three worlds to explore
DESCRIPTION
Look Up? (Astronomy). Three Worlds to Explore. Look at Surface? (Geology). Look Down? (Geophysics). The Earth’s Interior. Deep wells and boreholes (4 to 12 km). Astronomical Observations. The Earth: What’s it made of?. Gravity. Seismology. N. S. Magnetism. Heat Flow. - PowerPoint PPT PresentationTRANSCRIPT
Three Worlds
to Explore
Look Up?(Astronomy)
Look Down?(Geophysics)
Look at Surface?(Geology)
The Earth’s Interior
Deep wells and boreholes(4 to 12 km)
The Earth:
What’s it made
of?
Gravity
Seismology
Magnetism
S
N
Heat Flow
Astronomical Observations
Crust2.6-3.1 gm/cm3
Mantle3.3-5.7 gm/cm3
Outer Core10-12 gm/cm3
Inner Core13-14 gm/cm3
Density of Water1 gm/cm3
P and S Wave Paths
Relatively simple experiment to estimate some basic properties of the Earth’s interior:
Mass = M
Radius = R
Average Density = D
Rough Estimate of Variation of Density in
Interior
Newton’s Law of Gravitation
M
Fr
mF
Force of attraction (F) is proportional to the masses, and is inversely proportional to the square of the distances between the
masses.
€
F = GMmr2
Newton’s Law of Gravitation
MF
r
mF
Henry Cavendish (1731-1810) determined the universal constant of gravitation G in 1798.
massive lead spheres
torsion fiber
€
F = GMmR2
M
F m
R
€
M = F R2
Gm
M
F m
R
€
M = F R2
Gm
Measure the force
Use a known mass
Can measure in lab
?
If we could measure R,we could determine M.
How can we measure R?
Greek Scientist:
Eratosthenes
(276-194 BCE)
Eratosthenes (276-194 BCE)
Observed the angles of the noonday Sun in two Egyptian cities that were roughly north and south of each other.
Syene (presently Aswan) and Alexandria
Eratosthenes (276-194 BCE)
The angles differed by 7 degrees (or 1/50 of a complete circle).
Circumference of the Earth must be 50 times the distance between the cities.
Eratosthenes (276-194 BCE)
The cities are 788 km apart.
Circumference of the Earth must be 50 x 788 km= 39,400 km
R = 39,400/2 = 6,271 km (modern value = 6,371 km)
The Earth:
What’s it made
of?
Gravity
Seismology
Magnetism
S
N
Heat Flow
Astronomical Observations
M
F m
R
€
M = F R2
Gm
Measure the force
Use a known mass
Can measure in lab
M = 6x1027 gm =6,000,000,000,000,000,000,000,000,000 gm
Eratosthenes
M
R
€
Density = Mass
Volume
Average Density = 5.5 gm/cm3
€
Volume = 4
3πR3
Average density of the Earth = 5.5
gm/cm3
Average density of
crustal rocks= 2.7 gm/cm3
Density must increase with
depth.
Dense Material?
Density must increase with
depth.
But, how can we obtain a
more detailed picture of the variation of density with
depth?
Dense Material?
Astronomical Observations
Earth’s axis of rotation points towards different stars at different times.
Gravitational forces from the Sun and the Moon cause the Earth to twist and turn in its orbit around the Sun.
“Precession” of the Earth causes the North Pole to point to different parts of the sky during a 26,000 year cycle.
“Precession” of the Earth is similar to the motion of a spinning top.
From precession of the Earth it is possible to measure the moment of inertia of the Earth.
Moment of inertia is a measure of how hard it is to twist an object.
Moment of inertia is a measure of how hard it is to twist an object.
The more that the mass is concentrated towards the center of an object, the easier it is to twist the object.
Lower moment of inertia
Higher moment of inertia
Crust2.6-3.1 gm/cm3
Mantle3.5-5.7 gm/cm3
Outer Core10-12 gm/cm3
Inner Core13-14 gm/cm3
Density of Water1 gm/cm3
The Earth:
What’s it made
of?
Gravity
Seismology
Magnetism
S
N
Heat Flow
Astronomical Observations
Earthquake in JapanMagnitude 8.0
September 25, 200319:50 UTC
Izmit Turkey Seismogram
P and S Wave Paths