SlideShare a Scribd company logo
Move it, move it !!
 Fault: a break or fracture in the crust of Earth.
 Earthquakes: shaking or trembling of the earth
caused by movement along a fault.
 Uplift: upward movement of Earth’s crust.
■ Faults are blocks of the earth’s crust that meet together.
Scientists identify four types of faults, characterized by the
position of the fault plane, the break in the rock and the
movement of the two rock blocks.
■ Faults lines are under enormous pressure from the two
pieces of the earth’s crust pushing together.
■ The faults will eventually give way to the pressure causing
earthquakes and creating mountain ranges.
Strike-slip fault Normal fault Reverse fault
Earthquakes-Powerpoint-2.pptx
A fault is very important to the
cave. Through the fault line the
water can flow through the crack
and form beautiful cave
formations
 ■Earthquakes occur when rock shifts or slips
along fault lines.
 ■Earthquakes generate waves that travel
through the earths surface.
 ■These waves are what is felt and cause
damage around the epicenter of the
earthquake.
 Measuring earthquakes is a vital part to letting us
know how big the earthquake was and what activity
might be going on in the earth’s surface.
 Earthquakes are measured by seismographs. A
seismograph is an instrument that measures the size
and strength of the seismic waves that are released
during an earthquake.
Earthquakes-Powerpoint-2.pptx
■ Uplift often
occurs
throughout
mountain
regions as the
crust of the earth
thrusts upward.
■Uplift typically
occurs as a result
of earthquakes
and mountain
building.
■ Many
different
examples of
uplift can be
seen in
Timpanogos
National
Monument and
throughout Utah.
Earthquakes-Powerpoint-2.pptx
1. Wash your hands!
2. Open your Snickers bar and use your fingernail to
make a few breaks in the “crust”
3. Pull the candy bar carefully apart. As the “plates”
move apart, you can see the caramel underneath and
will be able to see an example of tension.
4. Now push the candy bar back to where it originally
started. Move the ends of the candy bar in opposite
directions. This is shearing.
5. Now pinch the candy bar together. This is what
happens when plates collide and form mountain
ranges. Notice how some of your chocolate pieces are
overlapping each other.

More Related Content

PPT
Mountains, earthquakes, and volcanoes
harvey09
 
PPT
Chs 6 & 7 - Earthquakes & Volcanoes
nilsona
 
PPTX
Mulvey power point for earthquake vocabulary
harvey09
 
PDF
mountainsearthquakesandvolcanoes-120925073803-phpapp01.pdf
FloraMaeMasangcayDai
 
PPTX
Our changing earth
Techy Faz
 
PPT
#1 Earthquakes Volcanoes and Tsunamis.ppt
sunnyamar2
 
PPTX
G8 Science Q2- Week1- Earthquake.pptx 2.pptx
SarahChuaDonasco
 
PPTX
Divergence of Plates.pptx
jozettezamora2
 
Mountains, earthquakes, and volcanoes
harvey09
 
Chs 6 & 7 - Earthquakes & Volcanoes
nilsona
 
Mulvey power point for earthquake vocabulary
harvey09
 
mountainsearthquakesandvolcanoes-120925073803-phpapp01.pdf
FloraMaeMasangcayDai
 
Our changing earth
Techy Faz
 
#1 Earthquakes Volcanoes and Tsunamis.ppt
sunnyamar2
 
G8 Science Q2- Week1- Earthquake.pptx 2.pptx
SarahChuaDonasco
 
Divergence of Plates.pptx
jozettezamora2
 

Similar to Earthquakes-Powerpoint-2.pptx (20)

PPTX
mountainsearthquakesandvolcanoes-120925073803-phpapp01.pptx
CharmaineCanono
 
PPTX
unit iii ppt.pptx
ssuserbdc52c
 
PPT
5606920345-Ppt-Endogenic-Processes-1.ppt
JunrickVacal
 
PPTX
Endogenous disasters
MALLIKARJUNA REDDY KASIREDDY
 
PPT
Design Steps for Earthquake Resistant Structures
Ishan Garg
 
PPTX
Earthquake
Shah Naseer
 
PPTX
U11. the dynamics of the earth
anaruperez
 
PDF
Engineering Geology_Earthquakes: Causes and Effects
WantonoFrancis
 
PPT
Plate Tectonics.ppt
BrondialDonaFernande
 
PPT
G10 SCIENCE TECTONIC plate LESSON O4.ppt
JoanaBanasen1
 
PPTX
Plate tectonics
JohnReySabal
 
PPT
Plate Tectonics: Earth's plates and Continental Drift
LuciaLina1
 
PPT
earth and life science stem grade 11 yea
Earl Slaine Torrefiel
 
PPT
earth life and science .plate tectonics.ppt
wendelcayayare
 
PPTX
Presentation.pptx
ChristianCatacutan2
 
PPTX
Sara Arif - EDSC 304 - Teacher Lecture & Guided Notes - Plate Tectonics and E...
sararif16
 
PPTX
Makeup of the earth, lesson 1
Heather Schiesher
 
PPT
Plate Boundaries
Sells Middle School
 
PPTX
Earthquake
tanisichand
 
PPTX
Plate Tectonic Theory by Manoj Sir’s Geography Classes Medinipur
Manoj Sir’s Geography Classes Midnapore
 
mountainsearthquakesandvolcanoes-120925073803-phpapp01.pptx
CharmaineCanono
 
unit iii ppt.pptx
ssuserbdc52c
 
5606920345-Ppt-Endogenic-Processes-1.ppt
JunrickVacal
 
Endogenous disasters
MALLIKARJUNA REDDY KASIREDDY
 
Design Steps for Earthquake Resistant Structures
Ishan Garg
 
Earthquake
Shah Naseer
 
U11. the dynamics of the earth
anaruperez
 
Engineering Geology_Earthquakes: Causes and Effects
WantonoFrancis
 
Plate Tectonics.ppt
BrondialDonaFernande
 
G10 SCIENCE TECTONIC plate LESSON O4.ppt
JoanaBanasen1
 
Plate tectonics
JohnReySabal
 
Plate Tectonics: Earth's plates and Continental Drift
LuciaLina1
 
earth and life science stem grade 11 yea
Earl Slaine Torrefiel
 
earth life and science .plate tectonics.ppt
wendelcayayare
 
Presentation.pptx
ChristianCatacutan2
 
Sara Arif - EDSC 304 - Teacher Lecture & Guided Notes - Plate Tectonics and E...
sararif16
 
Makeup of the earth, lesson 1
Heather Schiesher
 
Plate Boundaries
Sells Middle School
 
Earthquake
tanisichand
 
Plate Tectonic Theory by Manoj Sir’s Geography Classes Medinipur
Manoj Sir’s Geography Classes Midnapore
 

More from SadafQasim3 (20)

PPTX
shear strength.pptx GGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGG
SadafQasim3
 
PPTX
slopestability-170412060011.pptxmmmmmmmmm
SadafQasim3
 
PPT
5-2 Measuring Earthquakes.pptmmmmmmmmmmmmmm
SadafQasim3
 
PPT
DEQSDFGGGGGGGGGGGGJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJ
SadafQasim3
 
PPTX
Soil Mechanics-I.pptx gggggggghhhhhhhhbbbbbb
SadafQasim3
 
PPTX
dcccccccccccccccccccccccccccccccccccc.pptx
SadafQasim3
 
PPTX
method-of-slices-161012033456 (8)GG.Gpptx
SadafQasim3
 
PPTX
soil lectiure details.pptx weeeedeeeeeeeeeeeeeeeeeeeeeeeeeeeeeeeeeeeeeeee
SadafQasim3
 
PPTX
Todays lectuer WWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWW...
SadafQasim3
 
PPTX
dokumen.tips_liquefaction-ppt.pptx
SadafQasim3
 
PPT
Slope Stability Lectures-Pt1 (1).ppt
SadafQasim3
 
PPTX
Geologic time.pptx
SadafQasim3
 
PPTX
Soil dynamic Earth Quick Engineering.pptx
SadafQasim3
 
PDF
LEP.pdf
SadafQasim3
 
PPTX
Final draft Comparitive study of deterministic and non-deterministic approach...
SadafQasim3
 
PPTX
THEORY OF VIBRATION.pptx
SadafQasim3
 
PPT
91619433-Ppt-of-Advances-in-Geotechnology.ppt
SadafQasim3
 
PPTX
12._stresses_in_a_soil_mass_fall_36-37.pptx
SadafQasim3
 
PPTX
co6 (2).pptx
SadafQasim3
 
PPT
slide 4.ppt
SadafQasim3
 
shear strength.pptx GGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGGG
SadafQasim3
 
slopestability-170412060011.pptxmmmmmmmmm
SadafQasim3
 
5-2 Measuring Earthquakes.pptmmmmmmmmmmmmmm
SadafQasim3
 
DEQSDFGGGGGGGGGGGGJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJJ
SadafQasim3
 
Soil Mechanics-I.pptx gggggggghhhhhhhhbbbbbb
SadafQasim3
 
dcccccccccccccccccccccccccccccccccccc.pptx
SadafQasim3
 
method-of-slices-161012033456 (8)GG.Gpptx
SadafQasim3
 
soil lectiure details.pptx weeeedeeeeeeeeeeeeeeeeeeeeeeeeeeeeeeeeeeeeeeee
SadafQasim3
 
Todays lectuer WWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWWW...
SadafQasim3
 
dokumen.tips_liquefaction-ppt.pptx
SadafQasim3
 
Slope Stability Lectures-Pt1 (1).ppt
SadafQasim3
 
Geologic time.pptx
SadafQasim3
 
Soil dynamic Earth Quick Engineering.pptx
SadafQasim3
 
LEP.pdf
SadafQasim3
 
Final draft Comparitive study of deterministic and non-deterministic approach...
SadafQasim3
 
THEORY OF VIBRATION.pptx
SadafQasim3
 
91619433-Ppt-of-Advances-in-Geotechnology.ppt
SadafQasim3
 
12._stresses_in_a_soil_mass_fall_36-37.pptx
SadafQasim3
 
co6 (2).pptx
SadafQasim3
 
slide 4.ppt
SadafQasim3
 

Recently uploaded (20)

PDF
Best 10 Website To Buy Instagram Accounts Bulk 2025 USA
pvabest USA 2025
 
PDF
Data Sheet Cloud Integration Platform - dataZap
Chainsys SEO
 
PPTX
Buy Chaos Software – V-Ray, Enscape & Vantage Licenses in India
PI Software
 
PDF
SparkLabs Primer on Artificial Intelligence 2025
SparkLabs Group
 
PPTX
斯特灵大学文凭办理|办理UOS毕业证成绩单文凭复刻学历学位认证多久
1cz3lou8
 
PPTX
Virbyze_Our company profile_Preview.pptx
myckwabs
 
PPTX
How to best Address your professional Training Program - August 2025.pptx
PaulYoung221210
 
PDF
A Complete Guide to Data Migration Services for Modern Businesses
Aurnex
 
PDF
2025 07 29 The Future, Backwards Agile 2025.pdf
Daniel Walsh
 
PDF
MDR Services – 24x7 Managed Detection and Response
CyberNX Technologies Private Limited
 
PPTX
BUSINESS FINANCE POWER POINT PRESENTATION
JethSrey
 
PPTX
Memorandum and articles of association explained.pptx
Keerthana Chinnathambi
 
PDF
Tariff Surcharge and Price Increase Decision
Joshua Gao
 
PDF
Employnova Global Services : Outsourcing
Employnova Global Services
 
DOCX
unit 1 BC.docx - INTRODUCTION TO BUSINESS COMMUICATION
MANJU N
 
PPT
How to Protect Your New York Business from the Unexpected
Sam Vohra
 
PDF
Danielle Oliveira New Jersey - A Seasoned Lieutenant
Danielle Oliveira New Jersey
 
PPTX
GenAI at FinSage Financial Wellness Platform
SUBHANKARGHOSH126678
 
PDF
Keppel Ltd. 1H 2025 Results Presentation Slides
KeppelCorporation
 
PDF
HOT DAY CAFE , Café Royale isn’t just another coffee shop
PINKY PARLOUR
 
Best 10 Website To Buy Instagram Accounts Bulk 2025 USA
pvabest USA 2025
 
Data Sheet Cloud Integration Platform - dataZap
Chainsys SEO
 
Buy Chaos Software – V-Ray, Enscape & Vantage Licenses in India
PI Software
 
SparkLabs Primer on Artificial Intelligence 2025
SparkLabs Group
 
斯特灵大学文凭办理|办理UOS毕业证成绩单文凭复刻学历学位认证多久
1cz3lou8
 
Virbyze_Our company profile_Preview.pptx
myckwabs
 
How to best Address your professional Training Program - August 2025.pptx
PaulYoung221210
 
A Complete Guide to Data Migration Services for Modern Businesses
Aurnex
 
2025 07 29 The Future, Backwards Agile 2025.pdf
Daniel Walsh
 
MDR Services – 24x7 Managed Detection and Response
CyberNX Technologies Private Limited
 
BUSINESS FINANCE POWER POINT PRESENTATION
JethSrey
 
Memorandum and articles of association explained.pptx
Keerthana Chinnathambi
 
Tariff Surcharge and Price Increase Decision
Joshua Gao
 
Employnova Global Services : Outsourcing
Employnova Global Services
 
unit 1 BC.docx - INTRODUCTION TO BUSINESS COMMUICATION
MANJU N
 
How to Protect Your New York Business from the Unexpected
Sam Vohra
 
Danielle Oliveira New Jersey - A Seasoned Lieutenant
Danielle Oliveira New Jersey
 
GenAI at FinSage Financial Wellness Platform
SUBHANKARGHOSH126678
 
Keppel Ltd. 1H 2025 Results Presentation Slides
KeppelCorporation
 
HOT DAY CAFE , Café Royale isn’t just another coffee shop
PINKY PARLOUR
 

Earthquakes-Powerpoint-2.pptx

  • 2.  Fault: a break or fracture in the crust of Earth.  Earthquakes: shaking or trembling of the earth caused by movement along a fault.  Uplift: upward movement of Earth’s crust.
  • 3. ■ Faults are blocks of the earth’s crust that meet together. Scientists identify four types of faults, characterized by the position of the fault plane, the break in the rock and the movement of the two rock blocks. ■ Faults lines are under enormous pressure from the two pieces of the earth’s crust pushing together. ■ The faults will eventually give way to the pressure causing earthquakes and creating mountain ranges.
  • 4. Strike-slip fault Normal fault Reverse fault
  • 6. A fault is very important to the cave. Through the fault line the water can flow through the crack and form beautiful cave formations
  • 7.  ■Earthquakes occur when rock shifts or slips along fault lines.  ■Earthquakes generate waves that travel through the earths surface.  ■These waves are what is felt and cause damage around the epicenter of the earthquake.
  • 8.  Measuring earthquakes is a vital part to letting us know how big the earthquake was and what activity might be going on in the earth’s surface.  Earthquakes are measured by seismographs. A seismograph is an instrument that measures the size and strength of the seismic waves that are released during an earthquake.
  • 10. ■ Uplift often occurs throughout mountain regions as the crust of the earth thrusts upward. ■Uplift typically occurs as a result of earthquakes and mountain building. ■ Many different examples of uplift can be seen in Timpanogos National Monument and throughout Utah.
  • 12. 1. Wash your hands! 2. Open your Snickers bar and use your fingernail to make a few breaks in the “crust” 3. Pull the candy bar carefully apart. As the “plates” move apart, you can see the caramel underneath and will be able to see an example of tension. 4. Now push the candy bar back to where it originally started. Move the ends of the candy bar in opposite directions. This is shearing. 5. Now pinch the candy bar together. This is what happens when plates collide and form mountain ranges. Notice how some of your chocolate pieces are overlapping each other.