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Places To Find Volcanoes

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1

Places To Find Volcanoes

Subduction Zones, Divergent Boundaries,

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2

Subduction Zones at Volcanies

Subduction Zones have soggy plates and if you add water there is a mass melting curve

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3

Divergent Boundaries

Rift zones wehere continet breaks apart

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6

 

 

 

 

Volcanoes are not;

 

 

at plate boundaries

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7

How to tell if there are volcanoes?

Hotspots; intraplate volcanism by forming mantle plume

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10

Map View of Present Vs 100 million years ago of Volcanoes

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11

Volacno Eruption Characteristics

Explosive vs. Effusive Eruptions

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12

Explosive

more dangerous

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13

Effusive

gentle eruption like lava flows

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14

What makes an eruption explosive or not?

 

Viscosity

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15

Viscosity

more viscous= resistance to flow, thicker + sticker

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16

 Higher viscosity=

 more explosive/ less flow

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17

Lower viscosiy=

more flow

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18

Body Waves

P-Waves + S Waves, energy moves from one place to another in the Earth's interior

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19

P Waves

primary waves; compressional through solid, liquid, gas, faster than S waves, parallel,

 

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20

S Waves

Secondary waves, perpendicular, only travel through solids, more damaging than P Waves

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21

  Long Term Predictions (Definition)

Indicate Earthquakes in the future.

 

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22

Long Term Predictions (2)

  1. History; written remarks of what/when in the past.

  2. Seismic Gaps; Spatial & temporal

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23

Spatial gap;

a physical area where  eqs are expected; but we don't see any

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25

Temporal gap;

 

relates to time---> timeline

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27

  Where do we find EQs? (3)

  • Any Plate boundaries  (divergent convergent, transform)

  • Anywhere with volcanism (subduction + hotspots)

  • Faults (crack in a rock where there is movement along the crack)

 

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28

Elastic Deformation

brittle/breakable, will go back back to original form after stoss is released or will break.

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29

Plastic deformation

impose stress on a material  + it doesn't break, ductile/ foldable

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30

Material Side Effects/Hazards (5)

  • Ground shakes

  • Tsunami; a big wave caused by the displacement of water  

  • Land displacement

  • Fires

  • Mass wasting

 

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31

Seche

 liquid water that is slashed back and forth

 

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32

Liquifaction

ground that appeared to be solid, movemennt causes the ground to liquefy; to liquidfy by freezing up groundwater.

 

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33

Short Term EQ Predictors (Definition)

change in well (water, gas) level, indicates movement/breaking of rocks underground

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34

Short Term EQ Predictors

Sudden radan emmissions

  • Laser strikes across faults to detect movement

  strange animal behavior

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35

Mass Wasting

lose material moving down a hill

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36

Requirements of Mass Wasting

1. hill/slope where the gradient is not zero. 2. lose material; something connected to the hill  3. Gravity

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37

Angel of Repose

the angel a slope needs 1/10 to be at for mass wasting to happening: factors/processes that change angels.

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38

Spatial Gap

physical location

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39

Temporal Gap

gaps in time

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40

Can spaital + temporal gaps go together

overlap yes

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45

Saltation

materials that bounce/jump along the bottom.

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47

Transport of Materials/Transportation (3)

Bed load, dissolve load, suspend load

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48

Bed Load

More heavier materials that roll bounce along the bottom

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49

Dissolve Load

Chemically broken down ions/molecules

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50

Suspend Load

Materials that float somewheare in the water

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52

Normal Fault

hanging wall moves down relative to footwall

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53

Reverse Fault

hanging wall moves up relative to footwall

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56

Geologic Jobs of Moving Water

  1. Transportation

  2. Erosion

  3. Deposition

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57

Erosion= (2)

weather + move it

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58

Deposition

is how rocks, soil, and sediments are added to landforms by natural forces like water, wind, or ice

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59

Deposition where it is and what it is


Left side of curve line of river, point bar, fuffles


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60

Cut Bank (Definition + location)


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61

Stream Piracy


Occur when a stream diverted from its own bed and flow instead down bed of neighbour system.


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62

Mender River Dynamics

Point Bars, Cut Banks, Oxbow lakes, the tale of the meander cutoff


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63

Chance annual floods


1/100

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64

Recurrence Interval Example


100 yr flood


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65

How to deal with floods? (6)


  • build on '“stilts”

  • use flood walls

  • levee

  • create drainage paths/ retention ponds

  • Dams

  • channelization


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66

Recurrence Interval


The time between two consecutive occurrences of an event. Helps estimate the likelihood of an event happening again in a given timeframe.


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67

Point Bars (2)


are crescent-shaped deposits of sediment that accumulate on the inside bend of streams and rivers below the slip-off slope. They are composed of sediment that is well-sorted and typically reflect the overall capacity of the stream.


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70

Mender River Dynamics (4)


Point Bars, Cut Banks, Oxbow lakes, the tale of the meander cutoff


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71

Types of Volcanoes for Viscosity (3)

Shield Volcanoes, Strato Volcanoes/Composite Volcanoes, Cinder Cone

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72

Pycrolastics (2)

the material shot into the air by a volcano + indicates explosive eruption

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73

Material Inside Pyroclastics

ash + volcanoes

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74

Strato Volcano/Composite Volcano

 more viscous/ more explosive

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75

Cinder Cone

rarerly explosive + has all pyroclastics

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76

Lava vs magma

lava: above ground

magma; below ground

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77

Shield Volcanoes

 lower viscosity

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78

Types of Mass Wasting (5)

Creep, Flow, Slump, Slide, Fall

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79

Creep

Slowest type

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80

Flow

downhill flow of liquidy material

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81

Slump

Sliding down a curved surface

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82

Slump Indicators

Round scarp, hummanky terrain

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83

Slide

Solid block becomes disemented + slides down

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84

To Change Angel (2)

add/remove water, type of material

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85

Mass Wasting

Lose material moving down a hill

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86

Positives of Dams (2)

renewable energy + stop flooding

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87

Negatives of Dams (4)

disrupt our ecosystem, flood the upstream, dam can also break, load is deposited upstream

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88

What controls viscosity of Volcano

Mafic vs Felsic

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89

Felsic

abundant Si + Al, explosive

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90

Mafic

Low silica + less explosive

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