Geology test #3

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What are 3 ways to melt the mantle?

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1

What are 3 ways to melt the mantle?

  • decrease temperature

  • Increase temperature

  • add violates

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2

What is the geotherm?

The change in temperature with depth(red/ green line in diagrams)

<p>The change in temperature with depth(red/ green line in diagrams)</p>
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3

Lithospheric Geotherm

Conductive heat transvers

  • temperature changes significantly with depth

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4

Asthenosphere geotherm

Convection heat transvers

  • Adiabatic Geotherm : pressure changes a lot, temperature changes very little

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5
<p>On What side of the curve does it remain solid or melt?</p>

On What side of the curve does it remain solid or melt?

  • A mantle curves that resides at T and P to the left of the curve with remin solide

  • Where as to the right it will be at a high enough T and P to melt

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6

Where does hot spot volcanism most occur

  • occurs within plates

  • away from plate boundaries

<ul><li><p>occurs within plates </p></li><li><p>away from plate boundaries </p></li></ul>
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7

What is decomposition melting?

  • Thinning of the lithosphere

  • which allows partial melting to occur where geotherm crosses the solidus

  • 0987u5y4tfgn h

<ul><li><p>Thinning of the lithosphere</p></li><li><p>which allows partial  melting to occur where geotherm crosses the solidus</p></li><li><p><strong> </strong>0987u5y4tfgn h </p></li></ul>
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8

How is decomposition melting accomplished

  • Extension at midocean ridges

  • continental rifts

  • divergent boundaries

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9

Adding volatics: Flux melting

  • changes the melting curve/ solidus/ liquidus such that it cross the geotherm

  • The blue lines is the wet solius

  • Cause by convergent margins

<ul><li><p>changes the melting curve/ solidus/ liquidus such that it cross the geotherm</p></li><li><p>The blue lines is the wet solius</p></li><li><p>Cause by <strong>convergent margins</strong></p></li></ul>
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10

What is an example of adding volatiles

Ocean-continetial and ocean-ocean convergent plate boudries

  • The deceding slab contains wet sediment and hydrate minerals formed by alteration of the basalt on the seafloor

  • As the plate subducts is driven off the slub and into the overlaying mantle wedge

  • The hyrdate mantle melts at lower temp than dry mantle

<p>Ocean-continetial and ocean-ocean convergent plate boudries</p><ul><li><p>The deceding slab contains wet sediment and hydrate minerals formed by alteration of the basalt on the seafloor </p></li><li><p>As the plate subducts is driven off the slub and into the overlaying mantle wedge</p></li><li><p>The hyrdate mantle melts at lower temp than dry mantle </p></li></ul>
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11

How can melts be created

  • Plates seperate and mantle rises at mid-ocean ridges ( decompostion melting)

  • Hot spot- localized plumes of melt

  • Fluid fluxing

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12

Where is the only part of earth where the mantle can melt?

Outermost 200km of earth

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13

How does the geotherm slope change?

the slope is a function of geotherm thickness

  • lithopsheric geotherm increase as you move the curve up

  • astherospheric remains constant

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14

Mantle plumes

increase the geotherm by the addition of heat from the mantle

  • allow melting to occur in the triangular region

  • happens at hot spots in Hawaii

<p>increase the geotherm by the addition of heat from the mantle</p><ul><li><p>allow melting to occur in the triangular region</p></li><li><p>happens at hot spots in Hawaii</p></li></ul>
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15

1.      What is the name given to the region surrounding the Pacific Ocean where most subaerial (land-based) volcanoes occur?

  • The ring of fire

  • cotnains 75% of planets voclanoes

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16

1.      Why do volcanoes occur here—what is the tectonic setting of this region?

Is is where multiple tectonic plates meet

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17

What is the Volcanic Explosivity Index (VEI)

It measure and classify eruptions. It starts at zero and is a log scale. Does not have a upperlimit

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18

1.      What was the most explosive (higher VEI) volcano recorded?

VEI 8 which ocured thosands of millions of years ago

The most explosive volcanoe recorded was in Indonesia in 1815 which was a VEI of 7

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19

1.      List 2 benefits of volcanic eruptions

  • volcanic ash provide nutriest to nearby soil making the land fertile

  • when lava hardens into rock and creates new landforms

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20

what characterists of an eruption are used to classify volcanoes according to this Index?

volume of lava gas and other emmsions from the volcanoe

height of the eruption cloud above the summit

the degree of fragmentation

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21

What produces the contrast in explosivity

  1. melting viscosity (the main control)

    Composition and temperature: felsic vs mafic

  2. Volcaltiles- context of gasses

  3. Interaction with external water

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22

Melting Viscosity

The higher the silica content and the lower content of FE and MG, the more viscous the melt

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23
<p>Which of the compositions would have the higher viscosity </p>

Which of the compositions would have the higher viscosity

  • this mean that these compsotions tend to be more explosive

<ul><li><p>this mean that these compsotions tend to be more explosive</p></li></ul>
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24

What type of characteristic have less viscous (less explosive)

  • more mafic/ bastlic melts

  • higher temerature

  • more fluid

<ul><li><p>more mafic/ bastlic melts</p></li><li><p>higher temerature</p></li><li><p>more fluid</p></li></ul>
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25

Where do you get partial melts of the matnle reaching the surface of the earth without getting throguh the crust?

  • Oceanic divergent plate boudnries

  • oceanic hot spots

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26

Where are more felsic melts produced

  • contiential divergent plate boundries

  • contienal hot spots

  • convergent plate boundries

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27

What is the role of expanding gas on volcanic erruptions

  • they drive the volcanic erruptions

  • dissolved magmas under pressure

  • come out of solution and expand as magma rise

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28

What are the mian magetic gas that are associated with expanding gases

  • H20, C02, so2

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29

What is an example of expanding gases?

Mount St. Helens

  • magma rises in the chamber

  • at lower pressures the gases began to exsolve and the chamber expands

  • creates a bulge in the side of the mountain

<p>Mount St. Helens</p><ul><li><p>magma rises in the chamber </p></li><li><p>at lower pressures the gases began to exsolve and the chamber expands </p></li><li><p>creates a bulge in the side of the mountain</p></li></ul><p></p>
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30

What is the role of external water ?

If rising magma contacts water the water can vaporize

Intermingle with melt and cause an erruption

<p>If rising magma contacts water the water can vaporize </p><p>Intermingle with melt and cause an erruption </p>
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31

What is the classification of volcanic explosive index based of?

The volume of ejecta

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32

What was the largest recored on the VEI

Tambora 1815

<p>Tambora 1815</p>
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33

Do volcanoes always have the same classification during their life time ?

No, depends on composition and volatiles which change through the life of a volcano

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34

Hawaiian

  • basaltic ( low viscosity magmas)

  • volatile bubble out quietly

  • not very explosive

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35

Strombolian

  • bit more explosive

  • erruption chacterized by short term out put of pasty lava

  • results in scoria cones

  • example

  • MT etna Italy

  • Particun mexico

<ul><li><p>bit more explosive</p></li><li><p>erruption chacterized by short term out put of pasty lava </p></li><li><p>results in scoria cones  </p></li><li><p>example </p></li><li><p>MT etna Italy</p></li><li><p>Particun mexico</p><p></p></li></ul>
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36

Plinian

  • much stronger

  • eruption columns reach 45 km into stratosphere

  • Examples

    Naples, Italy

    Vesuvius ( one of the most dangerous volcanoes in the world)

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37

Surtseyan

  • results from basaltic eruption interacting with groundwater or surface water

  • wet equivalent of Strombolian eruption

  • water cause to be more explosive

<ul><li><p>results from basaltic eruption interacting with groundwater or surface water</p></li><li><p>wet equivalent of Strombolian eruption</p></li><li><p>water cause to be more explosive</p></li><li><p></p></li></ul>
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38

Vulcianian

  • more explosive that surtseyan

  • discrete canon like explosions

  • followed by sustained eruption

<ul><li><p>more explosive that surtseyan</p></li><li><p>discrete canon like explosions </p></li><li><p>followed by sustained eruption </p></li></ul>
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39

Phreatophian

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40

What is a glacier

Mass of compressed ice on land that moves under its own wight

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41

What are the different types of glacier

Alpine, conteinal ice sheets

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42

Where are continental ice sheets only found

Antarctica and Greenland

<p>Antarctica and Greenland </p>
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43

How do alphine glacier move ?

downhill

<p>downhill</p>
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44

How do continental icesheets?

move outward from the center where mass of ice is the greatest

<p>move outward from the center where mass of ice is the greatest</p>
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45

How do glaciers move?

plastic flow

basalt sliding

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46

What happen when more snow is add than lost?

accumulation> ablation

Glacier advances (grows)

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47

What happens when more snow is lost than gained

accumulation> ablation

Glacier retreats shrinks

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48

What are the two forms of weathering for glacier?

Abrasion and frost wedging

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49

Glacial deposits

angular poorly sorted grains

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50

Glacial erratic

isolated large-grain remnants of glacial deposits

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51

Moraine

piles of sediment dropped or spit out by glacier

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52

Which landromed is produced through meltwater dissoposits from the toe of a glacier

outwash plain

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53

The bigger the glacier, the bigger the valley and …

bigger the cirque

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54

Glacier cover blank% of land surve todya and blank% 18,000 years ago(iceage)

10 and 30

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55

Clastic

fragment of pre-existing rack (sandstone)

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56

Chemical

precepted from solution Carbonate)

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57

Biochemical

organisms play a role (shell material)

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58

Organic

comprising large amounts of organic material

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59

Weathering

The decomposition and disintegration of rocks and minerals at the earth’s surface by machinal and chemical processes

  • converts rock to gravel, sand, clay and soil

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60

Erosion

The removal of weathered rocks and minerals for the place they were found

  • water

  • wind

  • glaciers

  • gravidity

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61

Mechanical weathering

The physical disintegration rock into smaller pieces each retaining there original characteristics

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62

Chemical weathering

decomposition of rock and minerals and as a result f chemical reactions (removal and/or addition of elements)

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63

What are the main processes of chemical weather?

  • frost wedging

  • salt cracking

  • abrasion

  • biological activity

  • thermal expansion and contracting

  • pressure release fracturing

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64

Frost wedging

when water freezes it expands and water migrates into cracks in rocks. Ice crystals growth puts tremendous pressure on surrounding rocks

Most effective in mountain areas where daily freeze/ thaw. Dangers to hikers

<p>when water freezes it expands and water migrates into cracks in rocks. Ice crystals growth puts tremendous pressure on surrounding rocks </p><p>Most effective in mountain areas where daily freeze/ thaw. Dangers to hikers </p>
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65

Salt cracking

salts crystallize in cracks puts pressure on surrounding rock

Important in

dry climate:

costal areas

<p>salts crystallize in cracks puts pressure on surrounding rock</p><p>Important in </p><p>dry climate: </p><p>costal areas</p>
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66

Abrasion

breakdown of rock by fiction and impact

  • gilders(effective)

  • wind

  • running water(effective)

  • waves(effective)

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67

Biological activity

  • plants growing in cracks in rocks

  • burrowing animals

  • human blasting for roads, development exploration

<ul><li><p>plants growing in cracks in rocks</p></li><li><p>burrowing animals</p></li><li><p>human blasting for roads, development exploration </p></li></ul>
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68

Pressure release fracturing

  • buried rocks are under confining pressure

  • when exposed they expand due to releasing

  • problem for miners

<ul><li><p>buried rocks are under confining pressure</p></li><li><p>when exposed they expand due to releasing</p></li><li><p>problem for miners</p></li></ul>
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69

What is the main agent of chemical weathering

water

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70

Dissolution

produces ions ( not minerals) and are reversable is the solvent is removed

Ex dissolving soluble materials in water, the salt is re-participated if the water evaporates

Salt deposits are creating with the drying of ancient seas

<p>produces ions ( not minerals) and are reversable is the solvent is removed </p><p>Ex dissolving soluble materials in water, the salt is re-participated if the water evaporates </p><p>Salt deposits are creating with the drying of ancient seas</p><p></p>
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71

Example of dissolution

Natural rain water fall through the soil and reacts with C02 to form carbonic acid.

Carbonic acid reacts with calcite (Limestone) to produce it

<p>Natural rain water fall through the soil and reacts with C02 to form carbonic acid.</p><p>Carbonic  acid reacts with calcite (Limestone) to produce it</p>
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72

Hydrolosis

where dissolution involves the release of ions from a mineral

  • is a reaction with water to form a hydrated mineral

<p>where dissolution involves the release of ions from a mineral</p><ul><li><p>is a reaction with water to form a hydrated mineral</p></li></ul>
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73

Oxidation

reaction with oxygen

ex iron bearing minerals oxdize to form rust

<p>reaction with oxygen </p><p>ex iron bearing minerals oxdize to form rust </p>
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74

What are the control on rates and types of weathering

  • climate

  • Oxygen and C02 in the atmosphere and soil

  • Minerology

  • Surface area- how fragmented the rock is

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75

What are characteristics of sedimentary rocks?

Clast textures:

Size

Shape

Sorting

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76

What is the majour control on size, shape, and sorting?

Agents of transportation:

  • gravity

  • wind

  • water

  • ice

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77

What is an example of chemical; and biochemical sediment

Limestone

  • formed from shell fragments and test (shells of microfossils)

<p>Limestone</p><ul><li><p>formed from shell fragments and test (shells of microfossils)</p></li></ul>
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78

What are the four general ways that produce volcanic rocks of different compositions

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