Types of volcanoes:fatoumata camara 4ºa
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There are three main types of volcanoes classified based on their activity and structure: 1) Active volcanoes erupt regularly, dormant volcanoes have erupted in the past but are currently quiet, and extinct volcanoes are unlikely to erupt again due to lack of lava supply. 2) Shield volcanoes have broad, gentle slopes built by fluid lava flows. Composite volcanoes have a steep, conical shape formed from layers of hardened lava and ash. 3) Examples include Mauna Loa, a shield volcano in Hawaii, and Mount St. Helens, a composite volcano in Washington, USA.
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Types of the volcanoes
There are many different types of volcanoes beyond the Hollywood version of a tall conical mountain. Some of the main types include shield volcanoes, which are broad with flat tops and low slopes like those in Hawaii; composite volcanoes like Mount Fuji which are tall and steep; cinder cones which are small, steep-sided mounds formed from loose debris; and submarine volcanoes common on ocean floors, which form underwater without disturbing the surface. Fissure volcanoes have cracks that erupt vast quantities of lava to form flat plains rather than a central mountain.
History of earth
The document summarizes key events in Earth's history from the formation of the solar system to the present. It describes the origin of life beginning with simple prokaryotes over 3 billion years ago. The first complex eukaryotic cells emerged around 1.7 billion years ago, followed by multicellular organisms over 700 million years ago. The development of land plants and animals is outlined through the Precambrian, Paleozoic, Mesozoic and Cenozoic eras, along with changing climates and configurations of the Earth's continents and oceans. Absolute and relative dating methods are also summarized that are used to determine the age of geological features and fossils.
Plate Movements Ppt
The document discusses the four spheres of the Earth - atmosphere, hydrosphere, lithosphere, and biosphere. It then describes the layers that make up Earth's interior - crust, mantle, outer core, and inner core. The rest of the document discusses plate tectonic theory, the three types of plate boundaries and movements (divergent, convergent, transform), associated volcanic and earthquake activity, and the impacts of earthquakes and volcanoes.
Hotspots
Three key points about hotspots:
1) Hotspots are volcanic regions thought to be fed by anomalously hot mantle material rising independently of tectonic plate boundaries. Well-known examples include Hawaii, Iceland, and Yellowstone.
2) There are two hypotheses for the origin of hotspots - one involving mantle plumes rising from the core-mantle boundary, the other involving passive rising of melt from shallow depths.
3) Hotspot tracks provide evidence for the plate tectonics model, as volcanic chains like the Hawaiian Islands can be explained by plates migrating over fixed mantle plumes.
Seafloor Spreading
Earth and Life Science
Earth Materials and Processes: Deformation of the Crust
The learners shall be able to:
1) explain how the seafloor spreads (S11/12ESId-23);
2) describe the structure and evolution of ocean basins (S11/12ES-Id-24); and
3) explain how the movement of plates leads to the formation of folds and faults (S11/12ES-Id-22).
Specific Learning Outcomes
At the end of the lesson, the learners will be able to:
1. Discuss the history behind the Theory of Continental Drift;
2. Describe the Continental Drift Theory;
3. Enumerate and explain the evidence used to support the idea of drifting continents;
4. Identify major physiographic features of ocean basins
5. Describe the process of seafloor spreading
TYPES OF PLATE BOUNDARIES
This document discusses three main types of plate boundaries: divergent boundaries, convergent boundaries, and transform boundaries. It provides examples and describes the geological effects of each boundary type. It also discusses processes at divergent boundaries like mid-ocean ridges and continental rift valleys. Convergent boundaries include oceanic-oceanic convergence forming island arcs, and continental-oceanic convergence forming volcanic mountain ranges. Transform boundaries involve strike-slip faulting along plate edges. Additionally, the document touches on hot spot volcanism unrelated to plate boundaries.
Folds and faults ppt
The document provides information about folds and faults. It defines folds as bent or curved rock layers, and describes common fold types like anticlines and synclines. It also defines various fault types including normal faults, thrust faults, strike-slip faults, and oblique faults. Specific structures are described like the San Andreas Fault, which is a major strike-slip fault in California. Dip, strike, heave and throw are also defined in relation to describing the orientation and movement of geological structures.
Plate Tectonics
The document discusses plate tectonics and the structure and dynamics of the Earth's interior. It describes how the crust is broken into plates that move atop the mantle due to convection currents, and the three types of plate boundaries: divergent where plates move apart, convergent where they move together, and transform where they slide past each other. It provides examples of associated geological features like mid-ocean ridges, subduction zones, volcanoes, and earthquakes.
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Types of the volcanoes
There are many different types of volcanoes beyond the Hollywood version of a tall conical mountain. Some of the main types include shield volcanoes, which are broad with flat tops and low slopes like those in Hawaii; composite volcanoes like Mount Fuji which are tall and steep; cinder cones which are small, steep-sided mounds formed from loose debris; and submarine volcanoes common on ocean floors, which form underwater without disturbing the surface. Fissure volcanoes have cracks that erupt vast quantities of lava to form flat plains rather than a central mountain.
History of earth
The document summarizes key events in Earth's history from the formation of the solar system to the present. It describes the origin of life beginning with simple prokaryotes over 3 billion years ago. The first complex eukaryotic cells emerged around 1.7 billion years ago, followed by multicellular organisms over 700 million years ago. The development of land plants and animals is outlined through the Precambrian, Paleozoic, Mesozoic and Cenozoic eras, along with changing climates and configurations of the Earth's continents and oceans. Absolute and relative dating methods are also summarized that are used to determine the age of geological features and fossils.
Plate Movements Ppt
The document discusses the four spheres of the Earth - atmosphere, hydrosphere, lithosphere, and biosphere. It then describes the layers that make up Earth's interior - crust, mantle, outer core, and inner core. The rest of the document discusses plate tectonic theory, the three types of plate boundaries and movements (divergent, convergent, transform), associated volcanic and earthquake activity, and the impacts of earthquakes and volcanoes.
Hotspots
Three key points about hotspots:
1) Hotspots are volcanic regions thought to be fed by anomalously hot mantle material rising independently of tectonic plate boundaries. Well-known examples include Hawaii, Iceland, and Yellowstone.
2) There are two hypotheses for the origin of hotspots - one involving mantle plumes rising from the core-mantle boundary, the other involving passive rising of melt from shallow depths.
3) Hotspot tracks provide evidence for the plate tectonics model, as volcanic chains like the Hawaiian Islands can be explained by plates migrating over fixed mantle plumes.
Seafloor Spreading
Earth and Life Science
Earth Materials and Processes: Deformation of the Crust
The learners shall be able to:
1) explain how the seafloor spreads (S11/12ESId-23);
2) describe the structure and evolution of ocean basins (S11/12ES-Id-24); and
3) explain how the movement of plates leads to the formation of folds and faults (S11/12ES-Id-22).
Specific Learning Outcomes
At the end of the lesson, the learners will be able to:
1. Discuss the history behind the Theory of Continental Drift;
2. Describe the Continental Drift Theory;
3. Enumerate and explain the evidence used to support the idea of drifting continents;
4. Identify major physiographic features of ocean basins
5. Describe the process of seafloor spreading
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This document discusses three main types of plate boundaries: divergent boundaries, convergent boundaries, and transform boundaries. It provides examples and describes the geological effects of each boundary type. It also discusses processes at divergent boundaries like mid-ocean ridges and continental rift valleys. Convergent boundaries include oceanic-oceanic convergence forming island arcs, and continental-oceanic convergence forming volcanic mountain ranges. Transform boundaries involve strike-slip faulting along plate edges. Additionally, the document touches on hot spot volcanism unrelated to plate boundaries.
Folds and faults ppt
The document provides information about folds and faults. It defines folds as bent or curved rock layers, and describes common fold types like anticlines and synclines. It also defines various fault types including normal faults, thrust faults, strike-slip faults, and oblique faults. Specific structures are described like the San Andreas Fault, which is a major strike-slip fault in California. Dip, strike, heave and throw are also defined in relation to describing the orientation and movement of geological structures.
Plate Tectonics
The document discusses plate tectonics and the structure and dynamics of the Earth's interior. It describes how the crust is broken into plates that move atop the mantle due to convection currents, and the three types of plate boundaries: divergent where plates move apart, convergent where they move together, and transform where they slide past each other. It provides examples of associated geological features like mid-ocean ridges, subduction zones, volcanoes, and earthquakes.
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This document provides an introduction to the theory of plate tectonics. It discusses the internal structure of the Earth and how the crust is made up of different types of plates. It then explains Alfred Wegener's theory of continental drift from 1915 and describes the major tectonic plates. Various lines of evidence that support plate tectonics are mentioned, such as the fit of continental shelves, matching rock units and mountain ranges, and similar fossil distributions. The importance of understanding plate tectonics to explain landforms and predict natural hazards is also noted. Finally, the different types of plate boundaries are outlined, including where earthquakes and volcanoes are most common.
Natural Hazards: Earthquake and Volcanic Hazards + Mitigation and Adaptation
Created by: Karl Ruelan; Philippines (c) David G.
Educational Purposes Only
For Science - 11 Presentation; 8/30/16
About Natural Hazards
Specifically: Earthquake and Volcanic Hazards
It also includes: Mitigation and Adaptation to this hazards.
Powerpoint
What is Earthquake?
The minimal to rapid shaking of the ground due to the movement of rocks along fractures known as faults.
Earthquake Hazards
Surface Rupture & Physical Damage
Liquefaction
Fires
Tsunami
Landslide
Volcanic Hazards
Pyroclastic Flows and Materials
People unable to run
Bury people and agriculture
Mudflow or LAHAR
Poisonous gases
Tsunami
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Explosive Eruption
Non-Explosive Eruption
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One of the government’s response to mitigate and adapt to the hazards.
Developed to indicate the places where most of the natural disasters usually occur and will most likely occur.
by the shaking itself or by the ground beneath them settling to a different level than it was before the earthquake (subsidence) or (uplift).
Subsidence is the motion of a surface (usually, the Earth's surface) as it shifts downward relative to a datum such as sea-level.
A fault is a fracture or zone of fractures between two blocks of rock. Faults allow the blocks to move relative to each other.
Philippines experience a lot of Earthquakes because it is located in the Circum-Pacific Belt, situated in the Pacific Ring of Fire
Pacific Ring of Fire is term used for VOLCANOES only.
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Plate movement ppt
This document provides an overview of plate tectonics and the evidence that supports the theory. It discusses how early scientists like Alfred Wegener proposed that continents move over time (continental drift). Wegener noticed matching land features and fossil evidence between continents. Later, Harry Hess confirmed Wegener's ideas by discovering that new crust forms at mid-ocean ridges, providing evidence of sea-floor spreading as plates move apart. Convection currents in the mantle caused by heat from the Earth's core are now understood to drive the movement of tectonic plates.
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Earth as a System
The document discusses several key concepts about Earth's systems:
1. Earth is made up of several interacting systems - the geosphere, hydrosphere, atmosphere and biosphere - that exchange matter and energy.
2. The geosphere includes the solid layers that make up Earth's interior and crust.
3. The hydrosphere contains all of Earth's water and cycles through the other systems.
4. Matter and energy continuously move between these systems, transforming from one form to another.
Divergent plate boundary PPT
Divergent plate boundaries occur when two tectonic plates move away from each other. As the plates separate, new crust is formed in between through volcanic activity and magma solidifying. This results in the creation of geological features such as mid-ocean ridges under the ocean or rift valleys on land. Over millions of years, continued separation at divergent boundaries can lead to the formation of new oceans as the crust spreads out.
Midoceanic ridges
Mid-ocean ridges are underwater mountain systems formed at divergent tectonic plate boundaries where new oceanic crust is generated. They consist of a chain of mountains linked by a central rift valley and result from mantle upwelling and melting in response to plate spreading. As the buoyant magma rises to the seafloor at the plate boundary, it emerges as lava to form new ocean crust upon cooling.
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Transform boundary
A transform boundary is a plate boundary where plates move horizontally past each other in opposite directions. Convection currents in the mantle cause plate movement. Transform boundaries collect energy from plate movement that is eventually released through earthquakes and tsunamis, as seen at the San Andreas Fault and from a Pacific Ocean earthquake that caused a major tsunami. While they do not form volcanoes or mountains, transform boundaries can create dangerous earthquakes and tsunamis.
Plate boundaries ppt
Earth's outer shell is divided into tectonic plates that slowly move over the mantle below. Plates interact at boundaries where they either converge and collide, causing volcanoes and earthquakes, diverge and form rift valleys and ocean ridges, or slide past each other along transform boundaries, also producing earthquakes. The movement of these plates over geological time scales shapes the earth's surface features and geography.
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This document provides information about volcanoes and volcanic hazards from the Philippine Institute of Volcanology and Seismology (PHIVOLCS). It defines what volcanoes are, explains why volcanism occurs, and classifies volcanoes in the Philippines as active, inactive, or potentially active. The document also describes different types of volcanoes based on composition and eruption style, including shield volcanoes, stratovolcanoes, and calderas. Finally, it covers different styles of volcanic eruptions from effusive to explosive.
Fault
A fault is a break or fracture between two blocks of rocks in response to stress.
One block has moved relative to the other block.
The surface along which the blocks move is called a fault plane.
Faulting produced the earthquakes.
Thus earthquakes may occur because:
a) Rocks are initially broken to produce a fault.
b) Movement or re-activation of an already existing fault.
Types of Volcanoes
Volcanoes form in different types depending on the composition of the magma and tectonic setting, with shield volcanoes being non-explosive and forming from basalt in oceanic settings, composite volcanoes sometimes having explosive eruptions from more viscous magma in continental settings, and cinder cones being the smallest from pyroclastic eruptions.
Plate tectonics
Plate tectonics is the theory that Earth's outer shell is divided into several plates that glide over the mantle, the rocky inner layer above the core. The plates act like a hard and rigid shell compared to Earth's mantle. This strong outer layer is called the lithosphere.
PLATE TECTONICS
The document discusses plate tectonics and describes how the Earth's lithosphere is broken into plates that move over time. It explains that plate tectonics built upon Alfred Wegener's theory of continental drift, which proposed that the continents were once joined together in a supercontinent called Pangaea. There are nine major tectonic plates and three types of plate boundaries - divergent boundaries which create mid-ocean ridges and rift valleys, convergent boundaries which cause subduction and mountain building, and transform boundaries where plates slide past each other like the San Andreas Fault. Convection currents in the Earth's mantle provide the driving force for plate movements.
Intro to volcanoes module
Provided to the METSAT Element of the Weather Intelligence flight, to help the analysts get a better understanding of volcanoes.
Types of volcanoes_geology
There are 3 main types of volcanoes: composite volcanoes, cinder cones, and shield volcanoes. There are also 5 special case volcanoes: caldera volcanoes, mega-volcanoes, spatter cones, dome volcanoes, and lava plateaus. The document discusses the characteristics of each type of volcano.
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This document provides an introduction to the theory of plate tectonics. It discusses the internal structure of the Earth and how the crust is made up of different types of plates. It then explains Alfred Wegener's theory of continental drift from 1915 and describes the major tectonic plates. Various lines of evidence that support plate tectonics are mentioned, such as the fit of continental shelves, matching rock units and mountain ranges, and similar fossil distributions. The importance of understanding plate tectonics to explain landforms and predict natural hazards is also noted. Finally, the different types of plate boundaries are outlined, including where earthquakes and volcanoes are most common.
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Created by: Karl Ruelan; Philippines (c) David G.
Educational Purposes Only
For Science - 11 Presentation; 8/30/16
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Specifically: Earthquake and Volcanic Hazards
It also includes: Mitigation and Adaptation to this hazards.
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What is Earthquake?
The minimal to rapid shaking of the ground due to the movement of rocks along fractures known as faults.
Earthquake Hazards
Surface Rupture & Physical Damage
Liquefaction
Fires
Tsunami
Landslide
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Pyroclastic Flows and Materials
People unable to run
Bury people and agriculture
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Poisonous gases
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One of the government’s response to mitigate and adapt to the hazards.
Developed to indicate the places where most of the natural disasters usually occur and will most likely occur.
by the shaking itself or by the ground beneath them settling to a different level than it was before the earthquake (subsidence) or (uplift).
Subsidence is the motion of a surface (usually, the Earth's surface) as it shifts downward relative to a datum such as sea-level.
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Philippines experience a lot of Earthquakes because it is located in the Circum-Pacific Belt, situated in the Pacific Ring of Fire
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This document discusses plate tectonics and related landforms, earthquakes, and volcanoes. It begins by describing the four main types of plate boundaries and associated landforms such as mid-oceanic ridges, trenches, and island arcs. It then covers causes of earthquakes including sudden stress release along faults, and factors that influence earthquake damage such as magnitude, building design, and population density. Prediction methods like elastic rebound theory and seismic gaps are also mentioned. Finally, it discusses volcanoes, noting where they form at plate boundaries and hotspots, how scientists monitor and predict eruptions, associated hazards from lava to tsunamis, and ways to reduce risks like controlling lava flows and using hazard maps.
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This document provides an overview of plate tectonics and the evidence that supports the theory. It discusses how early scientists like Alfred Wegener proposed that continents move over time (continental drift). Wegener noticed matching land features and fossil evidence between continents. Later, Harry Hess confirmed Wegener's ideas by discovering that new crust forms at mid-ocean ridges, providing evidence of sea-floor spreading as plates move apart. Convection currents in the mantle caused by heat from the Earth's core are now understood to drive the movement of tectonic plates.
Geological hazard and hazard map
This document provides information on various geological hazards including earthquakes, volcanoes, landslides, and tsunamis. It defines an earthquake as the shaking of the earth's surface from a sudden release of energy in the lithosphere. It describes the focus and epicenter of an earthquake and different types of volcanic eruptions and associated hazards. It also outlines different types of landslides and tsunamis, explaining they are large waves caused by displacement of water.
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The document discusses several key concepts about Earth's systems:
1. Earth is made up of several interacting systems - the geosphere, hydrosphere, atmosphere and biosphere - that exchange matter and energy.
2. The geosphere includes the solid layers that make up Earth's interior and crust.
3. The hydrosphere contains all of Earth's water and cycles through the other systems.
4. Matter and energy continuously move between these systems, transforming from one form to another.
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Divergent plate boundaries occur when two tectonic plates move away from each other. As the plates separate, new crust is formed in between through volcanic activity and magma solidifying. This results in the creation of geological features such as mid-ocean ridges under the ocean or rift valleys on land. Over millions of years, continued separation at divergent boundaries can lead to the formation of new oceans as the crust spreads out.
Midoceanic ridges
Mid-ocean ridges are underwater mountain systems formed at divergent tectonic plate boundaries where new oceanic crust is generated. They consist of a chain of mountains linked by a central rift valley and result from mantle upwelling and melting in response to plate spreading. As the buoyant magma rises to the seafloor at the plate boundary, it emerges as lava to form new ocean crust upon cooling.
Understanding Typhoons
According to PAGASA, about 20 tropical cyclones called typhoons enter the Philippine Area of Responsibility (PAR) each year, with PAR located within 115°E-135°E longitude and 5°N-25°N latitude. A typhoon is a tropical cyclone characterized by counterclockwise rotating winds around a low pressure eye, with typhoons having maximum wind speeds over 64 kph and categorized from tropical depression to super typhoon. The key differences between typhoons and hurricanes are the geographical regions where they occur, with typhoons specific to the northwest Pacific and hurricanes occurring in the northeast Pacific and northern Atlantic.
Transform boundary
A transform boundary is a plate boundary where plates move horizontally past each other in opposite directions. Convection currents in the mantle cause plate movement. Transform boundaries collect energy from plate movement that is eventually released through earthquakes and tsunamis, as seen at the San Andreas Fault and from a Pacific Ocean earthquake that caused a major tsunami. While they do not form volcanoes or mountains, transform boundaries can create dangerous earthquakes and tsunamis.
Plate boundaries ppt
Earth's outer shell is divided into tectonic plates that slowly move over the mantle below. Plates interact at boundaries where they either converge and collide, causing volcanoes and earthquakes, diverge and form rift valleys and ocean ridges, or slide past each other along transform boundaries, also producing earthquakes. The movement of these plates over geological time scales shapes the earth's surface features and geography.
Major mountain ranges of the world
Geologically and geographically it is very important, in this this slide you will learn how major mountain ranges of the world were formed.
Types and characteristics of magma
This document summarizes the key characteristics and types of magma. It defines magma as a mixture of molten or semi-molten rock found beneath the Earth's surface. Magma forms through mechanisms like decompression melting when hot mantle material rises and melts lower pressure rock, or flux melting when water or carbon dioxide lowers the melting temperature of mantle rock. Magma can be classified based on its chemical composition into basaltic, andesitic, or rhyolitic types depending on silicon and iron/magnesium content, and each type has distinct physical properties like temperature, viscosity, and gas content that determine explosiveness. Magma is also differentiated based on how it formed, such as primitive, primary, parental
2.3 volcanoes & volcanic hazards
This document provides information about volcanoes and volcanic hazards from the Philippine Institute of Volcanology and Seismology (PHIVOLCS). It defines what volcanoes are, explains why volcanism occurs, and classifies volcanoes in the Philippines as active, inactive, or potentially active. The document also describes different types of volcanoes based on composition and eruption style, including shield volcanoes, stratovolcanoes, and calderas. Finally, it covers different styles of volcanic eruptions from effusive to explosive.
Fault
A fault is a break or fracture between two blocks of rocks in response to stress.
One block has moved relative to the other block.
The surface along which the blocks move is called a fault plane.
Faulting produced the earthquakes.
Thus earthquakes may occur because:
a) Rocks are initially broken to produce a fault.
b) Movement or re-activation of an already existing fault.
Types of Volcanoes
Volcanoes form in different types depending on the composition of the magma and tectonic setting, with shield volcanoes being non-explosive and forming from basalt in oceanic settings, composite volcanoes sometimes having explosive eruptions from more viscous magma in continental settings, and cinder cones being the smallest from pyroclastic eruptions.
Plate tectonics
Plate tectonics is the theory that Earth's outer shell is divided into several plates that glide over the mantle, the rocky inner layer above the core. The plates act like a hard and rigid shell compared to Earth's mantle. This strong outer layer is called the lithosphere.
PLATE TECTONICS
The document discusses plate tectonics and describes how the Earth's lithosphere is broken into plates that move over time. It explains that plate tectonics built upon Alfred Wegener's theory of continental drift, which proposed that the continents were once joined together in a supercontinent called Pangaea. There are nine major tectonic plates and three types of plate boundaries - divergent boundaries which create mid-ocean ridges and rift valleys, convergent boundaries which cause subduction and mountain building, and transform boundaries where plates slide past each other like the San Andreas Fault. Convection currents in the Earth's mantle provide the driving force for plate movements.
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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 - Types & Volcanic Hazards
Everything about volcanoes, their types and different volcanic hazards. Complete with high definition images. Enjoy!
Volcanoes intro
Volcanoes come in different types and erupt in various ways. They form where tectonic plates meet in the Earth's crust. The main types are shield volcanoes which erupt fluid lava flows, composite volcanoes which alternate between explosive eruptions and lava flows, and cinder cone volcanoes which erupt ash and cinders. Volcanoes can be active, dormant, or extinct depending on how recently they have erupted.
Volcanoes
Volcanoes form when magma rises from below the Earth's surface and erupts through openings called vents. As magma accumulates at the vent it builds up a mountain-like structure called a volcano. There are three main types of volcanoes defined by their shape and eruption characteristics: shield volcanoes which have broad bases and gentle slopes formed by fluid basaltic lava flows; cinder cone volcanoes which are steep-sided with a small base formed from explosive eruptions of thick sticky lava; and composite or stratovolcanoes which are large mountains formed by alternating explosive and effusive eruptions that build tall layers of ash and lava.
Volcanoes powerpoint
Volcanoes form as a result of tectonic plate movement and pressure changes below the earth's surface. When magma breaks through the crust, a volcanic eruption occurs, expelling lava, steam, ash and other materials. Mount Vesuvius is a famous volcano near Naples, Italy that formed over 25,000 years ago. Its last eruption in 1944 caused widespread damage, destroying villages and aircraft at a nearby airfield. Volcanic eruptions are powerful natural events that can have significant effects on the surrounding area.
Grade 9 Module 1, Lesson 1.1: Volcanoes (Teacher's Guide for Discussion)
A PowerPoint Presentation for Grade 9 teachers. This presentation is ONLY suggested guide for teachers to assist them on the discussion after the activities as suggested in the Learner's Module were performed. Please feel free to add comments and suggestions. Thanks!
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Grade 9 Module 1, Lesson 1.1: Volcanoes (Teacher's Guide for Discussion)
Grade 9 Module 1, Lesson 1.1: Volcanoes (Teacher's Guide for Discussion)
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Volcanoes
Volcanoes form at plate boundaries where tectonic plates are diverging or converging. There are three main types of volcanoes based on location: shield volcanoes at divergent boundaries, stratovolcanoes at subduction zones, and hotspots formed by mantle plumes. Volcanoes pose hazards from lava flows, explosions, and ashfall. Classification systems describe volcanoes based on activity levels from dormant to active. Monitoring systems use alert levels and colors to communicate volcanic unrest and eruptions.
8. Engineering Geology - Volcanoes and Earthquake.pptx
8. Engineering Geology - Volcanoes and Earthquake.pptxUniversity of Northern Philippines, Vigan City
The document provides information about volcanoes and earthquakes. It defines key terms like volcano, magma, lava, caldera, and describes different types of volcanoes like shield volcanoes, composite volcanoes, and cinder cone volcanoes. It also discusses what causes volcanic activity and describes different types of volcanic eruptions. The document then covers earthquakes, defining terms like focus and epicenter, and describing how seismic waves and intensity scales are used to measure earthquakes.Presentation on volcanos
This presentation provides an overview of volcanoes, including their formation from plate tectonics or hotspots, the different types of volcanic features and erupted materials, classifications of volcanic activity, and notable examples. Volcanic activity can have effects on global climate through emissions into the stratosphere and impacts soil through added nutrients.
module1Lesson2.pptx
Volcanoes are classified based on their shape, structure, and activity. There are three main types of volcanoes: cinder cone volcanoes, which are simple conical structures built from ejected cinders; shield volcanoes, which have wide bases created from fluid lava flows; and composite or stratovolcanoes, which are large symmetrical cones made of layers of lava and ash. Volcanoes can also be classified based on their activity as active, dormant, or extinct depending on whether they are currently erupting, may erupt in the future, or are not expected to erupt again.
Characteristics of different volcanoes and their types
Volcanoes can be classified in several ways:
1) By frequency of eruption - active, dormant, or extinct
2) By shape and mode of eruption - shield, composite, caldera, cinder cone, lava domes
3) By lava composition - those with basic or acidic lava
Other types include supervolcanoes, flood basalt provinces, and submarine volcanoes. Volcanoes form due to pressure from magma escaping through cracks in the earth's crust.
GRADE 9 EARTH AND SPACE - VOLCANOES
This document provides information about different types of volcanoes. It describes volcanoes as vents where hot gases, rocks, and lava are ejected from the Earth's surface. Volcanoes form at plate boundaries, and can also form when plates separate under the ocean. The document then classifies volcanoes according to their shape (cinder cone, shield, composite) and activity level (active, dormant, extinct). Specific examples are given for each type of volcano classification.
Volcanoes
Volcanoes form when magma rises up from below the Earth's surface and erupts through openings called vents. There are several types of volcanoes defined by their shape and eruption characteristics. Shield volcanoes have gentle slopes and erupt runny basalt lava, while composite volcanoes are steep-sided and erupt thicker, stickier magma in more explosive eruptions. Cinder cones erupt small fragments and form small, cone-shaped volcanoes. Lava domes form when thick lava piles up in mounds. Volcanoes are caused by the movement of tectonic plates, which can allow magma to rise up in between the plates. Geysers, which are hot springs
Volcanoes PART 1
This document discusses different types of volcanoes. It provides descriptions of cinder cones, shield volcanoes, composite volcanoes, and lava domes. Cinder cones are symmetrical cones up to 1,200 feet tall formed from a single vent. Shield volcanoes are very broad with shallow slopes and can be over 30,000 feet tall. Composite volcanoes are also known as stratovolcanoes, ranging from 1-10 km wide and up to 10,000 feet tall with steep slopes. They have explosive, dangerous eruptions. Lava domes are much smaller formations that occur when lava is too viscous to flow, piling up in a dome shape around 100 feet tall. Examples of each type
VOLCANO_WEEK 1and2.pptx
1. Volcanoes are natural openings in the Earth's crust where molten rock and gases erupt.
2. The Philippines has many active volcanoes due to its location along the Pacific Ring of Fire. Some of the most notable active volcanoes include Taal Volcano, Mount Mayon, and Bulusan.
3. Volcanoes are classified based on their eruption history as either active or inactive, and by their shape as shield, cinder cone, or composite volcanoes.
Lesson 2 volcanoes
Volcanoes form at constructive and destructive plate boundaries. At constructive boundaries, volcanoes form as magma rises through gaps created as plates move apart. These volcanoes are usually shield volcanoes. At destructive boundaries, one plate is subducted and melts, creating excess magma that erupts violently as composite volcanoes. Volcanoes can be active and currently erupting, dormant but capable of future eruptions, or extinct and not likely to erupt again. Hot spot volcanoes form from stationary plumes of magma rising through weak crust, creating island chains as plates move over hot spots.
volcanoes-141105193527-conversion-gate02.pdf
Volcanoes form when magma rises from below the Earth's surface. There are two main types of volcanoes: shield volcanoes and stratovolcanoes. Shield volcanoes are wide and gently sloping due to fluid lava flows, while stratovolcanoes are steep and tall with layers of hardened lava and ash. The viscosity of magma depends on its temperature, composition, and gas content, and determines the type of eruption from a volcano. Active volcanoes are currently erupting or have erupted in the last 10,000 years, while dormant and extinct volcanoes have not erupted recently or in over 10,000 years respectively.
Science 9 Quarter 3; Types of volcano cone shapes.pptx
Volcanoes come in different types based on their shape and formation process. The main types are composite volcanoes, shield volcanoes, cinder cone volcanoes, dome volcanoes, caldera volcanoes, and fissure volcanoes. Composite volcanoes are tall with wide bases and layers of solidified material. Shield volcanoes have low, broad dome shapes due to slow moving lava. Cinder cones are small and steep with loose debris. Dome volcanoes form rounded mounds from thick, slow moving lava. Calderas are large depressions formed when the volcano collapses after an eruption. Fissure volcanoes erupt from cracks without a central vent.
classes of volcanoes
There are several main types of volcanoes classified based on their shape, eruptive behavior, and composition. Composite volcanoes, also known as stratovolcanoes, are conical mountains built up by viscous lava flows and explosive eruptions, examples being Mount St. Helens and Mount Pinatubo. Shield volcanoes are larger and less steeply sloped, constructed by fluid basaltic lava flows like those of Hawaii. Small cinder cones form from explosive eruptions of pyroclastic material. Fissure eruptions produce fluid lava flows from cracks in the crust along zones of weakness.
GEOGRAPHY YEAR 10: VOLCANIC ACTIVITY
1) Volcanoes form at boundaries where tectonic plates meet, such as where plates are subducting or spreading apart.
2) There are two main types of volcanoes - cone-shaped volcanoes which form from thick, slow-moving lava and shield volcanoes which have flatter slopes due to more fluid lava.
3) Examples of highly active volcanic regions include the Pacific Ring of Fire and areas around Alaska, Hawaii, and the Cascade Range in the western United States.
Volcanism & Deposit Activity
This document provides an overview of volcanism and volcanic processes. It discusses the types of volcanoes such as shield volcanoes, composite volcanoes, cinder cones and lava domes. It also describes volcanic deposits including lava, tephra and lava tubes. Additionally, it covers the distribution of volcanoes along plate boundaries and volcanic belts. The document outlines methods for predicting volcanic eruptions in both the long-term by examining geological records, and short-term by monitoring changes in gas emissions, earthquakes and ground deformation near active volcanoes. Finally, it discusses volcanic hazards such as lava flows, pyroclastic flows, lahars and toxic gases.
Types and classification of Volcanoes.pptx
The Philippines is located along the Ring of Fire. As a result, it is a home to many volcanoes. According to PHIVOLCS, our country is an ideal site for any volcanic activity. It is therefore important for us to know how this natural phenomenon happens to reduce the risks and effects it may cause.
Presentation of Group 2 - Topic Volcanoes
A volcano is a rupture in a planet's crust that allows magma, ash, and gases to escape from underground. They form at tectonic plate boundaries and underwater, with about 1,500 potentially active worldwide. Volcanoes are classified as active, dormant, or extinct based on recent eruptions. The three main types are cinder cones made of pyroclastic debris, shield volcanoes built from fluid lava, and composite or stratovolcanoes with steep sides formed from viscous lava. The 1815 eruption of Mount Tambora in Indonesia was the largest in recorded history, killing over 10,000 and contributing to global climate changes and crop failures for years after.
Volcanoes and other igneous activity
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Classification of volcanoes
This document classifies and describes the different types of volcanoes. It discusses 7 main types: fissure volcanoes which erupt from cracks without a central crater; composite volcanoes which are tall and symmetrical with layers of lava and ash like Mount Fuji; shield volcanoes which are broad with low slopes like those in Hawaii; cinder cones which are steep-sided hills formed from pyroclastic debris; lava domes which form bulbous masses that pile around vents; supervolcanoes which are extremely large and dangerous, capable of global cooling like Yellowstone Caldera; and submarine volcanoes which are common on ocean floors, often forming pillow lava and hydrothermal vents.
Volcano and related concepts
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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8. Engineering Geology - Volcanoes and Earthquake.pptx
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Trabajo naturales dominat and recessive genes.
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Types of volcanoes:fatoumata camara 4ºa
- 2. Volcano: It is an opening or rupture in a planet surface which allows magma and volcanis ashes an gases trhought the chamber or crater . DEFINITION:
- 4. There are many types of volcanoe, and to undertand it better we can clasify them in two subtypes: 1- Types of volcanoes related to the activity.(their frecuency of eruption) 2-Types of volcanoes related to the structure: There are a lot of subtypes but I'm going to talk about Shield Vocanoes and Composite ones. TYPES:
- 5. ACTIVE VOLCANO: there are those volcanoes that erupts regullary, very often. DORMANT VOLCANOES: there are those volcanoes that have erupted during the years but now are quiet. EXTINCT VOLCANOES: there are those volcanoes which scientist consider that it is very unusual to see them erupting again becuase of they don't have more lava supplies. RELATED TO THE ACTIVITY :
- 6. Kīlauea is an active volcano in the Hawaiian Islands
- 7. Hohentwiel is an extinct volcanoe in Baden Wurttemberg in the south of Germany.
- 8. The Vesuvius is an extinct volcanoe that is in Galf of Naples, Italy.
- 9. Composite volcano that are also known as Stratovolcano are tall and conical volcanoes built up with many layers of hardened lava.THey are characterized by a steep slope structure and periodic explosive eruptions. RELATED TO THE STRUCTURE:
- 10. Shield volcanoes are types of volcanoes usually built almost enternely of fluid lava flows. And they are broad slope and they have a large size and low profile forming like a warrior's shield. RELATED TO THE STRUCTURE(II):
- 11. COMPOSITE SHIELD Estructure Steep slope Broad, gentle slope Tectonic Plates Environment Convergent boundaries (subduction zones) Divergent plate boundaries and hot spots. Types of Rock Andesite Basalt Lava temperature 800ºC 1100ºC Lava viscousity 1-Hight (like smach potato): that is because of the temperature and the materials. 2- They have acid materials 1-Low(like the honey) 2- thay have basics materials. Eruptive Style Explosive Quiescent DIFFERENCES BETWEEN:
- 12. EXAMPLES:
- 13. Mauna-Loa (Hawai) Shield volcano.
- 14. Mount St Helens(Washington, USA): Composite volcano