Volcanoes
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This document discusses different types of volcanoes. It begins by defining a volcano as a mountain where molten rock, known as magma, rises up from below the earth's surface. Volcanoes form as a result of movement of tectonic plates, which causes fissures through which magma can escape from deep underground. There are three main types of volcanoes: active volcanoes, which frequently erupt; extinct volcanoes, which were once active but will not erupt again; and dormant volcanoes, which were active in the past but are not currently erupting, though could potentially erupt again in the future. Examples of each type are provided.
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Earthquakes and volcanoes
An earthquake is the shaking or vibration of the surface of the earth, ranging from a slight tremor to a violent shaking capable of damaging buildings. Earthquakes are caused by movements in the earth's crust or upper mantle. The document discusses different types of earthquakes based on their depth and magnitude. It also discusses the Richter and Mercalli scales used to measure earthquake magnitude and intensity. The document then summarizes types of volcanic eruptions ranging from relatively non-explosive eruptions to very explosive eruptions that send ash high into the atmosphere. It also discusses different types of volcanic landforms like cinder cones, composite cones, and shield volcanoes.
Volcano. b.ed modified
Volcanoes form when magma rises up from below the earth's crust and emerges at the surface. A volcano has a vent where magma and molten rock, called lava, escape. The lava accumulates to form a volcanic mountain over time. There are three main types of volcanoes: active volcanoes that frequently erupt like Mount Etna in Italy; dormant volcanoes that were once active but have not erupted recently, though could again, like Mount Vesuvius; and extinct volcanoes that were active in the past but will not erupt again, like Mount Kilimanjaro.
Endogenic Process
Volcanoes form as magma rises up from below the Earth's crust and erupts onto the surface. The type and violence of volcanic eruptions depends on factors like the amount of gas in the magma and how easily it can escape. The most common types of volcanoes are composite volcanoes, cinder cone volcanoes, and shield volcanoes, which erupt in different ways and produce different landforms. Most volcanoes occur along plate boundaries in the Pacific Ring of Fire and other convergence zones.
5 theories
Alfred Wegener first proposed the theory of continental drift in 1915, suggesting that the continents were once joined together before slowly drifting apart. His theory was controversial at the time due to a lack of understanding of the underlying mechanisms, but is now widely accepted as plate tectonics. Plate tectonics explains how convection currents in the Earth's mantle cause rigid tectonic plates to move and interact at their boundaries, resulting in phenomena like subduction and mountain building.
Presentation
Volcanoes are caused by molten rock flowing out of fissures in the Earth's surface created by the movement of tectonic plates. There are three types of volcanoes: active volcanoes that frequently erupt, like Mount Etna and Mount Fujiyama; extinct volcanoes that were once active but will not erupt again, such as Kilimanjaro; and dormant volcanoes that erupted in the past but are not currently active, though could erupt again, including Vesuvius.
Volcanoes
This document defines and describes key terms related to volcanoes. It explains that volcanoes form when a dense tectonic plate subducts under a less dense plate, allowing lava to rise to the surface. The main parts of a volcano are identified as the crater, vents, lava pipe, and magma chamber. Volcanic eruptions occur when pressure from magma building up under the crust is released as the magma rises and is pushed through vents and fissures to the surface. A variety of volcanic features and eruption types are also defined, such as shield volcanoes, composite volcanoes, calderas, cinder cones, pyroclastic flows, and more.
Types of volcanoes
This document summarizes the different types of volcanoes:
Fissure volcanoes erupt from long cracks in the ground, spreading vast quantities of lava over wide areas to form flat plains. Cinder cones are small, steep-sided hills formed from eruptions at a single vent that eject fragments of lava. Composite or strato-volcanoes are tall and symmetrical with alternating layers of lava and ash, such as Mount Fuji. Shield volcanoes have broad, low slopes and large craters, exemplified by Hawaiian volcanoes formed from numerous lava flows over great distances.
Volcanoes and eruptions
Volcanoes form at plate boundaries or in hotspots in the mantle not associated with plate boundaries. There are three main types of volcanoes: shield volcanoes which have gentle slopes built up from fluid lava flows; cinder cone volcanoes which are steep sided due to explosive eruptions throwing tephra into the air; and composite volcanoes which have layers of both lava and tephra from eruptions that alternate between explosive and nonexplosive. The amount of gas and silica in magma determines the explosiveness of an eruption, with more gas and less silica leading to more violent eruptions as the gas escapes quickly closer to the surface.
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An earthquake is the shaking or vibration of the surface of the earth, ranging from a slight tremor to a violent shaking capable of damaging buildings. Earthquakes are caused by movements in the earth's crust or upper mantle. The document discusses different types of earthquakes based on their depth and magnitude. It also discusses the Richter and Mercalli scales used to measure earthquake magnitude and intensity. The document then summarizes types of volcanic eruptions ranging from relatively non-explosive eruptions to very explosive eruptions that send ash high into the atmosphere. It also discusses different types of volcanic landforms like cinder cones, composite cones, and shield volcanoes.
Volcano. b.ed modified
Volcanoes form when magma rises up from below the earth's crust and emerges at the surface. A volcano has a vent where magma and molten rock, called lava, escape. The lava accumulates to form a volcanic mountain over time. There are three main types of volcanoes: active volcanoes that frequently erupt like Mount Etna in Italy; dormant volcanoes that were once active but have not erupted recently, though could again, like Mount Vesuvius; and extinct volcanoes that were active in the past but will not erupt again, like Mount Kilimanjaro.
Endogenic Process
Volcanoes form as magma rises up from below the Earth's crust and erupts onto the surface. The type and violence of volcanic eruptions depends on factors like the amount of gas in the magma and how easily it can escape. The most common types of volcanoes are composite volcanoes, cinder cone volcanoes, and shield volcanoes, which erupt in different ways and produce different landforms. Most volcanoes occur along plate boundaries in the Pacific Ring of Fire and other convergence zones.
5 theories
Alfred Wegener first proposed the theory of continental drift in 1915, suggesting that the continents were once joined together before slowly drifting apart. His theory was controversial at the time due to a lack of understanding of the underlying mechanisms, but is now widely accepted as plate tectonics. Plate tectonics explains how convection currents in the Earth's mantle cause rigid tectonic plates to move and interact at their boundaries, resulting in phenomena like subduction and mountain building.
Presentation
Volcanoes are caused by molten rock flowing out of fissures in the Earth's surface created by the movement of tectonic plates. There are three types of volcanoes: active volcanoes that frequently erupt, like Mount Etna and Mount Fujiyama; extinct volcanoes that were once active but will not erupt again, such as Kilimanjaro; and dormant volcanoes that erupted in the past but are not currently active, though could erupt again, including Vesuvius.
Volcanoes
This document defines and describes key terms related to volcanoes. It explains that volcanoes form when a dense tectonic plate subducts under a less dense plate, allowing lava to rise to the surface. The main parts of a volcano are identified as the crater, vents, lava pipe, and magma chamber. Volcanic eruptions occur when pressure from magma building up under the crust is released as the magma rises and is pushed through vents and fissures to the surface. A variety of volcanic features and eruption types are also defined, such as shield volcanoes, composite volcanoes, calderas, cinder cones, pyroclastic flows, and more.
Types of volcanoes
This document summarizes the different types of volcanoes:
Fissure volcanoes erupt from long cracks in the ground, spreading vast quantities of lava over wide areas to form flat plains. Cinder cones are small, steep-sided hills formed from eruptions at a single vent that eject fragments of lava. Composite or strato-volcanoes are tall and symmetrical with alternating layers of lava and ash, such as Mount Fuji. Shield volcanoes have broad, low slopes and large craters, exemplified by Hawaiian volcanoes formed from numerous lava flows over great distances.
Volcanoes and eruptions
Volcanoes form at plate boundaries or in hotspots in the mantle not associated with plate boundaries. There are three main types of volcanoes: shield volcanoes which have gentle slopes built up from fluid lava flows; cinder cone volcanoes which are steep sided due to explosive eruptions throwing tephra into the air; and composite volcanoes which have layers of both lava and tephra from eruptions that alternate between explosive and nonexplosive. The amount of gas and silica in magma determines the explosiveness of an eruption, with more gas and less silica leading to more violent eruptions as the gas escapes quickly closer to the surface.
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The document discusses the origin of the word volcano and the three main types of volcanoes: composite volcanoes, cinder cones, and shield volcanoes. It provides examples of children creating composite and cinder cone volcanoes with household materials. The concept of volcanoes is explained as vents in the earth's crust that allow magma and gases to escape, usually forming near boundaries where tectonic plates meet.
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The document provides information about volcanoes and volcanic landforms and processes. It defines key terms like caldera, crater, lava, magma, tuff, and describes different types of volcanoes like Hawaiian, Strombolian, Vulcanian, and Vesuvius. It also summarizes the 1991 eruption of Mount Pinatubo in the Philippines, which was the second largest terrestrial eruption of the 20th century and ejected around 10 cubic km of magma and 20 million tons of sulfur dioxide into the atmosphere.
The Earth¨S Struct Ii]
Faults are fractures in rock where one side has moved relative to the other. There are three main types of faults: dip-slip, where one side moves up or down; strike-slip, where one side moves horizontally; and oblique-slip, which is a combination of the two. Earthquakes are caused by the sudden release of energy along faults. While most quakes are minor, major ones can cause significant damage. Protecting buildings from earthquake damage through careful engineering can help reduce risks to people. Volcanoes form when magma rises to the surface through openings and erupts. They can be active, dormant, or extinct based on current activity levels. Supervolcanoes are the largest type of volcano
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The Earth's crust is made up of large tectonic plates that are cracked and move, with magma from the mantle able to rise up through these cracks. When pressure builds from below, volcanoes erupt as the magma finds a way to escape either through faults between plates or by bursting through weak spots in the crust. Inside volcanoes is a magma chamber where magma collects until pressure is great enough for an eruption to occur, expelling lava, tephra, ash, and gases. The type of eruption depends on the viscosity of the magma and amount of dissolved gases, with more gas and thick magma causing explosive eruptions that blast material high into the air.
powerpoint
Volcanoes form when magma rises up through fissures in the Earth's crust caused by movement of tectonic plates. The opening where magma emerges onto the surface is called a vent, and the funnel-shaped depression at the top of an erupting volcano is termed a crater. Active volcanoes frequently erupt, while dormant volcanoes were active in the past but are not currently erupting, though they could become active again. Areas around volcanoes are rich in minerals and some have developed healing hot springs, fertile soil, and tourist attractions.
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Volcano terms
caldera
cinder cone
dacite
debris avalanche
dike
dome
dome lava fountain
effusive eruption
eruption cloud
eruption size
fault
fissure
fumarole
gas
geyser
hornito
hummock
kipuka
lahar
lapilli
lava
lava cascade
lava channel
lava delta
lava drapery
lava flow
lava fountain
lava fountain dome
lava lake
lava spillway
lava surge
lava tube
limu
littoral cone
maar
magma
mineral
mud volcano
obsidian
pahoehoe
pahoehoe blister
pahoehoe coil
pahoehoe entrail
pahoehoe - ropy
pahoehoe toe
Pele's hair
Pele's tears
phreatic eruption
pillow lava
plinian eruption
pit crater
pumice
pyroclastic flow
reticulite
rhyolite
rift zone
rock
rootless shield
scoria
shield volcano
spatter
spatter cone and rampart
spatter and cinder cone
stratovolcano
Strombolian eruption
tephra
tree mold
tsunami
tumulus
vent
volcanic dome
volcano
volcanic rocks
volcanic gases
Vulcanian eruption
caldera
cinder cone
hornito
maar
mud volcano
shield volcano
spatter cone
stratovolcano
volcanic dome
Volcanes
A volcano emits melted rock (magma) that hardens into lava and gases from the planet's interior. Magma cools and hardens into lava. The Chaiten volcano in Chile erupted in 2008 after 9,000 years of dormancy, spewing ash for miles and devastating the nearby town of Chaiten through ash and flooding, claiming at least one life. Underwater volcanoes increase water temperatures through thermal heating, affecting the earth's atmosphere, and form from cracks in the ocean floor caused by differences in density between the ocean surface and mantle.
Volcanoesrevised
A volcano is a mountain formed by erupted lava and ash from vents in the Earth's crust. It consists of a magma chamber, conduit, and vent. Volcanoes can have different features like rugged peaks or summit craters depending on how lava is emitted. Magma rises from underground chambers and erupts due to pressure or plate collisions. When magma reaches the surface it is called lava. Volcanoes are classified as active, dormant, or extinct based on recent eruption activity. Eruptions can endanger nearby populations through poisonous gases and have caused over 200,000 deaths in the last 500 years.
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Volcanoes are openings in the earth's crust that eject lava, pyroclasts, and gases during eruptions. There are three main types of volcanoes: shield volcanoes, cinder cone volcanoes, and composite or stratovolcanoes. Cinder cone volcanoes are small, steep-sided hills made of loose cinders ejected during eruptions. Volcanic eruptions can be either explosive or violent, ejecting pyroclasts and ash, or quiet and non-explosive, with gentle lava flows.
The Tectonic Plates And Volcanoes
1) Tectonic plates slowly move across the Earth's surface over the course of a year, occasionally crashing into each other. When they crash, it can cause natural disasters like volcanic eruptions and earthquakes.
2) Volcanoes form as magma cools and piles up from cracks in the Earth's crust caused by the movement of tectonic plates and resulting earthquakes.
3) Tectonic plate collisions, though slow, continually form new landforms like mountains and volcanoes as the plates interact within the limited space available.
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The document discusses different types of volcanoes and how they can change Earth's surface quickly. It describes cinder cone, shield cone, and composite cone volcanoes. Cinder cones are small and circular, forming from ejected cinders. Shield cones are large and shield-shaped, building up from lava flows. Composite cones like Mount St. Helens are steep-sided and cone-shaped, often erupting explosively due to trapped viscous magma. Volcanoes can quickly change Earth's surface through lava flows and explosive eruptions that spread rock and ash over wide areas.
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This document discusses different types of volcanoes and mountains. It describes volcanoes as being caused by molten rock flowing through fissures in the earth's surface. Volcanoes are classified as active, extinct, or dormant based on their eruption patterns. There are four types of mountains based on their origin: fold mountains formed by faulting, block mountains also formed by faulting, relict mountains formed by erosion of old mountains, and volcanic mountains associated with volcanic activity. The document also briefly mentions various landforms caused by erosion from running water like V-shaped valleys, waterfalls, flood plains, and deltas.
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This document appears to be an intervention material for teaching about the three main types of volcanoes: cinder cones, composite volcanoes, and shield volcanoes. It includes descriptions of each type of volcano along with examples. There are also activity and assessment sections that ask students to classify volcanoes and illustrate similarities and differences between the three types in a Venn diagram. The overall goal seems to be helping students learn the distinguishing characteristics of cinder cones, composite volcanoes, and shield volcanoes.
Types of Volcanoes
There are three main types of volcanoes that form from different geological processes:
1) Hotspot volcanoes like those in Hawaii form when magma rises from a hotspot in the mantle as a tectonic plate moves over it. Eruptions are less explosive due to fluid magma.
2) Shield volcanoes form at divergent plate boundaries and from hotspots, with low, wide shapes from fluid basaltic magma.
3) Composite volcanoes form at convergent plate boundaries, where one plate subducts under another. They have steep sides due to more viscous magma and explosive eruptions, producing hazards like pyroclastic flows and lahars.
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Numeracy@English
CLIL workshop
Teacher: Angeles Cabrera Hernandes
Valsequillo, Gran Canaria
November, 2017
Volcanoes
This document discusses volcanoes, including how they form, the different types of volcanoes, and where they are located. It provides details on four main types of volcanoes: cinder cones, composite volcanoes, shield volcanoes, and lava domes. Cinder cones are simple structures built from ejected cinders. Composite volcanoes are large symmetrical cones made of layers of material. Shield volcanoes are broad structures composed of fluid lava flows. Lava domes are small, bulbous masses that pile over the vent. Volcanoes can be located both under water and on land.
Earth Science 6.3 : Causes of Volcanic Eruptions
Magma forms deep underground due to decreasing pressure and rising temperature, and volcanoes erupt when this magma reaches the surface. Most volcanoes are located along plate boundaries, where tectonic plates are moving apart or colliding. Scientists can predict volcanic eruptions by monitoring earthquake activity, volcanic gas emissions, changes in slope and surface temperature at volcanoes, all of which indicate rising magma.
Volcanoes
This document discusses different types of volcanoes. It begins by defining a volcano as a mountain where molten rock, known as magma, rises up from below the earth's surface. Volcanoes form as a result of movement of tectonic plates, which causes fissures through which magma can escape from the asthenosphere onto the earth's crust through vents. The document then describes three types of volcanoes: active volcanoes that frequently erupt, such as Mount Etna; extinct volcanoes that were once active but will not erupt again, like Kilimanjaro; and dormant volcanoes that were active in the past but are not currently erupting, though could become active again in the
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The document discusses the origin of the word volcano and the three main types of volcanoes: composite volcanoes, cinder cones, and shield volcanoes. It provides examples of children creating composite and cinder cone volcanoes with household materials. The concept of volcanoes is explained as vents in the earth's crust that allow magma and gases to escape, usually forming near boundaries where tectonic plates meet.
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The document provides information about volcanoes and volcanic landforms and processes. It defines key terms like caldera, crater, lava, magma, tuff, and describes different types of volcanoes like Hawaiian, Strombolian, Vulcanian, and Vesuvius. It also summarizes the 1991 eruption of Mount Pinatubo in the Philippines, which was the second largest terrestrial eruption of the 20th century and ejected around 10 cubic km of magma and 20 million tons of sulfur dioxide into the atmosphere.
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The Earth's crust is made up of large tectonic plates that are cracked and move, with magma from the mantle able to rise up through these cracks. When pressure builds from below, volcanoes erupt as the magma finds a way to escape either through faults between plates or by bursting through weak spots in the crust. Inside volcanoes is a magma chamber where magma collects until pressure is great enough for an eruption to occur, expelling lava, tephra, ash, and gases. The type of eruption depends on the viscosity of the magma and amount of dissolved gases, with more gas and thick magma causing explosive eruptions that blast material high into the air.
powerpoint
Volcanoes form when magma rises up through fissures in the Earth's crust caused by movement of tectonic plates. The opening where magma emerges onto the surface is called a vent, and the funnel-shaped depression at the top of an erupting volcano is termed a crater. Active volcanoes frequently erupt, while dormant volcanoes were active in the past but are not currently erupting, though they could become active again. Areas around volcanoes are rich in minerals and some have developed healing hot springs, fertile soil, and tourist attractions.
Intro to volcanoes module
Provided to the METSAT Element of the Weather Intelligence flight, to help the analysts get a better understanding of volcanoes.
Volcano terms
caldera
cinder cone
dacite
debris avalanche
dike
dome
dome lava fountain
effusive eruption
eruption cloud
eruption size
fault
fissure
fumarole
gas
geyser
hornito
hummock
kipuka
lahar
lapilli
lava
lava cascade
lava channel
lava delta
lava drapery
lava flow
lava fountain
lava fountain dome
lava lake
lava spillway
lava surge
lava tube
limu
littoral cone
maar
magma
mineral
mud volcano
obsidian
pahoehoe
pahoehoe blister
pahoehoe coil
pahoehoe entrail
pahoehoe - ropy
pahoehoe toe
Pele's hair
Pele's tears
phreatic eruption
pillow lava
plinian eruption
pit crater
pumice
pyroclastic flow
reticulite
rhyolite
rift zone
rock
rootless shield
scoria
shield volcano
spatter
spatter cone and rampart
spatter and cinder cone
stratovolcano
Strombolian eruption
tephra
tree mold
tsunami
tumulus
vent
volcanic dome
volcano
volcanic rocks
volcanic gases
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caldera
cinder cone
hornito
maar
mud volcano
shield volcano
spatter cone
stratovolcano
volcanic dome
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A volcano emits melted rock (magma) that hardens into lava and gases from the planet's interior. Magma cools and hardens into lava. The Chaiten volcano in Chile erupted in 2008 after 9,000 years of dormancy, spewing ash for miles and devastating the nearby town of Chaiten through ash and flooding, claiming at least one life. Underwater volcanoes increase water temperatures through thermal heating, affecting the earth's atmosphere, and form from cracks in the ocean floor caused by differences in density between the ocean surface and mantle.
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A volcano is a mountain formed by erupted lava and ash from vents in the Earth's crust. It consists of a magma chamber, conduit, and vent. Volcanoes can have different features like rugged peaks or summit craters depending on how lava is emitted. Magma rises from underground chambers and erupts due to pressure or plate collisions. When magma reaches the surface it is called lava. Volcanoes are classified as active, dormant, or extinct based on recent eruption activity. Eruptions can endanger nearby populations through poisonous gases and have caused over 200,000 deaths in the last 500 years.
How tides work
Tides are caused by the gravitational pull of the moon and sun on Earth's oceans, with the moon having the strongest influence due to its closer proximity. Other factors like strong winds, underwater seismic events, and explosions can also influence tidal patterns and heights to a lesser extent. The regular waxing and waning of the tides is due to Earth's revolution around the sun and the moon's revolution around Earth.
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Volcanoes are openings in the earth's crust that eject lava, pyroclasts, and gases during eruptions. There are three main types of volcanoes: shield volcanoes, cinder cone volcanoes, and composite or stratovolcanoes. Cinder cone volcanoes are small, steep-sided hills made of loose cinders ejected during eruptions. Volcanic eruptions can be either explosive or violent, ejecting pyroclasts and ash, or quiet and non-explosive, with gentle lava flows.
The Tectonic Plates And Volcanoes
1) Tectonic plates slowly move across the Earth's surface over the course of a year, occasionally crashing into each other. When they crash, it can cause natural disasters like volcanic eruptions and earthquakes.
2) Volcanoes form as magma cools and piles up from cracks in the Earth's crust caused by the movement of tectonic plates and resulting earthquakes.
3) Tectonic plate collisions, though slow, continually form new landforms like mountains and volcanoes as the plates interact within the limited space available.
Volcanoes and Earthquakes
The document discusses different types of volcanoes and how they can change Earth's surface quickly. It describes cinder cone, shield cone, and composite cone volcanoes. Cinder cones are small and circular, forming from ejected cinders. Shield cones are large and shield-shaped, building up from lava flows. Composite cones like Mount St. Helens are steep-sided and cone-shaped, often erupting explosively due to trapped viscous magma. Volcanoes can quickly change Earth's surface through lava flows and explosive eruptions that spread rock and ash over wide areas.
ppt practicum
This document discusses different types of volcanoes and mountains. It describes volcanoes as being caused by molten rock flowing through fissures in the earth's surface. Volcanoes are classified as active, extinct, or dormant based on their eruption patterns. There are four types of mountains based on their origin: fold mountains formed by faulting, block mountains also formed by faulting, relict mountains formed by erosion of old mountains, and volcanic mountains associated with volcanic activity. The document also briefly mentions various landforms caused by erosion from running water like V-shaped valleys, waterfalls, flood plains, and deltas.
Intervention Material in Science: Types of Volcanoes
This document appears to be an intervention material for teaching about the three main types of volcanoes: cinder cones, composite volcanoes, and shield volcanoes. It includes descriptions of each type of volcano along with examples. There are also activity and assessment sections that ask students to classify volcanoes and illustrate similarities and differences between the three types in a Venn diagram. The overall goal seems to be helping students learn the distinguishing characteristics of cinder cones, composite volcanoes, and shield volcanoes.
Types of Volcanoes
There are three main types of volcanoes that form from different geological processes:
1) Hotspot volcanoes like those in Hawaii form when magma rises from a hotspot in the mantle as a tectonic plate moves over it. Eruptions are less explosive due to fluid magma.
2) Shield volcanoes form at divergent plate boundaries and from hotspots, with low, wide shapes from fluid basaltic magma.
3) Composite volcanoes form at convergent plate boundaries, where one plate subducts under another. They have steep sides due to more viscous magma and explosive eruptions, producing hazards like pyroclastic flows and lahars.
Inside a volcano
Numeracy@English
CLIL workshop
Teacher: Angeles Cabrera Hernandes
Valsequillo, Gran Canaria
November, 2017
Volcanoes
This document discusses volcanoes, including how they form, the different types of volcanoes, and where they are located. It provides details on four main types of volcanoes: cinder cones, composite volcanoes, shield volcanoes, and lava domes. Cinder cones are simple structures built from ejected cinders. Composite volcanoes are large symmetrical cones made of layers of material. Shield volcanoes are broad structures composed of fluid lava flows. Lava domes are small, bulbous masses that pile over the vent. Volcanoes can be located both under water and on land.
Earth Science 6.3 : Causes of Volcanic Eruptions
Magma forms deep underground due to decreasing pressure and rising temperature, and volcanoes erupt when this magma reaches the surface. Most volcanoes are located along plate boundaries, where tectonic plates are moving apart or colliding. Scientists can predict volcanic eruptions by monitoring earthquake activity, volcanic gas emissions, changes in slope and surface temperature at volcanoes, all of which indicate rising magma.
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The document summarizes the process an artist took to create a final piece of artwork inspired by Cubism. It describes how the artist conducted research on Cubist artists like Picasso and Feininger, experimented with Cubist drawing techniques, and developed prototypes using different colors and styles. The artist settled on a style inspired by Charles Sheeler's industrial works, creating a final piece that broke down an image into colored sections and added texture through cut-out shapes.
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The document outlines the artist's plan to create a mixed media collage inspired by cubist works. They intend to use various materials like tissue paper, card, paint, and more to represent the complexity, color, and structure of a bike shelter on campus in an abstract, cubist style. The collage will be framed at A3 size to hang in the office of their client Dan Dean, who commissioned a piece exploring part of the college in an original way.
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Short note on shed
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Android L
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Volcanoes
- 1. REJANI.R [SOCIAL SCIENCE} CANDIDATE CODE :13340017
- 2. INTRODUCTION A volcano is a mountain that opens downward to a pool of molten rock below the surface of the earth. When pressure builds up, eruptions occur. Volcanoes are caused when molten rocks flows out onto earth’s surface through fissures that are caused due to the movement of plates. The fissures through which the magma comes out from the aesthenosphere on to the crust of the earth is known as the vent.
- 3. VOLCANOES
- 4. DIFFERENT TYPES OF VOLCANOES Active:-Those that frequently erupt. Eg. Mt.Etna in Italy.
- 5. Extinct: Active at time . But will not erupt again Eg. Kilimanjaro.
- 6. Dormant: Those that have erupted earlier and not active in the recent past.But can become active. Eg. Vsuvius in Italy