Post on 03-Jan-2016
Topic: volcanoes and Volcanoes Locations
• Objectives:
– I will understand what a volcano is and how it is formed
– I will understand the 3 locations where volcanoes form at
Volcanoes and You
• A volcano is an opening in the earth’s surface that often forms a mountain when layers of lava and ash build up over time
What is a Volcano?
• A volcano is an opening in the earth’s surface that often forms a mountain as ____of lava and ash build up
over time
Answer Bankapart
constantrises
collidelayers
Magma Rising• How does magma make it
to the surface?• Magma is hotter, lighter
and less dense than the rock around it
• This process is similar to a lava lamp
• Therefore, it slowly makes its way upward toward the earth’s surface
• Eventually it finally makes it’s way to the surface exiting a volcano
How does Magma make it to the Earth’s surface?
• Because it is hotter and less dense, therefore it _____ up to the surface exiting a volcano
Answer Bankapart
constantrises
collidelayers
Volcano Locations
• Volcanoes form at:- Divergent plate boundaries Here plates pull apart as new magma rises
(Ex—Iceland)- Convergent plate boundaries
Here plates collide and one plate subducts where it melts feeding volcanoes at the surface
(Ex—Mt. St. Helens WA)-Hot spots
Here a constant steady flow of magma rises to the surface to form volcanoes
(Ex—Hawaii)
Volcano Locations
• Volcanoes form at:- Divergent plate boundaries Here plates pull apart as new magma rises
(Ex—Iceland)
Divergent Plate Boundary:Spreading Iceland apart
Iceland Hot Springs
Volcano Locations
• Volcanoes form at:- Convergent plate boundaries
Here plates collide & one plate subducts where it melts feeding volcanoes at the surface (Ex—Mt. St. Helens)
Cascade Volcanoes
• From Northern California up to Canada lies a series of volcanoes called the Cascade Mountain Range
• Here the Juan de fuca plate subducts under the north American plate forming a series of volcanoes that stretch form Northern California Up to Canada
• As the Juan de fuca plate subducts, it melts, feeding the volcanoes at the surface
Mount St. Helens
• In 1980, Mt. Saint Helens erupted in the state of Washington
• It was one of the largest recent volcanic eruptions in North America
• Geologists warned people to leave, but despite this, 63 people lost their lives from this eruption
• Heat from the eruption caused snow to melt, creating major floods
The Re-Birth of Mt. Saint Helens
Shockwave blast blew the trees down like toothpicks!
Which way was the blast coming from?Trees behind the mountain were spared
Where did all that ash go?
Volcano Locations
• Volcanoes form at:- Hot Spots
Here a constant steady flow of magma rises to the surface to form volcanoes(Ex—Hawaii)
Hot Spots
Lithospheric Plate
Ocean
• Hawaii formed as the Pacific plate slowly moved over a Hot Spot
• Over Ten Million Years, A chain of Islands formed
Stationary Hot Spot
Where are the 3 locations volcanoes form?
- Divergent plate boundaries Here plates pull _____ as new magma rises
(Ex—Iceland)
- Convergent plate boundaries Here plates _____ and one plate subducts
where
it melts feeding volcanoes at the surface (Ex—Mt. St. Helens WA)
-Hot spots Here a ____steady flow of magma rises to the
surface to form volcanoes (Ex—Hawaii)
Answer Bankapart
constantrises
collidelayers
= Volcanoes
Ring of Fire
• Convergent plate boundaries are located all around the Pacific Rim
• Because of this, volcanoes are located all around the Pacific Ocean
• These volcanoes make up the Ring of Fire
What is the Ring of Fire?
• A chain or ring of volcanoes ____ the pacific ocean created by convergent boundaries
Answer Bankapart
constantrises
Collidearoundlayers
Volcanoes Form at:
_______ Plate Boundaries
Hot ____Divergent Plate
Boundaries
Plates____as magma
rises Plates collide Feeding volcanic
______ above
______ flow of magma to the surface
Answer BankConvergent
Spotsconstant
mountainsspread
Summarize:
Topic: Magma Composition
• Objectives:
– To understand how magma composition effects whether a volcano will erupt violently or quietly
– To understand how silica effects the viscosity or thickness of magma
2 Types of Eruptions
• Some volcanic eruptions are explosive, & violent and while others are non-explosive erupting quietly
• For example, Mt. Saint Helens erupt violently (explosive)
• Kilauea in Hawaii erupts quietly (non-explosive)
Explosive!
Non-Explosive
What are the 2 types of Volcanic Eruptions?
-Explosive, ____eruptions: (Ex: Mt. Saint Helens)
-Non-Explosive, _____ eruptions (Ex: Kilauea)
Answer BankTrapssilicaQuiet
Releasesgasesviolent
Magma Composition
• Why do some volcanoes erupt explosively and others non-explosively?
• It has to do with 3 factors:-the amount of trapped gases in the magma
-viscosity or thickness of the magma
-silica content
Rhyolitic Magma = Explosive Eruptions
Basaltic Magma = Non-Explosive Eruptions
What factors make volcanoes explosive?
• The amount of trapped ____
the magma• Viscosity or thickness of magma• _____ content
Answer BankTrapssilicaQuiet
Releasesgasesviolent
Magma Composition
•Rhyolitic Felsic magma is high in silica, therefore it has a high viscosity (thick) and traps gases producing violent explosive eruptions
•Basaltic Mafic (dark
color) magma is low in silica, therefore it has a low viscosity and releases gases producing quiet non-explosive eruptions
Rhyolitic Magma = Explosive Eruptions
Basaltic Magma = Non-Explosive Eruptions
What is the difference between Rhyolitic and Basaltic magma?
• Rhyolitic magma: – High in silica – High Viscosity (thick)– ____gases (increasing pressure)– creates violent, explosive
eruptions• Basaltic magma:
– Low in silica– Low Viscosity (Very fluid)– _____gas (reducing pressure)– creates quiet, non-Explosive
eruptions
Answer BankTrapssilicaQuiet
Releasesgasesviolent
Magma Link
• http://dsc.discovery.com/convergence/pompeii/interactive/interactive.html
Who has been listening?Which one has the most silica?Which one has the least silica?
Basaltic Rhyolitic
Which magmatraps gases?
Which magma Releases gases?
Which magma contains more silica?
Silica Silica
Summarize!
Explosive Eruptions?
High in Silica?
Traps gases?
High or low Viscosity?
Example
Rhyolitic
___ Yes ___ ____ Viscosity
Mt. St. Helens
Basaltic
___ No ___ ____Viscosity
KilaueaHawaii
• Magma high in _____ is _____ giving it a high viscosity therefore trapping gases
• Magma low in silica is _____ giving it a ____viscosity therefore releasing gases
Answer BankThickHighsilica
viscosityYes(2)Fluidlow
No(2)
Topic: Volcano Types
• Objectives:
– To understand the differences between the 3 major types of volcanoes
– To understand how magma affects the shape and steepness of a volcano
Forms of Volcanoes
• There are three basic types:– Cinder Cone Volcano– Composite Volcano– Shield Volcano
What are the 3 types of Volcanoes?
– Cinder Cone Volcano– Composite Volcano– Shield Volcano
Cinder ConeCinder Cone
Layers of Ash and Cinder
Volcanic Bombs
Pipe
-Smallest type-Steep slopes-Made by layers of Ash and Cinder
-Example: Paracutin, Mexico
3,000m
Paricutin Cinder Cone, Mexico
Sunset Crater
Cinder Cone,Arizona, USA
What is a Cinder What is a Cinder Cone Volcano?Cone Volcano?
Layers of Ash and Cinder
Volcanic Bombs
Pipe
-____ in size-Made of layers Cinder (hot rock) and ash which produce _____slopesEx. Paracutin Mexico
3,000m
Answer BankFlat
Steepmassive
small
Composite Cone
-Composite cones are built up by layers of Ash and thick rhyolitic lava -High viscosity magma traps gases therefore they erupt with great explosive & violent power-Thick rhyolitic magma produces moderately Steep slopes-Example: Mount Saint Helens
Smallcone
Dyke
Crater
Lava Layer Flank eruption
LavaFlow
Crust
Pyroclastic Flow
Mt. Saint Helens,Composite Volcano,
Washington, USA
Mt. Fuji, Composite Volcano, Japan
What is ACompositeVolcano?
-Volcano Made of layers Ash, and _____(thick) lava which produce moderately steep slopes-Thick, ____viscosity magma traps gases producing very explosive & violent eruptionsEx. Mt. St. Helens
Smallcone
Dyke
Crater
Ash layer
Lava Layer Flank eruption
LavaFlow
Crust
Pyroclastic Flow
Answer basalticRhyolitic
Highlow
Shield Volcano-Shield Volcanoes are massive volcanoes built up only from layers of basaltic (fluid) lava giving them a flat gentle sloping shape
-Low viscosity magma releases gases producing quiet, non-explosive eruptions
-Ex: Big Island of Hawaii, USA and Olympus Mons, Mars
250 miles wide!
10,000m
Composite volcano to scale
Layers of Lava Lava Flow
Big Island Hawaii, USA
Big Island, Hawaii
Olympus Mons & Arizona?
What is a Shield Volcano?
-Shield Volcanoes are ______ volcanoes built up only from layers of ______ (fluid) lava giving them a flat gentle sloping shape
-_____ viscosity magma _____ gases producing quiet, non-explosive eruptions
-Ex: Big Island of Hawaii, USA
250 miles wide!
10,000m
Composite volcano to scale
Layers of Lava Lava Flow
AnswerBanksmall
massivebasalticreleases
low
• http://almandine.geol.wwu.edu/~dave/courses/2008/fall/101/lectures/media/Lecture07/VolcanoTypes.swf
Review-Where is a Cinder Cone Volcano?-Where is a Composite Volcano-Where is a Shield Volcano-Which volcano erupts explosively?-Which 2 volcanoes have steep sides?-Which volcano is made of layers of lava,
producing flat sides
A
BC
Cinder Cone
Composite cone
Shield
-____ in size-made of layers Cinder (hot rock) and ash-SteepEx. Paracutin Mexico
-____ in sizeMade of layers Ash and _____ (thick) magma producing ____slopes- High viscosity magma traps gases producing very___& __ eruptions
Ex. Mt. St. Helens
-____ in size-made of layers of _____ (fluid) lava producing flat gentle slopes-Low viscosity magma releases gases producing non-explosive & ____ eruptions-Ex. Big island Hawaii
Summarize:Summarize: please draw table
Answer Bank
RhyoliticModerate(2)
violentSmall
basalticExplosive
quietmassive
Shield
Composite Cinder Cone