Chapter 7- Terrestrial Planets and the Moon Flashcards
3 Main Shaping Processes
Impacts from space
Volcanism
Tectonics
Impacts from Space
Heavy bombardment in the early solar system – lots of cratering on all five bodies (Moon, Mercury, Venus, Earth, Mars)
Meteor
Bright streak in the sky when a meteorite passes
Meteorite
A fragment of a meteoroid which survives its fall to Earth’s surface
Meteoroid
A small body in space
Formation of an impact crater
ejecta, rays, crater walls, secondary craters, central peak
Why the difference in cratering?
Atmospheres- dense atmospheres prevent most meteoroids from reaching the surface
Evolution of surfaces- some surfaces evolve over time and obliterate signs of impact (Earth- tectonics, Venus- volcanism)
Magnetic fields
Earth reverses its magnetic field every hundred thousand years
Moon has no magnetic field due to cooling
Mercury has a weak field- small and slow rotation rate
Venus and Mars have small magnetic fields
Planetary interiors
Density calculation- compare measured value of density of surface materials with calculated overall density to see interior density
Seismic waves- p wave, s waves. Both types are sent out during earthquakes, patterns give clue to the interior
Tectonics
Plates of rock float on plastic outer mantle, powered by convection currents of hot mantle material. Seafloor spreading pushes plates apart.
No signs or Mercury, Moon, or Venus. Uncertain but unlikely on Mars.
Volcanism
Occurs when plates collide and subduct.
Hot spot volcanism- hot spot develops in the crust, magma wells up for long periods of time