Tectonic Plates Flashcards

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1
Q

What layers does the earth consist of?

A

Continental crust, oceanic crust, mantle, outer core, inner core.

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2
Q

What are the properties of the continential crust?

A

10-70km thick, rich in silicates and aluminium minerals

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3
Q

What are the properties of the oceanic crust?

A

5km think, more dense with composition similar to basalt

Rich in magnesium and silicate minerals

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4
Q

What are some properties of the mantle?

A

Thickest layer of the earth, molten rock with convection currents in the upper mantle, high tempreture and pressure

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5
Q

What are some properties of the outer core?

A

Liquid, contains Fe, Ni and some lighter elements, convection currents in the outer core may be responsible for the earths magnetic field

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6
Q

What are some properties of the inner core?

A

Solid, made mostly of Fe with some Ni

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7
Q

What is the total depth of the crust?

A

0-100km

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8
Q

What is the total depth of the mantle?

A

100-2900km deep

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9
Q

What is the total depth of the outer core?

A

2900-5100km deep

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10
Q

What is the total depth of the inner core?

A

5100-6378km deep

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11
Q

What happens when a seismic wave passes from a slower velocity layer to a higher velocity layer?

A

The seismic wave is refracted up

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12
Q

What happens when a seismic wave passes from a higher velocity layer to a slower velocity layer?

A

The seismic wave is refracted down

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13
Q

What can the reflection of seismic waves be used for?

A

It can be used to determine the depth of a layer within the earth

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14
Q

What was the shrinking theory?

A

The shrinking theory rose in the 1800s when geologists believed that due to the crust cooling down it formed continents valleys and mountains and when it cooled the heaver metals sunk to the core while less dense materials stayed or rose the surface.

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15
Q

What does continental drift mean?

A

It means that millions of years ago all the continents made one large super continent which eventually broke up leaving singlular continents.

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16
Q

Who proposed the continental drift theory?

A

In 1912, a German meteorologist named Alfred Wegener proposed a new theory.
He had noticed that the present day continents looked as though they would fit together very much like a jigsaw puzzle.

17
Q

What did Alfred Wegener propose?

A

Wegener suggested that the continents were floating, or drifting, on a denser material underneath.
He proposed that the continents were breaking apart and rejoining in a process that he called continental drift.

18
Q

What was Pangea?

A

Pangea was surrounded by a global ocean called Panthalassa, and it was fully assembled 299 million to 272 million years ago
The supercontinent began to break apart about 200 million years ago
Eventually forming the modern continents and the Atlantic and Indian Oceans

19
Q

What was Laurasia?

A

Laurasia,ancient continental mass in the Northern Hemisphere that included North America, Europe, and Asia (except peninsular India)
Wegener had postulated a single supercontinent, Pangea
Du Toit, another scientist, theorised that there were two landmasses: Laurasia in the north and Gondwana in the south, separated by an oceanic area called Tethys

20
Q

What was Gondwana?

A

Gondwana, ancient supercontinent that incorporated present-day South America, Africa, Arabia, Madagascar, India, Australia, and Antarctica
The first stage of its breakup began about 180 million years ago
Alfred Wegener, envisioned a single great landmass, Gondwana comprised the southern half of his supercontinent

21
Q

What was the evidence for the continental drift?

A

The same fossils of plants and animals could be found on different continents
Mountains were formed when the edge of a drifting continent collided with another, causing it to crumple and fold

22
Q

What is the atmosphere?

A

A blanket of gases that surrounds the Earth to a height of approximately 145km. Mostly made up of nitrogen and oxygen, which support life on earth.

23
Q

What is the tempreture of the mantle? (celcius)

A

500-2000

24
Q

What is the tempreture of the outer core?

A

4000-6000

25
Q

What is the hydroshpere?

A

The water on or at the surface of the Earth including oceans, lakes, rivers, rain and mist.

26
Q

What is the tempreture of the inner core?

A

up to 7000

27
Q

What is the evidence for plate tectonics?

A

Mapping of the ocean floor revealed the presence of mid-ocean ridges
Mid-ocean ridges are undersea volcanic mountain ranges
New seafloor is formed at these ridges in a process known as seafloor spreading
Molten rock from inside the Earth rises into the gap and cools and solidifies into new rock
As it solidifies a record of the Earth’s magnetic field is locked into the new rock
As you move further away from the ridge the age of the rock increases
Magnetic particles in molten rock align with Earth’s magnetic field
Magnetic record is stored within the rocks when they cool and solidify
The pattern of reversed polarity repeats on either side of mid-ocean ridges

28
Q

What are convetion currents and how do they work?

A

Hot metallic core causes the mantle directly above it to heat up
As the liquid rock in the mantle heats up it rises
When it reaches the top of the mantle it gets pushed aside by more mantle rising below it
As the hot liquid spreads out it cools and sicks to the bottom of the mantle layer
It is reheated by the core and the cycle of heating and cooling begins again

29
Q

What are convection shells?

A

The closed system of the mantle results in ‘convection cells’
Local regions of liquid or gas that form a relatively stable cycle of heating, rising, moving aside, cooling and sinking

30
Q

What are tectonic plates?

A

Earth composed of many plates which are in constant motion due to the convection currents beneath them
Plate boundaries have been identified by mapping zones of earthquake and volcanic activity along with mid ocean ridges

31
Q

What is a Divergent and its properties?

A

plates pull apart, creates a ridge/rift, allows volcanic activity and creates oceanic lithiosphere.

32
Q

What is a Convergent and its properties?

A

Its the collision of plates, subducts, destroys oceanic lithiospheres creats trenches and allows for volcanic activity.

33
Q

What is a Transform?

A

Plates grind past each other, lateral sliding, a lithiosphere is not created or destroyed, no major effect on land, and doesnt allow for volcanic activity.

34
Q

Extra information on Divergent boundaries (don’t recall but still good to know for exam)

A

Mid-ocean ridges, Iceland, African rift Valley
Produce few earthquakes because plates pulling apart
Not storing up energy as they collide or rub past each other
Plates moving apart forming a gap where magma is pushed up from the mantle below
Lots of volcanoes, thermal vents and great broken rifts in the Earth occur at divergent boundaries

35
Q

Extra information on Convergent boundaries (don’t recall but still good to know for exam)

A

Subducting convergent boundaries can be found along the north-western edges of the Pacific Plate, the west coast of South America and the north-eastern edges of the Indo-Australian Plate
Produce a combination of volcanoes and earthquakes
A lighter plate floats on top while another plate dives below – subduction
Submerging plate melts and the resulting magma bubbles up through cracks in the overlaying crust to form volcanoes
Continent-to-continent convergent boundaries, such as Himalayas
Produce lots of earthquakes but very little volcanic activity
Continental crust on both sides is light and resists subduction
Continents buckle and crumble against one another, gradually rising skywards

36
Q

Extra information on Transform boundaries (don’t recall but still good to know for exam)

A

San Andreas fault on land, most others lie on the ocean floor
Produce lots of earthquakes and only occasional volcanic activity
Plates moving past one another
Store energy between them until the friction holding them together gives way in the form of an earthquake

37
Q

What is a hotspot?

A

Volcanic regions thought to be fed by underlying mantle that is anomalously hot compared with the surrounding mantle
They may be on, near to, or far from tectonic plate boundaries.
Well known examples include Hawaii and Yellowstone