tekstong argumentatibo
Tekstong argumentatiboTekstong argumentatibo
Tekstong argumentatiboCharmenSodoso
 
A report on a field trip
A report on a field tripA report on a field trip
A report on a field tripOppong Francis
 

Similaire à Plates of the earth (20)

Intorduction to Volcanology, Weathering, Erotion, Dispertion and Soil.
Intorduction to Volcanology, Weathering, Erotion, Dispertion and Soil.Intorduction to Volcanology, Weathering, Erotion, Dispertion and Soil.
Intorduction to Volcanology, Weathering, Erotion, Dispertion and Soil.
 
Constructive and deconstructive
Constructive and deconstructiveConstructive and deconstructive
Constructive and deconstructive
 
Erosion Ppt
Erosion PptErosion Ppt
Erosion Ppt
 
Geological History of New Zealand
Geological History of New ZealandGeological History of New Zealand
Geological History of New Zealand
 
Erosion and Deposition
Erosion and DepositionErosion and Deposition
Erosion and Deposition
 
Ch 3 Our Changing Earth 2.pptx
Ch 3 Our Changing Earth 2.pptxCh 3 Our Changing Earth 2.pptx
Ch 3 Our Changing Earth 2.pptx
 
Geography our changing earth notes class 7. Nityant Singhal
Geography our changing earth notes class 7. Nityant SinghalGeography our changing earth notes class 7. Nityant Singhal
Geography our changing earth notes class 7. Nityant Singhal
 
Works Of The Sea And Development Of The Related Landforms For Presentation
Works Of The Sea And Development Of The Related Landforms   For PresentationWorks Of The Sea And Development Of The Related Landforms   For Presentation
Works Of The Sea And Development Of The Related Landforms For Presentation
 
Our Changing Earth (Grade 7)
Our Changing Earth (Grade 7)Our Changing Earth (Grade 7)
Our Changing Earth (Grade 7)
 
Landform Notes
Landform NotesLandform Notes
Landform Notes
 
Class 7 chapter 3 part 2 pdf
Class 7 chapter 3 part 2 pdfClass 7 chapter 3 part 2 pdf
Class 7 chapter 3 part 2 pdf
 
W.E.D. Review
W.E.D. ReviewW.E.D. Review
W.E.D. Review
 
Our changing earth
Our changing earth Our changing earth
Our changing earth
 
Erosion
ErosionErosion
Erosion
 
Processes of River
Processes of RiverProcesses of River
Processes of River
 
Our changing earth
Our changing earthOur changing earth
Our changing earth
 
Other landforms
Other landformsOther landforms
Other landforms
 
Chapter 2 lesson 2 sci
Chapter 2 lesson 2 sciChapter 2 lesson 2 sci
Chapter 2 lesson 2 sci
 
Tekstong argumentatibo
Tekstong argumentatiboTekstong argumentatibo
Tekstong argumentatibo
 
A report on a field trip
A report on a field tripA report on a field trip
A report on a field trip
 

Dernier

Rising Above_ Dubai Floods and the Fortitude of Dubai International Airport.pdf
Rising Above_ Dubai Floods and the Fortitude of Dubai International Airport.pdfRising Above_ Dubai Floods and the Fortitude of Dubai International Airport.pdf
Rising Above_ Dubai Floods and the Fortitude of Dubai International Airport.pdfOrbitshub
 
Cloud Frontiers: A Deep Dive into Serverless Spatial Data and FME
Cloud Frontiers:  A Deep Dive into Serverless Spatial Data and FMECloud Frontiers:  A Deep Dive into Serverless Spatial Data and FME
Cloud Frontiers: A Deep Dive into Serverless Spatial Data and FMESafe Software
 
Vector Search -An Introduction in Oracle Database 23ai.pptx
Vector Search -An Introduction in Oracle Database 23ai.pptxVector Search -An Introduction in Oracle Database 23ai.pptx
Vector Search -An Introduction in Oracle Database 23ai.pptxRemote DBA Services
 
Apidays New York 2024 - Passkeys: Developing APIs to enable passwordless auth...
Apidays New York 2024 - Passkeys: Developing APIs to enable passwordless auth...Apidays New York 2024 - Passkeys: Developing APIs to enable passwordless auth...
Apidays New York 2024 - Passkeys: Developing APIs to enable passwordless auth...apidays
 
Apidays New York 2024 - Scaling API-first by Ian Reasor and Radu Cotescu, Adobe
Apidays New York 2024 - Scaling API-first by Ian Reasor and Radu Cotescu, AdobeApidays New York 2024 - Scaling API-first by Ian Reasor and Radu Cotescu, Adobe
Apidays New York 2024 - Scaling API-first by Ian Reasor and Radu Cotescu, Adobeapidays
 
How to Troubleshoot Apps for the Modern Connected Worker
How to Troubleshoot Apps for the Modern Connected WorkerHow to Troubleshoot Apps for the Modern Connected Worker
How to Troubleshoot Apps for the Modern Connected WorkerThousandEyes
 
Corporate and higher education May webinar.pptx
Corporate and higher education May webinar.pptxCorporate and higher education May webinar.pptx
Corporate and higher education May webinar.pptxRustici Software
 
Strategies for Landing an Oracle DBA Job as a Fresher
Strategies for Landing an Oracle DBA Job as a FresherStrategies for Landing an Oracle DBA Job as a Fresher
Strategies for Landing an Oracle DBA Job as a FresherRemote DBA Services
 
Why Teams call analytics are critical to your entire business
Why Teams call analytics are critical to your entire businessWhy Teams call analytics are critical to your entire business
Why Teams call analytics are critical to your entire businesspanagenda
 
Modular Monolith - a Practical Alternative to Microservices @ Devoxx UK 2024
Modular Monolith - a Practical Alternative to Microservices @ Devoxx UK 2024Modular Monolith - a Practical Alternative to Microservices @ Devoxx UK 2024
Modular Monolith - a Practical Alternative to Microservices @ Devoxx UK 2024Victor Rentea
 
Repurposing LNG terminals for Hydrogen Ammonia: Feasibility and Cost Saving
Repurposing LNG terminals for Hydrogen Ammonia: Feasibility and Cost SavingRepurposing LNG terminals for Hydrogen Ammonia: Feasibility and Cost Saving
Repurposing LNG terminals for Hydrogen Ammonia: Feasibility and Cost SavingEdi Saputra
 
WSO2's API Vision: Unifying Control, Empowering Developers
WSO2's API Vision: Unifying Control, Empowering DevelopersWSO2's API Vision: Unifying Control, Empowering Developers
WSO2's API Vision: Unifying Control, Empowering DevelopersWSO2
 
Strategize a Smooth Tenant-to-tenant Migration and Copilot Takeoff
Strategize a Smooth Tenant-to-tenant Migration and Copilot TakeoffStrategize a Smooth Tenant-to-tenant Migration and Copilot Takeoff
Strategize a Smooth Tenant-to-tenant Migration and Copilot Takeoffsammart93
 
ICT role in 21st century education and its challenges
ICT role in 21st century education and its challengesICT role in 21st century education and its challenges
ICT role in 21st century education and its challengesrafiqahmad00786416
 
Exploring Multimodal Embeddings with Milvus
Exploring Multimodal Embeddings with MilvusExploring Multimodal Embeddings with Milvus
Exploring Multimodal Embeddings with MilvusZilliz
 
Artificial Intelligence Chap.5 : Uncertainty
Artificial Intelligence Chap.5 : UncertaintyArtificial Intelligence Chap.5 : Uncertainty
Artificial Intelligence Chap.5 : UncertaintyKhushali Kathiriya
 
"I see eyes in my soup": How Delivery Hero implemented the safety system for ...
"I see eyes in my soup": How Delivery Hero implemented the safety system for ..."I see eyes in my soup": How Delivery Hero implemented the safety system for ...
"I see eyes in my soup": How Delivery Hero implemented the safety system for ...Zilliz
 
Polkadot JAM Slides - Token2049 - By Dr. Gavin Wood
Polkadot JAM Slides - Token2049 - By Dr. Gavin WoodPolkadot JAM Slides - Token2049 - By Dr. Gavin Wood
Polkadot JAM Slides - Token2049 - By Dr. Gavin WoodJuan lago vázquez
 
Apidays New York 2024 - Accelerating FinTech Innovation by Vasa Krishnan, Fin...
Apidays New York 2024 - Accelerating FinTech Innovation by Vasa Krishnan, Fin...Apidays New York 2024 - Accelerating FinTech Innovation by Vasa Krishnan, Fin...
Apidays New York 2024 - Accelerating FinTech Innovation by Vasa Krishnan, Fin...apidays
 
MINDCTI Revenue Release Quarter One 2024
MINDCTI Revenue Release Quarter One 2024MINDCTI Revenue Release Quarter One 2024
MINDCTI Revenue Release Quarter One 2024MIND CTI
 

Dernier (20)

Rising Above_ Dubai Floods and the Fortitude of Dubai International Airport.pdf
Rising Above_ Dubai Floods and the Fortitude of Dubai International Airport.pdfRising Above_ Dubai Floods and the Fortitude of Dubai International Airport.pdf
Rising Above_ Dubai Floods and the Fortitude of Dubai International Airport.pdf
 
Cloud Frontiers: A Deep Dive into Serverless Spatial Data and FME
Cloud Frontiers:  A Deep Dive into Serverless Spatial Data and FMECloud Frontiers:  A Deep Dive into Serverless Spatial Data and FME
Cloud Frontiers: A Deep Dive into Serverless Spatial Data and FME
 
Vector Search -An Introduction in Oracle Database 23ai.pptx
Vector Search -An Introduction in Oracle Database 23ai.pptxVector Search -An Introduction in Oracle Database 23ai.pptx
Vector Search -An Introduction in Oracle Database 23ai.pptx
 
Apidays New York 2024 - Passkeys: Developing APIs to enable passwordless auth...
Apidays New York 2024 - Passkeys: Developing APIs to enable passwordless auth...Apidays New York 2024 - Passkeys: Developing APIs to enable passwordless auth...
Apidays New York 2024 - Passkeys: Developing APIs to enable passwordless auth...
 
Apidays New York 2024 - Scaling API-first by Ian Reasor and Radu Cotescu, Adobe
Apidays New York 2024 - Scaling API-first by Ian Reasor and Radu Cotescu, AdobeApidays New York 2024 - Scaling API-first by Ian Reasor and Radu Cotescu, Adobe
Apidays New York 2024 - Scaling API-first by Ian Reasor and Radu Cotescu, Adobe
 
How to Troubleshoot Apps for the Modern Connected Worker
How to Troubleshoot Apps for the Modern Connected WorkerHow to Troubleshoot Apps for the Modern Connected Worker
How to Troubleshoot Apps for the Modern Connected Worker
 
Corporate and higher education May webinar.pptx
Corporate and higher education May webinar.pptxCorporate and higher education May webinar.pptx
Corporate and higher education May webinar.pptx
 
Strategies for Landing an Oracle DBA Job as a Fresher
Strategies for Landing an Oracle DBA Job as a FresherStrategies for Landing an Oracle DBA Job as a Fresher
Strategies for Landing an Oracle DBA Job as a Fresher
 
Why Teams call analytics are critical to your entire business
Why Teams call analytics are critical to your entire businessWhy Teams call analytics are critical to your entire business
Why Teams call analytics are critical to your entire business
 
Modular Monolith - a Practical Alternative to Microservices @ Devoxx UK 2024
Modular Monolith - a Practical Alternative to Microservices @ Devoxx UK 2024Modular Monolith - a Practical Alternative to Microservices @ Devoxx UK 2024
Modular Monolith - a Practical Alternative to Microservices @ Devoxx UK 2024
 
Repurposing LNG terminals for Hydrogen Ammonia: Feasibility and Cost Saving
Repurposing LNG terminals for Hydrogen Ammonia: Feasibility and Cost SavingRepurposing LNG terminals for Hydrogen Ammonia: Feasibility and Cost Saving
Repurposing LNG terminals for Hydrogen Ammonia: Feasibility and Cost Saving
 
WSO2's API Vision: Unifying Control, Empowering Developers
WSO2's API Vision: Unifying Control, Empowering DevelopersWSO2's API Vision: Unifying Control, Empowering Developers
WSO2's API Vision: Unifying Control, Empowering Developers
 
Strategize a Smooth Tenant-to-tenant Migration and Copilot Takeoff
Strategize a Smooth Tenant-to-tenant Migration and Copilot TakeoffStrategize a Smooth Tenant-to-tenant Migration and Copilot Takeoff
Strategize a Smooth Tenant-to-tenant Migration and Copilot Takeoff
 
ICT role in 21st century education and its challenges
ICT role in 21st century education and its challengesICT role in 21st century education and its challenges
ICT role in 21st century education and its challenges
 
Exploring Multimodal Embeddings with Milvus
Exploring Multimodal Embeddings with MilvusExploring Multimodal Embeddings with Milvus
Exploring Multimodal Embeddings with Milvus
 
Artificial Intelligence Chap.5 : Uncertainty
Artificial Intelligence Chap.5 : UncertaintyArtificial Intelligence Chap.5 : Uncertainty
Artificial Intelligence Chap.5 : Uncertainty
 
"I see eyes in my soup": How Delivery Hero implemented the safety system for ...
"I see eyes in my soup": How Delivery Hero implemented the safety system for ..."I see eyes in my soup": How Delivery Hero implemented the safety system for ...
"I see eyes in my soup": How Delivery Hero implemented the safety system for ...
 
Polkadot JAM Slides - Token2049 - By Dr. Gavin Wood
Polkadot JAM Slides - Token2049 - By Dr. Gavin WoodPolkadot JAM Slides - Token2049 - By Dr. Gavin Wood
Polkadot JAM Slides - Token2049 - By Dr. Gavin Wood
 
Apidays New York 2024 - Accelerating FinTech Innovation by Vasa Krishnan, Fin...
Apidays New York 2024 - Accelerating FinTech Innovation by Vasa Krishnan, Fin...Apidays New York 2024 - Accelerating FinTech Innovation by Vasa Krishnan, Fin...
Apidays New York 2024 - Accelerating FinTech Innovation by Vasa Krishnan, Fin...
 
MINDCTI Revenue Release Quarter One 2024
MINDCTI Revenue Release Quarter One 2024MINDCTI Revenue Release Quarter One 2024
MINDCTI Revenue Release Quarter One 2024
 

Plates of the earth

  • 2. WORLD MAP LOCATING THE PLATES
  • 3.
  • 4.
  • 6.
  • 7.
  • 8.
  • 9. THE MOVEMENT OF THESE PLATES CAUSES CHANGES ON SURFACE ON THEOF THE EARTH.
  • 10. THE EARTH MOVEMENTARE DIVIDED ONTHE BASIS OFTHE FORCESWHICH CAUSETHEM.
  • 13. HOW DOES EARTHQUAKE OCCUR DUE TO THE PLATES
  • 15.  A volcano is an opening, or rupture, in a planet's surface or crust, which allows hot magma, volcanic ash and gases to escape from the magma chamber below the surface.
  • 16.  Deep below the Earth's crust, the temperatures and pressures are great enough to melt rock. When this molten rock blasts to the surface, the result is a volcano - and for the inhabitants of the place, it's as if Hell has been let loose.
  • 17.  Why doVolcanoes occur?  Volcanoes occur when the Earth's plates pull apart causing magma to rise to the surface.Volcanoes can also occur over hotspots and where one plate dives beneath another, forcing magma to rise to the surface. Plates diving under one another is known as subduction.  Where doVolcanoes occur?  Volcanoes usually occur on the edges of plates, similar to where earthquakes occur. A lot of volcanoes occur in the area around the edge of the Pacific ocean called the Pacific Ring of Fire.Volcanoes can also occur in the middle of plates, in hotspots. One such hotspot has formed the Hawaiian islands chain. As the earth rotated, it passed over the hotspot and new islands were formed.
  • 19.  What are landslides and how do they occur?  Landslides have always existed on our planet. Generally classified as mass movements of rock, debris, and soil down a slope of land. While landslides are a naturally occurring environmental hazard they have recently increased in frequency in certain areas due to human activity. Although there are many different causes of landslides, they all have two things in common.They are the results of the failure of the soil and rock materials that make up the hill-slope and they are driven by gravity."
  • 20. EXOGENIC FORCES • glaciers• wind • River and Seawaves
  • 21. WORK OF A RIVER
  • 22. WEATHERING  Weathering is the breaking down of rocks, soils and minerals as well as artificial materials through contact with the Earth's atmosphere, biota and waters.Weathering occurs in situ, or "with no movement", and thus should not be confused with erosion, which involves the movement of rocks and minerals by agents such as water, ice, snow, wind, waves and gravity.
  • 23. Erosion The removal of solids like sediments, soil rocks and other particles in the natural environment.
  • 24. THE ERODED MATERIALS GETS SET DOWN INTHE EARTH SURFACE.
  • 25.  DUETOTHESE PROCESS DIFFERENT LANDFORMSONTHE SURFACE OFTHE EARTH . LANDFORMS FORMED BYTHE RIVER
  • 26.
  • 27. WATERFALL  AWATERFALL IS A PLACE WHERE FLOWING WATER RAPIDLY DRROPS IN ELEVATION AS IT FLOWS OVER A STEEP REGION OR A CLIFF. MEANDERS A meander, in general, is a bend in a sinuous watercourse or river.A meander is formed when the moving water in a stream erodes the outer banks and widens its valley and the inner part of the river has less energy and deposits what it is carrying.
  • 28. OX BOW LAKE An oxbow is a crescent-shaped lake lying alongside a winding river. The oxbow lake is created over time as erosion and deposits of soil change the river's course.
  • 29. FLOODPLAIN A floodplain or flood plain is an area of land adjacent to a stream or river that stretches from the banks of its channel to the base of the enclosing valley walls and experiences flooding during periods of high discharge.
  • 30. LEVEES  Naturally formed raised bank along the side of a river channel are called natural environment . The river approaches the sea the river begins to break up into many streams called distributaries
  • 31. LANDFORMS FORMED BYTHE SEA WAVES Dueto continuous strikesof sea wavesat the rocks,cracks appear in therocks.Changes appear in the rocks.
  • 32.
  • 33. LANDFORMS FORMED BY THE GLACIERS
  • 34.  THE DEPOSITSOF MATERIAL CARRIED BY THE GLACIER IS CALLED GLACIAL MORAINES.
  • 37. LOESS