EESA06 Topic 3: Divergent Margins

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Lecture 4 - Embryonic and Juvenile Oceans; Lecture 5 - Mature Ocean Basins

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1
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What is the Wilson cycle?

  • Describes how oceans open and close

  • i.e., ocean basin lifecycle

<ul><li><p>Describes how oceans open and close</p></li><li><p>i.e., ocean basin lifecycle </p></li></ul><p></p>
2
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What is the most important group of minerals? Why?

  • Silicate minerals

    • i.e., those containing silica and oxygen

  • Accounts for 90% of all minerals

3
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How does silica content differ across the lithosphere?

  • Continental crust - felsic

    • high levels of silica + feldspar

  • Oceanic crust - mafic

    • less than 50% silica; mostly magnesium and iron

  • Mantle - ultramafic

    • less than 40% silica; mostly magnesium and iron

4
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How is silica related to magma's properties?

  • It controls most of magma's properties

  • e.g., velocity

5
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Describe how magma is generated.

  • From melting of rock

  • i.e., when rocks

    • Undergo decompression

    • Are heated

    • Get wet

<ul><li><p>From melting of rock</p></li><li><p>i.e., when rocks</p><ul><li><p>Undergo decompression</p></li><li><p>Are heated</p></li><li><p>Get wet</p></li></ul></li></ul><p></p>
6
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Describe decompression melting.

  • Rock rises from an area of high pressure to lower pressure

  • Change in pressure causes rock to (partially) melt

<ul><li><p>Rock rises from an area of high pressure to lower pressure</p></li><li><p>Change in pressure causes rock to (partially) melt</p></li></ul><p></p>
7
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Describe Flux-Induced melting

  • Adding water to rock changes how it behaves (i.e., melts) at different pressures or temperatures

<ul><li><p>Adding water to rock changes how it behaves (i.e., melts) at different pressures or temperatures</p></li></ul><p></p>
8
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Where does decompression happen? Explain.

  • At mantle plumes

  • This is where mantle rock is brought up

    • i.e., moves from higher to lower pressure

<ul><li><p>At mantle plumes</p></li><li><p>This is where mantle rock is brought up</p><ul><li><p>i.e., moves from higher to lower pressure</p></li></ul></li></ul><p></p>
9
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Is melting usually partial melting or full melting? How does this influence the resulting magma?

  • Partial; silica-rich melts before silica-poor

  • Magma is more silica-rich than melting rock

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Differentiate between wet magma and dry magma

Hint: location, silica, viscosity, colour, density, other

 

Wet

Dry

Location

Convergent margins

Divergent margins

Silica content

Higher

Lower

Viscosity

Higher

Lower

Colour

Lighter

Darker

Density

Lower

Higher

Other Notes

Water causes melting where we would usually see solid rock

Produced from melting of the top of the mantle

<table style="minWidth: 75px"><colgroup><col><col><col></colgroup><tbody><tr><td colspan="1" rowspan="1"><p><strong>&nbsp;</strong></p></td><td colspan="1" rowspan="1"><p><strong>Wet</strong></p></td><td colspan="1" rowspan="1"><p><strong>Dry</strong></p></td></tr><tr><td colspan="1" rowspan="1"><p><strong>Location</strong></p></td><td colspan="1" rowspan="1"><p>Convergent margins</p></td><td colspan="1" rowspan="1"><p>Divergent margins</p></td></tr><tr><td colspan="1" rowspan="1"><p><strong>Silica content</strong></p></td><td colspan="1" rowspan="1"><p>Higher</p></td><td colspan="1" rowspan="1"><p>Lower</p></td></tr><tr><td colspan="1" rowspan="1"><p><strong>Viscosity</strong></p></td><td colspan="1" rowspan="1"><p>Higher</p></td><td colspan="1" rowspan="1"><p>Lower</p></td></tr><tr><td colspan="1" rowspan="1"><p><strong>Colour</strong></p></td><td colspan="1" rowspan="1"><p>Lighter</p></td><td colspan="1" rowspan="1"><p>Darker</p></td></tr><tr><td colspan="1" rowspan="1"><p><strong>Density</strong></p></td><td colspan="1" rowspan="1"><p>Lower</p></td><td colspan="1" rowspan="1"><p>Higher</p></td></tr><tr><td colspan="1" rowspan="1"><p><strong>Other Notes</strong></p></td><td colspan="1" rowspan="1"><p>Water causes melting where we would usually see solid rock</p></td><td colspan="1" rowspan="1"><p>Produced from melting of the top of the mantle</p></td></tr></tbody></table><p></p>
11
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How do high silica magmas compare to low silica magmas?

  • They're more viscous

  • They crystalize minerals with more silica tetrahedra in their structure

 

12
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Why is ocean floor mostly basalt (i.e., more silica-rich than mantle)?

  • Ultramafic mantle → melts a little through decompression → mafic ocean floor

 

13
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What minerals are abundant in convergent margins?

  • Silica

  • i.e., felsic

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What volcano types are associated with convergent margins? Describe these volcanoes.

  • Stratovolcanoes

  • High viscosity magma

  • Magma doesn't get far → pointy volcano

<ul><li><p>Stratovolcanoes</p></li><li><p>High viscosity magma</p></li><li><p>Magma doesn't get far → pointy volcano</p></li></ul><p></p>
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What minerals are abundant in divergent margins?

  • Iron

  • i.e., mafic

16
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What volcano types are associated with divergent margins? Describe these volcanoes.

  • Shield volcanoes

  • Mafic magma

  • Lower volcanos, wide-reaching flows (lower viscosity magma)

  • e.g., erte ale volcano

<ul><li><p>Shield volcanoes</p></li><li><p>Mafic magma</p></li><li><p>Lower volcanos, wide-reaching flows (lower viscosity magma)</p></li><li><p>e.g., erte ale volcano</p></li></ul><p></p>
17
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How does cooling time and time spend underground influence magma?

  • Give examples of each instance.

  • does silica amount differ across instances?

  • Rapid cooling → low crystal count

    • e.g., obsidian

  • Medium cooling → slightly more crystals

    • e.g., rhyolite

  • Slow cooling + completely underground → high crystal count

    • e.g., granite

In each instance, silica amount is similar

<ul><li><p>Rapid cooling → low crystal count</p><ul><li><p>e.g., obsidian</p></li></ul></li><li><p>Medium cooling → slightly more crystals</p><ul><li><p>e.g., rhyolite</p></li></ul></li><li><p>Slow cooling + completely underground → high crystal count</p><ul><li><p>e.g., granite</p></li></ul><p></p></li></ul><p>In each instance, silica amount is similar</p>
18
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What are igneous rocks? List the two types.

  • The product of cooled magma

  • Volcanic rocks: erupt at surface

  • Plutonic rocks: cool underground

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Where does igneous rock cool? Give examples.

  • Earth's surface (extrusive/volcanic)

    • e.g., lava flow

  • Underground (intrusive/plutonic)

    • e.g., dikes

<ul><li><p>Earth's surface (extrusive/volcanic)</p><ul><li><p>e.g., lava flow</p></li></ul></li><li><p>Underground (intrusive/plutonic)</p><ul><li><p>e.g., dikes</p></li></ul></li></ul><p></p>
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What are examples of heterogenous rocks?

  • Granites

  • Other igneous ricks

  • Sedimentary and metamorphic rocks

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why do shield and stratovolcanoes produce different magma?

difference in silica content

22
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What is continental rifting?

Pulling apart/extension of land

<p>Pulling apart/extension of land</p>
23
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How does continental rifting relate to the creation of passive margins?

  • First 2 major stages of the Wilson Cycle

  • Rifting → continent extends, thinning the crust and allowing a valley to form

  • Continent then becomes two, separated by oceanic crust formed from basalt eruptions

  • The land that meets the water = passive margin

<ul><li><p>First 2 major stages of the Wilson Cycle</p></li><li><p>Rifting → continent extends, thinning the crust and allowing a valley to form</p></li><li><p>Continent then becomes two, separated by oceanic crust formed from basalt eruptions</p></li><li><p>The land that meets the water = passive margin</p></li></ul><p></p>
24
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Differentiate between a rock and a mineral.

  • Rock = naturally formed, consolidated material

    • composed of grains of one or more minerals

  • Mineral = naturally occurring, inorganic, crystalline solid

    • Has a specific chemical composition

    • Building blocks of rocks

25
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How do new oceans form?

  • Triple junctions

  • Passing over mantle plumes gradually weakens continental crust

  • Eventually, crust becomes so weak, a rift is created

  • With the expansion of the rift, water fills in an oceanic crust is created

<ul><li><p>Triple junctions</p></li><li><p>Passing over mantle plumes gradually weakens continental crust</p></li><li><p>Eventually, crust becomes so weak, a rift is created</p></li><li><p>With the expansion of the rift, water fills in an oceanic crust is created</p></li></ul><p></p>
26
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What is an embryonic ocean?

  • Early-stage ocean basin

  • Forms when a continental rift begins to separate a landmass

  • Allows water to accumulate in the widening gap

<ul><li><p>Early-stage ocean basin</p></li><li><p>Forms when a <strong>continental rift begins to separate a landmass</strong></p></li><li><p>Allows water to accumulate in the widening gap</p></li></ul><p></p>
27
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What is a triple junction?

a point on Earth where the boundaries of three tectonic plates meet

<p>a point on Earth where the boundaries of three tectonic plates meet</p>
28
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Discuss thermal doming above plume heads.

Passing over mantle plumes → doming/uplifting of the continental crust above

<p>Passing over mantle plumes → doming/uplifting of the continental crust above</p>
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What are failed rifts (Aulocogens)?

a rift that begins to split a continent but does not fully develop into an ocean basin

30
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What are flood basalts?

subset of LIPs, consisting of thick, widespread lava flows that cover large areas

31
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what is a juvenile ocean?

  • an early-stage ocean basin that forms as a result of continental rifting and the initial separation of tectonic plates

  • represents the second stage in the Wilson Cycle

32
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describe juvenile ocean shelves

  • Sediment from continent collects where land meets water

  • shallow, submerged edges of newly formed continental margins

  • Form on the transition from continental to oceanic crust

  • Sediments wash into basins where they are buried and lithified

<ul><li><p><span>Sediment from continent collects where land meets water</span></p></li><li><p><span>shallow, submerged edges of newly formed continental margins</span></p></li><li><p><span>Form on the transition from continental to oceanic crust</span></p></li><li><p><span>Sediments wash into basins where they are buried and lithified</span></p></li></ul><p></p>
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what are incipient oceaninc crust?

newly forming or embryonic oceanic crust that develops in an area where continental rifting is leading to the creation of a new ocean basin

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What causes the uplift of the East African Rift?

Thermal doming

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Where are most sediments today?

  • Continental shelves

  • i.e., passive continental margins

36
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Describe the tectonic activity of continental shelves.

  • Tend to be stable

  • Shelves on active margins get destroyed consistently

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Continental shelves are home to what?

  • A lot of biological activity

  • Most of the world's

    • Oil

    • Gas

    • Fisheries

38
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<p>Why is there such a large cliff in the Grand Banks, Newfoundland?</p>

Why is there such a large cliff in the Grand Banks, Newfoundland?

  • High part = mostly continental crust

  • Low part = all ocean crust

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Why is the Red Sea considered a juvenile ocean?

  • Has started to accumulate a shelf

  • There is creation of ocean crust at the centre

40
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What plates form the triple junction at the East African Rift?

  • African

  • Arabian

  • Somalian

<ul><li><p>African</p></li><li><p>Arabian</p></li><li><p>Somalian</p></li></ul><p></p>
41
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<p>What are horsts and grabens?</p>

What are horsts and grabens?

  • H = highs

  • G = lows

  • Occur at a rift

<ul><li><p><span>H = highs</span></p></li><li><p><span>G = lows</span></p></li><li><p><span>Occur at a rift</span></p></li></ul><p></p>
42
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What are large igneous provinces (LIPs)?

  • New ocean crust (basalt) along the rift

  • Include flood basalts

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Differentiate between Pahoehoe lava, Ropey lava, and AA lava

44
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How does the Red Sea's opening influence surrounding plates? (Plate reconfiguration)

  • Pushes Arabian plate north into Europe

  • This is happening

    • Along the Dead Sea Fault Zone

    • Faster than the African Plate is moving NW

<ul><li><p>Pushes Arabian plate north into Europe</p></li><li><p>This is happening</p><ul><li><p>Along the Dead Sea Fault Zone</p></li><li><p>Faster than the African Plate is moving NW</p></li></ul></li></ul><p></p>
45
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what is the Dead Sea Fault?

transform plate boundary between master moving Arabian and African plates

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What is an endorheic basin?

  • closed drainage basin where water has no outlet to the ocean

  • e.g., Dead Sea

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What are salt diapirs?

  • upward movements of salt within a layer of overlying rock

  • typically caused by buoyancy and pressure differences in the Earth’s crust

<ul><li><p><strong>upward movements of salt</strong> within a layer of overlying rock</p></li><li><p>typically caused by <strong>buoyancy</strong> and <strong>pressure differences</strong> in the Earth’s crust</p></li></ul><p></p>
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How do salt diapirs relate to the Atlantic Ocean's creation?

  • Salt accumulated in rifts during Pangea

  • They broke up, forming early Atlantic

 

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What can we learn from EQs of antiquity?

  • How often did they happen?

    • i.e., fault's activity

  • Are there no EQs where there should be?

  • When might the next EQ be?

<ul><li><p>How often did they happen?</p><ul><li><p>i.e., fault's activity</p></li></ul></li></ul><ul><li><p><span>Are there no EQs where there should be?</span></p></li><li><p><span>When might the next EQ be?</span></p></li></ul><p></p>
50
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How does the Red Sea's opening influence Turkey?

T's moving westward along the North Anatolian Fault (NAT) and the East Anatolian Fault (EAF)

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Why is NAT Fault one of the world's most dangerous faults?

Escape tectonics

  • i.e., a tectonic block or region is forced out or moved laterally due to the compressive forces exerted by surrounding tectonic plates

  • Cascading EQs propagate along here

<p>Escape tectonics</p><ul><li><p>i.e., a tectonic block or region is <strong>forced out</strong> or <strong>moved laterally</strong> due to the <strong>compressive forces</strong> exerted by surrounding tectonic plates</p></li><li><p>Cascading EQs propagate along here</p></li></ul><p></p>
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How does ocean floor change with age? What does this do in terms of the ocean floor's behaviour?

  • Older

    • Denser

    • higher mineral content

    • thicker lithosphere

    • More sediment

    • Farther from MOR

  • Eventually, floor will subduct due to density

53
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<p>In this image, what does the width of each band represent?</p>

In this image, what does the width of each band represent?

  • The rate of spreading

  • e.g., during the Miocene, Atlantic spread slower than Pacific

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Does the ocean spread at the same rate at all points across the global mid-ocean ridge system?

No

<p>No</p>
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What is the total length of the global mid-ocean ridge system?

80 000km

<p>80 000km</p>
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what are the two controls of seafloor spreading rate?

  • slab pull

  • ridge push

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describe slab pull

(seafloor spreading)

subducting older oceanic lithosphere exerts greater tension to mid-ocean ridge relative to younger oceanic lithosphere

<p>subducting older oceanic lithosphere exerts greater tension to mid-ocean ridge relative to younger oceanic lithosphere</p>
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describe ridge push

thermal uplift of the midocean ridge causes gravitational sliding of the plates odd the ridge

<p>thermal uplift of the midocean ridge causes gravitational sliding of the plates odd the ridge</p>
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How does the rate of spreading influence ridge morphology?

  • Centre axial magma chamber is

    • Big when there's fast rate

    • Small when there's slow rate

  • Fast flows lead to

    • Broad, more diffuse volcanism

    • Broad shape

    • Pointy tops

    • Far lava spread

<ul><li><p>Centre axial magma chamber is</p><ul><li><p>Big when there's fast rate</p></li><li><p>Small when there's slow rate</p></li></ul></li><li><p>Fast flows lead to</p><ul><li><p>Broad, more diffuse volcanism</p></li><li><p>Broad shape</p></li><li><p>Pointy tops</p></li><li><p>Far lava spread</p></li></ul></li></ul><p></p>
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How can you study mid-ocean ridges and sea floor spreading?

  • Direct observation with submersibles (mostly autonomous vehicles now)

    • e.g., smokers, seafloor minerals

  • Studying ancient MORS

    • i.e., Ophiolites

  • Iceland

    • i.e., Mid-Atlantic Ridge is on land

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What are smokers?

  • Active hydrothermal vents

  • Cold water filters through fractures and heats up, absorbing minerals

  • Deposits formed when hot mineral-filled water meets cold water

  • Water cools and minerals rain out

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What do the voids in smokers allow?

Water to move up

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What does the colour of the smoke from smokers/hydrothermal vents indicate?

  • Black = metal-filled, hot water

  • White = calcium carbonate filled, warm water

    • i.e., fluid isn't metal-rich

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What are Ophiolites?

  • Accretion of obducted ocean crust

  • Remnants of ancient crust and mid-ocean ridges

  • Exposed to land because of ocean closure

<ul><li><p>Accretion of obducted ocean crust</p></li><li><p>Remnants of ancient crust and mid-ocean ridges</p></li><li><p>Exposed to land because of ocean closure</p></li></ul><p></p>
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When does precipitation of minerals happen?

When mineral-rich water cools quickly

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What is rock alteration?

  • When minerals move in or out of a rock

  • Depends on the chemical composition (e.g., pH) and temperature of the water

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Where do Pillow Lavas form?

  • a.k.a., pillow basalts

  • From where lava erupts under water

 

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What are sheeted dikes and where do they form?

  • Lava trails through a linear conduit

  • Form where basalts are repeatedly injected

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Where do layered Gabbros form?

Where basaltic magma cools very slowly in an axial magma chamber

<p>Where basaltic magma cools very slowly in an axial magma chamber</p>
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Describe the onion model of building oceanic crust at mid-ocean ridges

  • Pillow basalts erupt at surface

  • Intrusion of sheeted sikes at depth

  • Settling of gabbro from magma chambers

<ul><li><p>Pillow basalts erupt at surface</p></li><li><p>Intrusion of sheeted sikes at depth</p></li><li><p>Settling of gabbro from magma chambers</p></li></ul><p></p>
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Why is the mid-Atlantic Ridge above sea level in Iceland?

The Iceland Plume has lifted it

<p>The Iceland Plume has lifted it</p>
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How does the Afar Triangle relate to the Mid-Atlantic Ridge in Iceland?

  • Similar creation

  • Mantle plume under continental crust caused release of flood basalts to form LIP

 

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How does the Icelandic Plume relate to the separation of the British Isles and Greenland?

  • It's responsible for the separation and releasing flood basalts

  • 40 MA

<ul><li><p>It's responsible for the separation and releasing flood basalts</p></li><li><p>40 MA</p></li></ul><p></p>
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How is the mid-Atlantic Ridge moving relative to the Iceland Plume?

  • Northwest away from the plume

  • i.e., moving off the plume

 

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Differentiate between relative and absolute motion

  • Relative = rate of motion of one plate relative to another

  • Absolute = entire plate movement

<ul><li><p>Relative = rate of motion of one plate relative to another</p></li><li><p>Absolute = entire plate movement</p></li></ul><p></p>
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What is ridge jumping?

Ridge is moving away from plume

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Describe fissures.

  • Cracks in the crust

  • Can go down several kilometres

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What happens when magma exits a fissure?

  • Fissure eruption + magma flow

  • Usually low viscosity, not too dangerous

 

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What are protective berms?

  • Same material as lava used to redirect lava flow

  • Must predict where the fissure + flow will occur

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<p>Describe the elements seen in this picture</p>

Describe the elements seen in this picture

  1. ash

  2. fountain magma

  3. protective berm

  4. lava flow

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Can effusive eruptions have a global impact? Give an example.

  • Yes

  • e.g., Lakigigar large fissure eruption (1783)

  • 15 cubed km of magma and hydrofluoric acid + sulfur dioxide

  • Led to

    • Death of 50% Iceland's livestock

    • Famine

    • Destroyed 21 villages

    • Aerosols that influenced Europe and led to crop failure and, consequently, the French Revolution

 

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Describe columnar basalt

  • Pooled magma that cools from top and bottom

  • Forms columns

 

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How do successive lava flows impact oceanic crust?

Thicken crust

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Describe the Eyjafjallajokull volcano.

  • Sits underneath a small ice cap

  • More dangerous due to lava and water interactions

 

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Describe phreatomagmatic eruptions

  • Eruptions involving steam and magma

  • They become explosive and can lead to floods

 

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How many times has Katla erupted over the past 1100 year and how far of an impact has it had?

  • 20 times

  • Ash as far as Scotland

 

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How do phreatomagmatic eruptions influence the volcanic ash released?

  • Magma melts ice

  • Ice interacts with magma

  • "shattered rock" explodes out of the volcano

 

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What is tephra?

  • Anything thrown out of a volcano

  • e.g., ash, bombs

 

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What is Fjallsjokull?

An outlet glacier of the Vatnajokull Ice Cap

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How are flat-topped ("Moberg") mountains formed?

Volcanic eruptions under ice caps

<p>Volcanic eruptions under ice caps</p>
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What causes Hyaloclastite breccia formation?

"glassy fragments" formed by fast cooling

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Does ocean floor temperature change depending on distance from MOR?

  • Yes

  • Colder = farther

 

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Why is the ocean floor draped in sediment?

  • Once off the MOR, it sediment starts to settle over it

  • Due to

    • Primary productivity

      • i.e., biological activity in ocean (e.g., photosynthesis from phytoplankton)

    • Terrigenous sediment

      • Sediment moves from continents into ocean

 

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Other than sediment, what is on the ocean floor?

  • Ocean islands

  • Guyots

  • Seamounts

  • Atolls