Tectonic theory & Tectonic hazards

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What are the layers of the earth?

Inner core, outer core, lower mantle, upper mantle (asthenosphere), lithosphere, the crust (top of the lithosphere)

<p>Inner core, outer core, lower mantle, upper mantle (asthenosphere), lithosphere, the crust (top of the lithosphere)</p>
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Describe the inner core:

  • solid ball of iron/nickel

  • under huge amount of pressure as it has the weight of the whole Earth pushing against it - causes it to remain solid

  • within it, radioactive elements like uranium & thorium are decaying - radioactive decay gives off lots of heat

  • over 5000°C - responsible for Earth’s internal energy - spreads throughout the different layers

  • about 1400km in diameter

<ul><li><p><strong>solid</strong> ball of<mark data-color="green" style="background-color: green; color: inherit"> iron/nickel</mark></p></li><li><p>under <mark data-color="green" style="background-color: green; color: inherit">huge amount of pressure</mark> as it has the <strong>weight </strong>of the <strong>whole Earth </strong><mark data-color="green" style="background-color: green; color: inherit">pushing against it</mark><strong> - </strong>causes it to <strong><mark data-color="green" style="background-color: green; color: inherit">remain solid</mark></strong></p></li><li><p>within it,<mark data-color="green" style="background-color: green; color: inherit"> radioactive elements </mark>like <strong>uranium </strong>&amp; thorium are <mark data-color="green" style="background-color: green; color: inherit">decaying </mark>- radioactive decay<mark data-color="green" style="background-color: green; color: inherit"> gives off lots of heat</mark></p></li><li><p><strong><mark data-color="green" style="background-color: green; color: inherit">over </mark></strong><mark data-color="green" style="background-color: green; color: inherit">5000°C - </mark><strong>responsible </strong>for <mark data-color="green" style="background-color: green; color: inherit">Earth’s internal energy</mark> - <strong>spreads </strong>throughout the <mark data-color="green" style="background-color: green; color: inherit">different layers</mark></p></li><li><p>about<strong> 1400km </strong>in <mark data-color="green" style="background-color: green; color: inherit">diameter</mark></p></li></ul><p></p>
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Describe the outer core:

  • molten (liquid) layer of iron & nickel - surrounds inner core

  • heat from inner core creates convection currents in outer core - transfers heat to mantle

  • about 2100km thick

  • temperatures between 4000 - 6000°C

<ul><li><p><mark data-color="green" style="background-color: green; color: inherit">molten </mark>(liquid) layer of<mark data-color="green" style="background-color: green; color: inherit"> iron &amp; nickel -</mark> surrounds inner core</p></li><li><p><strong>heat from </strong><mark data-color="green" style="background-color: green; color: inherit">inner core </mark>creates<mark data-color="green" style="background-color: green; color: inherit"> convection currents in outer core</mark> - transfers <mark data-color="green" style="background-color: green; color: inherit">heat to mantle</mark></p></li><li><p>about<strong> 2100km thick</strong></p></li><li><p>temperatures between <mark data-color="green" style="background-color: green; color: inherit">4000 - 6000°C</mark></p></li></ul><p></p>
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Describe the mantle:

  • largest layer of the Earth - about 2900km thick

  • semi-molten - mainly solid rock apart from very top, where it behaves like a very dense fluid

  • split into two parts - lower mantle & upper mantle

  • upper mantle has two layers - rigid upper layer(part of lithosphere) and the asthenosphere

<ul><li><p><mark data-color="green" style="background-color: green; color: inherit">largest la</mark>yer of the Earth - about<mark data-color="green" style="background-color: green; color: inherit"> 2900km thick</mark></p></li><li><p><strong>semi-molten </strong>- <strong>mainly<mark data-color="green" style="background-color: green; color: inherit"> </mark></strong><mark data-color="green" style="background-color: green; color: inherit">solid rock</mark> apart from <strong>very top</strong>, where it<mark data-color="green" style="background-color: green; color: inherit"> behaves like a very dense fluid</mark></p></li><li><p>split into<strong> two parts </strong>- <mark data-color="green" style="background-color: green; color: inherit">lower </mark>mantle &amp; <mark data-color="green" style="background-color: green; color: inherit">upper </mark>mantle</p></li><li><p><strong>upper </strong>mantle has<mark data-color="green" style="background-color: green; color: inherit"> two layers </mark>- <mark data-color="green" style="background-color: green; color: inherit">rigid upper layer</mark>(part of <strong>lithosphere)</strong> and the <strong>asthenosphere</strong></p></li></ul><p></p>
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What is the asthenosphere?

The semi-molten top layer of the mantle which flows due to convection currents, moving the solid lithosphere above. Between 35-250km

<p>The <mark data-color="green" style="background-color: green; color: inherit">semi-molten top layer </mark>of the mantle which <mark data-color="green" style="background-color: green; color: inherit">flows due to </mark><strong><mark data-color="green" style="background-color: green; color: inherit">convection currents</mark></strong><mark data-color="green" style="background-color: green; color: inherit">, </mark><strong>moving </strong>the<mark data-color="green" style="background-color: green; color: inherit"> solid lithosphere above</mark>. Between<mark data-color="green" style="background-color: green; color: inherit"> 35-250km</mark></p>
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Describe the lithosphere:

  • solid rock layer that lies on top of asthenosphere

  • majority of lithosphere is technically in the mantle, very top is the Earth’s crust

  • crust is split into tectonic plates - range in thickness

<ul><li><p><mark data-color="green" style="background-color: green; color: inherit">solid rock layer </mark>that lies <strong>on top</strong> of <strong>asthenosphere</strong></p></li><li><p><strong>majority </strong>of lithosphere is<mark data-color="green" style="background-color: green; color: inherit"> technically in the ma</mark>ntle,<strong> very top</strong> is the <mark data-color="green" style="background-color: green; color: inherit">Earth’s crust</mark></p></li><li><p>crust is<mark data-color="green" style="background-color: green; color: inherit"> split into tectonic plates </mark>- <strong>range </strong>in thickness</p></li></ul><p></p>
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What are the two kinds of crust?

  • Oceanic crust

  • Continental crust

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What is the oceanic crust?

The crust that makes up the ocean floor - younger (still very old), denser and thinner(5-10km). It is composed mainly of basalt.

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What is the continental crust?

The crust that makes up our land - old, less dense & thick (25-100km). It is mainly composed of granite.

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Why is oceanic crust continually being created and destroyed?

Because of plate movement where it is denser than the continental crust and therefore subducts under the continental crust.

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What is the heat within the Earth generated by?

Radioactive decay.

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What are tectonic plates?

Large slabs of the Earth’s crust that sit and move on top of the liquid mantle.

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Describe how convection currents cause plate movement:

Energy from radioactive decay in the core heats up the fluid asthenosphere, this hot liquid is less dense than its surroundings, so it rises upwards. Upon reaching the top it cools and becomes more dense, therefore sinking back down to the bottom where it is heated up again, and the cycle continues. The plates, which lie on top, are pushed & pulled by the convection currents on the asthenosphere.

<p><mark data-color="green">Energy </mark>from<mark data-color="green"> radioactive decay</mark> in the <mark data-color="green">core heats up the fluid asthenosphere</mark>, this hot liquid is<mark data-color="green"> less dense</mark> than its surroundings, so it <mark data-color="green">rises upwards</mark>. Upon <mark data-color="green">reaching the top it cools </mark>and becomes<mark data-color="green"> more dense</mark>, therefore <mark data-color="green">sinking back down</mark> to the bottom where it is <mark data-color="green">heated up again,</mark> and the<mark data-color="green"> cycle continues</mark>. The plates, which <mark data-color="green">lie on top</mark>, are <mark data-color="green">pushed &amp; pulled</mark> by the<mark data-color="green"> convection currents</mark> on the <mark data-color="green">asthenosphere</mark>.</p>
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Describe the slab pull theory:

In addition to convection currents, plate movement is a result of the weight of denser oceanic plates subducting and dragging the rest of the plate along.

<p>In addition to <mark data-color="green">convection currents</mark>, plate movement is a result of the <mark data-color="green">weight of denser oceanic plates</mark> <mark data-color="green">subducting </mark>and <mark data-color="green">dragging </mark>the<mark data-color="green"> rest of the plate along.</mark></p>
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How many large tectonic plates is Earth’s crust broken into?

15

<p>15</p>
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What plate is North America in?

North American plate.

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What plate is Asia in?

Eurasian plate.

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What is a plate boundary?

The point at which two plates meet.

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What was Wegener’s theory of continental drift?

That all land masses were once one supercontinent called Pangaea that split off to form today’s continents.

<p>That <mark data-color="green">all land masses</mark> were once one <mark data-color="green">supercontinent</mark> called <mark data-color="green">Pangaea </mark>that split off to form today’s continents. </p>
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What was the evidence for Wegener’s theory?

  • The outlines of the continents fit together like a jigsaw. e.g. there is a match in shape between the east coast of South America & the west coast of Africa

  • There are similar patterns of rocks on both sides of the Atlantic

  • There are similar fossils on both sides of the Atlantic - including fossils of land animals that would have been unable to swim across from one side to the other

<ul><li><p>The <mark data-color="green">outlines of the continents fit together</mark> like a <mark data-color="green">jigsaw</mark>. e.g. there is a match in shape between the <mark data-color="green">east coast of South America</mark> &amp; the <mark data-color="green">west coast of Africa</mark></p></li><li><p>There are<mark data-color="green"> similar patterns of rocks on both sides of the Atlantic</mark></p></li><li><p>There are<mark data-color="green"> similar fossils on both sides of the Atlantic </mark>- including<mark data-color="green"> fossils of land animals</mark> that would have been <mark data-color="green">unable to swim across</mark> from one side to the other</p></li></ul>
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What are the three main type of plate boundaries?

  1. Divergent

  2. Convergent

  3. Conservative

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Divergent plate boundary movement:

Plates move away from each other.

<p>Plates move <mark data-color="green">away </mark>from each other.</p>
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Convergent plate boundary movement:

Plates move towards each other.

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Conservative plate boundary movement:

Plates move alongside each other.

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What is an earthquake?

The sudden, violent shaking of the ground as a result of pressure building when tectonic plates move.

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What is the focus?

The point where the earthquake starts below the Earth’s surface - the energy released by the earthquake travels out from the focus.

<p>The <strong>point</strong> where the<mark data-color="green" style="background-color: green; color: inherit"> earthquake </mark><strong><mark data-color="green" style="background-color: green; color: inherit">starts below </mark></strong><mark data-color="green" style="background-color: green; color: inherit">the Earth’s surface</mark> - the <strong><mark data-color="green" style="background-color: green; color: inherit">energy </mark>released </strong>by the earthquake<mark data-color="green" style="background-color: green; color: inherit"> travels </mark><strong><mark data-color="green" style="background-color: green; color: inherit">out </mark></strong><mark data-color="green" style="background-color: green; color: inherit">from the focus.</mark></p>
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What is the epicentre?

The point on the Earth’s surface directly above the focus.

<p>The <strong>point </strong>on the <mark data-color="green" style="background-color: green; color: inherit">Earth’s surfac</mark>e <strong>directly above </strong>the <mark data-color="green" style="background-color: green; color: inherit">focus</mark>.</p>
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What scale is the magnitude of an earthquake measure on?

The Richter Scale.

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How does the Richter Scale work?

The scale is logarithmic, which means that each number in the scale is 10x bigger than the last.

e.g. a 5.0 magnitude earthquake is 10x stronger/bigger than a 4.0 magnitude earthquake

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What device is used to measure the magnitude of an earthquake?

Seismometer.

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What scale is the damage caused by an earthquake measured on?

The Mercalli Scale.

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What hazards can occur at divergent plate boundaries?

Volcanic eruptions and Earthquakes.

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What happens at a divergent boundary to form hazards?

When the two plates are pulled apart, magma rises between the gap left by the two plates separating. Lava then pours out onto the surface - volcanoes form in the areas where lava pours out & the lava is usually runny & free-flowing creating flatter volcanoes. Earthquakes also occur here as plates shake & vibrate when plates move apart.

<p>When the two plates are <mark data-color="green">pulled apart</mark>, <mark data-color="green">magma rises </mark>between the <mark data-color="green">gap</mark> left by the two plates separating. <mark data-color="green">Lava then pours out onto the surface </mark>- <mark data-color="green">volcanoes </mark>form in the areas <mark data-color="green">where lava pours out</mark> &amp; the lava is usually <mark data-color="green">runny &amp; free-flowing</mark> creating <mark data-color="green">flatter volcanoes.</mark> <mark data-color="green">Earthquakes </mark>also occur here as<mark data-color="green"> plates shake &amp; vibrate </mark>when<mark data-color="green"> plates move apart.</mark></p>
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What is sea floor spreading?

When new land is formed on the ocean floor due to a divergent plate boundary on oceanic crust. Causes the floor to spread and get wider.

<p>When <mark data-color="green">new land is formed on the ocean floor</mark> due to a<mark data-color="green"> divergent plate boundary </mark>on<mark data-color="green"> oceanic crust.</mark> Causes the <mark data-color="green">floor to spread and get wider.</mark></p>
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What do divergent plate boundaries cause on continental crust?

They cause huge fractures in the land, creating lowland regions called rift valleys.

e.g. the East African Rift

<p>They cause <mark data-color="green">huge fractures </mark>in the land, creating<mark data-color="green"> lowland regions</mark> called <mark data-color="green">rift valleys. </mark></p><p>e.g. the East African Rift</p>
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What is an example of a divergent plate boundary?

The Mid Atlantic Ridge.

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What hazards can occur at convergent plate boundaries?

Strong, deep earthquakes and explosive volcanoes.

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What happens at a convergent boundary to form hazards?

The plates move towards each other and the denser oceanic crust is subducted below the continental crust. The plate that is subducting leaves a deep ocean trench. Friction between the two plates causes strong & deep earthquakes. The oceanic crust is melted as it is pulled deeper into the mantle, creating magma. This magma causes pressure to build up under the crust and eventually the magma pushes out through weaknesses in the crust - creating explosive volcanoes.

<p>The plates <mark data-color="green">move towards each other</mark> and the <mark data-color="green">denser oceanic crust is subducted </mark>below the continental crust. The plate that is <mark data-color="green">subducting leaves a deep ocean trench</mark>. <mark data-color="green">Friction </mark>between the <mark data-color="green">two plates causes strong &amp; deep earthquakes. </mark>The <mark data-color="green">oceanic crust is melted </mark>as it is <mark data-color="green">pulled deeper into the mantle</mark>, creating <mark data-color="green">magma</mark>. This <mark data-color="green">magma causes pressure to build up under the crust</mark> and eventually the <mark data-color="green">magma pushes out through weaknesses</mark> in the <mark data-color="green">crust </mark>- creating <mark data-color="green">explosive volcanoes.</mark></p>
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What happens when two oceanic plates converge?

The denser plate sinks below and islands in the ocean can form. e.g. Mariana trench.

<p>The <mark data-color="green">denser plate sinks below </mark>and<mark data-color="green"> islands in the ocean can form</mark>. e.g. <mark data-color="green">Mariana trench.</mark></p>
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What happens when two continental plates converge?

Forms a collision zone where neither plate can subduct below the other. Instead the crust is crumpled upwards by the pressure building between two plates, creating fold mountains.

<p>Forms a <mark data-color="green" style="background-color: green; color: inherit">collision zone</mark> where <strong>neither </strong>plat<mark data-color="green" style="background-color: green; color: inherit">e can subduct below the other</mark>. Instead the <mark data-color="green" style="background-color: green; color: inherit">crust is </mark><strong><mark data-color="green" style="background-color: green; color: inherit">crumpled upwards</mark> </strong>by the <strong>pressure building </strong><mark data-color="green" style="background-color: green; color: inherit">between two plates</mark>, creating <mark data-color="green" style="background-color: green; color: inherit">fold mountains</mark>.</p>
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What is an example of a collision zone?

Where the Eurasian and Indian plate meet to form the Himalayas.

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What hazards can occur at conservative plate boundaries?

Earthquakes.

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What happens at a conservative boundary to form earthquakes?

At a conservative boundary, parallel plates move in different directions/at different speeds in relation to each other. When these plates move side by side, friction builds between the plates. This friction builds up over many years and eventually the pressure becomes so large that the plates eventually move in a sudden jolt. This releases a lot of energy which sends vibrations through the ground - this is the earthquake.

<p>At a <mark data-color="green" style="background-color: green; color: inherit">conservative boundary</mark>, <strong>parallel </strong>plates <mark data-color="green" style="background-color: green; color: inherit">move in different </mark><strong><mark data-color="green" style="background-color: green; color: inherit">directions</mark></strong><mark data-color="green" style="background-color: green; color: inherit">/at different </mark><strong><mark data-color="green" style="background-color: green; color: inherit">speeds</mark> </strong>in relation to each other. When these<mark data-color="green" style="background-color: green; color: inherit"> plates move </mark><strong><mark data-color="green" style="background-color: green; color: inherit">side by side</mark></strong>, <strong>friction</strong> <mark data-color="green" style="background-color: green; color: inherit">builds </mark>between the plates. This <mark data-color="green" style="background-color: green; color: inherit">friction </mark><strong><mark data-color="green" style="background-color: green; color: inherit">builds </mark></strong><mark data-color="green" style="background-color: green; color: inherit">up over</mark><strong><mark data-color="green" style="background-color: green; color: inherit"> many years </mark></strong>and eventually the <strong><mark data-color="green" style="background-color: green; color: inherit">pressure </mark></strong><mark data-color="green" style="background-color: green; color: inherit">becomes </mark><strong><mark data-color="green" style="background-color: green; color: inherit">so large</mark> </strong>that the <mark data-color="green" style="background-color: green; color: inherit">plates eventually move in a </mark><strong><mark data-color="green" style="background-color: green; color: inherit">sudden jolt.</mark></strong> This<mark data-color="green" style="background-color: green; color: inherit"> releases a lot of energy</mark> which <mark data-color="green" style="background-color: green; color: inherit">sends </mark><strong><mark data-color="green" style="background-color: green; color: inherit">vibrations </mark></strong><mark data-color="green" style="background-color: green; color: inherit">through the ground </mark>- this is the earthquake.</p>
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What is an example of a conservative plate boundary?

The San Andreas Fault in California.

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What can conservative boundaries on oceanic crust cause?

The movement of earthquakes formed at conservative boundaries can displace a lot of water, causing large waves called tsunamis.

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What can conservative boundaries on continental crust cause?

On continental crust, fault lines can occur where the ground is cracked by the movement.

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What are hotspots?

Areas of volcanic activity where unusually hot magma breaks through the middle of a plate and travels up to the surface, creating a volcano. They are not related to plate boundaries

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How do hotspots form?

Formed when hot magma plumes from the mantle rise and burn through weaker parts of the crust. This can create volcanoes and islands.

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How do long chains of islands form?

Long chains of islands form because the plume stays in the same place but the plates continue to move slowly over the magma plume.

e.g. Hawaii

<p>Long chains of islands form because the <mark data-color="#d9f99d" style="background-color: #d9f99d; color: inherit">plume stays in the same place</mark> but the <mark data-color="#d9f99d" style="background-color: #d9f99d; color: inherit">plates continue to move slowly</mark> over the magma plume.</p><p>e.g. Hawaii</p>
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When is a volcano formed?

When magma erupts onto the Earth’s surface as lava through a vent in the Earth’s crust.

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What is the magnitude of a volcanic eruption measured on?

The Volcanic Explosivity Index (VEI).

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Features of a volcano:

knowt flashcard image
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What are the characteristics of a composite volcano?

  • Steep-sided due to slow-moving lava

  • Sticky, viscous lava

  • More explosive - due to higher gas content

  • Formed from alternating layers of ash & lava

  • Tend to form on convergent plate boundaries

<ul><li><p><mark data-color="#d9f99d" style="background-color: #d9f99d; color: inherit">Steep-sided</mark> due to <mark data-color="#d9f99d" style="background-color: #d9f99d; color: inherit">slow-moving lava</mark></p></li><li><p><mark data-color="#d9f99d" style="background-color: #d9f99d; color: inherit">Sticky, viscous lava</mark></p></li><li><p><mark data-color="#d9f99d" style="background-color: #d9f99d; color: inherit">More explosive </mark>- due to <mark data-color="#d9f99d" style="background-color: #d9f99d; color: inherit">higher gas content</mark></p></li><li><p>Formed from <mark data-color="#d9f99d" style="background-color: #d9f99d; color: inherit">alternating layers of ash &amp; lava</mark></p></li><li><p><mark data-color="#d9f99d" style="background-color: #d9f99d; color: inherit">Tend </mark>to <mark data-color="#d9f99d" style="background-color: #d9f99d; color: inherit">form on convergent plate boundaries</mark></p></li></ul><p></p>
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What are the characteristics of a shield volcano?

  • Gentle sloping sides due to fast-moving, runny lava that travels a further distance before solidifying

  • low viscosity (runny), thin lava

  • Less explosive - due to lower gas content - gentle eruptions

  • Tend to form on divergent plate boundaries or hot spots

  • Frequent eruptions

<ul><li><p><mark data-color="#d9f99d" style="background-color: #d9f99d; color: inherit">Gentle sloping sides</mark> due to <mark data-color="#d9f99d" style="background-color: #d9f99d; color: inherit">fast-moving, runny lava</mark> that travels a <mark data-color="#d9f99d" style="background-color: #d9f99d; color: inherit">further distance before solidifying</mark></p></li><li><p><mark data-color="#d9f99d" style="background-color: #d9f99d; color: inherit">low viscosity (runny), thin lava</mark></p></li><li><p><mark data-color="#d9f99d" style="background-color: #d9f99d; color: inherit">Less explosive</mark> - due to<mark data-color="#d9f99d" style="background-color: #d9f99d; color: inherit"> lower gas conten</mark>t - <mark data-color="#d9f99d" style="background-color: #d9f99d; color: inherit">gentle </mark>eruptions</p></li><li><p>Tend to form on <mark data-color="#d9f99d" style="background-color: #d9f99d; color: inherit">divergent plate boundaries </mark>or <mark data-color="#d9f99d" style="background-color: #d9f99d; color: inherit">hot spots</mark></p></li><li><p><mark data-color="#d9f99d" style="background-color: #d9f99d; color: inherit">Frequent</mark> eruptions</p></li></ul><p></p>
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Active volcano:

The volcano has recently erupted & is likely to erupt again.

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Dormant volcano:

Has erupted in the last 2000 years and may possibly erupt again.

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Extinct volcano:

Shows no evidence of eruption in historic times & there is no evidence of a magma reservoir.

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Explain one difference between the type of volcanoes found at divergent and convergent plate boundaries.

(3 Marks)

At divergent boundaries the volcanoes are less steep because of the low viscosity/runny lava that travels a greater distance before it solidifies.

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What is pyroclastic flow?

Fast-moving, very hot clouds of poisonous gases mixed with ash. Average speeds of about 100km/h - can move at up to 700km/h.

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What are lahars?

When volcanoes erupt, snow & ice on the peak melts & combines with the ash/pyroclastic material. This creates fast moving mudflows called lahars.

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Describe volcanic eruptions at divergent plate boundaries and the kind of volcanoes they form:

  • Eruptions are non-explosive with runny, fast-flowing lava

  • The lava is made up of basalt - very hot and low viscosity

  • Low viscosity lava creates shallow sided (flat) shield volcanoes.

<ul><li><p>Eruptions are <mark data-color="#d9f99d" style="background-color: #d9f99d; color: inherit">non-explosive</mark> with <mark data-color="#d9f99d" style="background-color: #d9f99d; color: inherit">runny, fast-flowing lava</mark></p></li><li><p>The lava is made up of <mark data-color="#d9f99d" style="background-color: #d9f99d; color: inherit">basalt </mark>- <mark data-color="#d9f99d" style="background-color: #d9f99d; color: inherit">very hot</mark> and <mark data-color="#d9f99d" style="background-color: #d9f99d; color: inherit">low viscosity</mark></p></li><li><p><mark data-color="#d9f99d" style="background-color: #d9f99d; color: inherit">Low viscosity lava</mark> creates<mark data-color="#d9f99d" style="background-color: #d9f99d; color: inherit"> shallow sided (flat) shield volcanoes.</mark></p></li></ul><p></p>
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Describe volcanic eruptions at convergent plate boundaries and the kind of volcanoes they form:

  • Eruptions are usually explosive due to the high pressure the magma is under

  • Hot gas, ash & rock is spewed from the volcano due to high pressure

  • Fast, extremely hot clouds of gas, ash & debris can roll down the side of the volcano in a pyroclastic flow - can incinerate anything in its path

  • Lava is made of andesite - causes lava to be viscous & slow flowing

  • Steep sided composite volcanoes are formed

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Describe earthquakes on conservative boundaries:

  • Very destructive & intense - up to 8.5 magnitude

  • If an earthquake is shallow (close to surface) the earthquake can cause very intense shaking - can bring down buildings, break pipes & destroy infrastructure

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Describe earthquakes on convergent boundaries:

  • Very strong earthquakes due to pressure built up and then released between subducting plates - up to 9.5+ magnitude

  • Can be very severe especially if shallow - however are usually deep as the plate is sinking

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Describe earthquakes on divergent boundaries:

  • Usually smaller & cause less damage as there is less built up pressure at these boundaries

  • 5.0-6.0 on the Richter Scale

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Where do most earthquakes occur?

Along the Pacific Ring of Fire’. Around 90% occur there.

<p>Along the <mark data-color="#d9f99d" style="background-color: #d9f99d; color: inherit">Pacific </mark>‘<mark data-color="#d9f99d" style="background-color: #d9f99d; color: inherit">Ring of Fire</mark>’. Around 90% occur there.</p>
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Where do most volcanoes occur?

Around the rim of the Pacific Ocean called the ‘Ring of Fire’. Around 75% occur there.

<p>Around the<mark data-color="#d9f99d" style="background-color: #d9f99d; color: inherit"> rim of the Pacific Ocean </mark>called the <mark data-color="#d9f99d" style="background-color: #d9f99d; color: inherit">‘Ring of Fire’. Around 75% occur there.</mark></p>
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At what plate boundaries do earthquakes tend to be stronger?

Convergent & conservative plate boundaries.

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How do you strengthen a building against earthquakes?

  • Installing a ring beam at roof level stopping walls falling outwards.

  • Very strong framework in skyscrapers.

  • Rubber and steel foundations which can move slightly.

  • Deeper foundations.

  • Reinforcing gas and water pipes so they don't break.

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The impacts of earthquakes and volcanic eruptions are categorised into…

  • Primary hazards - direct result of the earthquake or eruption

  • Secondary hazards - occur as a result of the primary effects

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What are some primary hazards of an earthquake?

  • Ground shaking

  • Surface rupture

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What are some secondary hazards of an earthquake?

  • Liquefaction - when loose material like soil & rocks act like a liquid

  • Landslides

  • Tsunamis

  • Fires

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What are some primary hazards of a volcanic eruption?

  • Pyroclastic flow

  • Lava flow

  • Volcanic bombs

  • Lahars (mudflow)

  • Earthquakes

  • Direct ash fall

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What is pyroclastic flow?

Fast-moving, hot mixture of gas, ash, and volcanic debris that erupts from a volcano during an explosive eruption

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What are some secondary hazards of a volcanic eruption?

  • Landslides

  • Tsunamis

  • Acid rain

  • Ash fallout from the atmosphere

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What is a tsunami?

A large wave caused by a large amount of water being displaced when plates move.

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Describe how a tsunami can form:

  • When an oceanic crust is jolted during an earthquake, all of the water above this plate is displaced

  • The water travels fast but with a low amplitude (height)

  • As it gets closer to the coast, the sea level decreases so there is friction between the sea bed and the waves

  • This causes the wave to slow down and the wavelength becomes compressed, which leads to an increase in height - creating a wall of water that can reach 5-10 meters

<ul><li><p>When an <strong><mark data-color="green" style="background-color: green; color: inherit">oceanic </mark></strong><mark data-color="green" style="background-color: green; color: inherit">crust is </mark><strong><mark data-color="green" style="background-color: green; color: inherit">jolted</mark></strong><mark data-color="green" style="background-color: green; color: inherit"> during an earthquake</mark>, all of the <strong>water above</strong> this plate is <mark data-color="green" style="background-color: green; color: inherit">displaced</mark></p></li><li><p>The <mark data-color="green" style="background-color: green; color: inherit">water travels fas</mark>t but with a<mark data-color="green" style="background-color: green; color: inherit"> low amplitude (height)</mark></p></li><li><p>As it <strong>gets closer </strong>to the coast, the <strong><mark data-color="green" style="background-color: green; color: inherit">sea level</mark></strong><mark data-color="green" style="background-color: green; color: inherit"> decreases </mark>so there is <strong><mark data-color="green" style="background-color: green; color: inherit">friction </mark></strong><mark data-color="green" style="background-color: green; color: inherit">between the</mark><strong><mark data-color="green" style="background-color: green; color: inherit"> sea bed </mark></strong><mark data-color="green" style="background-color: green; color: inherit">and the </mark><strong><mark data-color="green" style="background-color: green; color: inherit">waves</mark></strong></p></li><li><p>This causes the <mark data-color="green" style="background-color: green; color: inherit">wave to slow dow</mark>n and the <mark data-color="green" style="background-color: green; color: inherit">wavelength becomes compresse</mark>d, which leads to an<mark data-color="green" style="background-color: green; color: inherit"> increase in height</mark> - creating a <mark data-color="green" style="background-color: green; color: inherit">wall of wate</mark>r that can<mark data-color="green" style="background-color: green; color: inherit"> reach </mark><strong><mark data-color="green" style="background-color: green; color: inherit">5-10</mark></strong><mark data-color="green" style="background-color: green; color: inherit"> meters</mark></p></li></ul><p></p>
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Impacts of earthquakes and volcanic eruptions:

  • Loss of life & injury - may be immediate through falling buildings/ash fall or days and weeks after the event due to unclean water or disease

  • Collapse or destruction of buildings - leads to people being homeless for months & even years after the event

  • Transport network - roads, bridges and railways may be damaged or destroyed - can impact speed aid can reach affected areas

  • Loss of jobs and businesses - impacts the economy when factories & offices are destroyed or damaged

  • Loss of crops - leads to food shortages & affects farmers income

  • Power and water supplies are damaged - affects the supply of potable water

  • Damage to the environment - loss of vegetation & habitats, ash affects climate

  • Closure of airports - dangerous for jet planes to fly through ash clouds due to possible engine failure - flights are cancelled