SlideShare a Scribd company logo
Photographic Evidence
By: Manibah
Convergent Boundary
Continental-Continental= Mountains
Himalayan Mountains are the tallest
mountain range in the world.
Cause: Two continental plates collide together.
Effect: The oceanic crust goes under continental
creating mountain.
Subduction Zone
Crater Lake National Park created due to
plates collision.
Cause: The two plates colliding.
Effect: Volcanic eruptions and
trenches.
Convergent Boundary-Subduction Zone
Oceanic-Oceanic= Trench
Marianas trench ocean is
one of the deepest part of
ocean.
Cause: When two plates carrying oceanic
crust meet.
Effect: Oceanic Trench is formed as the
massive.
Convergent Boundary-Subduction Zone
Oceanic -Oceanic= Volcanic Island
Mauna Loa Erupting in Hawaii
Cause: When tectonic plate comes together,
magma rises upward until it erupts on the sea.
Effect: Creates Volcanic Island.
Convergent Boundary-Subduction Zone
Oceanic-Continental= Trench and Volcanic Arc
Aleutian Arc is a large volcanic arc in the State of Alaska.
Aleutian Trench is an Oceanic Trench along a convergent plate boundary
Cause: When a continental plate converges with an
oceanic plate a subduction zone forms.
Effects: Which creates trenches and volcanic arc.
Analysis
At convergent boundary, two tectonic plates come together. It either happens at continental crust,
oceanic or both which is lead to different features. One real-world event example could be Mauna Loa
which, volcanic island erupting in Hawaii, 1984. The eruption of Mauna Loa began suddenly, following
a period of years of slowly increasing earthquake activity beneath the volcano. When tectonic plate
comes together, magma rises upward until it erupts on the sea floor creating an volcanic island. Lava
builds up on the seafloor over millions of years. The lava cool fastly as it reaches the ocean and
forms solid rock creating an island. Another example of real-world event could be Himalayan
mountains. For at least 80 million years the oceanic Indian Plate continued its unavoidable collision
with southern Asia, including Tibet. The collision of plates is making Himalaya to move more. In
conclusion, when two tectonic plates converge, it creates beautiful yet dangerous features such as
volcanic island and mountains.
Transform Boundary
Continental-continental= Earthquake
San Andreas fault earthquake was
dangerous and destructive earthquake.
Cause: When rock underground suddenly
breaks along a fault.
Effect: Causes a destructive earthquake.
Transform Boundary
Oceanic-Oceanic=Tsunami
Tsunami occurred in Japan, 2011 causing
massive destruction with the magnitude of 7.3
Cause: Large waves caused by sudden movement
on the ocean floor that can result from an
earthquake.
Effect: Causes a great destruction from Tsunami.
Analysis
At Transform boundary, two plates move past each other without breaking. Two main features of
Transform boundary are Earthquake and Tsunami. One example of real-world event could be the San
Andreas fault earthquake in 1906. It had magnitude between 7.7-7.9 and it was destructive and
dangerous. Many buildings were shaken to pieces by the earthquake. Due to plates on either side of
a transform boundary are sliding past each other and not tearing or crunching each other causes
earthquake. Another example of an event is Tsunami in Japan, 2011 causing massive destruction.
Tsunami is a harbor wave caused by sudden movement in oceanic plates. In conclusion, when two
plates move past each other causes tsunami and earthquake at transform boundary.
Divergent Boundary
Continental-Continental= Rift Valley
Olduvai Gorge, Tanzania's Great Rift
Valley.Great Rift valley is spreading apart.
Cause: Tectonic plates break apart
from each other. Where plates move
apart, the Earth’s crust separates.
Effect: Rift valleys lead to the creation.
Divergent Boundary
Oceanic-Oceanic= Mid Ocean Ridge
Juan De Fuca Ridge,
mid-oceanic mountain
range. The land splitting
apart.
Cause: Uplifting of the ocean floor occurs when
convection currents rise in the mantle under oceanic
crust.
Effect:Mid-Oceanic Ridge occurs when the pressure of
the ridge pushes the rest of the tectonic plate away from
the ridge.
Analysis
At Divergent boundary, two plates moves apart. When the mantle of earth moves, both crusts of earth
moves. Split in the crust molten rocks and magma are forced up into the split and they move
sideways. At divergent boundary,rift valley and mid-oceanic ridge could be created. One example of
real-world event is Olduvai Gorge, Tanzania's Great Rift Valley. Great Rift valley is spreading apart.
Another example of real-world event could be Juan De Fuca Ridge, mid-oceanic mountain range. The
land splitting apart created mid oceanic ridge.This uplifting of the ocean floor occurs when
convection currents rise in the mantle under the oceanic crust and create magma where two
tectonic plates meet at a divergent boundary. In conclusion, when two plates moves apart causes
different feature to appear such as mid-oceanic ridge and rift valley.

More Related Content

What's hot

Tectonic terror
Tectonic terrorTectonic terror
Tectonic terror
Kristy Smith
 
Revisons 1
Revisons 1Revisons 1
Revisons 1
geographybn
 
Earth Science 5.1: What are Earthquakes?
Earth Science 5.1: What are Earthquakes?Earth Science 5.1: What are Earthquakes?
Earth Science 5.1: What are Earthquakes?Chris Foltz
 
Earthquake plate tectonic- Geomorphology Chapter
Earthquake plate tectonic- Geomorphology ChapterEarthquake plate tectonic- Geomorphology Chapter
Earthquake plate tectonic- Geomorphology Chapter
Kaium Chowdhury
 
Earthquake ppt
Earthquake pptEarthquake ppt
Earthquake ppt
ICRISAT
 
Unique Landforms Locate At Plate Margins Bv
Unique Landforms Locate At Plate Margins BvUnique Landforms Locate At Plate Margins Bv
Unique Landforms Locate At Plate Margins Bvtudorgeog
 
The Tectonic Plates And Volcanoes
The Tectonic Plates And VolcanoesThe Tectonic Plates And Volcanoes
The Tectonic Plates And Volcanoes
theorgil
 
5.1Movement of Rock Builds Mountains
5.1Movement of Rock Builds Mountains5.1Movement of Rock Builds Mountains
5.1Movement of Rock Builds Mountains
Melisa Kelly
 
Earthquakes
EarthquakesEarthquakes
Earthquakescharsh
 
Constructive Plate Boundaries Conservative Boundaries Bv
Constructive Plate Boundaries  Conservative Boundaries BvConstructive Plate Boundaries  Conservative Boundaries Bv
Constructive Plate Boundaries Conservative Boundaries Bvtudorgeog
 
Earthquake
EarthquakeEarthquake
Earthquake
sahindas1
 
Earthquakes And Evs
Earthquakes And EvsEarthquakes And Evs
Earthquakes And Evs
sjcc
 
The greatest risk of living near volcanic areas is the landslides ld essay
The greatest risk of living near volcanic areas is the landslides ld essayThe greatest risk of living near volcanic areas is the landslides ld essay
The greatest risk of living near volcanic areas is the landslides ld essay
ivisdude82
 
Earthquake and earthquake resistant design
Earthquake   and earthquake resistant designEarthquake   and earthquake resistant design
Earthquake and earthquake resistant design
PARVEEN JANGRA
 
3.4.1 Earthquake Hazards
3.4.1 Earthquake Hazards3.4.1 Earthquake Hazards
3.4.1 Earthquake Hazardstudorgeog
 
Collisional Plate Boundaries
 Collisional Plate Boundaries  Collisional Plate Boundaries
Collisional Plate Boundaries cheergalsal
 
Pacific ring of fire
Pacific ring of firePacific ring of fire
Pacific ring of fire
tahoecap
 
Volcanoes and earthquakes education powerpoint
Volcanoes and earthquakes education powerpointVolcanoes and earthquakes education powerpoint
Volcanoes and earthquakes education powerpoint
Shubham Saha
 
Earthquakes
EarthquakesEarthquakes
Earthquakes
AHMAD GHANI
 

What's hot (20)

Tectonic terror
Tectonic terrorTectonic terror
Tectonic terror
 
Revisons 1
Revisons 1Revisons 1
Revisons 1
 
Earth Science 5.1: What are Earthquakes?
Earth Science 5.1: What are Earthquakes?Earth Science 5.1: What are Earthquakes?
Earth Science 5.1: What are Earthquakes?
 
Earthquake plate tectonic- Geomorphology Chapter
Earthquake plate tectonic- Geomorphology ChapterEarthquake plate tectonic- Geomorphology Chapter
Earthquake plate tectonic- Geomorphology Chapter
 
Earthquake ppt
Earthquake pptEarthquake ppt
Earthquake ppt
 
Unique Landforms Locate At Plate Margins Bv
Unique Landforms Locate At Plate Margins BvUnique Landforms Locate At Plate Margins Bv
Unique Landforms Locate At Plate Margins Bv
 
The Tectonic Plates And Volcanoes
The Tectonic Plates And VolcanoesThe Tectonic Plates And Volcanoes
The Tectonic Plates And Volcanoes
 
5.1Movement of Rock Builds Mountains
5.1Movement of Rock Builds Mountains5.1Movement of Rock Builds Mountains
5.1Movement of Rock Builds Mountains
 
Earthquakes
EarthquakesEarthquakes
Earthquakes
 
Constructive Plate Boundaries Conservative Boundaries Bv
Constructive Plate Boundaries  Conservative Boundaries BvConstructive Plate Boundaries  Conservative Boundaries Bv
Constructive Plate Boundaries Conservative Boundaries Bv
 
Earthquake
EarthquakeEarthquake
Earthquake
 
Plate Boundaries
Plate BoundariesPlate Boundaries
Plate Boundaries
 
Earthquakes And Evs
Earthquakes And EvsEarthquakes And Evs
Earthquakes And Evs
 
The greatest risk of living near volcanic areas is the landslides ld essay
The greatest risk of living near volcanic areas is the landslides ld essayThe greatest risk of living near volcanic areas is the landslides ld essay
The greatest risk of living near volcanic areas is the landslides ld essay
 
Earthquake and earthquake resistant design
Earthquake   and earthquake resistant designEarthquake   and earthquake resistant design
Earthquake and earthquake resistant design
 
3.4.1 Earthquake Hazards
3.4.1 Earthquake Hazards3.4.1 Earthquake Hazards
3.4.1 Earthquake Hazards
 
Collisional Plate Boundaries
 Collisional Plate Boundaries  Collisional Plate Boundaries
Collisional Plate Boundaries
 
Pacific ring of fire
Pacific ring of firePacific ring of fire
Pacific ring of fire
 
Volcanoes and earthquakes education powerpoint
Volcanoes and earthquakes education powerpointVolcanoes and earthquakes education powerpoint
Volcanoes and earthquakes education powerpoint
 
Earthquakes
EarthquakesEarthquakes
Earthquakes
 

Similar to Untitled presentation

Notes on living with tectonic hazards 0 levels
Notes on living with tectonic hazards 0 levelsNotes on living with tectonic hazards 0 levels
Notes on living with tectonic hazards 0 levels
ivisdude82
 
Tectonic Processes and Landscapes
Tectonic Processes and LandscapesTectonic Processes and Landscapes
Tectonic Processes and Landscapes
jess2011
 
Notes on living with tectonic hazards n levels
Notes on living with tectonic hazards n levelsNotes on living with tectonic hazards n levels
Notes on living with tectonic hazards n levels
ivisdude82
 
Meath Earthquakes 1 1 1 [1]
Meath Earthquakes 1 1 1 [1]Meath Earthquakes 1 1 1 [1]
Meath Earthquakes 1 1 1 [1]
smeath
 
Plate movements (teach)
Plate movements (teach)Plate movements (teach)
Plate movements (teach)
Moira Whitehouse
 
Photographic Evidences - Qihua
Photographic Evidences - QihuaPhotographic Evidences - Qihua
Photographic Evidences - Qihuaihsl
 
Photographic evidence
Photographic evidencePhotographic evidence
Photographic evidence
ShirleykaHector
 
Plate Tectonics Photographic Evidence - QiHua
Plate Tectonics Photographic Evidence - QiHuaPlate Tectonics Photographic Evidence - QiHua
Plate Tectonics Photographic Evidence - QiHuaihsl
 
Subduction Zone
Subduction ZoneSubduction Zone
Subduction Zone
KDilshod7
 
Destructive plate boundaries
Destructive plate boundariesDestructive plate boundaries
Destructive plate boundariesanicholls1234
 
Q1-L001.pptx
Q1-L001.pptxQ1-L001.pptx
Q1-L001.pptx
grethelparreo1
 
Submarine earthquake
Submarine earthquakeSubmarine earthquake
Submarine earthquake
Lavanya Singh
 
Plate Tectonics
Plate TectonicsPlate Tectonics
Plate Tectonics
Donald Johnson
 
Plate tectonics
Plate tectonicsPlate tectonics
Plate tectonics
Arshaghosh Ajayan
 
What happens when the plates meet
What happens when the plates meetWhat happens when the plates meet
What happens when the plates meetMrs Coles
 
plate-tectonics-power-point.ppt
plate-tectonics-power-point.pptplate-tectonics-power-point.ppt
plate-tectonics-power-point.ppt
SalveBatalla2
 
ELS.pdf
ELS.pdfELS.pdf
ELS.pdf
ninobitas16
 

Similar to Untitled presentation (20)

Notes on living with tectonic hazards 0 levels
Notes on living with tectonic hazards 0 levelsNotes on living with tectonic hazards 0 levels
Notes on living with tectonic hazards 0 levels
 
Tectonic Processes and Landscapes
Tectonic Processes and LandscapesTectonic Processes and Landscapes
Tectonic Processes and Landscapes
 
Notes on living with tectonic hazards n levels
Notes on living with tectonic hazards n levelsNotes on living with tectonic hazards n levels
Notes on living with tectonic hazards n levels
 
Meath Earthquakes 1 1 1 [1]
Meath Earthquakes 1 1 1 [1]Meath Earthquakes 1 1 1 [1]
Meath Earthquakes 1 1 1 [1]
 
Plate movements (teach)
Plate movements (teach)Plate movements (teach)
Plate movements (teach)
 
Photographic Evidences - Qihua
Photographic Evidences - QihuaPhotographic Evidences - Qihua
Photographic Evidences - Qihua
 
Photographic evidence
Photographic evidencePhotographic evidence
Photographic evidence
 
Plate tectonics
Plate tectonicsPlate tectonics
Plate tectonics
 
Plate Tectonics Photographic Evidence - QiHua
Plate Tectonics Photographic Evidence - QiHuaPlate Tectonics Photographic Evidence - QiHua
Plate Tectonics Photographic Evidence - QiHua
 
Subduction Zone
Subduction ZoneSubduction Zone
Subduction Zone
 
Destructive plate boundaries
Destructive plate boundariesDestructive plate boundaries
Destructive plate boundaries
 
Q1-L001.pptx
Q1-L001.pptxQ1-L001.pptx
Q1-L001.pptx
 
Plate boundaries
Plate boundariesPlate boundaries
Plate boundaries
 
Submarine earthquake
Submarine earthquakeSubmarine earthquake
Submarine earthquake
 
Plate Tectonics
Plate TectonicsPlate Tectonics
Plate Tectonics
 
Plate tectonics
Plate tectonicsPlate tectonics
Plate tectonics
 
What happens when the plates meet
What happens when the plates meetWhat happens when the plates meet
What happens when the plates meet
 
plate-tectonics-power-point.ppt
plate-tectonics-power-point.pptplate-tectonics-power-point.ppt
plate-tectonics-power-point.ppt
 
Plate tectonics
Plate tectonicsPlate tectonics
Plate tectonics
 
ELS.pdf
ELS.pdfELS.pdf
ELS.pdf
 

Recently uploaded

SAR of Medicinal Chemistry 1st by dk.pdf
SAR of Medicinal Chemistry 1st by dk.pdfSAR of Medicinal Chemistry 1st by dk.pdf
SAR of Medicinal Chemistry 1st by dk.pdf
KrushnaDarade1
 
Mudde & Rovira Kaltwasser. - Populism - a very short introduction [2017].pdf
Mudde & Rovira Kaltwasser. - Populism - a very short introduction [2017].pdfMudde & Rovira Kaltwasser. - Populism - a very short introduction [2017].pdf
Mudde & Rovira Kaltwasser. - Populism - a very short introduction [2017].pdf
frank0071
 
platelets_clotting_biogenesis.clot retractionpptx
platelets_clotting_biogenesis.clot retractionpptxplatelets_clotting_biogenesis.clot retractionpptx
platelets_clotting_biogenesis.clot retractionpptx
muralinath2
 
Richard's aventures in two entangled wonderlands
Richard's aventures in two entangled wonderlandsRichard's aventures in two entangled wonderlands
Richard's aventures in two entangled wonderlands
Richard Gill
 
Unveiling the Energy Potential of Marshmallow Deposits.pdf
Unveiling the Energy Potential of Marshmallow Deposits.pdfUnveiling the Energy Potential of Marshmallow Deposits.pdf
Unveiling the Energy Potential of Marshmallow Deposits.pdf
Erdal Coalmaker
 
Orion Air Quality Monitoring Systems - CWS
Orion Air Quality Monitoring Systems - CWSOrion Air Quality Monitoring Systems - CWS
Orion Air Quality Monitoring Systems - CWS
Columbia Weather Systems
 
Comparing Evolved Extractive Text Summary Scores of Bidirectional Encoder Rep...
Comparing Evolved Extractive Text Summary Scores of Bidirectional Encoder Rep...Comparing Evolved Extractive Text Summary Scores of Bidirectional Encoder Rep...
Comparing Evolved Extractive Text Summary Scores of Bidirectional Encoder Rep...
University of Maribor
 
Travis Hills' Endeavors in Minnesota: Fostering Environmental and Economic Pr...
Travis Hills' Endeavors in Minnesota: Fostering Environmental and Economic Pr...Travis Hills' Endeavors in Minnesota: Fostering Environmental and Economic Pr...
Travis Hills' Endeavors in Minnesota: Fostering Environmental and Economic Pr...
Travis Hills MN
 
bordetella pertussis.................................ppt
bordetella pertussis.................................pptbordetella pertussis.................................ppt
bordetella pertussis.................................ppt
kejapriya1
 
NuGOweek 2024 Ghent programme overview flyer
NuGOweek 2024 Ghent programme overview flyerNuGOweek 2024 Ghent programme overview flyer
NuGOweek 2024 Ghent programme overview flyer
pablovgd
 
mô tả các thí nghiệm về đánh giá tác động dòng khí hóa sau đốt
mô tả các thí nghiệm về đánh giá tác động dòng khí hóa sau đốtmô tả các thí nghiệm về đánh giá tác động dòng khí hóa sau đốt
mô tả các thí nghiệm về đánh giá tác động dòng khí hóa sau đốt
HongcNguyn6
 
Phenomics assisted breeding in crop improvement
Phenomics assisted breeding in crop improvementPhenomics assisted breeding in crop improvement
Phenomics assisted breeding in crop improvement
IshaGoswami9
 
Toxic effects of heavy metals : Lead and Arsenic
Toxic effects of heavy metals : Lead and ArsenicToxic effects of heavy metals : Lead and Arsenic
Toxic effects of heavy metals : Lead and Arsenic
sanjana502982
 
Red blood cells- genesis-maturation.pptx
Red blood cells- genesis-maturation.pptxRed blood cells- genesis-maturation.pptx
Red blood cells- genesis-maturation.pptx
muralinath2
 
Shallowest Oil Discovery of Turkiye.pptx
Shallowest Oil Discovery of Turkiye.pptxShallowest Oil Discovery of Turkiye.pptx
Shallowest Oil Discovery of Turkiye.pptx
Gokturk Mehmet Dilci
 
Seminar of U.V. Spectroscopy by SAMIR PANDA
 Seminar of U.V. Spectroscopy by SAMIR PANDA Seminar of U.V. Spectroscopy by SAMIR PANDA
Seminar of U.V. Spectroscopy by SAMIR PANDA
SAMIR PANDA
 
原版制作(carleton毕业证书)卡尔顿大学毕业证硕士文凭原版一模一样
原版制作(carleton毕业证书)卡尔顿大学毕业证硕士文凭原版一模一样原版制作(carleton毕业证书)卡尔顿大学毕业证硕士文凭原版一模一样
原版制作(carleton毕业证书)卡尔顿大学毕业证硕士文凭原版一模一样
yqqaatn0
 
DERIVATION OF MODIFIED BERNOULLI EQUATION WITH VISCOUS EFFECTS AND TERMINAL V...
DERIVATION OF MODIFIED BERNOULLI EQUATION WITH VISCOUS EFFECTS AND TERMINAL V...DERIVATION OF MODIFIED BERNOULLI EQUATION WITH VISCOUS EFFECTS AND TERMINAL V...
DERIVATION OF MODIFIED BERNOULLI EQUATION WITH VISCOUS EFFECTS AND TERMINAL V...
Wasswaderrick3
 
Lateral Ventricles.pdf very easy good diagrams comprehensive
Lateral Ventricles.pdf very easy good diagrams comprehensiveLateral Ventricles.pdf very easy good diagrams comprehensive
Lateral Ventricles.pdf very easy good diagrams comprehensive
silvermistyshot
 
Chapter 12 - climate change and the energy crisis
Chapter 12 - climate change and the energy crisisChapter 12 - climate change and the energy crisis
Chapter 12 - climate change and the energy crisis
tonzsalvador2222
 

Recently uploaded (20)

SAR of Medicinal Chemistry 1st by dk.pdf
SAR of Medicinal Chemistry 1st by dk.pdfSAR of Medicinal Chemistry 1st by dk.pdf
SAR of Medicinal Chemistry 1st by dk.pdf
 
Mudde & Rovira Kaltwasser. - Populism - a very short introduction [2017].pdf
Mudde & Rovira Kaltwasser. - Populism - a very short introduction [2017].pdfMudde & Rovira Kaltwasser. - Populism - a very short introduction [2017].pdf
Mudde & Rovira Kaltwasser. - Populism - a very short introduction [2017].pdf
 
platelets_clotting_biogenesis.clot retractionpptx
platelets_clotting_biogenesis.clot retractionpptxplatelets_clotting_biogenesis.clot retractionpptx
platelets_clotting_biogenesis.clot retractionpptx
 
Richard's aventures in two entangled wonderlands
Richard's aventures in two entangled wonderlandsRichard's aventures in two entangled wonderlands
Richard's aventures in two entangled wonderlands
 
Unveiling the Energy Potential of Marshmallow Deposits.pdf
Unveiling the Energy Potential of Marshmallow Deposits.pdfUnveiling the Energy Potential of Marshmallow Deposits.pdf
Unveiling the Energy Potential of Marshmallow Deposits.pdf
 
Orion Air Quality Monitoring Systems - CWS
Orion Air Quality Monitoring Systems - CWSOrion Air Quality Monitoring Systems - CWS
Orion Air Quality Monitoring Systems - CWS
 
Comparing Evolved Extractive Text Summary Scores of Bidirectional Encoder Rep...
Comparing Evolved Extractive Text Summary Scores of Bidirectional Encoder Rep...Comparing Evolved Extractive Text Summary Scores of Bidirectional Encoder Rep...
Comparing Evolved Extractive Text Summary Scores of Bidirectional Encoder Rep...
 
Travis Hills' Endeavors in Minnesota: Fostering Environmental and Economic Pr...
Travis Hills' Endeavors in Minnesota: Fostering Environmental and Economic Pr...Travis Hills' Endeavors in Minnesota: Fostering Environmental and Economic Pr...
Travis Hills' Endeavors in Minnesota: Fostering Environmental and Economic Pr...
 
bordetella pertussis.................................ppt
bordetella pertussis.................................pptbordetella pertussis.................................ppt
bordetella pertussis.................................ppt
 
NuGOweek 2024 Ghent programme overview flyer
NuGOweek 2024 Ghent programme overview flyerNuGOweek 2024 Ghent programme overview flyer
NuGOweek 2024 Ghent programme overview flyer
 
mô tả các thí nghiệm về đánh giá tác động dòng khí hóa sau đốt
mô tả các thí nghiệm về đánh giá tác động dòng khí hóa sau đốtmô tả các thí nghiệm về đánh giá tác động dòng khí hóa sau đốt
mô tả các thí nghiệm về đánh giá tác động dòng khí hóa sau đốt
 
Phenomics assisted breeding in crop improvement
Phenomics assisted breeding in crop improvementPhenomics assisted breeding in crop improvement
Phenomics assisted breeding in crop improvement
 
Toxic effects of heavy metals : Lead and Arsenic
Toxic effects of heavy metals : Lead and ArsenicToxic effects of heavy metals : Lead and Arsenic
Toxic effects of heavy metals : Lead and Arsenic
 
Red blood cells- genesis-maturation.pptx
Red blood cells- genesis-maturation.pptxRed blood cells- genesis-maturation.pptx
Red blood cells- genesis-maturation.pptx
 
Shallowest Oil Discovery of Turkiye.pptx
Shallowest Oil Discovery of Turkiye.pptxShallowest Oil Discovery of Turkiye.pptx
Shallowest Oil Discovery of Turkiye.pptx
 
Seminar of U.V. Spectroscopy by SAMIR PANDA
 Seminar of U.V. Spectroscopy by SAMIR PANDA Seminar of U.V. Spectroscopy by SAMIR PANDA
Seminar of U.V. Spectroscopy by SAMIR PANDA
 
原版制作(carleton毕业证书)卡尔顿大学毕业证硕士文凭原版一模一样
原版制作(carleton毕业证书)卡尔顿大学毕业证硕士文凭原版一模一样原版制作(carleton毕业证书)卡尔顿大学毕业证硕士文凭原版一模一样
原版制作(carleton毕业证书)卡尔顿大学毕业证硕士文凭原版一模一样
 
DERIVATION OF MODIFIED BERNOULLI EQUATION WITH VISCOUS EFFECTS AND TERMINAL V...
DERIVATION OF MODIFIED BERNOULLI EQUATION WITH VISCOUS EFFECTS AND TERMINAL V...DERIVATION OF MODIFIED BERNOULLI EQUATION WITH VISCOUS EFFECTS AND TERMINAL V...
DERIVATION OF MODIFIED BERNOULLI EQUATION WITH VISCOUS EFFECTS AND TERMINAL V...
 
Lateral Ventricles.pdf very easy good diagrams comprehensive
Lateral Ventricles.pdf very easy good diagrams comprehensiveLateral Ventricles.pdf very easy good diagrams comprehensive
Lateral Ventricles.pdf very easy good diagrams comprehensive
 
Chapter 12 - climate change and the energy crisis
Chapter 12 - climate change and the energy crisisChapter 12 - climate change and the energy crisis
Chapter 12 - climate change and the energy crisis
 

Untitled presentation

  • 2. Convergent Boundary Continental-Continental= Mountains Himalayan Mountains are the tallest mountain range in the world. Cause: Two continental plates collide together. Effect: The oceanic crust goes under continental creating mountain.
  • 3. Subduction Zone Crater Lake National Park created due to plates collision. Cause: The two plates colliding. Effect: Volcanic eruptions and trenches.
  • 4. Convergent Boundary-Subduction Zone Oceanic-Oceanic= Trench Marianas trench ocean is one of the deepest part of ocean. Cause: When two plates carrying oceanic crust meet. Effect: Oceanic Trench is formed as the massive.
  • 5. Convergent Boundary-Subduction Zone Oceanic -Oceanic= Volcanic Island Mauna Loa Erupting in Hawaii Cause: When tectonic plate comes together, magma rises upward until it erupts on the sea. Effect: Creates Volcanic Island.
  • 6. Convergent Boundary-Subduction Zone Oceanic-Continental= Trench and Volcanic Arc Aleutian Arc is a large volcanic arc in the State of Alaska. Aleutian Trench is an Oceanic Trench along a convergent plate boundary Cause: When a continental plate converges with an oceanic plate a subduction zone forms. Effects: Which creates trenches and volcanic arc.
  • 7. Analysis At convergent boundary, two tectonic plates come together. It either happens at continental crust, oceanic or both which is lead to different features. One real-world event example could be Mauna Loa which, volcanic island erupting in Hawaii, 1984. The eruption of Mauna Loa began suddenly, following a period of years of slowly increasing earthquake activity beneath the volcano. When tectonic plate comes together, magma rises upward until it erupts on the sea floor creating an volcanic island. Lava builds up on the seafloor over millions of years. The lava cool fastly as it reaches the ocean and forms solid rock creating an island. Another example of real-world event could be Himalayan mountains. For at least 80 million years the oceanic Indian Plate continued its unavoidable collision with southern Asia, including Tibet. The collision of plates is making Himalaya to move more. In conclusion, when two tectonic plates converge, it creates beautiful yet dangerous features such as volcanic island and mountains.
  • 8. Transform Boundary Continental-continental= Earthquake San Andreas fault earthquake was dangerous and destructive earthquake. Cause: When rock underground suddenly breaks along a fault. Effect: Causes a destructive earthquake.
  • 9. Transform Boundary Oceanic-Oceanic=Tsunami Tsunami occurred in Japan, 2011 causing massive destruction with the magnitude of 7.3 Cause: Large waves caused by sudden movement on the ocean floor that can result from an earthquake. Effect: Causes a great destruction from Tsunami.
  • 10. Analysis At Transform boundary, two plates move past each other without breaking. Two main features of Transform boundary are Earthquake and Tsunami. One example of real-world event could be the San Andreas fault earthquake in 1906. It had magnitude between 7.7-7.9 and it was destructive and dangerous. Many buildings were shaken to pieces by the earthquake. Due to plates on either side of a transform boundary are sliding past each other and not tearing or crunching each other causes earthquake. Another example of an event is Tsunami in Japan, 2011 causing massive destruction. Tsunami is a harbor wave caused by sudden movement in oceanic plates. In conclusion, when two plates move past each other causes tsunami and earthquake at transform boundary.
  • 11. Divergent Boundary Continental-Continental= Rift Valley Olduvai Gorge, Tanzania's Great Rift Valley.Great Rift valley is spreading apart. Cause: Tectonic plates break apart from each other. Where plates move apart, the Earth’s crust separates. Effect: Rift valleys lead to the creation.
  • 12. Divergent Boundary Oceanic-Oceanic= Mid Ocean Ridge Juan De Fuca Ridge, mid-oceanic mountain range. The land splitting apart. Cause: Uplifting of the ocean floor occurs when convection currents rise in the mantle under oceanic crust. Effect:Mid-Oceanic Ridge occurs when the pressure of the ridge pushes the rest of the tectonic plate away from the ridge.
  • 13. Analysis At Divergent boundary, two plates moves apart. When the mantle of earth moves, both crusts of earth moves. Split in the crust molten rocks and magma are forced up into the split and they move sideways. At divergent boundary,rift valley and mid-oceanic ridge could be created. One example of real-world event is Olduvai Gorge, Tanzania's Great Rift Valley. Great Rift valley is spreading apart. Another example of real-world event could be Juan De Fuca Ridge, mid-oceanic mountain range. The land splitting apart created mid oceanic ridge.This uplifting of the ocean floor occurs when convection currents rise in the mantle under the oceanic crust and create magma where two tectonic plates meet at a divergent boundary. In conclusion, when two plates moves apart causes different feature to appear such as mid-oceanic ridge and rift valley.