Volcanoes
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Volcanoes can be dangerous due to hazards like lava flows, ash falls, and pyroclastic flows. Lava is very hot liquid that can burn people. Ash falls make the air dirty and hard to breathe. Climate change from volcanoes can also make people ill by changing the climate too quickly. However, volcanoes are less dangerous than earthquakes, tsunamis, and hurricanes. The document also discusses different types of volcanic rocks like magma, igneous, andesite, ryolite, and basalt that are formed from lava, as well as the parts of a volcano.
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What are volcanic hazards 1
The USGS monitors almost 70 active and potentially active volcanoes in the US to assess hazards and closely monitor the most dangerous ones. Volcanoes produce many hazards including eruption columns and clouds, lava and pyroclastic flows, landslides, and lahars (mudflows) that can kill people and destroy property even long distances away. The USGS works to detect signs of unrest and warn the public of impending eruptions and hazards in order to protect lives and property.
Volcanoes
Volcanoes form when molten rock from beneath the earth's crust, called magma, reaches the surface. They occur at places where tectonic plates are moving apart or colliding. Magma originates from heat generated by radioactive elements and pressure changes caused by plate movement. It ascends due to gases and vapors, erupting at the surface as either lava or explosive pyroclastic materials. Volcanoes are classified based on their eruption periodicity and can have varying eruption styles from fissure eruptions to more explosive types.
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Volcanic Hazard
Pyroclastic flows are one of the most dangerous aspects of volcanism as they can travel rapidly and kill through suffocation and burning. Lava flows are generally less explosive but can destroy anything in their path. Large eruptions can also trigger secondary hazards like mudflows, landslides, and tsunamis that increase damage far from the volcano. Long term effects include crop damage, famine, disease, and global cooling from volcanic gases that reflect sunlight.
Where Plates Meet
Destructive plate boundaries occur where an oceanic plate subducts under a continental plate. As the oceanic plate descends it starts to melt from friction, forming magma. This magma can rise to the surface and form volcanoes. Examples of destructive plate boundaries include the Andes Mountains, formed by the subduction of the Nazca Plate under the South American Plate. Living in areas near destructive plate boundaries poses challenges from earthquakes and volcanic eruptions.
Plate Tectonics
The earth's crust is made up of 7 large plates that are constantly moving and interacting, which can cause mountains to form, earthquakes, volcanoes and tsunamis. When plates collide they can push the earth's crust up to form mountain ranges like the Himalayas. Earthquakes happen when plates scrape against each other. Volcanoes are formed in gaps in plates where magma rises up. Tsunamis are generated by large shifts of plates under the ocean.
Volcano
Volcanoes form when lava reaches the Earth's surface. There are three main types of volcanoes: shield volcanoes which have a gentle slope, cinder cones made of blown cinder, and composite volcanoes with layers of cinder and lava. Mount Shasta is described as a composite volcano that has erupted on average every 800 years over the last 10,000 years. Diamond Head is an eroded cinder cone volcano formed by explosions when magma hit ocean water. Kohala is identified as an extinct shield volcano on Hawaii that has not erupted for 60,000 years.
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What are volcanic hazards 1
The USGS monitors almost 70 active and potentially active volcanoes in the US to assess hazards and closely monitor the most dangerous ones. Volcanoes produce many hazards including eruption columns and clouds, lava and pyroclastic flows, landslides, and lahars (mudflows) that can kill people and destroy property even long distances away. The USGS works to detect signs of unrest and warn the public of impending eruptions and hazards in order to protect lives and property.
Volcanoes
Volcanoes form when molten rock from beneath the earth's crust, called magma, reaches the surface. They occur at places where tectonic plates are moving apart or colliding. Magma originates from heat generated by radioactive elements and pressure changes caused by plate movement. It ascends due to gases and vapors, erupting at the surface as either lava or explosive pyroclastic materials. Volcanoes are classified based on their eruption periodicity and can have varying eruption styles from fissure eruptions to more explosive types.
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Pyroclastic flows are one of the most dangerous aspects of volcanism as they can travel rapidly and kill through suffocation and burning. Lava flows are generally less explosive but can destroy anything in their path. Large eruptions can also trigger secondary hazards like mudflows, landslides, and tsunamis that increase damage far from the volcano. Long term effects include crop damage, famine, disease, and global cooling from volcanic gases that reflect sunlight.
Where Plates Meet
Destructive plate boundaries occur where an oceanic plate subducts under a continental plate. As the oceanic plate descends it starts to melt from friction, forming magma. This magma can rise to the surface and form volcanoes. Examples of destructive plate boundaries include the Andes Mountains, formed by the subduction of the Nazca Plate under the South American Plate. Living in areas near destructive plate boundaries poses challenges from earthquakes and volcanic eruptions.
Plate Tectonics
The earth's crust is made up of 7 large plates that are constantly moving and interacting, which can cause mountains to form, earthquakes, volcanoes and tsunamis. When plates collide they can push the earth's crust up to form mountain ranges like the Himalayas. Earthquakes happen when plates scrape against each other. Volcanoes are formed in gaps in plates where magma rises up. Tsunamis are generated by large shifts of plates under the ocean.
Volcano
Volcanoes form when lava reaches the Earth's surface. There are three main types of volcanoes: shield volcanoes which have a gentle slope, cinder cones made of blown cinder, and composite volcanoes with layers of cinder and lava. Mount Shasta is described as a composite volcano that has erupted on average every 800 years over the last 10,000 years. Diamond Head is an eroded cinder cone volcano formed by explosions when magma hit ocean water. Kohala is identified as an extinct shield volcano on Hawaii that has not erupted for 60,000 years.
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This document discusses various natural disasters including avalanches, floods, earthquakes, tornados, volcanoes, hurricanes, wildfires, tsunamis. It provides brief definitions and descriptions of each type of natural disaster, noting that they can cause significant damage but are natural occurrences beyond full human control. Natural disasters discussed include landslides, storms, seismic events, and fires.
Volcano hazards
1. The document discusses various volcano hazards such as lahars, ash fall, pyroclastic flows, ballistic projectiles, volcanic gases, and lava flows.
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Volcanic eruptions can be either explosive or effusive depending on the viscosity and gas content of the magma. Explosive eruptions are hazardous and can send ash clouds high into the atmosphere, affecting climate. Products of explosive eruptions like pyroclastic flows can travel far from the volcano at high speeds, burying anything in their path like the city of Pompeii. To monitor and mitigate volcanic hazards, observatories study seismic activity, deformation, and gas emissions to help predict eruptions and develop warning systems.
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The earth's crust is made up of plates that float on molten rock in the mantle. These plates collide and separate, causing geological events. When plates collide, fold mountains like the Alps are formed through compression, and earthquakes occur along plate boundaries. When plates separate, volcanic islands and mid-ocean ridges result from magma rising through cracks between the plates. Examples are the Mid-Atlantic Ridge and volcanoes in Iceland. The Pacific Ring of Fire is a zone with many volcanoes and earthquakes caused by plate tectonics in the Pacific Ocean region.
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A supervolcano eruption would have devastating effects. Supervolcanoes emit over 1,000 km3 of material and form calderas, which are large depressions formed by the partial emptying of magma chambers. An eruption of the Yellowstone supervolcano would fling magma 50 km into the air and kill all life within 1,000 km through falling ash, lava flows, and the force of the explosion. 100 km3 of lava would flow from the volcano and ash would block the sun, triggering a freezing cold volcanic winter that could cause crop failure and starvation as economies collapse.
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Earthquakes occur when tectonic plates shift beneath the Earth's surface, causing the ground to shake and sometimes displace. Large offshore earthquakes can displace the seabed enough to create tsunamis. Earthquakes may also trigger landslides or volcanic eruptions in rare cases. Volcanic eruptions happen when gas and magma build up underground, releasing lava, rocks, and ash during more explosive eruptions. Eruptions with less gas and thicker magma tend to be less dramatic and result in lava flows from the vent.
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1. The document discusses various volcano hazards such as lahars, ash fall, pyroclastic flows, ballistic projectiles, volcanic gases, and lava flows.
2. It also differentiates between subduction, rift, and hot spot volcanoes.
3. The document provides signs of an impending volcanic eruption and describes appropriate measures that can be taken before, during, and after an eruption including evacuating to higher ground, using protective masks, and cleaning ash after the eruption.
volcanohazards-190108013605.pptx
1. The document discusses various volcano hazards such as lahars, ash fall, pyroclastic flows, ballistic projectiles, volcanic gases, and lava flows.
2. It also differentiates between subduction, rift, and hot spot volcanoes.
3. The document provides signs of an impending volcanic eruption and describes appropriate measures that can be taken before, during, and after an eruption including evacuating to higher ground, using protective masks, and cleaning ash after the eruption.
Volcanoes
Volcanoes form when lava from below the Earth's surface reaches the surface. The largest volcanoes in the world can erupt in dangerous ways such as lava rivers that burn people and animals, ash clouds containing toxic gases, and lava bombs that explode. Volcanologists study volcanoes to understand their eruptions and predict future activity in order to keep people safe from the hazards volcanoes can pose.
Volcanoes #scichallenge2017
This document provides information about volcanoes. It defines a volcano as a geological phenomenon on Earth's surface that usually appears as a hill or mountain formed by eruptions of magma from below the surface. Volcanoes have a main vent and sometimes side vents where lava and gases escape. The top of the volcano forms a crater. Most volcanoes are underwater, and their eruptions can cause dangerous events like lava flows, ash falls, and toxic gas releases that threaten nearby people. Prior to eruptions, signs like bubbling gases and dying vegetation may occur. The largest recorded eruption was Krakatoa in Indonesia in 1883, which could be heard over 1,000 km away and generated a ts
Vulkani eng #scichallenge2017
This document provides information about volcanoes. It defines a volcano as a geological phenomenon on Earth's surface that usually appears as a hill or mountain formed by eruptions of magma from below the surface. Volcanoes have a main vent and sometimes side vents where lava and gases escape. The top of the volcano forms a crater. Most volcanoes are underwater, and their eruptions can cause dangerous events like lava flows, ash falls, and toxic gas releases that threaten nearby people. Prior to eruptions, signs like bubbling gases and dying vegetation may occur. The largest recorded eruption was Krakatoa in Indonesia in 1883, whose sounds were heard over 1,000 km away and caused a ts
Lecture 2 global significance of volcanic activity
Volcanic eruptions occur along tectonic plate boundaries and above mantle hotspots. [1] On average, volcanic disasters kill about 1,000 people per year, though large eruptions can be devastating. [2] Eruptions vary in size, from many small eruptions to rare "great eruptions". [3] There are around 450 volcanoes classified as active that have erupted historically, and over 200 considered capable of future eruptions. [4] The type of eruption depends on the volcano's magma composition, with basaltic volcanoes generally less explosive than rhyolitic volcanoes. [5] The greatest volcanic threats are from intermediate volcanoes located in den
DISASTER MANAGEMENT.pptx
This document provides an overview of volcanoes and volcanic disasters. It defines volcanoes as vents through which lava and gases are ejected from below the earth's surface. The document outlines some key factors that can trigger volcanic eruptions and describes the devastating impacts eruptions can have. Specifically, it discusses how the collision of tectonic plates can cause magma to rise and fuel eruptions. The Ring of Fire, a zone of volcanic and earthquake activity around the Pacific Ocean, is also mentioned.
DISASTER MANAGEMENT.pptx
This document provides an overview of volcanoes and volcanic disasters. It defines volcanoes as vents through which lava and gases are ejected from below the earth's surface. The document outlines some key factors that can trigger volcanic eruptions and describes the devastating impacts eruptions can have. Specifically, it discusses how the Ring of Fire zone experiences high volcanic activity along the Pacific coasts. The phases of volcanoes - active, dormant and extinct - are also summarized.
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.
VOLCANOES for CAMBRIDGE A LEVEL
this power point talks about the causes, impacts and management strategies of volcanoes. it describe about the types of lava flow and types of volcanoes also,
volcanoes-221110025957-35821762 (2).pptx
This document provides information about volcanoes, including how they are classified and the signs of an impending volcanic eruption. It discusses the different types of volcanoes based on their activity, composition/structure, and eruption patterns. Active volcanoes are those currently erupting or likely to erupt soon, while dormant volcanoes have not erupted in a long time but could in the future. Shield, cinder cone, and stratovolcanoes are classified based on their shape and composition. Signs of an impending eruption include increased seismic activity, changes in steaming/gas emissions, and ground deformation. The document also outlines hazards like pyroclastic flows, lahars, ash falls and lava flows, and provides guidance on
Earthquakes and Volcanoes
Earthquakes are caused by the sudden movement of parts of the Earth's crust. The three main types of seismic waves produced are P waves, S waves, and surface waves. Volcanoes form when magma reaches the Earth's surface through vents. There are three main types of volcanoes - cinder cones, shield volcanoes, and composite volcanoes - which are determined by the type of eruption and lava. Most earthquakes and volcanic activity occur along three zones - the Ring of Fire around the Pacific Ocean, the Mediterranean zone, and the Mid-Atlantic Ridge.
Dijitha ppt
The document discusses volcanoes and defines key terms. Volcanoes are formed when magma flows from the Earth's interior through fissures caused by plate movement. The vent is where magma exits through fissures to the surface. The crater is the funnel-shaped depression at the volcano's summit. Volcanoes are classified as active, extinct, or dormant based on eruption likelihood. Active volcanoes frequently erupt, extinct volcanoes will not erupt again, and dormant volcanoes erupted previously but could erupt again. In conclusion, while eruptions threaten human life, volcanic areas provide minerals and fertile soil.
volcanoppt-150926053432-lva1-app6892 (1).pdf
The document discusses volcanoes and volcanic activity. It defines volcanoes as vents through which lava, steam, and ashes are expelled from the earth's crust. It notes that volcanoes are commonly located along the Ring of Fire, a belt around the Pacific Ocean. Volcanic eruptions occur when tectonic plates collide and magma breaks through the crust. The document summarizes different types of volcanoes and describes some effects of volcanic eruptions.
Volcano ppt
Volcanoes form when tectonic plates collide and magma rises up through the crust. The document discusses the Ring of Fire around the Pacific Ocean which has many active volcanoes. It also defines key volcanic terms and describes the three main types of volcanoes: shield, composite, and cinder cone volcanoes. The effects of volcanic eruptions on humans and the environment are also summarized.
Volcano
This document discusses volcanoes and their characteristics. It describes the four main types of volcanoes: fissure, cinder cone, shield, and composite. Fissure volcanoes erupt through long vents and produce flood lavas. Cinder cone volcanoes have steep sides and short eruptions producing loose cinders. Shield volcanoes have gentle slopes and erupt fluid basaltic lava over long periods. Composite volcanoes are large mountains that erupt tephra and lava, building their size over millions of years. Volcanoes can be active, dormant, or extinct depending on their recent eruption history, and they produce both primary hazards during eruptions and secondary hazards after.
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Lecture 2 global significance of volcanic activity
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Volcanoes
- 1. Would you like to Visit a Volcano?
- 4. DANGERS OF VOLCANOS The Way that volcanos can be dangerous is from serious hazards Like: • Lava flow • Ash fall • Pyroclastic flow • Climate change Lava is a very hot liquid that can burn people, Ash fall is dangerous because the ashes in the air causes the air to become dirty and harder to breathe, Climate change can harm people because of how fast the climate changes that peoples body are not use to and it can make the extremely ill. But volcanos are less dangerous the earthquakes, tsunamis, and hurricanes
- 5. DIFFERENT TYPE OF VOLCANO ROCKS The different rocks are: • Magma • Igneous • Andesite • Ryolite • Basalt Most of these rocks where made from most the lava with the rocks.
- 6. PARTS OF A VOLCANO