Different Types of Volcanic Hazards | DRRR | SHS

Science Simplified
31 Jan 202114:03

Summary

TLDRThis video script delves into the diverse volcanic hazards, teaching viewers to identify and differentiate between them. It covers the common types of eruptions, such as effusive and explosive, and their impacts. The script also discusses various hazards like lava flows, ash fall, pyroclastic flows, lahars, volcanic gases, debris avalanches, ballistic projectiles, and tsunamis, explaining their formation, dangers, and mitigation strategies, particularly emphasizing the importance of understanding these phenomena for community safety.

Takeaways

  • πŸŒ‹ The video discusses various types of volcanic hazards and aims to help viewers differentiate among them.
  • πŸ” The learning outcomes include identifying common volcano-related hazards in the Philippines and understanding the differences between various hazards.
  • πŸ—Ί The script mentions several Philippine volcanoes, including Pinatubo and Mayon, with a focus on Taal's Beninteyang Malaki crater.
  • ⚠️ Volcanic eruptions can have negative impacts such as destruction of properties, injuries, and displacement of people.
  • πŸŒͺ The video distinguishes between effusive (quiet) and explosive (violent) eruptions, with examples provided.
  • πŸ’₯ Volcanic hazards include lava flows, which can bury, crush, cover, and burn everything in their path.
  • 🌫 Ash fall, or tephra fall, can cause low visibility, slippery roads, and damage to crops, machinery, and buildings.
  • πŸ”₯ Pyroclastic flows and surges are highly destructive due to their mass, high temperature, and velocity.
  • 🌊 Lahars are rapidly flowing mixtures of volcanic sediments and water, which can destroy infrastructure and bury communities.
  • πŸ’¨ Volcanic gases, such as sulfur dioxide, carbon dioxide, and hydrogen sulfide, pose hazards to health and the environment.
  • 🏞 Debris avalanches or volcanic landslides can result from volcanic collapse, affecting the surrounding areas.
  • πŸš€ Ballistic projectiles are ejected materials that can endanger life and property near the eruption site.
  • 🌊 The video also touches on tsunamis, which are generated by sudden displacement of water and can be related to volcanic activity.

Q & A

  • What are the learning competencies and outcomes discussed in the video script?

    -The learning competencies are to explain various volcano-related hazards and differentiate among different volcano hazards. The specific learning outcomes include identifying the most common volcano-related hazards in the Philippines and explaining the differences of the various volcano-related hazards.

  • Which volcanoes in the Philippines are mentioned in the script?

    -The script mentions Pinatubo and Ta'al as examples of volcanoes in the Philippines.

  • What is the difference between a crater and a volcano in the context of the script?

    -A crater is a bowl-shaped depression or vent through which volcanic materials are expelled, often forming part of a volcano. A volcano is a geological structure that vents molten rock, ash, and gases to the Earth's surface, which can include multiple craters.

  • What are the two types of volcanic eruptions described in the script?

    -The two types of volcanic eruptions described are effusive or quiet eruptions, where lava flows out of the volcano, and explosive or violent eruptions, where magma is blown into fragments.

  • What are volcanic hazards and why are they considered hazardous?

    -Volcanic hazards are phenomena arising from volcanic activity that pose potential threats to people or property. They are hazardous due to their potential to cause destruction, displacement, and various negative impacts depending on the type of volcanic activity.

  • How does the script differentiate between lava and magma?

    -The script differentiates by stating that magma is the molten rock inside the volcano, and it becomes lava when it reaches the surface.

  • What are the negative impacts of lava flows as described in the script?

    -Lava flows can bury, crush, cover, and burn everything in their path. They can also block bridges and highways, affecting mobility and accessibility. Additionally, viscous lava domes can trigger dangerous pyroclastic flows.

  • What is ash fall and why is it hazardous?

    -Ash fall, also known as tephra fall, is the shower of airborne volcanic particles that fall out from the plumes of volcanic eruptions. It is hazardous due to causing poor visibility, slippery roads, loss of agricultural lands, clogging filters and vents, and carrying harmful gases, acids, and salts.

  • What are pyroclastic flows and surges, and why are they considered highly destructive?

    -Pyroclastic flows are turbulent masses of ejected fragmented volcanic materials mixed with hot gases that flow downslope at high speeds. Pyroclastic surges are more dilute derivatives of pyroclastic flows. They are highly destructive due to their mass, high temperature, high velocity, and great mobility.

  • What are lahars and how do they impact the surrounding areas?

    -Lahars are rapidly flowing mixtures of volcanic sediments and water, often triggered by intense rainfall. They can destroy by direct impact, damage infrastructure, block tributary streams, bury valleys and communities with debris, and lead to long-term flooding problems.

  • What are the different types of volcanic gases mentioned in the script, and why are they hazardous?

    -The script mentions water vapor, carbon dioxide, sulfur dioxide, hydrogen sulfide, and hydrogen chloride as volcanic gases. They are hazardous because sulfur dioxide can lead to acid rain, high concentrations of carbon dioxide can be lethal, and fluorine compounds can deform and kill animals.

  • What is a debris avalanche or volcanic landslide, and how does it impact the surrounding areas?

    -A debris avalanche or volcanic landslide is a massive collapse of a volcano, often triggered by an earthquake or volcanic eruption. It can have a significant negative impact by causing slope failure, creating an amphitheater-like feature at the base of the volcano, and affecting the surrounding areas with debris.

  • What are ballistic projectiles and how do they pose a threat?

    -Ballistic projectiles are volcanic materials directly ejected from the volcano with force and trajectory. They pose a threat by endangering life and property through the force of impact and falling fragments, typically occurring close to an eruption site.

  • How are tsunamis related to volcanic activity as mentioned in the script?

    -Tsunamis, as mentioned in the script, are sea waves or trains generated by sudden displacement of water, which can be related to volcanic activity, such as undersea volcanic eruptions or landslides caused by volcanic events.

Outlines

00:00

πŸŒ‹ Types of Volcanic Hazards and Their Impacts

This paragraph introduces the video's focus on various volcanic hazards, aiming to explain and differentiate them. It outlines the learning objectives, including identifying common hazards in the Philippines and understanding their differences. The paragraph also mentions specific volcanoes, such as Pinatubo and Taal, and discusses the 2020 Taal eruption. It distinguishes between effusive and explosive eruptions and their respective impacts, such as destruction of properties and displacement of people.

05:01

πŸ”₯ Lava Flows and Ash Fall Hazards

The second paragraph delves into the specifics of lava flows, explaining the difference between magma and lava, and the formation of lava domes. It details the slow movement and potential hazards of lava, including the destruction and burial of property and vegetation. The paragraph then discusses ash fall, which consists of fine to coarse volcanic particles, and its hazards, such as reduced visibility, slippery roads, and damage to crops, buildings, and machinery. It also touches on the dangers of ash to aviation and the potential for ash to carry harmful substances.

10:01

πŸ’¨ Pyroclastic Flows, Lahars, and Other Volcanic Phenomena

This paragraph covers the dangers of pyroclastic flows and surges, which are high-speed, high-temperature mixtures of volcanic materials and gases. It explains the destructive potential of these phenomena and the importance of evacuation as a mitigation strategy. The paragraph also addresses lahars, which are mudflows composed of volcanic debris and water, and their ability to cause significant damage to infrastructure and communities. Additionally, it mentions volcanic gases, their composition, and their potential to cause acid rain and other environmental issues. The paragraph concludes with a discussion on debris avalanches, volcanic landslides, ballistic projectiles, and tsunamis, all of which can result from volcanic activity.

Mindmap

Keywords

πŸ’‘Volcanic Hazards

Volcanic hazards refer to the various dangers that arise from volcanic activity, posing threats to people and property. In the video's context, they are the central theme, encompassing a range of phenomena such as lava flows, ash fall, and pyroclastic flows. The script discusses different types of volcanic hazards and their impacts, such as the destruction of properties and displacement of people.

πŸ’‘Effusive Eruption

An effusive eruption is characterized by the outflow of lava from a volcano, typically occurring when the magma has low viscosity and gas content, allowing it to flow smoothly. The script mentions this type of eruption as one of the two main eruption styles, contrasting it with the more violent explosive eruptions, and explains that it is less likely to threaten human life due to the slow movement of lava.

πŸ’‘Explosive Eruption

An explosive eruption occurs when magma is blown into fragments due to high gas pressure, often resulting in a violent release of energy. The video script uses this term to describe a type of volcanic eruption that is more hazardous due to the potential for widespread destruction from the ejected materials and the generation of pyroclastic flows.

πŸ’‘Lava Flows

Lava flows are streams of molten rock that emerge from a volcanic eruption. The script explains that while lava flows are not typically a direct threat to human life due to their slow movement, they can cause significant damage by burying, crushing, and burning everything in their path, as well as blocking transportation routes and rendering affected areas useless.

πŸ’‘Ash Fall

Ash fall, also known as tephra fall, is the phenomenon where fine-grained volcanic particles are dispersed through the air and settle on the ground. The video script describes ash fall as a hazard due to its potential to reduce visibility, make roads slippery, damage crops, and clog machinery and respiratory systems. It also mentions the example of the ash fall from the Taal volcano eruption.

πŸ’‘Pyroclastic Flows

Pyroclastic flows are fast-moving, high-temperature currents of hot gas and volcanic matter that move downhill from a volcano. The script highlights their destructive nature, capable of incinerating and crushing everything in their path. The only effective mitigation strategy mentioned is evacuation, emphasizing the extreme hazard they pose.

πŸ’‘Lahars

Lahars are mudflows or debris flows composed of a slurry of pyroclastic material, rocky debris, and water. The video script discusses lahars as a significant hazard, particularly in areas where people live in valleys prone to lahar flows. It cites the 1991 Pinatubo eruption as an example where lahars caused extensive damage and loss of life.

πŸ’‘Volcanic Gases

Volcanic gases are various compounds released by volcanic activity, including water vapor, carbon dioxide, and sulfur dioxide. The script explains that these gases can pose a range of hazards, from acid rain to asphyxiation, and can also damage vegetation and animal life. Sulfur dioxide is specifically highlighted as a dangerous gas that can lead to the formation of sulfuric acid.

πŸ’‘Debris Avalanche

A debris avalanche is a massive landslide of volcanic material, often triggered by seismic activity or eruptions. The video script uses the term to describe a type of volcanic hazard that can have severe impacts, such as the creation of an amphitheater-like feature at the base of a volcano, as seen in the case of Mount Saint Helens in 1980.

πŸ’‘Ballistic Projectiles

Ballistic projectiles are chunks of volcanic material that are forcefully ejected from a volcano and follow a ballistic trajectory. The script mentions these as a hazard close to the eruption site, capable of causing damage and injury due to the impact of falling fragments.

πŸ’‘Tsunami

A tsunami is a series of large ocean waves caused by the sudden displacement of water, often associated with undersea earthquakes or volcanic eruptions. While not the primary focus of the script, the term is mentioned in the context of volcanic activity, such as when a volcanic eruption causes a landslide that displaces a significant volume of water.

Highlights

Introduction to different types of volcanic hazards and the learning competencies to explain and differentiate them.

Identification of the most common volcano-related hazards in the Philippines, including Pinatubo and Mayon.

Explanation of complex volcanoes, their craters, and how eruptions can transfer between them, exemplified by Ta'al Volcano.

Discussion on the 2020 eruption of Ta'al's main crater and the confusion regarding its location.

Illustration of the negative impacts of volcanic eruptions, such as destruction of properties and displacement of people.

Differentiation between effusive (quiet) and explosive (violent) volcanic eruptions with examples.

Definition of volcanic hazards as phenomena arising from volcanic activity that pose threats to people or property.

Description of lava flows, their formation, and the distinction between magma and lava.

Impacts of lava flows, including burying, crushing, covering, and burning everything in their path.

Introduction to ash fall or tephra fall, its causes, and its distribution dependent on wind direction.

Hazardous effects of ash fall, such as poor visibility, slippery roads, and damage to crops and machinery.

Explanation of pyroclastic flows and surges, their formation, and their high destructive potential.

The importance of evacuation as a mitigation strategy for pyroclastic flows and surges.

Lahars, their formation, and the long-term problems they can cause, such as flooding and sediment deposition.

Volcanic gases, their composition, and the hazards they pose to the environment and human health.

Debris avalanches or volcanic landslides, their triggers, and the resulting negative impacts.

Ballistic projectiles, their definition, and the dangers they pose to life and property near eruption sites.

Tsunamis, their generation by sudden displacement of water, and their relevance to volcanic activity.

Transcripts

play00:00

in this video we're going to talk about

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the different types of volcanic hazards

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the learning competencies are to explain

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various volcano related hazards

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and to differentiate among different

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volcano hazards

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now the specific learning outcomes are

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the following identify the most

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common volcano related hazards in the

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philippines

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and explain the differences of the

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various volcano related hazards

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now let's start with a discussion about

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volcanoes i hope you can name

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some of the volcanoes here in the

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philippines we have pinatubo

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and others okay now let's focus on

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volcano which you can see in this

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picture

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the volcano is a complex volcano which

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is made

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up of a lot of craters these craters are

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formed

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because of eruptions we have

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so eruptions since we have a lot of

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craters

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may transfer from one creator to another

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so in the books what you see is the

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beninteyang

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malaki crater of ta'al this is because

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it's the most

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visible at the highest part of the al in

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tagaytay

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so this 2020 the main crater erupted

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that's why most people were confused

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about the exact location of maybe some

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of you know some volcanic eruptions that

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happen in the philippines

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right we have mount pinatubo last june

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1991

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mount mayon in these years and the

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volcano

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1991 1965 and the latest

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last year 2020 this figure

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shows a lightning strike a style volcano

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spews columns of ashes

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as seen from the kaitai city so what are

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the negative

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impacts of an eruption i think we should

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have that conversation

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so we have destruction of properties

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that's an

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injuries displacement of people

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so those are the things that we're going

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to study

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later so this figure shows the al

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volcano erupting

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so you can see it's the main crater and

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not the most

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visible crater which is the benin

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now this two figures show eruptions of

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mount mayon i hope you can see the

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difference

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but this figures actually show the two

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types of volcanic eruption

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we have the effusive or quiet eruption

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and explosive or violent eruption

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so just to give you an overview it is an

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effusive eruption if

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lava is flowing out of the volcano and

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it is a violent

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eruption if the magma has been blown to

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pieces

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so what are volcanic hazards volcanic

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hazards are phenomena arising from

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volcanic activity

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that pose potential threat to people or

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property

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in a given area within a given period of

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time

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so let's discuss the different volcanic

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phenomena

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the negative impacts and the reason why

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they are hazardous

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to make it easier for you to take down

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notes please make a table

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like this so you have two columns and

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you just keep

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adding rows okay now let's start with

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the first volcanic phenomenon

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which are the lava flows okay lava flows

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are stream-like flows of incandescent

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molten rock

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erupted from a crater or fisher

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now please do not confuse lava and magma

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when we say magma we refer to the molten

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rock

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that is still inside the volcano it will

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become

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lava when it reaches the surface of the

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volcano

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okay now when a lava is the gas meaning

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removed of dissolved gases

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and or very viscous it tends to extrude

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extremely slowly

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forming lava domes okay so this picture

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is from the 1969 volcanic eruption

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in hawaii so what are the negative

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impacts

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so lava flows rarely threaten human life

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because

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lava usually moves slowly okay

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so silicic flow is about few centimeters

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per

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hour and for basaltic flow it's about

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several kilometers per hour we have a

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lot of hazards here we have burying

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crushing covering burning everything in

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their path

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okay lavas can burn so the intense heat

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of lavas

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melt and burn so the areas it covers are

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burnt

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okay it can also bury can vary homes

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and agricultural areas under meters of

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hardened rock

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areas affected by lava flows once

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solidified

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are also rendered useless this is

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because of the nature of lava deposit

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lavas can also block bridges and

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highways

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affecting mobility and accessibility of

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people

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and communities okay collapsing viscous

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lava domes can trigger dangerous

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pyroclastic flows

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which we are going to study later on

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okay but you have to know that

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a pyroclastic flow is a dense fast

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moving flow of solidified lava pieces

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as well as volcanic ash and hot gases as

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you can see

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in this picture next volcanic hazard is

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ash fall or death rafale

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so ash fall or tephra fall are showers

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of airborne

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fine to coarse grained volcanic

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particles that

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fall out from the plums of volcanic

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eruption

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asphalt distribution is dependent on the

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prevailing wind

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direction as you can see in this diagram

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so why is it hazardous during peak of

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eruption

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the excessive ash can cause poor or low

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visibility

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so it will be dangerous for people who

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are driving

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and the roads will be slippery

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it will also resort to a loss of

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agricultural lands

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especially if burial by asheville is

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greater than 10 centimeters

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depth this also produces suspensions of

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fine grained particles in air and water

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which clogs the filter and vents of

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motors

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human lungs industrial machines and

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nuclear power plants so ash

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suspended in the air is also dangerous

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for aircrafts

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as the abrasive ash can cause the

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engines to fail if the suspended ash

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is encountered by the airplane of course

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alongside with it

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is the poor visibility okay

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this asheville also carry harmful gases

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acids and salts okay so burial by tefra

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can collapse

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roofs of buildings break power and

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communication lines and damage or kill

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vegetation okay so even

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less than two centimeters of ash can

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damage

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such critical facilities as hospitals

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electric generating plants pumping

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stations storm sewers

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and more so the pictures that i'm going

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to show you are taken from the alpha

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queen

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eruption last year

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as you can see here so this vegetation

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near the side of the volcano

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is print this one shows a man or a

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resident

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cleaning ash from his roof so this

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figure shows the roofs of homes

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in takaytai on january 14.

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next hazard is the pyroclastic flows

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and surges so this figure shows a

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pyroclastic flow races

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down the flanks of mount merapi in

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indonesia

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during the volcanic event in 2006.

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pyroclastic flows or also called the

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spiroclastic density current

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are turbulent mass of ejected fragmented

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volcanic materials

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or ash and rocks mixed with hot gases

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that flow downslope at very high speeds

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okay so pyroclastic surges on the other

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hand are the more dilute or more mobile

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derivatives

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of pyroclastic flows so why are they

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hazardous

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pyroclastic flows and surges are

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potentially highly destructive

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due to their mass high temperature high

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velocity

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and great mobility so pyroclastic flows

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can destroy

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anything on its path by direct impact

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they can burn sights with hot rock

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debris

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and burnt forest farmlands destroy crops

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and buildings

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that the effects include affixiation

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burial incineration

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and crushing from impacts now the only

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effective method of prism mitigation

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is of course evacuation prior to such

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eruptions

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from areas likely to be affected by

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pyroclastic density

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currents next hazard are the

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lahars lahars are rapidly flowing thick

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mixture of volcanic sediments

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from pyroclastic materials and water

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okay so this is usually triggered by

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intense rainfall

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during typhoons monsoons and

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thunderstorms

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the hearts can occur immediately after

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an eruption

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or it can become long-term problem if

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there is

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voluminous pyroclastic materials erupted

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one example is the case of 1991 pinatubo

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eruption the hearts can also occur after

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an eruption has taken place

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such as the lahars at the mayon volcano

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after the 1984

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eruption okay so the hearts have

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destroyed many villages

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and lives living on pinatubo and my own

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volcano

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because most people live in valleys

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where lahars

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flow so what are the negative impacts

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the hearts can destroy by direct impact

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so it can prove in or damage bridges

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roads and houses the hearts can also

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block tributary stream

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and then form a lake so when we say

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tributary it is a fresh water stream

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that feeds into a larger stream or river

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so this

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event can submerge villages within the

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valley

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of the tributary that was blocked the

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hearts can also bury valleys and

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communities with

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debris basically it can lead to

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increased deposition of sediments

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along affected rivers and result to

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long-term flooding problems

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in the low-lying downstream communities

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such as

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this picture next we have the volcanic

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gases

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these are gases and aerosols released

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into the atmosphere

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which include water vapor carbon dioxide

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sulfur

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hydrogen sulfide and hydrogen chloride

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this table shows the percentage of gases

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in the atmosphere

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so these are some of the volcanic gases

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that pose

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hazard to people animals agriculture

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and properties other gases include

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carbon disulfide

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carbonyl sulfide and hydrogen fluoride

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so one of the most dangerous gases here

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is the sulfur dioxide sulfur dioxide can

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lead to acid grain

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when it mixed to oxygen and form sulfur

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trioxide

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now this sulfur trioxide will react with

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water from

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the rain to form sulfuric acid

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so high concentrations of carbon dioxide

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which is color less and other less can

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be lethal to people

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animals and vegetation as well as

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fluorine compounds they can deform and

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kill animals that

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rest on vegetation covered with volcanic

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ash

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next hazard is debris avalanche or

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volcanic landslide

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so this is a massive collapse of a

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volcano

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usually triggered by an earthquake or

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volcanic eruption

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okay so an example of recent debris

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avalanche event

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occurred during the 1980 eruption of

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mount saint helens now in the

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philippines

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we have some volcanoes too based on the

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present morphology of some volcanoes

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here

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for example the iriga volcano and

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camarina sewer

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and the banajo volcano in castle

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province they had prehistoric debris

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avalanche events

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so this will have a negative impact

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especially when a huge portion of the

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site of a volcano collapses

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due to slope failure so how did

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volcanologists and geologists know that

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a debris avalanche happened

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so huge volcanic debris avalanches

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typically

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live an amphitheater like feature at the

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base of volcanoes

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with debris avalanche effect okay as you

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can see

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here okay next we have the ballistic

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projectiles

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ballistic projectiles are volcanic

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materials directly ejected from the

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volcanoes event

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with force and trajectory so ballistic

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projectiles endanger

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life and property by the force of impact

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of falling fragments

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but this only occurs close to an

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eruption

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bent as you can see in this figure this

play13:31

rock actually fell

play13:32

and it's bigger than a shovel lastly we

play13:35

have

play13:36

the tsunami which you are very familiar

play13:39

with

play13:39

because we have discussed this in the

play13:41

previous video

play13:43

so tsunami again are sea waves or trains

play13:46

that are generated by sudden

play13:48

displacement of

play14:00

water

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Related Tags
Volcanic HazardsPhilippinesEruptionsLava FlowsAshfallPyroclastic FlowsLaharsVolcanic GasesDebris AvalancheBallistic ProjectilesTsunamis