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How can we study quakes on other planets?

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Title Insert Planetoid here -quakes and Seismology: a tool for understanding Planetary Interiors Author: Andrew Newman Created Date: 3/12/2003 7:08:46 PM – PowerPoint PPT presentation

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Title: How can we study quakes on other planets?


1
How can we study quakes on other planets?
  • Cannot do it entirely from earth
  • Need to send people or landers to the planet

On the Moon
Apollo Mission sent astronauts to the moon
1969-1972 where they installed 6 seismometers (4
were operational) on the near side. Stations
returned data through 1977 (8 yrs) Recorded
between 600-3000 moonquakes per year
2
Lunar Seismic Events
  • More than 12,000 quakes recorded (between M
    0.5-1.5)
  • Three types of events were recorded
  • meteor impacts (pea size impacts up to 1000 km
    away)
  • Astronaut noise (landings and rocket boosts, and
    even foot
  • steps)
  • moonquakes
  • some shallow events lt 60 km deep
  • mostly deep focus
  • deep events form a partial spherical shell
    between 600-1,000 km depth

Near side
3
Shallow lunar structure from seismology
Both P and S velocities increase regularly with
depth. Inferred density shows that a material
with r3 exists to 60 km consistent with basalt
and gabbro (crust) Deeper than 60 km assumed
density is consistent with pyroxenes (mantle)
crust
mantle
4
Moonquakes
With no active tectonics or volcanism, what is
causing the moonquakes, and why are they so deep?
  • Something must be causing applied stresses
  • Possibly thermal stress from cooling
  • more likely tidal stresses from the Earth (6x
    greater than on earth)
  • Why are the quakes only on the near side?
  • Similar tidal stresses exist on back side
  • quakes probably exist on backside too but not
    easily detected (size, distance)

?
5
Seismicity on other planetoids
  • Mars 1970s Viking I II landers were equipped
    with seismometers.
  • Though there are no active tectonics, Mars is
    expected to have considerable thermal stress
    (actively cooling) and is thought to be more
    active than the moon.
  • Seismometer on Viking
  • I did not work
  • II worked for 2years but only recorded
  • 1 marsquake
  • poorly coupled to surface
  • significant wind noise
  • considerable temperature
  • variations
  • Seismometers have not been deployed to any other
    planetary object

What planetoids would be good candidates for
future seismic studies?
6
What planetoids would be good candidates for
future seismic studies?
  • body should be composed of brittle elastic solids
    for quakes (no gas giants Jupiter, Saturn,
    Uranus, Neptune)
  • must be accessible with a lander and return data
    (stay within the solar system)
  • Must have induced stresses (tidal, thermal,
    cratering)

7
What planetoids would be good candidates for
future seismic studies?
  • Great candidates include
  • Venus
  • possible volcanism (quakes associated)
  • thick atmosphere tough to penetrate!

8
What planetoids would be good candidates for
future seismic studies?
  • Great candidates include
  • Venus
  • possible volcanism (quakes associated)
  • thick atmosphere tough to penetrate!
  • Galilean Moons
  • Io most active body in solar system

9
What planetoids would be good candidates for
future seismic studies?
  • Great candidates include
  • Venus
  • possible volcanism (quakes associated)
  • thick atmosphere tough to penetrate!
  • Galilean Moons
  • Io most active body in solar system
  • Europa Ice tectonics

10
What planetoids would be good candidates for
future seismic studies?
  • Great candidates include
  • Venus
  • possible volcanism (quakes associated)
  • thick atmosphere tough to penetrate!
  • Galilean Moons
  • Io most active body in solar system
  • Europa Ice tectonics
  • Callisto Cratering
  • Almost any large rocky
  • body would work
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