plate tecs gw 2 Flashcards

1
Q

how are fold mountains formed?

A
  • formed along convergent plate boundaries
  • compressional force creates immense pressure
  • layers of rock buckle and fold
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2
Q

what are some examples of fold mountains?

A
  • atlas mountain
  • swiss alps
  • andes
  • himalayas (tibet)
  • barisan
  • rocky mountains (NA plate)
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3
Q

name locations of fold mountains

A
  • convergent plate boundaries
  • himalayas: across southern asia (indian and erusian plate)
  • rocky mountains (juan de fuca and north american plate)
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4
Q

how are rift valleys formed?

A
  • valley with steep sides and flat floor
  • formed due to tensional forces
  • fault lines are formed
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5
Q

how are block mountains formed?

A
  • block of land with steep sides

- formed when sections of the crust extends along fault lines and rock masses

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6
Q

where are rift valleys and block mountains found?

A
  • divergent plate boundaries
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7
Q

what are the characteristics of volcanoes?

A
  • viscosity
  • low-silica
  • high-silica
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8
Q

define viscosity?

A

viscosity is the stickiness of lava/resistance to flow

like you compre pouring water to pouring chocolate sauce right chocolate sauce got higher viscosity

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9
Q

how does low-silica affect the volcano?

A
  • lower viscosity –> less explosive eruptions
  • allows gases to escape easily –> flows more easily through the vent by reaching surface
  • outer layer of the cooling lava forms a thin crust
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10
Q

how does high-silica affect the volcano?

A
  • higher viscosity –> more explosive eruptions
  • traps gases easily –> built up pressure below earth’s surface
  • magma rises through earth’s surfaces –> gases expand –> outward explosion
  • ejects: lava, ash, rock fragments and gases into the surrounding environment
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11
Q

what are the physical characteristics of shield volcanoes?

A
  • gently sloping sides

- broad summit

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12
Q

how are shield volcanoes formed?

A
  • formed when low silica lava (lsl) is ejected
  • lsl flows easily and spreads out over a large are before solidifying
  • lava doesn’t trap as much gas, not as explosive
  • base of volcano increases in size as lava accumulates
  • usually near divergent plate boundaries where magma can rise directly
  • i.e. mount washington in USA
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13
Q

how are stratovolcanoes formed?

A
  • develop from successive eruption of lava and pyroclastic
  • subsequent eruption ejects lava which covers pyroclastic and prevents it from eroding
  • successive eruptions build a high volcano with slightly concave profile
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14
Q

what are the physical characteristics of stratovolcanoes?

A
  • steeper at the top and gentler at the base; secondary cones may develop
  • mainly found at convergent plate boundaries
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15
Q

what is an active volcano?

A
  • currently erupting

- i.e. pacific ring of fire

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16
Q

what is a dormant volcano?

A
  • currently inactive but may erupt in future

- i.e. mount hood, oregon, USA

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17
Q

what is an extinct volcano?

A

volcanoes w/o seismic activity/geological evidence of eruption for past thousand years

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18
Q

what are the risks of living near volcanic areas?

A
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19
Q

what are the risks of living near volcanic areas?

A
  • massive destruction by volcanic areas

- pollution

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20
Q

explain massive destruction by volcanic materials

A
  • lava and pyroclast consists of ash, rock fragments, volcanic bombs
  • widespread damage to property
  • lava: has high temperature of 500-1400 degrees celsius and burns the area if it flows through
  • low-silica lava: moves rapidly and flows long distances; damage to larger areas
  • pyroclastic flow: destroys everything in its path with hot rock fragments at great speeds :( inhaling hot ash and gases can result to serious injury/death
  • volcanic bombs: fall in areas surrounding volcanoes and causes damage to property
  • landslides: have potential to obstruct flow of rivers; block roads, bury village and farmlands
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21
Q

name an example of massive destruction by volcanic materials

A
  • i.e. andes mountain, south america, 1985
  • pyroclastic flow
  • mixing of pyroclastic and glacial ice triggered laharas
  • engulfed the town and killed more than 20000 people
22
Q

explain pollution as a risk of living near volcanic areas

A
  • ash: disrupts human activities over large distances; thick plumes of ash settle on the ground; blocks sunlight; suffocates crops; severe respiratory problems to people and animals
  • gases: carbon dioxide; sulfur dioxide; hydrogen; carbon monoxide –> HARMFUL TO PEOPLE
23
Q

how is fertile soil a benefit of living near volcanoes?

A
  • lava and ash break down to form FERTILE volcanic soils
  • richest soils on earth
  • super favourable to agriculture
  • although rich in minerals, they are not available for planting when the rocks are not broken down (only avail. after 1000+ years)
24
Q

what is example of a area with fertile soil?

A
  • i.e. volcanic soils of java and bali in indonesia cultivate tea, coffee and rice
25
how is precious stones and minerals a benefit of living near volcanoes?
- can only be extracted from volcani areas after millions of years when upper layer of volcanic rocks are eroded
26
example of an area for precious stones and minerals
- i.e. diamond: cold volcanic rocks at kimberly, south africa; heated and pressured carbon; can be used for industrial tools and scientific research and jewellry
27
how is tourism a benefit of living near a volcano?
- hiking; camping; enjoy the scenery | - rich in history, can learn about the volcano
28
what is an example of tourism?
- i.e. ruins of pompeii italy - roman town buried by layers of ash from mount vesuvius in 79CE; unearthed to reveal building, pottery, mosaic, visited by almost 3 mil people every year
29
how is geothermal energy a benefit of living near volcanoes?
- derived from the heat in earth's crust - grounwater in contact with hot rocks beneath surface --> heats up --> erupts as hot water/steam --> drive turbines and produce electricity
30
what is an example of geothermal energy?
- i.e. iceland's electricity: 70% from geothermal power
31
what are earthquakes?
- vibration in the earth's crust caused by sudden release of stored energy in rocks along fault lines - plate movements along plate boundaries
32
how are earthquakes formed?
friction between moving plates --> slow build up of stress on rocks on sides of fault --> rocks can no longer withstand increasing stress (same) --> rocks suddenly slip many metres
33
explain further the formation of earthquakes?
- releases energy in the form of seismic waves - most of the energy released by EQ travels along surface of earth - stress from ground after EQ may cause aftershocks - series of aftershocks may occur for several months
34
what are the characteristics of deep-focus EQ?
- 70-700km below earth's surface | - takes a longer time to reach surface has lost most energy by the time reached ES smaller impact on land
35
what are the characteristics of shallow-focus EQ?
- in upper 70km of earth's crust | - seismic waves reach ES quickly greater impact on land
36
what are the factors affecting the extent of an earthquake?
- population density - level of prepardness - distance from epicentre - time of occurrence - type of soil
37
how does population density affect the extent of an earthquake?
- number of people living in affected area - more people, more affected - EQ in cities can cause more casualties and damage
38
how does the level of prepardness affect the extent of an earthquake?
- amount of preparation by authorities and citizens - evacuation plans. trained rescue workers, actions plans, drills - more prepared, fewer casualties, less chaos
39
how does the distance from epicentre affect the extent of the earthquake?
- closer to epicentre, more damage - i.e. christchurch, new zealand, 2011; epicentre in town a few km from city centre --> further from city centre had less damage --> city a lot of damage
40
how does the time of occurence affect the extent of an earthquake?
- at night --> people sleeping --> no time to evacuate --> more damage
41
how does the type of soil affect the extent of an earthquake?
- sediments loose and unconsolidated --> seismic waves amplified - structures built on saturated and unconsolidated sediments --> liquefaction
42
where are most earthquakes located at?
- can occur on convergent, divergent, transform - mostly @ convergent - 75% of pacific ring of fire
43
what are the risk associated with living in earthquake zones?
- tsunamis - disruption of services - landslides - destruction of property - desturction of infrastructure - loss of lives
44
how are tsunamis formed?
- formed by: movement of sea floor during large EQ; explosive underwater volcanic eruption; underwater landslide above sea level
45
explain the formation of tsunamis in greater detail
- seismic energy from offshore EQ forces out mass of seawater - tsunami waves may start at height of <1m, wavelengths of 100-150km, but pass undetected - point of impact on coast, tsunami waves could be travelling at 30-50km/h, may reach heights of 15m - sometimes sea recedes from coast before advancing offshore, minutes before the tsunami reaches above - can travel long distances and cuase widespread destruction @ coastal areas
46
what is an example of a tsunami?
- i.e. indian ocean , 9.2 EQ, 2004 - triggered tsunami; waves spread throughout indian ocean - damage to coastal communities of 12 countries
47
explain disruption of services as a risk of living in earthquake zones?
- supply of electricity, gas, water - vibrations can snap pipes and break cables - cause fires - communication servies disrupted
48
example of disruption of services?
- i.e. kobe, japan, 1995: damaged pipes and transmissiom lines, disrupted gas and water, affected 1.4 million residents
49
explain landslides as a risk of living near earthquake zones?
- shaking of ground can weaken slopes of hills and mountains - unstable slopes --> landslides - rapid downslop movements of soil, rock, vegetation and debris - mudflow occur if there is heavy rainfall, saturating soil, mixed soilid debris flow down
50
explain destruction of property as a risk of living near earthquake zones?
- widespread destruction of homes - homelessness - can only reside in temporary shelters as homes are rebuilt
51
explain destruction of infrastructure as a risk of living near earthquake zone?
- EQ may cause cracks to forms in infrastructure - road and bridges damaged - affects transporation, unsafe to use damaged roads - takes longer for help to arrive, increased death toll