Chapter 6 Flashcards
1
Q
what does the solar system look like?
A
- some planets have unusual tilts, large moons, or moons with unusual orbits
- some planets are rocky and some are large hydrogen rich jovian planets
- swarms of asteroids and comets populate the solar system (steroids between mars and Jupiter, oort cloud (even more comets))
2
Q
planets are are very tiny compared to what?
A
distances between them
3
Q
Describe the Sun..
A
- over 99.8% of solar system’s mass
- 100 times bigger than the sun
- made mostly of Hydrogen and Helium gas (plasma)
4
Q
Describe Mercury…
A
- made of metal and rock: large iron core
- desolate, cratered; long, tall, steep cliffs, no moon
- very hot and very cold: 425C during day and 170C at night
- closest to the sun
5
Q
Describe Venus…
A
- is it the hottest bc of thick atmosphere
- nearly identical size to earth
- no moon
- extreme green house effect
6
Q
Describe Jupiter
A
- father from sun than inner planets
- No solid surface (mostly H/He) like sun
- 300 times more massive than earth
- many moons and rings
- jupiter has 4 galilean moons
7
Q
Four Galilean moons
A
- Io ; active volcanoes all over
- Europa; possible subsurface ocean
- Ganymede; Largest moon in solar system
- Callisto- a large cratered “ice ball’
8
Q
Jovian ring systems
A
- all four jovian planets
- others have ring particles that are smaller and darker than saturn’s
- jovian ring system just means they have moons
9
Q
Icy bodies are
A
many icy bodies like pluto, beyond neptune (kuiper belt objects)
-largest ones are compared to the earths moons (eris is bigger than pluto)
10
Q
pluto and other dwarf planets
A
- icy comet like composition
- much smaller than other planets
11
Q
major planet types
A
- terrestrial planets are rocky, relatively small and close to the sun
- jovian planets are gaseous, larger, and farther from the sun
12
Q
why are there two major types of planets?
A
-most mass is h/he 98%
13
Q
inside of the frost line
A
too hot for hydrogen compounds to form ice
- hydrogen compounds stay gaseous
- metals and rocks condense
14
Q
outside of the frost line
A
cold enough for ice to condensate
15
Q
Formation of terrestrial planets
A
- small particles of rocks and metal were present inside the frost line
- planetesimals of rocks and metal built up as these particles are collided
- they collide and they make planets