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Earth > Easter > Flashcards

Easter Flashcards

1
Q

What is the Caledonian orogeny associated to?

A

The closure of the Iapetus ocean
Scotland and England colliding
Grampian, Scandian, Acadian

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2
Q

What is a terrane?

A

An area bounded by a fault with distinct features and geological history

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3
Q

What is the hinterland and the foreland?

A

Hinterland- land near a deformation front
Foreland- land far away from a deformation front

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4
Q

What is type locality?

A

Internationally agreed location where the boundary between 2 periods can be seen.
Based of fossil assemblages, such as graptolites in Dob’s Lin, Scotland

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5
Q

What are the 5 main sutures in Scotland?

A

Moine Thrust
Great Glen Fault
Highland Boundary Fault
Southern Uplands Fault
Iapetus Suture

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6
Q

What are the 3 main orogenies and when did they occur?

A

Cadomian (Neoproterozoic- Cambrian)
Caledonian (Ordovician- Devonian)
Variscan (Carboniferous)

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7
Q

What are glaciations and evidence for them?

A

When ice isn’t only found at the poles
E.g. Quaternary glacial and interglacial cycles
Evidence are dropstones, boulder clay at Ketton Quarry found at the end of a glacier when it melts

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8
Q

How can past temperatures be determined?

A

Oxygen isotopes O18/O16
Look at foraminifera, greater means less O16 so more ice= colder temps

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9
Q

How does atmospheric CO2 correlate with length of subducting zones?

A

More subducting zones more CO2 in the atmosphere, this is due to volcanic gassing
So more CO2 is released, and may also be correlated with temp as it can act as a greenhouse gas

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10
Q

What is the difference between eustatic and isostatic?

A

Eustatic changes worldwide, in sea level
Isostatic local changes in topography due to uplift

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11
Q

What is extensional subduction?

A

Cold dense oceanic lithosphere subducting
Leads to slab roll back
Leads to extensional basin

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12
Q

What is contractional subduction?

A

Warm oceanic lithosphere subducts
Subducts as a flat slab, which can be detected by using seismography
Causes orogenic shortening

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13
Q

What is the arc-continental collision?

A

Causes flipping of subduction direction
e.g. Taiwan

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14
Q

What is continental- continental collision?

A

Causes the formation fold mountains
Plates are thrust up
e.g. Himalayas

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15
Q

What are the key points in the history of UK?

A

550Ma- Iapetus subducting beneath Gondwana, passive margin
490Ma- Iapetus subducting under, however no longer passive
470Ma- Taconic arc and Laurentia, Arc-continent collision
440Ma- Avalonia, Baltica and Gondwana close Iapetus
360Ma- Pangea forms
200Ma- Thulean plume opens up the Atlantic Ocean

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16
Q

What are the stages in rifting?

A

Extension- Rising melt causes crustal thinning
Subsidence- lithosphere cools and sags, creates accommodation space

17
Q

What is the earthquake cycle?

A

Stages in the formation of an earthquake (easily drawn), where pressure builds up due to dragging down of a plate.
Further away from subduction experiences subsidence (Banda Aceh, Indonesia)
close experiences uplift (simeulue Island, Indonesia)

18
Q

What is evidence for earthquakes?

A
  • Changes in river location
  • Movement of lake beds
  • Movement of qanats (water extractors)
  • Radio interferometry (satellites)
19
Q

What are tsunamis?

A

Shallow water waves where wavelength is longer than the water depth, their speed is only dependent on depth

20
Q

What are the effects of a tsunami and earthquake?

A

Lateral and vertical movement (uplift and subsidence) also in Japan, detected lateral movement of cities due to squeezing then stretching of plate

21
Q

What are two types of basaltic eruptions?

A

Strombolian- large gas bubbles build up, shorter eruption duration
Hawaiian- Fountain like, on eruption time

22
Q

What are the different regions in an eruption column?

A

Gas thrust region
Convective region
Umbrella region

23
Q

How is the density changed in the eruption column?

A

Speed of ejection of ash
Amount of air entrained in the convective region
Radius of conduit, larger radius, greater area for air entrainment

24
Q

What are the two types of rhyolitic eruptions?

A

Plinian- high up into the atmosphere, fast exit velocity and lots of entrainment of air, less dense
Vulcanian- collapse of ash column, slow exit velocity, denser = Pyroclastic flow

25
Q

What are volcano examples?

A

Mt Tambora, Indonesia 1816- year with no summer
Krakatoa, Indonesia 1883- 0.6 degree cooling
Mt Pinatubo, Philippines 1991- led to global cooling of -0.5degrees for 2 years
Eyjafjallajokull - 2010, grounded planes due to the large ash cloud

26
Q

What are long term and short term changes to climate?

A

Short- Milankovitch, burning fossil fuels, feedback cycles
Long- Volcanic degassing, weathering

27
Q

What is silicate weathering?

A

Weathering of silicate rocks by acid rain, leading to ions being washed into the sea and taken up by organisms incorporating it into their shell, when they die form carbonate rock, and remove CO2

28
Q

How has demand and sourcing of energy changed?

A

Demand has increased massively, more in industry, transport and household
Slowly reducing coal, and increasing renewable energy, however oil and gas still very big providers

29
Q

How do oil and gas reserves form?

A

Organic rich rock provides carbon
Migrates to porous rock (sandstone)
Trapped by a seal of rock
Heated to around 100 degrees

30
Q

What are critical metals?

A

Metals that can’t easily be substituted for another and are essential in modern technology

31
Q

What are the case studies for aquifiers and water use?

A

Southern Spain
Mexico city
Bangladesh (As poisoning)

32
Q

What are the different types of aquifiers?

A

Unconfined- open to infiltration by rainwater
Confined- trapped under a seal rock

33
Q

What makes a good aquifier?

A

Porosity- gaps for water to be stored
Controlled by cementation, grain size, grain organisation

34
Q

What are different types of well?

A

Artesian- comes out by itself, surface of the well is below the water table
Water table well- water needs to be pumped out, surface of the well is above the water table
Water table being the boundary between the zone of aeration and zone of saturation

Earth (4 decks)

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