2. causes of volcanoes keh
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This document discusses plate tectonics and continental drift. It explains that Alfred Wegener first proposed that continents were once joined together in a supercontinent called Pangaea before drifting apart. This theory of continental drift involves the slow movement of tectonic plates over time. The document provides evidence for continental drift, including matching fossil records, continental shapes, and rock patterns found on separated continents. It also notes that the study of tectonic plates is called plate tectonics.
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Volcanoes
Volcanoes form when molten magma forces its way through cracks in the Earth's crust. They can take cone shapes but also other forms. The melted rock that emerges from the volcano's crater is called lava, which destroys everything in its path due to its extreme heat. Most volcanoes occur on land, but some exist on the ocean floor and can emerge from the water if tall enough. Volcanoes erupt when magma and gases find a way to escape through vents to the surface. Eruptions can be gentle or violent.
13398107 volcanoes-a-presentation
Volcanoes form when magma rises up from the Earth's mantle and crust and erupts. There are three main types of volcanoes defined by their activity level - active volcanoes that are currently erupting or may erupt soon, dormant volcanoes that have not erupted in a long time, and extinct volcanoes that have not erupted for over 10,000 years. Volcanic eruptions expel gases, ash, lava, and other materials from the vent of the volcano. The movement of tectonic plates is responsible for volcanism in many parts of the world.
Volcanoes and volcanic erruptions
The document provides information about different types of volcanoes and volcanic features including:
- Shield volcanoes which are built by basalt lava flows and have gentle slopes.
- Lava domes which are built by thick, viscous lava that cools too quickly to flow very far from the eruption.
- Cinder cones which are steep sided hills made of volcanic fragments blown from eruptions of stratovolcanoes.
- Stratovolcanoes which have steep sides and are formed by violent eruptions of lava flows, tephra, and pyroclastic flows from multiple vents.
- Mud volcanoes which form from eruptions of wet
Geology of Maui
A lesson on the geology of Maui, HI designed for high school Earth Science students, based on a Duke-UNC Geology field trip.
All about volcanoes
This document defines key terms related to volcanoes such as ash cloud, conduit, crust, lava, and magma chamber. It then describes volcanoes as vents that connect molten rock from within the Earth's crust to the surface. There are three main types of volcanoes: shield volcanoes which erupt fluid lava flows, cinder cone volcanoes which have a simple bowl shape, and composite volcanoes which develop from repeated eruptions and are the largest. The document provides examples of each type and diagrams depicting how volcanoes erupt through the conduit from the magma chamber.
Volcanoes Information Report
This document provides information about volcanoes. It defines volcanoes as openings in the Earth's surface that allow magma, ash, and gases to escape during eruptions. It notes they are usually located at tectonic plate boundaries, especially around the Pacific Ring of Fire. The document describes how magma rises through the volcano's vent and turns to lava before erupting. It lists some facts about volcanoes and provides a diagram of a volcano's structure. It also discusses impacts of volcanoes on people and the environment, both positive and negative, as well as strategies for preparing for a volcanic eruption.
Natural disasterPPT-Volcanoes made by Agastya Dhanorkar
This PPT consists slides and matter on Volcanoes please coment below if you liked this. This is my first upload. thank you...... ALSO my youtube channel is Agastya Dhanorkar
Volcanoes
This document provides information about volcanoes. It defines a volcano as a vent or chimney that connects molten rock from within the Earth's crust to the surface. Volcanoes form cone shapes and erupt when magma and gases find a way to escape through the vent. The document describes the different types of volcanoes as active, dormant, or extinct based on recent eruption patterns. It also provides examples of volcanoes that fit each type and defines key terms related to volcanic features and eruptions.
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Volcanoes
Volcanoes form when molten magma forces its way through cracks in the Earth's crust. They can take cone shapes but also other forms. The melted rock that emerges from the volcano's crater is called lava, which destroys everything in its path due to its extreme heat. Most volcanoes occur on land, but some exist on the ocean floor and can emerge from the water if tall enough. Volcanoes erupt when magma and gases find a way to escape through vents to the surface. Eruptions can be gentle or violent.
13398107 volcanoes-a-presentation
Volcanoes form when magma rises up from the Earth's mantle and crust and erupts. There are three main types of volcanoes defined by their activity level - active volcanoes that are currently erupting or may erupt soon, dormant volcanoes that have not erupted in a long time, and extinct volcanoes that have not erupted for over 10,000 years. Volcanic eruptions expel gases, ash, lava, and other materials from the vent of the volcano. The movement of tectonic plates is responsible for volcanism in many parts of the world.
Volcanoes and volcanic erruptions
The document provides information about different types of volcanoes and volcanic features including:
- Shield volcanoes which are built by basalt lava flows and have gentle slopes.
- Lava domes which are built by thick, viscous lava that cools too quickly to flow very far from the eruption.
- Cinder cones which are steep sided hills made of volcanic fragments blown from eruptions of stratovolcanoes.
- Stratovolcanoes which have steep sides and are formed by violent eruptions of lava flows, tephra, and pyroclastic flows from multiple vents.
- Mud volcanoes which form from eruptions of wet
Geology of Maui
A lesson on the geology of Maui, HI designed for high school Earth Science students, based on a Duke-UNC Geology field trip.
All about volcanoes
This document defines key terms related to volcanoes such as ash cloud, conduit, crust, lava, and magma chamber. It then describes volcanoes as vents that connect molten rock from within the Earth's crust to the surface. There are three main types of volcanoes: shield volcanoes which erupt fluid lava flows, cinder cone volcanoes which have a simple bowl shape, and composite volcanoes which develop from repeated eruptions and are the largest. The document provides examples of each type and diagrams depicting how volcanoes erupt through the conduit from the magma chamber.
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This document provides information about volcanoes. It defines volcanoes as openings in the Earth's surface that allow magma, ash, and gases to escape during eruptions. It notes they are usually located at tectonic plate boundaries, especially around the Pacific Ring of Fire. The document describes how magma rises through the volcano's vent and turns to lava before erupting. It lists some facts about volcanoes and provides a diagram of a volcano's structure. It also discusses impacts of volcanoes on people and the environment, both positive and negative, as well as strategies for preparing for a volcanic eruption.
Natural disasterPPT-Volcanoes made by Agastya Dhanorkar
This PPT consists slides and matter on Volcanoes please coment below if you liked this. This is my first upload. thank you...... ALSO my youtube channel is Agastya Dhanorkar
Volcanoes
This document provides information about volcanoes. It defines a volcano as a vent or chimney that connects molten rock from within the Earth's crust to the surface. Volcanoes form cone shapes and erupt when magma and gases find a way to escape through the vent. The document describes the different types of volcanoes as active, dormant, or extinct based on recent eruption patterns. It also provides examples of volcanoes that fit each type and defines key terms related to volcanic features and eruptions.
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.
Information on volcano for school
Volcanoes are openings in the Earth's crust that allow magma, ash, and gases to escape from below the surface. There are three types of volcanoes: active, dormant, and extinct. Magma is molten rock underground, while lava is magma that flows out of a volcano. Ash, cinders, and pumice are other materials emitted from volcanoes. Over half of the world's volcanoes are located on the Ring of Fire around the Pacific Ocean. Volcanic eruptions are caused by the movement of tectonic plates, which squeezes magma up in between. Eruptions can endanger people through lava, tsunamis, earthquakes, and toxic gases
Types of volcanic eruption ppt
There are several different types of volcanic eruptions that are classified based on their eruption dynamics and behavior. The main types include magmatic eruptions driven by gas decompression, phreatomagmatic eruptions driven by gas compression, and phreatic eruptions caused by steam superheating. Specific eruption styles like Hawaiian, Strombolian, Vulcanian, Pelean, Plinian, Surtseyan, submarine, subglacial and phreatic eruptions each have unique characteristics in terms of the materials erupted and speeds of eruption columns or pyroclastic flows. The crystal, gas and temperature properties of magma influence whether an eruption will be explosive or effusive
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This document defines volcanoes as openings in the Earth's crust that allow molten rock and gases to escape. It notes that over half of the world's active volcanoes above sea level are located along the Ring of Fire. Volcanoes form when tectonic plates collide, spread apart, or interact under a plate. The parts of a volcano include the crater, pipe, cone, and vent. There are three main types of volcanoes: composite/strato volcanoes, shield volcanoes, and cinder cone volcanoes. Volcanic eruptions can have both beneficial effects like adding nutrients to soil or creating new islands, and harmful effects like releasing aerosols or abandoning land.
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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.
Mount pelee science project
Mount Pelée is a volcano located on the island of Martinique. In 1902, it erupted with little warning, destroying the city of St. Pierre and killing nearly all 30,000 inhabitants within minutes. The eruption produced two pyroclastic flows - one that shot vertically into the sky and another that raced laterally down the mountain at 100 mph, engulfing St. Pierre in hot ash and gases. Only two people survived the eruption. Mount Pelée formed as a result of the subduction of the Cocos tectonic plate under the Caribbean plate. While there was no lava flow, the eruption deposited large amounts of ash that could have later lithified into sedimentary rock.
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Volcanoes are openings in the Earth's crust where magma and gases erupt. During an eruption, volcanoes expel lava, ash, dust, gas and vapor. There are three types of volcanoes: active volcanoes that are currently erupting or may erupt soon, dormant volcanoes that have not erupted for a long time, and extinct volcanoes that have not erupted for over 10,000 years. Volcanic eruptions produce rocks and lava that make soil fertile for farming and also provide geothermal energy for human use, but they can also endanger lives through hazards like lava and ash flows, bombs and clouds during an eruption.
Volcanoes sample
A volcano is a mountain formed when magma reaches the Earth's surface through weak spots, erupting gases, ashes, and rocks. Volcanic eruptions can destroy nearby homes and populations, as seen at Pompeii. However, volcanoes also provide benefits as the hot rocks expelled are rich in minerals that improve soil quality for growing plants. The document questions whether scientists can predict volcanic eruptions.
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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
This presentation contains the basic details on the Volcano. It also includes how to make a Volcano and the experiment how to erupt the volcano.
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.
Volcanoes, Volcano PowerPoint Quiz Game, Earth Science Lesson PowerPoint
The document appears to be a review game about volcanoes for students. It contains 20 multiple choice questions about volcanoes, their characteristics, famous examples, and effects. It also includes 5 bonus questions about volcano movies. The review game instructs students to use class notes and materials to answer the questions in small groups without sharing answers between groups.
Volcano Features, Earth Science Lesson PowerPoint, Buld a Volcano
This PowerPoint is one small part of the Geology Topics unit from www.sciencepowerpoint.com. This unit consists of a five part 6000+ slide PowerPoint roadmap, 14 page bundled homework package, modified homework, detailed answer keys, 12 pages of unit notes for students who may require assistance, follow along worksheets, and many review games. The homework and lesson notes chronologically follow the PowerPoint slideshow. The answer keys and unit notes are great for support professionals. The activities and discussion questions in the slideshow are meaningful. The PowerPoint includes built-in instructions, visuals, and review questions. Also included are critical class notes (color coded red), project ideas, video links, and review games. This unit also includes four PowerPoint review games (110+ slides each with Answers), 38+ video links, lab handouts, activity sheets, rubrics, materials list, templates, guides, 6 PowerPoint review Game, and much more. Also included is a 190 slide first day of school PowerPoint presentation.
Areas of Focus within The Geology Topics Unit: -Plate Tectonics, Evidence for Plate Tectonics, Pangea, Energy Waves, Layers of the Earth, Heat Transfer, Types of Crust, Plate Boundaries, Hot Spots, Volcanoes, Positives and Negatives of Volcanoes, Types of Volcanoes, Parts of a Volcano, Magma, Types of Lava, Viscosity, Earthquakes, Faults, Folds, Seismograph, Richter Scale, Seismograph, Tsunami's, Rocks, Minerals, Crystals, Uses of Minerals, Types of Crystals, Physical Properties of Minerals, Rock Cycle, Common Igneous Rocks, Common Sedimentary Rocks, Common Metamorphic Rocks.
This unit aligns with the Next Generation Science Standards and with Common Core Standards for ELA and Literacy for Science and Technical Subjects. See preview for more information
If you have any questions please feel free to contact me. Thanks again and best wishes. Sincerely, Ryan Murphy M.Ed www.sciencepowerpoint@gmail.com
Volcanoes
Volcanoes form when magma travels through the earth's mantle and crust, reaching the surface as lava and building up in a mountain-like shape. They are composed of cooled lava and ash. Most volcanoes are located near tectonic plate boundaries under the oceans. There are four main types of volcanoes that differ in shape. Eruptions can be triggered by pressure from gases, chemical reactions, or new magma injections. When one occurs, magma explodes from the chamber as lava or ash, which can destroy nearby areas. Afterward, the volcano grows in size and the climate may cool temporarily due to atmospheric effects.
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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.
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This document provides information about volcanoes and volcanic eruptions. It begins with a 10 question pre-assessment about volcanic characteristics and types. It then discusses the classification of volcanoes as active or inactive. Key details are provided about iconic Philippine volcanoes like Mayon and Taal. The different types of volcanic eruptions such as Plinian and Strombolian are described. Finally, the document discusses the factors that affect eruption style and provides signs of an impending eruption.
Powerpoint ii
Volcanoes are formed when magma travels through the earth's mantle and crust, emerging as lava on the surface where it hardens into mountains. The main components of volcanoes are lava and ash. Most volcanoes are located near tectonic plate boundaries under the oceans. There are four main types of volcanoes that differ in shape. Volcanic eruptions can be triggered by pressure from gases, chemical reactions, or new magma injections. Eruptions expel lava, gas, and ash, which can block the sun for years and destroy nearby towns.
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The document discusses volcanic eruptions, including the process by which they occur, different types of eruptions, reasons for eruptions, and effects. It provides details on the top 10 deadliest eruptions in history. Safety tips are also listed, such as staying away from active volcanoes, keeping emergency supplies, knowing evacuation routes, and closing windows if ash is present.
Volcanoes
Volcanoes form when molten magma forces its way through cracks in the Earth's crust. They can take cone shapes but also other shapes. The melted rock that emerges from the volcano's crater is called lava, which destroys everything in its path due to its extreme heat. Volcanoes occur both on land and under the ocean floor, with some ocean volcanoes emerging from the water. They erupt when gases and magma find a way to escape through vents, causing eruptions of varying intensity.
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.
Sllideshare
Slideshare es un servicio para compartir presentaciones en línea de manera gratuita. Los usuarios pueden crear una cuenta, subir presentaciones en formato PowerPoint u PDF, y compartirlas con otros o hacerlas públicas. También permite añadir audio o video, incrustar presentaciones en sitios web, y encontrar presentaciones a través de etiquetas clave.
Presentation1
Forced convection involves inducing fluid motion using an external method like a pump or fan. It is characterized by the formation of a thermal boundary layer near the surface for heat transfer. Important dimensionless groups that describe forced convection include the Nusselt number, Reynolds number, and Prandtl number. Common correlations can be used to calculate heat transfer coefficients for internal flows like laminar and turbulent pipe flow, and external flows over configurations like flat plates and cylinders.
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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.
Information on volcano for school
Volcanoes are openings in the Earth's crust that allow magma, ash, and gases to escape from below the surface. There are three types of volcanoes: active, dormant, and extinct. Magma is molten rock underground, while lava is magma that flows out of a volcano. Ash, cinders, and pumice are other materials emitted from volcanoes. Over half of the world's volcanoes are located on the Ring of Fire around the Pacific Ocean. Volcanic eruptions are caused by the movement of tectonic plates, which squeezes magma up in between. Eruptions can endanger people through lava, tsunamis, earthquakes, and toxic gases
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There are several different types of volcanic eruptions that are classified based on their eruption dynamics and behavior. The main types include magmatic eruptions driven by gas decompression, phreatomagmatic eruptions driven by gas compression, and phreatic eruptions caused by steam superheating. Specific eruption styles like Hawaiian, Strombolian, Vulcanian, Pelean, Plinian, Surtseyan, submarine, subglacial and phreatic eruptions each have unique characteristics in terms of the materials erupted and speeds of eruption columns or pyroclastic flows. The crystal, gas and temperature properties of magma influence whether an eruption will be explosive or effusive
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This document defines volcanoes as openings in the Earth's crust that allow molten rock and gases to escape. It notes that over half of the world's active volcanoes above sea level are located along the Ring of Fire. Volcanoes form when tectonic plates collide, spread apart, or interact under a plate. The parts of a volcano include the crater, pipe, cone, and vent. There are three main types of volcanoes: composite/strato volcanoes, shield volcanoes, and cinder cone volcanoes. Volcanic eruptions can have both beneficial effects like adding nutrients to soil or creating new islands, and harmful effects like releasing aerosols or abandoning land.
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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.
Mount pelee science project
Mount Pelée is a volcano located on the island of Martinique. In 1902, it erupted with little warning, destroying the city of St. Pierre and killing nearly all 30,000 inhabitants within minutes. The eruption produced two pyroclastic flows - one that shot vertically into the sky and another that raced laterally down the mountain at 100 mph, engulfing St. Pierre in hot ash and gases. Only two people survived the eruption. Mount Pelée formed as a result of the subduction of the Cocos tectonic plate under the Caribbean plate. While there was no lava flow, the eruption deposited large amounts of ash that could have later lithified into sedimentary rock.
Milena
Volcanoes are openings in the Earth's crust where magma and gases erupt. During an eruption, volcanoes expel lava, ash, dust, gas and vapor. There are three types of volcanoes: active volcanoes that are currently erupting or may erupt soon, dormant volcanoes that have not erupted for a long time, and extinct volcanoes that have not erupted for over 10,000 years. Volcanic eruptions produce rocks and lava that make soil fertile for farming and also provide geothermal energy for human use, but they can also endanger lives through hazards like lava and ash flows, bombs and clouds during an eruption.
Volcanoes sample
A volcano is a mountain formed when magma reaches the Earth's surface through weak spots, erupting gases, ashes, and rocks. Volcanic eruptions can destroy nearby homes and populations, as seen at Pompeii. However, volcanoes also provide benefits as the hot rocks expelled are rich in minerals that improve soil quality for growing plants. The document questions whether scientists can predict volcanic eruptions.
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
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This presentation contains the basic details on the Volcano. It also includes how to make a Volcano and the experiment how to erupt the volcano.
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.
Volcanoes, Volcano PowerPoint Quiz Game, Earth Science Lesson PowerPoint
The document appears to be a review game about volcanoes for students. It contains 20 multiple choice questions about volcanoes, their characteristics, famous examples, and effects. It also includes 5 bonus questions about volcano movies. The review game instructs students to use class notes and materials to answer the questions in small groups without sharing answers between groups.
Volcano Features, Earth Science Lesson PowerPoint, Buld a Volcano
This PowerPoint is one small part of the Geology Topics unit from www.sciencepowerpoint.com. This unit consists of a five part 6000+ slide PowerPoint roadmap, 14 page bundled homework package, modified homework, detailed answer keys, 12 pages of unit notes for students who may require assistance, follow along worksheets, and many review games. The homework and lesson notes chronologically follow the PowerPoint slideshow. The answer keys and unit notes are great for support professionals. The activities and discussion questions in the slideshow are meaningful. The PowerPoint includes built-in instructions, visuals, and review questions. Also included are critical class notes (color coded red), project ideas, video links, and review games. This unit also includes four PowerPoint review games (110+ slides each with Answers), 38+ video links, lab handouts, activity sheets, rubrics, materials list, templates, guides, 6 PowerPoint review Game, and much more. Also included is a 190 slide first day of school PowerPoint presentation.
Areas of Focus within The Geology Topics Unit: -Plate Tectonics, Evidence for Plate Tectonics, Pangea, Energy Waves, Layers of the Earth, Heat Transfer, Types of Crust, Plate Boundaries, Hot Spots, Volcanoes, Positives and Negatives of Volcanoes, Types of Volcanoes, Parts of a Volcano, Magma, Types of Lava, Viscosity, Earthquakes, Faults, Folds, Seismograph, Richter Scale, Seismograph, Tsunami's, Rocks, Minerals, Crystals, Uses of Minerals, Types of Crystals, Physical Properties of Minerals, Rock Cycle, Common Igneous Rocks, Common Sedimentary Rocks, Common Metamorphic Rocks.
This unit aligns with the Next Generation Science Standards and with Common Core Standards for ELA and Literacy for Science and Technical Subjects. See preview for more information
If you have any questions please feel free to contact me. Thanks again and best wishes. Sincerely, Ryan Murphy M.Ed www.sciencepowerpoint@gmail.com
Volcanoes
Volcanoes form when magma travels through the earth's mantle and crust, reaching the surface as lava and building up in a mountain-like shape. They are composed of cooled lava and ash. Most volcanoes are located near tectonic plate boundaries under the oceans. There are four main types of volcanoes that differ in shape. Eruptions can be triggered by pressure from gases, chemical reactions, or new magma injections. When one occurs, magma explodes from the chamber as lava or ash, which can destroy nearby areas. Afterward, the volcano grows in size and the climate may cool temporarily due to atmospheric effects.
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 Grade 9
This document provides information about volcanoes and volcanic eruptions. It begins with a 10 question pre-assessment about volcanic characteristics and types. It then discusses the classification of volcanoes as active or inactive. Key details are provided about iconic Philippine volcanoes like Mayon and Taal. The different types of volcanic eruptions such as Plinian and Strombolian are described. Finally, the document discusses the factors that affect eruption style and provides signs of an impending eruption.
Powerpoint ii
Volcanoes are formed when magma travels through the earth's mantle and crust, emerging as lava on the surface where it hardens into mountains. The main components of volcanoes are lava and ash. Most volcanoes are located near tectonic plate boundaries under the oceans. There are four main types of volcanoes that differ in shape. Volcanic eruptions can be triggered by pressure from gases, chemical reactions, or new magma injections. Eruptions expel lava, gas, and ash, which can block the sun for years and destroy nearby towns.
Volcanic Eruption
The document discusses volcanic eruptions, including the process by which they occur, different types of eruptions, reasons for eruptions, and effects. It provides details on the top 10 deadliest eruptions in history. Safety tips are also listed, such as staying away from active volcanoes, keeping emergency supplies, knowing evacuation routes, and closing windows if ash is present.
Volcanoes
Volcanoes form when molten magma forces its way through cracks in the Earth's crust. They can take cone shapes but also other shapes. The melted rock that emerges from the volcano's crater is called lava, which destroys everything in its path due to its extreme heat. Volcanoes occur both on land and under the ocean floor, with some ocean volcanoes emerging from the water. They erupt when gases and magma find a way to escape through vents, causing eruptions of varying intensity.
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.
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Volcanoes, Volcano PowerPoint Quiz Game, Earth Science Lesson PowerPoint
Volcanoes, Volcano PowerPoint Quiz Game, Earth Science Lesson PowerPoint
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Volcano Features, Earth Science Lesson PowerPoint, Buld a Volcano
Intervention Material in Science: Types of Volcanoes
Intervention Material in Science: Types of Volcanoes
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Sllideshare
Slideshare es un servicio para compartir presentaciones en línea de manera gratuita. Los usuarios pueden crear una cuenta, subir presentaciones en formato PowerPoint u PDF, y compartirlas con otros o hacerlas públicas. También permite añadir audio o video, incrustar presentaciones en sitios web, y encontrar presentaciones a través de etiquetas clave.
Presentation1
Forced convection involves inducing fluid motion using an external method like a pump or fan. It is characterized by the formation of a thermal boundary layer near the surface for heat transfer. Important dimensionless groups that describe forced convection include the Nusselt number, Reynolds number, and Prandtl number. Common correlations can be used to calculate heat transfer coefficients for internal flows like laminar and turbulent pipe flow, and external flows over configurations like flat plates and cylinders.
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Convection is a process of heat transfer where hotter less dense material rises and cooler, denser material sinks, causing circulation within fluids like gases and liquids. Convection occurs due to differences in density caused by variations in temperature, allowing heat to be transferred through the movement of the fluid. Examples of convection include heat transfer through gases and liquids, as well as phenomena like sea breezes that transfer heat and demonstrate the principles of convection.
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This document discusses heat transfer via forced convection. It begins by outlining key topics like boundary layer thickness, skin surface coefficient, and dimensional relationships involving Reynolds and Prandtl numbers. It then discusses specific heat transfer processes like boiling and condensation. The majority of the document focuses on deriving the Blasius exact solution for laminar boundary layer flows over a flat plate through defining stream functions and solving the boundary layer equations and continuity equation to obtain the velocity profile. Key parameters like boundary layer thickness and skin friction coefficient are also defined and related to the dimensionless velocity profile.
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Heat can be transferred through three modes: conduction, convection, and radiation. Conduction requires physical contact between objects and involves heat transfer through vibrations in solids. Convection involves the movement of heated fluids like liquids and gases. Radiation transfers heat through electromagnetic waves and does not require a medium. Different materials conduct heat at different rates depending on properties like their molecular structure. Metals are generally good conductors while gases are poor conductors due to low molecular cohesion. Proper use of these conductive properties allows for efficient heat transfer in applications like cooking.
Multiple linear regression
Introduces and explains the use of multiple linear regression, a multivariate correlational statistical technique. For more info, see the lecture page at http://goo.gl/CeBsv. See also the slides for the MLR II lecture http://www.slideshare.net/jtneill/multiple-linear-regression-ii
Thermodynamics Chapter 3- Heat Transfer
The document discusses heat transfer through conduction, convection and radiation. It covers key concepts like Fourier's law of heat conduction, thermal conductivity of solids, liquids and gases, one dimensional and radial heat conduction, and heat transfer through composite walls. It also provides examples of calculating heat transfer through plane and cylindrical walls, determining the required thickness of insulation, and calculating critical thickness of insulation.
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Similar to 2. causes of volcanoes keh
Pangea
The document discusses Alfred Wegener's theory of continental drift from 1912. It explains that Wegener noticed that fossils found in South America were identical to those found in Africa and proposed that the continents were once joined together in a supercontinent called Pangea. The theory described the continents gradually drifting apart over millions of years due to plate tectonics.
Plate Tectonics I
This document provides an overview of plate tectonics and the key individuals and discoveries that led to the development of the theory. It discusses Alfred Wegener's idea of continental drift in the early 20th century, which was initially rejected. It then covers the discoveries of the mid-ocean ridge system and magnetic striping of the ocean floor in the 1950s-60s, which provided evidence that the continents are moving and new crust is generated at ocean ridges through seafloor spreading. This led to the acceptance of plate tectonics as a scientific theory to explain geological phenomena.
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Continental Drift And Plate Tectonics Andie
1) Alfred Wegener first proposed the theory of continental drift, which suggested that the continents were once joined together and have since drifted apart.
2) Wegener provided geological, fossil, and climate evidence to support his theory, but could not explain the force driving continental movement.
3) In the 1960s, the theory of plate tectonics was developed, explaining that convection currents in the mantle cause the movement of tectonic plates, resolving the issue that prevented acceptance of Wegener's theory.
t2-g-3768-all-about-volcanoes-information-powerpoint-_ver_5.pdf
Volcanoes form when magma leaks through the earth's crust and onto the surface. The word "volcano" comes from the island of Vulcano near Italy, named for the Roman god of fire Vulcan. There are over 1500 active volcanoes on earth, located primarily on tectonic plate boundaries. The three main types of volcanoes are composite, cinder, and shield. When magma pushes through the crust, it can erupt violently or gently flow as lava, depending on the volcano type and magma viscosity.
All about Volcanoes (presented by Angel) .pptx
All About Volcanoes
Volcanoes are remarkable geological structures formed by the eruption of molten rock, ash, and gases from the Earth's mantle. These natural phenomena can shape landscapes, create new landforms, and significantly impact both the environment and human societies. Understanding volcanoes involves exploring their types, formation processes, eruption mechanisms, and effects.
What is a Volcano?
A volcano is an opening in the Earth's crust through which magma, gases, and ash are expelled. When magma reaches the surface, it is called lava. Over time, repeated eruptions can build up a mountain or other landform around the volcanic vent.
Types of Volcanoes:
Shield Volcanoes:
Characteristics: Broad, gently sloping sides formed by the flow of low-viscosity basaltic lava that can travel long distances.
Examples: Mauna Loa and Kilauea in Hawaii.
Composite Volcanoes (Stratovolcanoes):
Characteristics: Steep, conical volcanoes made up of alternating layers of lava, ash, and volcanic debris. They are known for their explosive eruptions.
Examples: Mount Fuji in Japan, Mount St. Helens in the USA, and Mount Vesuvius in Italy.
Cinder Cone Volcanoes:
Characteristics: Small, steep-sided cones built from volcanic fragments such as ash, tephra, and volcanic rocks ejected during eruptions.
Examples: Parícutin in Mexico and Sunset Crater in the USA.
Lava Domes:
Characteristics: Rounded, steep-sided mounds formed by the slow extrusion of viscous lava.
Examples: Mount St. Helens’ Lava Dome in the USA.
Volcanic Features:
Crater:
Description: A bowl-shaped depression at the summit of a volcano, typically formed by explosive eruptions.
Caldera:
Description: A large depression formed when a volcano's summit collapses or is blown away during a massive eruption.
Examples: Yellowstone Caldera in the USA.
Lava Flows:
Description: Streams of molten rock that pour from a volcanic vent and solidify as they cool.
Pyroclastic Flows:
Description: Fast-moving currents of hot gas and volcanic material that can travel down the sides of a volcano during explosive eruptions.
Volcanic Ash:
Description: Fine particles of pulverized rock and glass created during volcanic eruptions that can travel long distances.
Formation of Volcanoes:
Subduction Zones:
Description: Volcanoes often form at convergent plate boundaries where an oceanic plate subducts beneath a continental plate, leading to magma formation.
Examples: The Ring of Fire around the Pacific Ocean.
Rift Zones:
Description: Volcanoes can also form at divergent plate boundaries where tectonic plates are pulling apart, allowing magma to rise.
Examples: Mid-Atlantic Ridge and East African Rift.
Hotspots:
Description: Volcanic activity that occurs away from plate boundaries, caused by plumes of hot material rising from deep within the mantle.
Examples: Hawaiian Islands and Yellowstone.
volcanoes.pptx
Volcanoes form when magma leaks through the earth's crust and onto the surface. There are over 1500 active volcanoes worldwide, with most located around the Pacific Ring of Fire. Volcanoes are classified as active, dormant, or extinct depending on recent eruption activity. The three main types are composite, cinder, and shield volcanoes. The largest active volcano is Mauna Loa in Hawaii. Other planets like Mars and Jupiter's moon Io also have volcanoes.
t2-g-3768-all-about-volcanoes-information-powerpoint-_ver_5.pptx
Volcanoes form when magma leaks through the earth's crust and onto the surface. The word "volcano" comes from Vulcan, the Roman god of fire believed to live within volcanoes. There are over 1500 active volcanoes worldwide, with most located along tectonic plate boundaries in the "Ring of Fire" in the Pacific Ocean. The three main types of volcanoes are composite, cinder, and shield volcanoes, which erupt in different ways.
Earth&PlateTectonics_Butler_ERBmod.ppt
The document discusses plate tectonics and the evidence that supports the theory. It explains that the Earth's crust is broken into plates that move relative to each other. There are three main types of plate boundaries: divergent, convergent, and transform. Evidence for plate tectonics includes the locations of earthquakes and volcanoes along plate boundaries, as well as the movement of continents over geologic time as described by Alfred Wegener's theory of continental drift.
Alfred Wegener, Pangea, A+.ppt.pptxhshsh
Alfred Wegener originally proposed the theory of continental drift in the early 20th century, hypothesizing that the continents are slowly drifting around the Earth. He suggested that hundreds of millions of years ago, all the continents were joined together in a single landmass called Pangea. Pangea has since broken apart, with evidence found in matching fossil and rock formations between separated continents and the way the continents appear to fit together like puzzle pieces. While initially criticized, Wegener's theory of continental drift has since been supported by further evidence of plate tectonics showing how the movement of tectonic plates can cause the continents to drift apart over millions of years.
The story of pangea and plate tectonics
The document summarizes the theory of plate tectonics and the existence of the supercontinent Pangaea. It describes how early scientists noticed that continents seemed to fit together like puzzle pieces. It then discusses how Alfred Wegener proposed the theory of continental drift and Pangaea in the early 1900s, but his colleagues rejected it due to a lack of evidence. Finally, it outlines how the theory of plate tectonics was developed in the 1960s based on findings of sea floor spreading and magnetic stripes on the ocean floor.
Continental Drift And Plate Tectonics Andie
1) Alfred Wegener first proposed the theory of continental drift in the early 20th century, suggesting that the continents were once joined together in a supercontinent called Pangaea before drifting apart.
2) Wegener provided geological, fossil, and climate evidence to support his theory, but his ideas were rejected by many scientists because he could not explain the force driving the continental movement.
3) In the 1960s, the theory of plate tectonics was developed, explaining that convection currents in the mantle cause the plates to move and providing the mechanism that Wegener could not.
Continental-Drift 2015.ppt
Continental drift is the theory that the continents were once joined together in a supercontinent called Pangaea before slowly drifting apart. Alfred Wegener first proposed this theory in 1912 based on matching coastline shapes, fossil evidence, and rock formations found on separated continents. The document discusses key terms like plate tectonics and Pangaea. It provides examples of fossil and geological evidence that support continental drift, such as the seed fossil Glossopteris being found across Africa, South America, India and Antarctica. The theory was controversial for decades but gained widespread acceptance when plate tectonics was developed in the 1960s to explain continental movement.
Convection currents and continental drift
Subduction zones occur where one tectonic plate slides under another, usually around the Ring of Fire. Convection currents in the mantle cause rocks to rise and fall, powering plate tectonics at the Asthenosphere. Continental drift is when tectonic plate movements cause continents to shift positions over time, an idea first proposed by Alfred Wegener based on matching coastlines, shared rock types, and fossil evidence between continents that were once joined together in the supercontinent Pangaea.
Subduction zones Convection currents and continental drift
Subduction zones occur where one tectonic plate slides under another, usually around the Ring of Fire. Convection currents in the mantle cause rocks to rise and fall, powering plate tectonics at the Asthenosphere. Continental drift is when tectonic plate movements cause continents to shift positions over time, an idea first proposed by Alfred Wegener based on matching coastlines, shared rock types, and fossil evidence between continents that were once joined together in the supercontinent Pangaea.
Continental Drift And Plate Tectonics Andie
1) Alfred Wegener first proposed the theory of continental drift, which suggested that the continents were once joined together and have since drifted apart.
2) Wegener provided geological, fossil, and climate evidence to support his theory, but could not explain the force driving continental movement.
3) In the 1960s, the theory of plate tectonics was developed, explaining that convection currents in the mantle cause the movement of tectonic plates. Sea floor spreading provided key evidence that the ocean floor continually forms at mid-ocean ridges.
Continental Drift And Plate Tectonics Andie
1) Alfred Wegener first proposed the theory of continental drift, which suggested that the continents were once joined together and have since drifted apart.
2) Wegener provided geological, fossil, and climate evidence to support his theory, but could not explain the force driving continental movement.
3) In the 1960s, the theory of plate tectonics was developed, explaining that convection currents in the mantle cause the movement of tectonic plates. Sea floor spreading provided key evidence that the ocean floor was pulling apart.
Continental Drift And Plate Tectonics Andie
1) Alfred Wegener first proposed the theory of continental drift, which suggested that the continents were once joined together and have since drifted apart.
2) Wegener provided geological, fossil, and climate evidence to support his theory, but could not explain the force driving continental movement.
3) In the 1960s, scientists discovered sea floor spreading and plate tectonics, which explained that convection currents in the mantle push and pull the tectonic plates. This provided the long-sought mechanism for continental drift.
Webquest answers
This document provides an overview of plate tectonics through a webquest containing various links about the theory. It discusses how convection in the mantle drives the movement of tectonic plates, and how this causes earthquakes and volcanic activity at plate boundaries. The document also explores earlier theories on the shifting of continents and formation of geological features, and how data like fossil and magnetic evidence supports the modern theory of plate tectonics.
Time traveling alfred wegener essay
Alfred Wegener traveled through time to collect evidence to prove his theory of continental drift. He discovered that plate tectonics caused the continents to drift apart. Wegener found six key pieces of evidence to support continental drift: 1) the coastlines of continents fit together like puzzle pieces, 2) matching rock sequences and ages across continents, 3) matching diamond patterns across oceans, 4) mountain ranges torn apart by continental movement, 5) matching past glacier patterns, and 6) matching fossil distributions across continents. Wegener concluded that billions of years ago the continents were joined together in a supercontinent called Pangaea, which later broke apart due to plate tectonics.
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Subduction zones Convection currents and continental drift
Subduction zones Convection currents and continental drift
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Christmas quiz 2013
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Yellowstone np eb
Yellowstone National Park poses a potential global risk due to its supervolcano.
1) Yellowstone sits atop one of the largest supervolcanoes on Earth, which last erupted 640,000 years ago.
2) An eruption could have devastating consequences, ejecting huge amounts of volcanic material into the atmosphere and potentially cooling the climate globally for years.
3) Millions of people living throughout North America would be at risk from the far-reaching effects of ash and gas from an eruption of the Yellowstone supervolcano.
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2. Students will learn about the particles that make up the nucleus, how this relates to elements in the periodic table, and the different types of radioactive decay. They will watch videos, draw diagrams, and build atoms on a website.
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The Geography Department fieldtrip to Arran in June 2014 has three main aims: to conduct fieldwork to enhance understanding of physical and human geography; to gather and partially write up data for GCSE controlled assessments; and to foster interest in geography and the outdoors. The week-long itinerary includes days studying coastal and river landforms and processes, as well as coastal data collection and the location of industry. Students will stay at the Lochranza Field Studies Centre and participate in evening learning sessions. The trip is led by two qualified teachers and expedition leaders and will prioritize health and safety. The total cost is £300 which covers transportation, accommodation, meals, materials, and insurance. Payment plans are available and scholarships may
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This document discusses how two countries, the USA and Myanmar, managed tropical storms and how they could better prepare for future storms in a more sustainable way. It provides learning objectives on understanding how these countries dealt with tropical storms in the past, such as Hurricane Katrina in 2005 and Cyclone Nargis in 2008, and how they could improve preparations. The document then lists activities for students, such as completing a table comparing how the two countries managed storms well and badly, drawing a diagram of sustainable storm management strategies, and annotating a map of New Orleans to show updated protections against disasters like Hurricane Katrina.
14. cyclone nargis
Cyclone Nargis caused severe damage in Myanmar in 2008. It formed over warm waters in the Bay of Bengal and traveled west, making landfall in Myanmar. The storm caused catastrophic damage due to strong winds and heavy rainfall. Over 138,000 people were killed or left missing. The damage was exacerbated by the lack of early warning systems and destruction of coastal mangrove forests that normally help protect against storm surges.
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- In LEDCs, droughts often result in widespread food shortages and malnutrition as crops fail, leading to deaths of over a million people in Ethiopia's 1984 drought.
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A powerful earthquake struck Southern California early this morning, causing widespread damage and loss of life. The 6.7 magnitude quake was centered in the community of Northridge, just outside of Los Angeles. It struck at 4:30 am local time, when many people were still asleep. The shaking caused buildings and highways to collapse. Over 20,000 residences were destroyed. Tragically, 57 people lost their lives in the disaster. Estimates put financial losses from the quake in the billions. Emergency responders are working around the clock to rescue trapped individuals and provide aid to those displaced. More aftershocks are expected in the
5. earthquakes keh
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HCL Notes and Domino License Cost Reduction in the World of DLAU
Webinar Recording: https://www.panagenda.com/webinars/hcl-notes-and-domino-license-cost-reduction-in-the-world-of-dlau/
The introduction of DLAU and the CCB & CCX licensing model caused quite a stir in the HCL community. As a Notes and Domino customer, you may have faced challenges with unexpected user counts and license costs. You probably have questions on how this new licensing approach works and how to benefit from it. Most importantly, you likely have budget constraints and want to save money where possible. Don’t worry, we can help with all of this!
We’ll show you how to fix common misconfigurations that cause higher-than-expected user counts, and how to identify accounts which you can deactivate to save money. There are also frequent patterns that can cause unnecessary cost, like using a person document instead of a mail-in for shared mailboxes. We’ll provide examples and solutions for those as well. And naturally we’ll explain the new licensing model.
Join HCL Ambassador Marc Thomas in this webinar with a special guest appearance from Franz Walder. It will give you the tools and know-how to stay on top of what is going on with Domino licensing. You will be able lower your cost through an optimized configuration and keep it low going forward.
These topics will be covered
- Reducing license cost by finding and fixing misconfigurations and superfluous accounts
- How do CCB and CCX licenses really work?
- Understanding the DLAU tool and how to best utilize it
- Tips for common problem areas, like team mailboxes, functional/test users, etc
- Practical examples and best practices to implement right away
Digital Banking in the Cloud: How Citizens Bank Unlocked Their Mainframe
Inconsistent user experience and siloed data, high costs, and changing customer expectations – Citizens Bank was experiencing these challenges while it was attempting to deliver a superior digital banking experience for its clients. Its core banking applications run on the mainframe and Citizens was using legacy utilities to get the critical mainframe data to feed customer-facing channels, like call centers, web, and mobile. Ultimately, this led to higher operating costs (MIPS), delayed response times, and longer time to market.
Ever-changing customer expectations demand more modern digital experiences, and the bank needed to find a solution that could provide real-time data to its customer channels with low latency and operating costs. Join this session to learn how Citizens is leveraging Precisely to replicate mainframe data to its customer channels and deliver on their “modern digital bank” experiences.
5th LF Energy Power Grid Model Meet-up Slides
5th Power Grid Model Meet-up
It is with great pleasure that we extend to you an invitation to the 5th Power Grid Model Meet-up, scheduled for 6th June 2024. This event will adopt a hybrid format, allowing participants to join us either through an online Mircosoft Teams session or in person at TU/e located at Den Dolech 2, Eindhoven, Netherlands. The meet-up will be hosted by Eindhoven University of Technology (TU/e), a research university specializing in engineering science & technology.
Power Grid Model
The global energy transition is placing new and unprecedented demands on Distribution System Operators (DSOs). Alongside upgrades to grid capacity, processes such as digitization, capacity optimization, and congestion management are becoming vital for delivering reliable services.
Power Grid Model is an open source project from Linux Foundation Energy and provides a calculation engine that is increasingly essential for DSOs. It offers a standards-based foundation enabling real-time power systems analysis, simulations of electrical power grids, and sophisticated what-if analysis. In addition, it enables in-depth studies and analysis of the electrical power grid’s behavior and performance. This comprehensive model incorporates essential factors such as power generation capacity, electrical losses, voltage levels, power flows, and system stability.
Power Grid Model is currently being applied in a wide variety of use cases, including grid planning, expansion, reliability, and congestion studies. It can also help in analyzing the impact of renewable energy integration, assessing the effects of disturbances or faults, and developing strategies for grid control and optimization.
What to expect
For the upcoming meetup we are organizing, we have an exciting lineup of activities planned:
-Insightful presentations covering two practical applications of the Power Grid Model.
-An update on the latest advancements in Power Grid -Model technology during the first and second quarters of 2024.
-An interactive brainstorming session to discuss and propose new feature requests.
-An opportunity to connect with fellow Power Grid Model enthusiasts and users.
Monitoring and Managing Anomaly Detection on OpenShift.pdf
Monitoring and Managing Anomaly Detection on OpenShift
Overview
Dive into the world of anomaly detection on edge devices with our comprehensive hands-on tutorial. This SlideShare presentation will guide you through the entire process, from data collection and model training to edge deployment and real-time monitoring. Perfect for those looking to implement robust anomaly detection systems on resource-constrained IoT/edge devices.
Key Topics Covered
1. Introduction to Anomaly Detection
- Understand the fundamentals of anomaly detection and its importance in identifying unusual behavior or failures in systems.
2. Understanding Edge (IoT)
- Learn about edge computing and IoT, and how they enable real-time data processing and decision-making at the source.
3. What is ArgoCD?
- Discover ArgoCD, a declarative, GitOps continuous delivery tool for Kubernetes, and its role in deploying applications on edge devices.
4. Deployment Using ArgoCD for Edge Devices
- Step-by-step guide on deploying anomaly detection models on edge devices using ArgoCD.
5. Introduction to Apache Kafka and S3
- Explore Apache Kafka for real-time data streaming and Amazon S3 for scalable storage solutions.
6. Viewing Kafka Messages in the Data Lake
- Learn how to view and analyze Kafka messages stored in a data lake for better insights.
7. What is Prometheus?
- Get to know Prometheus, an open-source monitoring and alerting toolkit, and its application in monitoring edge devices.
8. Monitoring Application Metrics with Prometheus
- Detailed instructions on setting up Prometheus to monitor the performance and health of your anomaly detection system.
9. What is Camel K?
- Introduction to Camel K, a lightweight integration framework built on Apache Camel, designed for Kubernetes.
10. Configuring Camel K Integrations for Data Pipelines
- Learn how to configure Camel K for seamless data pipeline integrations in your anomaly detection workflow.
11. What is a Jupyter Notebook?
- Overview of Jupyter Notebooks, an open-source web application for creating and sharing documents with live code, equations, visualizations, and narrative text.
12. Jupyter Notebooks with Code Examples
- Hands-on examples and code snippets in Jupyter Notebooks to help you implement and test anomaly detection models.
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2. causes of volcanoes keh
- 1. What causes earthquakes and volcanoes? To understand the theory of plate tectonics To be able to explain how convection currents work
- 2. Use page 184 to label your cross section with information and distances. Pictures to help you... piece
- 4. In 1912, a German scientist called Alfred Wegener proposed that South America and Africa were once joined together and had subsequently moved apart. He believed that all the continents were once joined together as one big land mass called Pangaea and this was intact until about 200 million years ago. The idea that continents are slowly shifting their positions is called continental drift. What is continental drift? http://www.youtube.com/watch?v=uGcDed 4xVD4
- 5. Study of fossils Similar fossils are found on different continents. This is evidence that these regions were once very close or joined together. Shapes of continents Some continents fit together like a jigsaw. Africa South America Pattern of rocks Similar pattern of rock layers on different continents is evidence that the rocks were once close together or joined. Evidence for continental drift
- 6. African Indo-Australian Plate North American South American Eurasian Pacific Nazca Antarctic Pacific Plate names – the study of these plates is referred to as plate tectonics
- 7. Can you name plates A and B? A B African Plate Indo-Australian Plate Plate names
- 8. Some plates are continental (like the North American Plate) Some are oceanic (like the Pacific Plate) It is at the MARGINS/ BOUNDARIES of these plates where the action usually happens
- 9. Tasks: pg 186 • Draw onto your map the plate boundaries. • Put arrows onto your map to show the direction that the plates are moving in.
- 10. So why do the plates move? Using only pencils, try to move the book across two tables. Now answer this question! Use page 187 to help you and include a diagram. http://www.youtube.com/w atch?v=ryrXAGY1dmE
- 11. • http://www.youtube.com/watch?v=ncut0iT nOgI You can actually see them working!
- 12. Structure of volcanoes Types of volcano Hazards associated with them
- 13. • One in 10 people in the world live within 'danger range' of an active volcano. • Magma is dangerous on the surface of the earth. • There are around 1510 'active' volcanoes in the world. • 1510 volcanoes have erupted in the last 10,000 years, which means they are active in the world of volcanoes. • There are thought to be many more volcanoes on the sea bed. • Russia has the worlds tallest volcano at 3050m • The biggest volcano in the world is Mauna Loa in Hawaii. Its whole volume is about 80,000 cubic kilometres. • Sometimes lightning is seen in volcanic clouds. It's not clear why this happens but it could be to do with lots of hot Lava
- 14. • This will explain why some volcanoes are tall and steep and others are wide and flat.
- 15. • http://www.absorblearning.com/media/item.action?quick=12s • http://www.absorblearning.com/media/item.action?quick=12y At ……………. boundaries, when oceanic crust pushes down underneath …………….. crust it is known as a subduction …………. Friction causes the oceanic crust to……….. The newly formed hot …………… rises up and erupts violently. The volcanoes formed here are called …………..volcanoes, meaning they are tall and …………. sided. An example of this type of volcano is ………………………. in the USA. destructive continental zone melt composite steep Mount St Helens magma
- 17. • http://www.science- resources.co.uk/KS3/Chemistry/Earth_Str ucture/volcanoes.html • Using page 198 and 188, make your own notes to explain how shield volcanoes form at these margins. • KEY TERMS TO USE: shield, less viscous, not explosive, less gas trapped, wide and gentle, moving apart, plates.
- 18. Quick Revision Test • You have 10 minutes to complete this test on the sheet on your own. • I will start the time when the majority of people are in the lesson and ready to go. • I will put your marks on the blog.
- 19. • http://education.sdsc.edu/optiputer/flash/h otSpots.htm • Draw the diagram and use the book to explain how these are formed.
- 21. Name the Hazard SwissEduc: Stromboli Online - Etna 1999 SwissEduc: Stromboli Online – Montserrat Lahars
- 22. Lava • Lava is magma which has escaped to the surface
- 23. Pyroclastic Flow/ Nuée ardentes These are fast moving destructive clouds of hot gas, and ash. They can travel up to 320km/h km per hour. Mt Pelee produced a pyroclastic flow in 1902 which killed 29 000 people.
- 24. Lahars A mixture of water and rock flowing down the volcano slope. A lahar looks like a mass of wet concrete that can carry rock debris more than 10 m in diameter and move up to 95km/h.
- 25. Tephra • Tephra is a general term for fragments of volcanic rock and lava that are blasted into the air by explosions.It can travel thousands of kilometers downwind from a volcano.
- 26. • Complete the summary sheet to show how volcanoes can differ from each other.
- 27. Structure of volcanoes Types of volcano Hazards associated with them