lecture 3 earths core and geomagnetism Flashcards

1
Q

how was the core mantle boundary discovered

A

s h a d o w z o n e

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2
Q

what is the shadow zone

A

an area of the earth where waves from an earthquakes are not detected. s waves disappear completely and p waves come back later than expected

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3
Q

how do you interpret the s h a d o w z o n e

A

waves are refracted away from the surface (towards the normal) at a low velocity layer

low velocity explains why p waves arrive later than expected

s waves don’t reappear so must be liquid

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4
Q

how deep is the core mantle boundary

A

2900km

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5
Q

how was the inner core discovered

A

identification of PKIKP phase in shadow zone

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6
Q

what does the main p wave shadow zone contain

A

some weak arrivals with long travel times

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7
Q

to what did inge lehmann attribute the some weak arrivals with long travel times

A

refractions and reflections from an inner core

p wave velocities increase in inner core

s waves reappear transformed from s waves so inner core must be solid

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8
Q

how deep is the inner core

A

5150km

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9
Q

what is the composition of the core

A

mostly iron with lighter elements like nitrogen, sulphur and oxygen

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10
Q

how do we know the cores composition

geochemical evidence

A

sun and meteorites have lots of iron

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11
Q

how do we know the cores composition

geophysical evidance 1 seismology

A

constrains density and elasticity which can be tested in a lab

Seismic waves through the inner core travel about 4
percent faster when they’re moving N-S, (along spin
axis), than when they’re moving E-W which explained by computer modelling could mean the core is one giant Fe crystal!

inner core is growing slowley as it cools

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12
Q

how do we know the cores composition

geophysical evidence 2 electric boogaloo geomagnetism

A

The Earth has a magnetic field, which must be
generated by convection of an electrically
conducting liquid in the outer core – liquid iron
fits the bill!

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13
Q

how many degrees is the earths magnetic field tilted from earths rotation axis

A

10 degrees

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14
Q

what is a dipmeter

A

• A compass whose needle can move in

a vertical plane is called a

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15
Q

what is another name for angle of dip

A

magnetic inclination

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16
Q

how is angle of dip measured

A

relative to the horizon

17
Q

if its horizontal dip =

A

0 degrees

18
Q

if its verticle dip =

A

90 degrees + or -

19
Q

magnetic field is strongest at

A

magnetic poles

20
Q

magnetic field is weakest at

A

magnetic equator

21
Q

how is the geomagnetic field generated

A

• The Earth’s interior is too hot (above the Curie temp) for
permanent magnetism to be possible.
• The geomagnetic field is generated by convection currents
in an electrically conducting (metallic) liquid in the outer
core. The core acts like a self-exciting dynamo. • The pattern of fluid flow is not well understood, but is
probably crucially affected by the presence of the solid inner
core, and the rotation of the Earth.
• This explains why the geomagnetic field is aligned, on
average, with the Earth’s spin axis.

22
Q

what happens every few thousand years

A

poles flip 180