Volcanoes-Enviromental Hazards,Effects and Remedies

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    VOLCANOGroup-8 Presents

    A Q E E L - 0 7S A L A R- 1 7RI A Z - 2 3H A RO O N - 1 2

    SHAMSHAD-02MANNAN-49 ( s )ASAD ( s )

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    VOLCANOGroup-8 Presents

    A Q E E L - 0 7

    S A L A R- 1 7RI A Z - 2 3H A RO O N - 1 2

    SHAMSHAD-02

    MANNAN-49 ( s )ASAD ( s )

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    Volcano

    ---is an opening ora vent through

    which magmaand

    the dissolvedgases in it are.discharged

    Magma ( - )a red hot liquid rock inside the earth

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    CAUSES

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    ,During subduction the subductedoceanic plate is heated as itplunges into the mantle and at

    - ,depth of 80 120 km melting beginsand volcanoes are produced whichare parallel to the subduction.zone

    Subduction zones

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    Hot spots

    Magmas at hot spotsare derived fromdeep within the.mantle

    The magmas are fed bydeep mantle plumeswhich are stationary

    relative to thedrifting tectonic

    .plates

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    Plate tectonics and

    volcanism

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    Global distribution of volcanoes

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    TYPES

    Up to 30 Degree slope

    Less than 10 Degreeslope

    30-40 Degree slope

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    VOLCANIC ERUPTIONS Non-explosive Eruptions Low gas content and low viscosity

    magmas

    basaltic magmas

    If the viscosity is low, non-explosive eruptions usually

    begin with fire fountains due torelease of dissolved gases.

    Lava flows are produced on thesurface and these run likeliquids down slope.

    If the viscosity is high, but the gas

    content is low, then the lavawill pile up over the vent toproduce a lava dome orvolcanic dome.

    Explosive Eruptions High gas content and high

    viscosity

    Andesitic to rhyolitic magmas

    Explosive bursting of bubbles willfragment the magma into clots

    of liquid that will cool as theyfall through the air. These solidparticles becomepyroclasts(meaning - hot fragments) andtephra orvolcanic ash, whichrefer to sand- sizedor smaller

    fragments

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    HAZARDS

    Size of eruptionComposition of eruptionEnvironment of eruption

    Primary hazards:

    Lava flow

    Pyroclastic flows /surges

    Ash and tephra fall

    Gases

    Volcanic earthquakes

    Secondary hazards:

    Lahars & landslides

    Acid rain

    Tsunamis

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    Destroy immobile object in( , )path houses roads Deaths by lava flows are

    ( )uncommon move slowly

    Block roads and highways Bury homes and agriculturalland

    ,Dam rivers change river

    , ,courses kill resident fish

    act as a barrier to.migrating fish

    LAVA FLOWS

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    PYROCLASTS

    , ,Extremely destructive destroy buildings,trees or any objects in their path by,impact burial or fire

    ,On margins of pyroclastic flows death andserious injury to people and animals may

    result from burns and inhalation of hot.ash and gases

    Pyroclastic flows may also interact with.snow and ice to generate lahars

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    Transportation

    BuildingsCommunicationHealth

    Power facilities and distribution systemsAgriculture Waste Water systems

    ASH FALL

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    Ash Transportation

    Poor visibility Airborne ash can obscure

    sunlight to cause

    temporary darkness andreduce visibility to zero During such conditions

    vehicle headlights andbrake lights are often

    ineffective and barelyvisible to other drivers

    Roads & Highways

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    Slippery surface When ash on roads become

    , -wet the mud like mixturecan cause vehicles tolose traction and drivers

    to lose control of.steering

    ,During such conditionsthe braking ability of

    vehicles may besignificantly reduced

    Ash Transportation

    Roads & Highways

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    Road markings covered Ash deposits thicker than about 1 mm will

    obscure or completely cover markings on

    , ,roads that identify lanes road shoulders,direction of travel and instructions to( , ).drivers for example stop or slow

    , When such road markings are not visibledrivers may become confused and

    .disoriented

    Ash Transportation

    Roads & Highways

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    &Abrasive clogging effect on vehicles Brakes and moving parts of vehicles are

    vulnerable to abrasion and clogging from

    . , -ash Also the tiny ash easily clog air,filtration systems on vehicles which canlead to overheating and engine failure

    Ash Transportation

    Roads & Highways

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    -Deposition of material on hot section.components

    -Erosion of compressor blades and rotor path.components

    Blockage of fuel nozzles and cooling.passages -Contamination of the oil system and bleed

    .air supply .Opacity of windscreen and landing lights .Contamination of electronics

    .Erosion of antenna surfaces -Plugging of the pitot static system whichindicates the airspeed of the aircraft

    Ash Transportation

    Aircraft

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    Damage to buildings andbuilding systems fromvolcanic ash can

    range from completeor partial roof

    collapse leading towidespread injuries

    and deaths to lesscatastrophic damage

    of exterior materials,and interior rooms

    including appliances,and computers floor,coverings andelectrical andmechanical systems

    Ash BUILDINGS

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    Electrically charged ash can cause

    interference to radio waves and renderradio and telephone systems inoperative

    Any ash entering telephone exchanges can, ,cause abrasion corrosion or conductivity

    damage to electrical and mechanical

    systems . .During most natural disasters i e volcaniceruption telephone and radio

    communications are susceptible tooverloading by public and emergency.services use

    Ash

    COMMUNICATION

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    nasal irritation ,throat irritation and sore throat sometimes accompanied

    by dry coughing -people with pre existing chest complaints have developed

    severe bronchitic symptoms which lasted some days beyond( , , ,exposure to ash for example cough wheezing or

    )shortness of breath ;airway irritation of people with asthma or bronchitis

    common complaints of people with asthma include, ,shortness of breath wheezing and coughing

    breathing becomes uncomfortable

    Ash HEALTH

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    Eye symptoms eyes feel irritated sticky discharge or tearing corneal abrasions or scratches inflammation of the eye sac that surrounds the eyeball

    , ,due to the presence of ash which leads to redness,burning of the eyes and photosensitivity

    Ash HEALTH

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    Free crystalline silica in volcanic ash Volcanic ash may contain varying proportions of free( , )crystalline silica silicon dioxide SiO2 in the form of

    , , .quartz cristobalite or tridymiteminerals Exposure torespirable particles of free crystalline silica can lead,to silicosis a disease resulting in scarring of the lungs

    .and impairment of their function

    Ash HEALTH

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    . .Ash falls destroy pastures i e no food will be

    available to the livestock -Natural water sources and man made ponds may be

    , -temporarily contaminated by ash and waterpumping equipment can be damaged by the abrasive

    .rock particles Ash falls may be poisonous to livestock and result

    , ,in clinical diseases including hypocalcaemiafluorosis and intestinal damage and secondarymetabolic disorders

    Ash AGRICULTURE

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    Ash from Etna

    volcano on thesurface ofcitrus fruit

    made ituneconomical to

    produce juicebecause it wastoo expensive toclean the fruit

    ( )image courtesy of La Sicilia

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    ( Waste water systems sewage and storm

    )water are vulnerable to damage fromvolcanic ash because the tiny rock,fragments can block pipes and canals

    increase wear on pumps and other-machinery and interfere with water

    .treatment processes

    Ash WASTE WATERSYSTEM

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    ,The different volcanic gases effect the earth

    .people and animals in different ways

    :Some are discussed below Carbon dioxide

    Sulfur dioxide

    Chlorine .Fluorine

    EFFECTS OF VOLCANIC

    GASES

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    Carbon dioxide can add to the effects of global.warming which contributes to the greenhouse effect

    Carbon dioxide behaves like a glass shield over the

    .earth The sun's rays penetrate the carbon dioxide gas butthe carbon dioxide shield prevents heat from

    .escaping into the atmosphere Volcanoes contribute about 110 million tons of carbon

    .dioxide per year

    Carbon dioxide

    (Greenhouse effect)

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    Volcanic eruptions enhance the haze effect to

    ,a greater extent than the greenhouse effectand thus they can lower mean global.temperatures by sulfur dioxide gas

    ,In the cold lower atmosphere it is convertedto sulfuric acid by the sun's rays reacting

    with stratospheric water vapor to form.sulfuric acid aerosol layers The aerosol remains in suspension long after

    solid ash particles have fallen to earthand forms a layer of sulfuric acid droplets

    .between 15 to 25 kilometers up

    Sulfur dioxide Haze effect

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    Chlorine is emitted from volcanoes in the

    ( ),form of hydrochloric acid HCl whichbreaks down into chlorine and chlorine( ) .monoxide ClO molecules

    The sulfate aerosols furnish sites forchemical reactions that release the

    .chlorine atoms The reactive chlorine atoms proceed to

    ,destroy ozone with each chlorine atom being.recycled many times

    Chlorine ozone depletion

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    Fluorine gas can condense in rain or on ash

    particles and coats grass and pollutes.streams and lakes with excess fluorine -Animals that eat grass coated with fluorine

    .tainted ash are poisoned ,Small amounts of fluorine can be beneficial

    ,but excess fluorine causes fluorisis anaffliction that eventually kills animals by.destroying their bones

    Fluorine Fluorisis

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    Acid rain is a rain or any other

    form of precipitation that is,unusually acidic meaning that it

    possesses elevated levels of( ).hydrogen ions low pH

    H2O (l) + CO2 (g) H2CO3 (aq)

    H2O (l) + H2CO3 (aq) HCO3 (aq) + H3O

    + (aq)

    ACID RAIN

    http://en.wikipedia.org/wiki/Hydrogenhttp://en.wikipedia.org/wiki/Oxygenhttp://en.wikipedia.org/wiki/Carbonhttp://en.wikipedia.org/wiki/Oxygenhttp://en.wikipedia.org/wiki/Hydrogenhttp://en.wikipedia.org/wiki/Carbonhttp://en.wikipedia.org/wiki/Oxygenhttp://en.wikipedia.org/wiki/Hydrogenhttp://en.wikipedia.org/wiki/Oxygenhttp://en.wikipedia.org/wiki/Hydrogenhttp://en.wikipedia.org/wiki/Carbonhttp://en.wikipedia.org/wiki/Oxygenhttp://en.wikipedia.org/wiki/Hydrogenhttp://en.wikipedia.org/wiki/Carbonhttp://en.wikipedia.org/wiki/Oxygenhttp://en.wikipedia.org/wiki/Hydrogenhttp://en.wikipedia.org/wiki/Oxygenhttp://en.wikipedia.org/wiki/Oxygenhttp://en.wikipedia.org/wiki/Hydrogenhttp://en.wikipedia.org/wiki/Oxygenhttp://en.wikipedia.org/wiki/Carbonhttp://en.wikipedia.org/wiki/Hydrogenhttp://en.wikipedia.org/wiki/Oxygenhttp://en.wikipedia.org/wiki/Carbonhttp://en.wikipedia.org/wiki/Hydrogenhttp://en.wikipedia.org/wiki/Oxygenhttp://en.wikipedia.org/wiki/Hydrogenhttp://en.wikipedia.org/wiki/Oxygenhttp://en.wikipedia.org/wiki/Carbonhttp://en.wikipedia.org/wiki/Hydrogenhttp://en.wikipedia.org/wiki/Oxygenhttp://en.wikipedia.org/wiki/Carbonhttp://en.wikipedia.org/wiki/Oxygenhttp://en.wikipedia.org/wiki/Hydrogen
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    Soils Soil biology and chemistry can be seriously

    .damaged by acid rain Some microbes are unable to.tolerate changes to low pHs and are killed The

    (enzymes of these microbes are denatured changed

    ) .in shape so they no longer function by the acid The hydronium ions of acid rain also mobilize,toxins such as aluminium and leach away

    essential nutrients and minerals such as.magnesium

    ACID RAIN-

    EFFECTS

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    Forests and other vegetationHigh altitude forests are especially

    vulnerable as they are often surroundedby clouds and fog which are more acidic

    .than rain

    Effect on food crops is minimized bythe application of lime and fertilizers.to replace lost nutrients

    ,In cultivated areas limestone may alsobe added to increase the ability of the

    .soil to keep the pH stable

    ACID RAIN-

    EFFECTS

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    ACID RAIN-

    EFFECTSOther adverse effectsAcid rain can also damage buildings,and historic monuments especially

    those made of rocks such aslimestone and marble containing

    .large amounts of calcium carbonateAcids in the rain react with thecalcium compounds in the stones to

    ,create gypsum which then flakes.off

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    VOLCANO

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    As magma is pushed into a volcano from the magma,chamber below via the magma vent the volcanoinflates causing slopes to become over

    ;steepened and unstable this can result in,larger more explosive eruptions than would

    .otherwise be expected Ground shaking associated with magma ascent can

    .also trigger a collapse Landslides generated during volcanic eruptions at-snow and ice covered volcanoes can be especially

    : ,dangerous As a landslide moves down slope thelarge blocks break into smaller and smaller,pieces when combined with water from melting

    ,snow or ice can transform the landslide into a

    ,debris avalanche carrying it farther than a- .similar sized rock avalanche

    LANDSLIDES AND DEBRIS

    AVALACHES

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    Volcanic earthquakes may be small events detectable

    ,only by instruments or larger events associated.with explosive eruptions They may serve as a useful indicator that a volcano

    ,is coming to life and can be used to help predict.when a volcano may erupt

    Earthquakes large enough for humans to feel may.damage property

    EARTHQUAKES

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    Volcanic eruptions along coastlines can generatetsunamis due to seismic activity or landslides.into water

    ,For example an 1883 eruption of Augustine volcanoin Alaska involved a collapse of a portion of the

    ,volcano into Cook Inlet resulting in a localized.tsunami that was about 15 m high Far greater, , ,damage including about 36 000 deaths was caused

    by the 1883 eruption of the Indonesian volcano,Krakatau which caused massive tsunamis to strike

    .the coasts of nearby Java and Sumatra

    TSUNAMIS

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    Geothermal resources

    Fertile soil Spectacular scenery Tourism

    Positive effect of Volcanoes

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    Volcanoes provide resources for

    ,energy extraction also called.geothermal resources Heat from the earth's crust is being

    .converted to energy The big advantages to this type of

    energy are that it is very cleanand the resources are nearly.inexhaustible

    Geothermal resources

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    When a volcano erupts it throws out a lot of

    .ash At short notice this ash can be very harmful to

    ,the environment but on the long term the ash, ,layer which contains many useful minerals will

    .be converted to a very fertile soil

    Nearly everywhere volcanoes are located people.use the rich soil for farming

    Even after an eruption people still return.because of the fertile soil around the volcano

    Fertile soil

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    Volcanoes can produce

    very spectacularscenery like thebeautiful sunsets

    caused by explosive.eruptions

    Other features include,stunning eruptionsbeautiful lava

    .fountains etc

    Spectacular scenery

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    A big economical

    advantage ofvolcanoes is that

    they generate.tourism

    A country such as

    Hawaii is getting alot income from.tourism

    Tourism

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    Hazard management

    http://volcanoes.usgs.gov/About/What/Monitor/monitor.html
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    -Tiltmeter measures the

    expansion of thevolcano

    -Seismograph determinesearthquakes

    Correlation-spectrometers measures

    amounts of sulfurdioxide

    Remote sensing and GPS

    TOOLS

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    HAZARD MITIGATION

    Awareness of whether the volcano in

    their regions are dorment or active effective warning and evacuation

    procedure

    careful monitoring look out for temperature increase magma releases gases movement of magma produces

    earthquakes and vibrations swelling of volcano's slope

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    ;The most obvious don't build any sort of town

    !around a volcano

    .Spray the oncoming Lava flow with seawater This.was done in Iceland during an eruption in 1983

    Military bombings to divert Lava flows Build walls in the way of the lava to block the

    flow

    Cool lava by breaking down the roof and sides of. ( )the tube feeding the lava flow Not tested yet .Have an evacuation plan .Educating the community / .Dig trenches away from nearby towns villages

    HAZARD MITIGATION

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    Q?Q?Only Few People On Earth Can Say Beautiful Landscapes Their

    Offices,

    We Are One Of Them