SlideShare a Scribd company logo
1 of 11
Name_________________                  Mountains, Earthquakes, andVolcanoes

S6E5. Students will investigate the scientific view of how the earth’s surface is
formed.
     c.   Describe processes that change rocks and the surface of the earth.


 Plate Boundaries
        3 Kinds of Plate Boundaries

        o _______________

        o _______________

        o _______________


Stress
Due mostly to plate movements, the earth’s crust is under a lot of stress.
There are 3 types:
   o “A” occurs where plates pull apart, divergent

        boundaries, and is called _____________________

   o “B” occurs where plates converge, and is called

        ___________

   o “C” occurs where plates move past each other, at

        transform fault boundaries and is called

        ____________________


Strain
Stress leads to strain on the crust which bends it. If it is warm, under the ground, it
can bend. The features are called _________.
Upturned folds are _________________ while downturned folds are ___________.




Label
Or the rock may break, if it is brittle. This causes _____________ –breaks of the
earth.


Different faults
Faults move in different ways, depending on the type of stress on them. Remember “3”
types form.
   1. ________________________
   2. ________________________
   3. ________________________

Plate Tectonic and Mountain Formation
The most common types of mountains:

         1. ____________________: from when rock layers are squeezed together

              and pushed upward –Ural Mountains (Russian)

         2. ____________________: form when tension causes land to drop down –

              Teton Range (USA)

         3. ____________________: molten material rises to the Earth’s surface

              and erupts on the surface - Mount Kilimanjaro (Africa)


Mountain Formation
Mountains can be a result of:

   1. ___________________________ (Himalayan Mountains; Alps in Europe)

   2. ______________________ (Mount Kilimanjaro-Africa; Parícutin-Mexico)

   3. ______________________ (Mauna Kea- Hawaiian Islands)

   4. ______________________ (Andes Mountains)

   5. ______________________ (Mt. Oraefajokull -Iceland: Mid-Atlantic Ridge)



Continent-Continent Collision
When ____________________ crust pushes against ____________________
crust both sides of the convergent boundary have the same properties.
Neither side of the boundary wants to sink beneath the other side, and as a result the
two plates ________________________________ and the crust buckles and
cracks, __________________ (and down into the mantle), forming ____________

__________________________________

Examples: 1. ___________________________

           2. ___________________________



Basic Earthquake Facts

      Mostly happen along/on _____________________________

      ____________________ can record earthquakes from all over the world

      above 2.5-3 on magnitudescale

      ___________________________________________________


Earthquakes
      _____________________ – The shaking and trembling that results from the
      sudden movement of part of the Earth’s crust
      Scientists predict over ________________________ earthquakes happen
      each year
      ________________________ is most common reason for Earthquakes

Fukushima’s Earthquake
An earthquake shook Fukushima in 11th March 2011. It caused a _______________.



Tsunamis
      Also called _________________________

      Large ocean waves caused by an ________________________________

      Ocean floor _______________________________________________.

      Can also be caused by a ______________________________________.

      Remember this huge wave is caused ________________________________

      They can travel at speeds of _____________________- MPH
They can reach heights of ____________ (the height of a 6 Story Building)


Seismic Waves

      Earthquake waves are known as ___________________________

      ____________- The point beneath the Earth’s surface where rocks break and
      move
      The focus is the point of origin for the earthquake

      ______________________- Directly above the focus on the Earth’s surface

      Earthquake waves reach the epicenter first


__________________________-

      “P-waves”: Seismic waves that travel the __________________

      They arrive at a given point before any other type of wave

      They travel through: _____________, ____________, ____________

      They move through the Earth differently depending on the material they are
      traveling through
      As they move deeper into the Earth, where it is more dense, they move faster

      They are _________________________________


Secondary Waves

___________________ – Seismic waves that do not travel through the Earth as fast
as P-waves do

S-waves arrive at a given point after P-waves do

S-waves travel through ____________________ but not liquids and gases



Surface Waves

          L-waves: They are the ____________________________________

They ___________________________________________________________
 They start at the epicenter and move along the Earth’s surface

       Earth’s surface _____________________________ like water waves do

       They ___________________________ to the Earth because they bend
         and twist the surface



Seismograph

____________________ – An instrument that detects and measures seismic waves

Consists of:
A weight attached to a spring or wire
A pen attached to the weight that records the movement of the Earth on a paper, that
is wound tightly around a constantly moving drum


________________________________ – Scientists who study earthquakes

      They can determine the strength of an earthquake by studying the height of the
      waves
      They look at a ____________________________
      They match the seismogram to a chart called the _______________________
         o Invented in 1935
         o The scale is from one to ten, with any earthquake above 6 being very
            destructive

List one of the major world Earthquakes ________________


Earthquakes may cause:
   1. ____________________________
   2. ____________________________
   3. ____________________________
   4. ____________________________
   5. ___________________________


These can also result from earthquake ___________________________
Volcanoes

   ________________________________________________________.

        o Caused by ________________________ along boundaries.

        o Occur at both ________________________________________.

Formation

____________________: Rock deep within Earth

     High temperature
     High Pressure
     Liquid State
     Found in pockets called __________________________

_______________________ constantly moves and works its way through cracks
toward the surface by _________________________________



_____________________ – Magma that has reached the Earth’s Surface

The place where magma becomes lava is called a _________________________

The opening through which lava erupts is called a ____________________

     Volcanoes can have more than one vent
     Lava will poor from the sides of a volcano as well as the top


All ___________________form from an expulsion of materials from deep within the

earth in the form of enormous amounts of _________________________________

________________________________________________________________.



All are not Alike

Some are ________________________
     Lava oozes from a vent
Others are _______________________
      With lava and other material hurled hundreds of feet in the air
      Gases and earth material mix to be seen from miles away


The opening through which lava erupts is called a ____________________
      Volcanoes can have more than one vent
      Lava will poor from the sides of a volcano as well as the top



Types of Volcanic Eruptions

Two factors determine the type of eruption:

    Amount of __________________________________in the magma

    The ___________________________________ of the magma


Eruptions
During eruptions many rock fragments are blown into the air
      Smallest     = ______________________
      Medium       = ______________________
      Largest      = _______________________
Small volcanic bombs the size of golf balls are called _____________
_______________ (_______________): mixture of ash, eroded land, and water
flowing down river valleys

________________:_______________, carbon dioxide, nitrogen, sulfur dioxide,
hydrogen sulfide, chlorine


Types ofVolcanoes
   Different types of volcanic eruptions form different types of volcanoes
   1. ______________________ - made mostly of ______________ and other
      rock particles that have been blown into the air
                   Form from explosive eruptions
                   Cones are not high
                   Narrow base & steep sides
2. _______________________ – composed of mostly quiet lava flows
                  Gently sloping, domed shaped mountain forms


   3. _____________________ – Built up of alternating layers of rock particles and
      lava
                  First is a violent eruption
                  Then a quiet eruption
                  After many alternating eruptions a cone shape is formed


Volcano Visuals

______________________– volcanic cone made up of layers of hardened lava

______________________– volcanic cone made up of rock particles, dust and ash.

______________________– volcanic cone made up of alternating layers of lava and

rock particles.


Volcano Anatomy




At the top of a funnel-shaped pit or depression is a pit: ___________________

If it becomes to large it is called a ____________________

______________: the above ground structure built from lava and/or tephra
_________________: a smaller secondary volcano built on the side of or near

        the main volcano, but sharing the same conduit to the magma chamber

_____________: a secondary vent that emitsonly gases

_______________: the path that magma takes from the magma chamber to the vent

__________________: a long fissure (crack) from which lava flows

Scientists study the makeup of the lava that spews from the __________________
to gain knowledge about the interior magma


Label




Types of Lava
              Dark-colored/ Water
              Light-colored/ little Water
              Chemical composition of both
              Large amounts of gases
              Steam and carbon dioxide
3 Types of Lava

   1. _______________________:
       Hot, thin, fast flowing
       harden with a relatively smooth surface
       Often has a ropy or wrinkled appearance


   2. ________________________:
          Cooler, thicker, slow moving
          Hardens with a rough, jagged, sharp edge surface


   3. ________________________:
          Lava suddenly cooled by water
          shows sack-like segments (stuffed pillows)


Ring of Fire
      A chain of volcanoes located in the _____________ Ocean


Hot Spots
A part of the mantle is REALLY hot and magma is forced up to the surface
      Creates islands.(Example: Hawaiian Islands)

Magma that may originate in the ___________________________________,

breaking the surface and forming a volcano, they are independent of plate boundaries

and a chain of volcanoes may form as the _______________________________.



Three Major Zones

      Nearly all the way around the edge of the Pacific Ocean: ________________

      Near the Mediterranean Sea: ______________________

      Third Extends through Iceland to the middle of the Atlantic Ocean

      ______________________ – Long ridge of volcanoes
Volcano Activity Levels (Stages)

  1. ________________ (awake): Has erupted within recent time and can erupt
      again at any time.

Pre-eruption activities:

            Increase in _________________________- under the cone

            increase in temperature of cone,

            __________________________-of ice/snow in the crater

            swelling of the cone

            __________________________________

            __________________________________

2. __________________ (sleeping):

      _______eruption within recent times, but there is record of past eruptions

      Can become ___________________________after a “wake up” period

      Example: Mt. Rainier


3. ______________________:

          _________________________within recorded history

          _______________________________________________

          Example: Mount Mazama (Crater Lake)




Make the Plate Boundary Chart.
      1. Fill in the types of boundaries;
      2. The faults associated with each;
      3. The type of stress;
      4. The results

More Related Content

Similar to Mountains%2c earthquakes%2c volcanoes notes

Earthquakes l10 l14
Earthquakes l10 l14Earthquakes l10 l14
Earthquakes l10 l14lkazantzis
 
Volcanoht[1]
Volcanoht[1]Volcanoht[1]
Volcanoht[1]charsh
 
C2c Does The Earth Move
C2c Does The Earth MoveC2c Does The Earth Move
C2c Does The Earth MoveM F Ebden
 
Earthquakes
EarthquakesEarthquakes
Earthquakesplbenton
 
oceanography
oceanographyoceanography
oceanographyplbenton
 

Similar to Mountains%2c earthquakes%2c volcanoes notes (20)

Earthquake Srevised Sci8
Earthquake Srevised Sci8Earthquake Srevised Sci8
Earthquake Srevised Sci8
 
Outline: Chapter 15.2: Volcanoes
Outline: Chapter 15.2: VolcanoesOutline: Chapter 15.2: Volcanoes
Outline: Chapter 15.2: Volcanoes
 
Earthquake Notes Slide show
Earthquake Notes Slide showEarthquake Notes Slide show
Earthquake Notes Slide show
 
Outline: Chapter 15.1: Earthquakes
Outline: Chapter 15.1: EarthquakesOutline: Chapter 15.1: Earthquakes
Outline: Chapter 15.1: Earthquakes
 
Chapter 15 Lesson 1: Earthquakes
Chapter 15 Lesson 1: EarthquakesChapter 15 Lesson 1: Earthquakes
Chapter 15 Lesson 1: Earthquakes
 
Earth Quake Outline
Earth Quake OutlineEarth Quake Outline
Earth Quake Outline
 
Earthquakes final
Earthquakes finalEarthquakes final
Earthquakes final
 
Earthquakes l10 l14
Earthquakes l10 l14Earthquakes l10 l14
Earthquakes l10 l14
 
Chapter 14.3: The Theory of Plate Tectonics
Chapter 14.3: The Theory of Plate TectonicsChapter 14.3: The Theory of Plate Tectonics
Chapter 14.3: The Theory of Plate Tectonics
 
Outline: Chapter 14.3: The Theory of Plate Tectonics
Outline: Chapter 14.3: The Theory of Plate TectonicsOutline: Chapter 14.3: The Theory of Plate Tectonics
Outline: Chapter 14.3: The Theory of Plate Tectonics
 
Dynamic Earth
Dynamic EarthDynamic Earth
Dynamic Earth
 
Trabajo recuperacion 1evaluacion 1bilingual
Trabajo recuperacion 1evaluacion 1bilingualTrabajo recuperacion 1evaluacion 1bilingual
Trabajo recuperacion 1evaluacion 1bilingual
 
Np rocks and minerals
Np rocks and mineralsNp rocks and minerals
Np rocks and minerals
 
Volcanoht[1]
Volcanoht[1]Volcanoht[1]
Volcanoht[1]
 
Interpreting Geologic History Outline
Interpreting Geologic History OutlineInterpreting Geologic History Outline
Interpreting Geologic History Outline
 
C2c Does The Earth Move
C2c Does The Earth MoveC2c Does The Earth Move
C2c Does The Earth Move
 
Trabajo recuperacion 1evaluacion 1bilingual (2)
Trabajo recuperacion 1evaluacion 1bilingual (2)Trabajo recuperacion 1evaluacion 1bilingual (2)
Trabajo recuperacion 1evaluacion 1bilingual (2)
 
Earthquakes
EarthquakesEarthquakes
Earthquakes
 
oceanography
oceanographyoceanography
oceanography
 
Deposition Outline
Deposition OutlineDeposition Outline
Deposition Outline
 

More from harvey09

The rock and fossil record
The rock and fossil recordThe rock and fossil record
The rock and fossil recordharvey09
 
Fossil definitions and words 2012
Fossil definitions and words 2012Fossil definitions and words 2012
Fossil definitions and words 2012harvey09
 
Power point mineral notes
Power point mineral notesPower point mineral notes
Power point mineral notesharvey09
 
Minerals vocabulary
Minerals vocabularyMinerals vocabulary
Minerals vocabularyharvey09
 
Rocks for class 2011
Rocks for class 2011Rocks for class 2011
Rocks for class 2011harvey09
 
The rock cycle vocabulary list
The rock cycle vocabulary listThe rock cycle vocabulary list
The rock cycle vocabulary listharvey09
 
Earthquakes and volcanoes new study guide
Earthquakes and volcanoes new study guideEarthquakes and volcanoes new study guide
Earthquakes and volcanoes new study guideharvey09
 
Earthquakes study guide
Earthquakes study guideEarthquakes study guide
Earthquakes study guideharvey09
 
Earthquakes and volcanoes vocabulary
Earthquakes and volcanoes vocabularyEarthquakes and volcanoes vocabulary
Earthquakes and volcanoes vocabularyharvey09
 
Earthquakes and volcanoes vocabulary
Earthquakes and volcanoes vocabularyEarthquakes and volcanoes vocabulary
Earthquakes and volcanoes vocabularyharvey09
 
09 24-12 earthquakes%2c mountains%2c volcanoes
09 24-12  earthquakes%2c mountains%2c volcanoes09 24-12  earthquakes%2c mountains%2c volcanoes
09 24-12 earthquakes%2c mountains%2c volcanoesharvey09
 
Mountains, earthquakes, and volcanoes
Mountains, earthquakes, and volcanoesMountains, earthquakes, and volcanoes
Mountains, earthquakes, and volcanoesharvey09
 
09 10-12 plate tectonics
09 10-12  plate tectonics09 10-12  plate tectonics
09 10-12 plate tectonicsharvey09
 
2012 updated plate tectonics new one use this one backup
2012 updated plate tectonics new one use this one backup2012 updated plate tectonics new one use this one backup
2012 updated plate tectonics new one use this one backupharvey09
 
Plate tectonics vocabulary
Plate tectonics vocabularyPlate tectonics vocabulary
Plate tectonics vocabularyharvey09
 
Earth interior power point
Earth interior power pointEarth interior power point
Earth interior power pointharvey09
 
Earth layer voc display
Earth  layer voc displayEarth  layer voc display
Earth layer voc displayharvey09
 
Earth layer voc
Earth  layer vocEarth  layer voc
Earth layer vocharvey09
 
Earth interior power point
Earth interior power pointEarth interior power point
Earth interior power pointharvey09
 
Earth’s layers
Earth’s layersEarth’s layers
Earth’s layersharvey09
 

More from harvey09 (20)

The rock and fossil record
The rock and fossil recordThe rock and fossil record
The rock and fossil record
 
Fossil definitions and words 2012
Fossil definitions and words 2012Fossil definitions and words 2012
Fossil definitions and words 2012
 
Power point mineral notes
Power point mineral notesPower point mineral notes
Power point mineral notes
 
Minerals vocabulary
Minerals vocabularyMinerals vocabulary
Minerals vocabulary
 
Rocks for class 2011
Rocks for class 2011Rocks for class 2011
Rocks for class 2011
 
The rock cycle vocabulary list
The rock cycle vocabulary listThe rock cycle vocabulary list
The rock cycle vocabulary list
 
Earthquakes and volcanoes new study guide
Earthquakes and volcanoes new study guideEarthquakes and volcanoes new study guide
Earthquakes and volcanoes new study guide
 
Earthquakes study guide
Earthquakes study guideEarthquakes study guide
Earthquakes study guide
 
Earthquakes and volcanoes vocabulary
Earthquakes and volcanoes vocabularyEarthquakes and volcanoes vocabulary
Earthquakes and volcanoes vocabulary
 
Earthquakes and volcanoes vocabulary
Earthquakes and volcanoes vocabularyEarthquakes and volcanoes vocabulary
Earthquakes and volcanoes vocabulary
 
09 24-12 earthquakes%2c mountains%2c volcanoes
09 24-12  earthquakes%2c mountains%2c volcanoes09 24-12  earthquakes%2c mountains%2c volcanoes
09 24-12 earthquakes%2c mountains%2c volcanoes
 
Mountains, earthquakes, and volcanoes
Mountains, earthquakes, and volcanoesMountains, earthquakes, and volcanoes
Mountains, earthquakes, and volcanoes
 
09 10-12 plate tectonics
09 10-12  plate tectonics09 10-12  plate tectonics
09 10-12 plate tectonics
 
2012 updated plate tectonics new one use this one backup
2012 updated plate tectonics new one use this one backup2012 updated plate tectonics new one use this one backup
2012 updated plate tectonics new one use this one backup
 
Plate tectonics vocabulary
Plate tectonics vocabularyPlate tectonics vocabulary
Plate tectonics vocabulary
 
Earth interior power point
Earth interior power pointEarth interior power point
Earth interior power point
 
Earth layer voc display
Earth  layer voc displayEarth  layer voc display
Earth layer voc display
 
Earth layer voc
Earth  layer vocEarth  layer voc
Earth layer voc
 
Earth interior power point
Earth interior power pointEarth interior power point
Earth interior power point
 
Earth’s layers
Earth’s layersEarth’s layers
Earth’s layers
 

Recently uploaded

Long journey of Ruby standard library at RubyConf AU 2024
Long journey of Ruby standard library at RubyConf AU 2024Long journey of Ruby standard library at RubyConf AU 2024
Long journey of Ruby standard library at RubyConf AU 2024Hiroshi SHIBATA
 
A Journey Into the Emotions of Software Developers
A Journey Into the Emotions of Software DevelopersA Journey Into the Emotions of Software Developers
A Journey Into the Emotions of Software DevelopersNicole Novielli
 
Digital Identity is Under Attack: FIDO Paris Seminar.pptx
Digital Identity is Under Attack: FIDO Paris Seminar.pptxDigital Identity is Under Attack: FIDO Paris Seminar.pptx
Digital Identity is Under Attack: FIDO Paris Seminar.pptxLoriGlavin3
 
Enhancing User Experience - Exploring the Latest Features of Tallyman Axis Lo...
Enhancing User Experience - Exploring the Latest Features of Tallyman Axis Lo...Enhancing User Experience - Exploring the Latest Features of Tallyman Axis Lo...
Enhancing User Experience - Exploring the Latest Features of Tallyman Axis Lo...Scott Andery
 
(How to Program) Paul Deitel, Harvey Deitel-Java How to Program, Early Object...
(How to Program) Paul Deitel, Harvey Deitel-Java How to Program, Early Object...(How to Program) Paul Deitel, Harvey Deitel-Java How to Program, Early Object...
(How to Program) Paul Deitel, Harvey Deitel-Java How to Program, Early Object...AliaaTarek5
 
Merck Moving Beyond Passwords: FIDO Paris Seminar.pptx
Merck Moving Beyond Passwords: FIDO Paris Seminar.pptxMerck Moving Beyond Passwords: FIDO Paris Seminar.pptx
Merck Moving Beyond Passwords: FIDO Paris Seminar.pptxLoriGlavin3
 
Decarbonising Buildings: Making a net-zero built environment a reality
Decarbonising Buildings: Making a net-zero built environment a realityDecarbonising Buildings: Making a net-zero built environment a reality
Decarbonising Buildings: Making a net-zero built environment a realityIES VE
 
Use of FIDO in the Payments and Identity Landscape: FIDO Paris Seminar.pptx
Use of FIDO in the Payments and Identity Landscape: FIDO Paris Seminar.pptxUse of FIDO in the Payments and Identity Landscape: FIDO Paris Seminar.pptx
Use of FIDO in the Payments and Identity Landscape: FIDO Paris Seminar.pptxLoriGlavin3
 
How AI, OpenAI, and ChatGPT impact business and software.
How AI, OpenAI, and ChatGPT impact business and software.How AI, OpenAI, and ChatGPT impact business and software.
How AI, OpenAI, and ChatGPT impact business and software.Curtis Poe
 
New from BookNet Canada for 2024: Loan Stars - Tech Forum 2024
New from BookNet Canada for 2024: Loan Stars - Tech Forum 2024New from BookNet Canada for 2024: Loan Stars - Tech Forum 2024
New from BookNet Canada for 2024: Loan Stars - Tech Forum 2024BookNet Canada
 
Modern Roaming for Notes and Nomad – Cheaper Faster Better Stronger
Modern Roaming for Notes and Nomad – Cheaper Faster Better StrongerModern Roaming for Notes and Nomad – Cheaper Faster Better Stronger
Modern Roaming for Notes and Nomad – Cheaper Faster Better Strongerpanagenda
 
TrustArc Webinar - How to Build Consumer Trust Through Data Privacy
TrustArc Webinar - How to Build Consumer Trust Through Data PrivacyTrustArc Webinar - How to Build Consumer Trust Through Data Privacy
TrustArc Webinar - How to Build Consumer Trust Through Data PrivacyTrustArc
 
Transcript: New from BookNet Canada for 2024: Loan Stars - Tech Forum 2024
Transcript: New from BookNet Canada for 2024: Loan Stars - Tech Forum 2024Transcript: New from BookNet Canada for 2024: Loan Stars - Tech Forum 2024
Transcript: New from BookNet Canada for 2024: Loan Stars - Tech Forum 2024BookNet Canada
 
Take control of your SAP testing with UiPath Test Suite
Take control of your SAP testing with UiPath Test SuiteTake control of your SAP testing with UiPath Test Suite
Take control of your SAP testing with UiPath Test SuiteDianaGray10
 
Genislab builds better products and faster go-to-market with Lean project man...
Genislab builds better products and faster go-to-market with Lean project man...Genislab builds better products and faster go-to-market with Lean project man...
Genislab builds better products and faster go-to-market with Lean project man...Farhan Tariq
 
Rise of the Machines: Known As Drones...
Rise of the Machines: Known As Drones...Rise of the Machines: Known As Drones...
Rise of the Machines: Known As Drones...Rick Flair
 
The Fit for Passkeys for Employee and Consumer Sign-ins: FIDO Paris Seminar.pptx
The Fit for Passkeys for Employee and Consumer Sign-ins: FIDO Paris Seminar.pptxThe Fit for Passkeys for Employee and Consumer Sign-ins: FIDO Paris Seminar.pptx
The Fit for Passkeys for Employee and Consumer Sign-ins: FIDO Paris Seminar.pptxLoriGlavin3
 
Moving Beyond Passwords: FIDO Paris Seminar.pdf
Moving Beyond Passwords: FIDO Paris Seminar.pdfMoving Beyond Passwords: FIDO Paris Seminar.pdf
Moving Beyond Passwords: FIDO Paris Seminar.pdfLoriGlavin3
 
Time Series Foundation Models - current state and future directions
Time Series Foundation Models - current state and future directionsTime Series Foundation Models - current state and future directions
Time Series Foundation Models - current state and future directionsNathaniel Shimoni
 
Why device, WIFI, and ISP insights are crucial to supporting remote Microsoft...
Why device, WIFI, and ISP insights are crucial to supporting remote Microsoft...Why device, WIFI, and ISP insights are crucial to supporting remote Microsoft...
Why device, WIFI, and ISP insights are crucial to supporting remote Microsoft...panagenda
 

Recently uploaded (20)

Long journey of Ruby standard library at RubyConf AU 2024
Long journey of Ruby standard library at RubyConf AU 2024Long journey of Ruby standard library at RubyConf AU 2024
Long journey of Ruby standard library at RubyConf AU 2024
 
A Journey Into the Emotions of Software Developers
A Journey Into the Emotions of Software DevelopersA Journey Into the Emotions of Software Developers
A Journey Into the Emotions of Software Developers
 
Digital Identity is Under Attack: FIDO Paris Seminar.pptx
Digital Identity is Under Attack: FIDO Paris Seminar.pptxDigital Identity is Under Attack: FIDO Paris Seminar.pptx
Digital Identity is Under Attack: FIDO Paris Seminar.pptx
 
Enhancing User Experience - Exploring the Latest Features of Tallyman Axis Lo...
Enhancing User Experience - Exploring the Latest Features of Tallyman Axis Lo...Enhancing User Experience - Exploring the Latest Features of Tallyman Axis Lo...
Enhancing User Experience - Exploring the Latest Features of Tallyman Axis Lo...
 
(How to Program) Paul Deitel, Harvey Deitel-Java How to Program, Early Object...
(How to Program) Paul Deitel, Harvey Deitel-Java How to Program, Early Object...(How to Program) Paul Deitel, Harvey Deitel-Java How to Program, Early Object...
(How to Program) Paul Deitel, Harvey Deitel-Java How to Program, Early Object...
 
Merck Moving Beyond Passwords: FIDO Paris Seminar.pptx
Merck Moving Beyond Passwords: FIDO Paris Seminar.pptxMerck Moving Beyond Passwords: FIDO Paris Seminar.pptx
Merck Moving Beyond Passwords: FIDO Paris Seminar.pptx
 
Decarbonising Buildings: Making a net-zero built environment a reality
Decarbonising Buildings: Making a net-zero built environment a realityDecarbonising Buildings: Making a net-zero built environment a reality
Decarbonising Buildings: Making a net-zero built environment a reality
 
Use of FIDO in the Payments and Identity Landscape: FIDO Paris Seminar.pptx
Use of FIDO in the Payments and Identity Landscape: FIDO Paris Seminar.pptxUse of FIDO in the Payments and Identity Landscape: FIDO Paris Seminar.pptx
Use of FIDO in the Payments and Identity Landscape: FIDO Paris Seminar.pptx
 
How AI, OpenAI, and ChatGPT impact business and software.
How AI, OpenAI, and ChatGPT impact business and software.How AI, OpenAI, and ChatGPT impact business and software.
How AI, OpenAI, and ChatGPT impact business and software.
 
New from BookNet Canada for 2024: Loan Stars - Tech Forum 2024
New from BookNet Canada for 2024: Loan Stars - Tech Forum 2024New from BookNet Canada for 2024: Loan Stars - Tech Forum 2024
New from BookNet Canada for 2024: Loan Stars - Tech Forum 2024
 
Modern Roaming for Notes and Nomad – Cheaper Faster Better Stronger
Modern Roaming for Notes and Nomad – Cheaper Faster Better StrongerModern Roaming for Notes and Nomad – Cheaper Faster Better Stronger
Modern Roaming for Notes and Nomad – Cheaper Faster Better Stronger
 
TrustArc Webinar - How to Build Consumer Trust Through Data Privacy
TrustArc Webinar - How to Build Consumer Trust Through Data PrivacyTrustArc Webinar - How to Build Consumer Trust Through Data Privacy
TrustArc Webinar - How to Build Consumer Trust Through Data Privacy
 
Transcript: New from BookNet Canada for 2024: Loan Stars - Tech Forum 2024
Transcript: New from BookNet Canada for 2024: Loan Stars - Tech Forum 2024Transcript: New from BookNet Canada for 2024: Loan Stars - Tech Forum 2024
Transcript: New from BookNet Canada for 2024: Loan Stars - Tech Forum 2024
 
Take control of your SAP testing with UiPath Test Suite
Take control of your SAP testing with UiPath Test SuiteTake control of your SAP testing with UiPath Test Suite
Take control of your SAP testing with UiPath Test Suite
 
Genislab builds better products and faster go-to-market with Lean project man...
Genislab builds better products and faster go-to-market with Lean project man...Genislab builds better products and faster go-to-market with Lean project man...
Genislab builds better products and faster go-to-market with Lean project man...
 
Rise of the Machines: Known As Drones...
Rise of the Machines: Known As Drones...Rise of the Machines: Known As Drones...
Rise of the Machines: Known As Drones...
 
The Fit for Passkeys for Employee and Consumer Sign-ins: FIDO Paris Seminar.pptx
The Fit for Passkeys for Employee and Consumer Sign-ins: FIDO Paris Seminar.pptxThe Fit for Passkeys for Employee and Consumer Sign-ins: FIDO Paris Seminar.pptx
The Fit for Passkeys for Employee and Consumer Sign-ins: FIDO Paris Seminar.pptx
 
Moving Beyond Passwords: FIDO Paris Seminar.pdf
Moving Beyond Passwords: FIDO Paris Seminar.pdfMoving Beyond Passwords: FIDO Paris Seminar.pdf
Moving Beyond Passwords: FIDO Paris Seminar.pdf
 
Time Series Foundation Models - current state and future directions
Time Series Foundation Models - current state and future directionsTime Series Foundation Models - current state and future directions
Time Series Foundation Models - current state and future directions
 
Why device, WIFI, and ISP insights are crucial to supporting remote Microsoft...
Why device, WIFI, and ISP insights are crucial to supporting remote Microsoft...Why device, WIFI, and ISP insights are crucial to supporting remote Microsoft...
Why device, WIFI, and ISP insights are crucial to supporting remote Microsoft...
 

Mountains%2c earthquakes%2c volcanoes notes

  • 1. Name_________________ Mountains, Earthquakes, andVolcanoes S6E5. Students will investigate the scientific view of how the earth’s surface is formed. c. Describe processes that change rocks and the surface of the earth.  Plate Boundaries 3 Kinds of Plate Boundaries o _______________ o _______________ o _______________ Stress Due mostly to plate movements, the earth’s crust is under a lot of stress. There are 3 types: o “A” occurs where plates pull apart, divergent boundaries, and is called _____________________ o “B” occurs where plates converge, and is called ___________ o “C” occurs where plates move past each other, at transform fault boundaries and is called ____________________ Strain Stress leads to strain on the crust which bends it. If it is warm, under the ground, it can bend. The features are called _________. Upturned folds are _________________ while downturned folds are ___________. Label
  • 2. Or the rock may break, if it is brittle. This causes _____________ –breaks of the earth. Different faults Faults move in different ways, depending on the type of stress on them. Remember “3” types form. 1. ________________________ 2. ________________________ 3. ________________________ Plate Tectonic and Mountain Formation The most common types of mountains: 1. ____________________: from when rock layers are squeezed together and pushed upward –Ural Mountains (Russian) 2. ____________________: form when tension causes land to drop down – Teton Range (USA) 3. ____________________: molten material rises to the Earth’s surface and erupts on the surface - Mount Kilimanjaro (Africa) Mountain Formation Mountains can be a result of: 1. ___________________________ (Himalayan Mountains; Alps in Europe) 2. ______________________ (Mount Kilimanjaro-Africa; Parícutin-Mexico) 3. ______________________ (Mauna Kea- Hawaiian Islands) 4. ______________________ (Andes Mountains) 5. ______________________ (Mt. Oraefajokull -Iceland: Mid-Atlantic Ridge) Continent-Continent Collision When ____________________ crust pushes against ____________________ crust both sides of the convergent boundary have the same properties.
  • 3. Neither side of the boundary wants to sink beneath the other side, and as a result the two plates ________________________________ and the crust buckles and cracks, __________________ (and down into the mantle), forming ____________ __________________________________ Examples: 1. ___________________________ 2. ___________________________ Basic Earthquake Facts Mostly happen along/on _____________________________ ____________________ can record earthquakes from all over the world above 2.5-3 on magnitudescale ___________________________________________________ Earthquakes _____________________ – The shaking and trembling that results from the sudden movement of part of the Earth’s crust Scientists predict over ________________________ earthquakes happen each year ________________________ is most common reason for Earthquakes Fukushima’s Earthquake An earthquake shook Fukushima in 11th March 2011. It caused a _______________. Tsunamis Also called _________________________ Large ocean waves caused by an ________________________________ Ocean floor _______________________________________________. Can also be caused by a ______________________________________. Remember this huge wave is caused ________________________________ They can travel at speeds of _____________________- MPH
  • 4. They can reach heights of ____________ (the height of a 6 Story Building) Seismic Waves Earthquake waves are known as ___________________________ ____________- The point beneath the Earth’s surface where rocks break and move The focus is the point of origin for the earthquake ______________________- Directly above the focus on the Earth’s surface Earthquake waves reach the epicenter first __________________________- “P-waves”: Seismic waves that travel the __________________ They arrive at a given point before any other type of wave They travel through: _____________, ____________, ____________ They move through the Earth differently depending on the material they are traveling through As they move deeper into the Earth, where it is more dense, they move faster They are _________________________________ Secondary Waves ___________________ – Seismic waves that do not travel through the Earth as fast as P-waves do S-waves arrive at a given point after P-waves do S-waves travel through ____________________ but not liquids and gases Surface Waves  L-waves: They are the ____________________________________ They ___________________________________________________________
  • 5.  They start at the epicenter and move along the Earth’s surface  Earth’s surface _____________________________ like water waves do  They ___________________________ to the Earth because they bend and twist the surface Seismograph ____________________ – An instrument that detects and measures seismic waves Consists of: A weight attached to a spring or wire A pen attached to the weight that records the movement of the Earth on a paper, that is wound tightly around a constantly moving drum ________________________________ – Scientists who study earthquakes They can determine the strength of an earthquake by studying the height of the waves They look at a ____________________________ They match the seismogram to a chart called the _______________________ o Invented in 1935 o The scale is from one to ten, with any earthquake above 6 being very destructive List one of the major world Earthquakes ________________ Earthquakes may cause: 1. ____________________________ 2. ____________________________ 3. ____________________________ 4. ____________________________ 5. ___________________________ These can also result from earthquake ___________________________
  • 6. Volcanoes  ________________________________________________________. o Caused by ________________________ along boundaries. o Occur at both ________________________________________. Formation ____________________: Rock deep within Earth High temperature High Pressure Liquid State Found in pockets called __________________________ _______________________ constantly moves and works its way through cracks toward the surface by _________________________________ _____________________ – Magma that has reached the Earth’s Surface The place where magma becomes lava is called a _________________________ The opening through which lava erupts is called a ____________________ Volcanoes can have more than one vent Lava will poor from the sides of a volcano as well as the top All ___________________form from an expulsion of materials from deep within the earth in the form of enormous amounts of _________________________________ ________________________________________________________________. All are not Alike Some are ________________________ Lava oozes from a vent
  • 7. Others are _______________________ With lava and other material hurled hundreds of feet in the air Gases and earth material mix to be seen from miles away The opening through which lava erupts is called a ____________________ Volcanoes can have more than one vent Lava will poor from the sides of a volcano as well as the top Types of Volcanic Eruptions Two factors determine the type of eruption:  Amount of __________________________________in the magma  The ___________________________________ of the magma Eruptions During eruptions many rock fragments are blown into the air Smallest = ______________________ Medium = ______________________ Largest = _______________________ Small volcanic bombs the size of golf balls are called _____________ _______________ (_______________): mixture of ash, eroded land, and water flowing down river valleys ________________:_______________, carbon dioxide, nitrogen, sulfur dioxide, hydrogen sulfide, chlorine Types ofVolcanoes Different types of volcanic eruptions form different types of volcanoes 1. ______________________ - made mostly of ______________ and other rock particles that have been blown into the air Form from explosive eruptions Cones are not high Narrow base & steep sides
  • 8. 2. _______________________ – composed of mostly quiet lava flows Gently sloping, domed shaped mountain forms 3. _____________________ – Built up of alternating layers of rock particles and lava First is a violent eruption Then a quiet eruption After many alternating eruptions a cone shape is formed Volcano Visuals ______________________– volcanic cone made up of layers of hardened lava ______________________– volcanic cone made up of rock particles, dust and ash. ______________________– volcanic cone made up of alternating layers of lava and rock particles. Volcano Anatomy At the top of a funnel-shaped pit or depression is a pit: ___________________ If it becomes to large it is called a ____________________ ______________: the above ground structure built from lava and/or tephra
  • 9. _________________: a smaller secondary volcano built on the side of or near the main volcano, but sharing the same conduit to the magma chamber _____________: a secondary vent that emitsonly gases _______________: the path that magma takes from the magma chamber to the vent __________________: a long fissure (crack) from which lava flows Scientists study the makeup of the lava that spews from the __________________ to gain knowledge about the interior magma Label Types of Lava Dark-colored/ Water Light-colored/ little Water Chemical composition of both Large amounts of gases Steam and carbon dioxide
  • 10. 3 Types of Lava 1. _______________________:  Hot, thin, fast flowing  harden with a relatively smooth surface  Often has a ropy or wrinkled appearance 2. ________________________:  Cooler, thicker, slow moving  Hardens with a rough, jagged, sharp edge surface 3. ________________________:  Lava suddenly cooled by water  shows sack-like segments (stuffed pillows) Ring of Fire A chain of volcanoes located in the _____________ Ocean Hot Spots A part of the mantle is REALLY hot and magma is forced up to the surface Creates islands.(Example: Hawaiian Islands) Magma that may originate in the ___________________________________, breaking the surface and forming a volcano, they are independent of plate boundaries and a chain of volcanoes may form as the _______________________________. Three Major Zones Nearly all the way around the edge of the Pacific Ocean: ________________ Near the Mediterranean Sea: ______________________ Third Extends through Iceland to the middle of the Atlantic Ocean ______________________ – Long ridge of volcanoes
  • 11. Volcano Activity Levels (Stages) 1. ________________ (awake): Has erupted within recent time and can erupt again at any time. Pre-eruption activities: Increase in _________________________- under the cone increase in temperature of cone, __________________________-of ice/snow in the crater swelling of the cone __________________________________ __________________________________ 2. __________________ (sleeping): _______eruption within recent times, but there is record of past eruptions Can become ___________________________after a “wake up” period Example: Mt. Rainier 3. ______________________:  _________________________within recorded history  _______________________________________________  Example: Mount Mazama (Crater Lake) Make the Plate Boundary Chart. 1. Fill in the types of boundaries; 2. The faults associated with each; 3. The type of stress; 4. The results