Title: How can we study quakes on other planets?
1How 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
2Lunar 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
3Shallow 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
4Moonquakes
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)
?
5Seismicity 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?
6What 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)
7What planetoids would be good candidates for
future seismic studies?
- Great candidates include
- Venus
- possible volcanism (quakes associated)
- thick atmosphere tough to penetrate!
8What 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
9What 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
10What 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