-
Processes that effect the surfaces of planets
- erosion
- tectonics
- volcanism
- meteor impacts
-
Tectonics
movement of the surface of the crust (mountain building, earthquakes)
-
*Volcanism
volcanoes and volcanic eruptions (almost every planet and moon)
-
*Meteor impacts
- one process most important for shaping surface of planets
- craters
-
Mars
evidence of water once flowing and erosion
-
Volcanic eruptions and erosion
can wear a surface smooth
-
Crater count
counting amount of craters in an area and dividing that number by the area (tells you how old a surface is)
-
Jupiter moons
- Callisto- oldest surface in solar system
- Io- youngest and most volcanically active
-
Craters
form 20 times bigger than object that caused crater
-
Types of craters
- punch bowl/simple crater
- central-peaked crater
- multi-ringed impact basin
-
Punch bowl crater
- smallest
- usually caused by objects less than 1 mile in diameter
-
Central-peaked crater
- group of mountains in middle of crater
- created by objects 1-5 miles wide
-
Multi-ringed impact basin crater
- largest
- multiple rings spread out from center
- at least 5 mile wide impacter
-
Near Earth Asteroids (NEAs)
asteroids we worry about hitting earth
-
Olympus Mons
- largest volcano in solar system (on mars)
- shield volcano
-
Shield volcano
- most common in solar system
- least violent eruptions
- large craters in center (caldera) irregularly shaped unlike impact craters
-
Mauna Loa
largest volcano on earth
-
Mare
- lava plains (largest volcanic feature)
- flood basalt
-
Revolution
- the planet's year
- amount of time to go once around the sun
-
Rotation
time it takes planet to rotate once on its axis
-
Solar day
time between consecutive sunrises or sunsets
-
-
Key to planetary geologic processes
size
-
Planetary geologic processes for a small planet (mercury)
- heat from formation- small = gone
- radioactive material- less = small amounts of heat = no heat now (cold)
- geological activity- dead (geologically)
-
Planetary geologic processes for a large planet (earth)
- heat from formation- lots = some left
- radioactive material- more = some left, large amounts of heat = still hot inside
- geological activity- active (geologically)
-
Atmospheres
initally: CO2 and H2O vapor (terrestrial planets)
-
Factors that affect the atmosphere
- size- mass = gravity
- temperature = average speed
-
Escape velocity
- minimum velocity an object needs to escape a planet's gravity
- earth = 11 km/s or 7 miles/s
- mars = 5 km/s or 3 miles/s
- mercury = 4 km/s or 2.5 miles/s
- moon = 2 km/s or 1 mile/s
-
Venus
- temp = 500 degress celsius (greenhous effects)
- no water in atmosphere
-
Mars
- temp = -60 degrees celsius
- weak gravity
- lost most of atmosphere due to ablation
-
Ablation
- stripping away of an atmosphere by impacts
- collisions strip away part of a planet's atmosphere
-
Lobate scarp
giant (mile high) cliff on Mercury and the moon (no internal heat)
-
Venus
- coronae
- regio
- maxwell montes (only male name on venus)
-
Earth
- only planet with water
- composition: 36% Fe, 28% O, 14% Si
- silicate crust and mantle
- liquid outer core
- solid inner core
-
Magnetosphere of a planet
the region of space surrounding a planet where its magnetic field deflects away the solar wind
-
Solar flares
- aurora borealis (northern lights)
- aurora australis (southern lights)
- solar wind, planet's magnetic field, and planet's atmosphere
-
Continental crust
- made of granite (light, buoyant)
- relativiely think, but light
-
Oceanic crust (sea floor)
- made of basalt (denser/heavier than granite, sinks into earth)
- makes up 2/3 of earth's crust
-
Tectonic/lithospheric plates
slide around on earth's surface and collide with each other or bounce off each other and separate
-
Convection cell
helps push plates around on surface
-
Plate tectonics
- the key to the existance of the asthenosphere is water
- plate tectonics would not exist without the asthenosphere
- *therefore, without water, there are no plate tectonics and no life
-
Types of plate tectonics
- 1. plates separate- divergent plate boundary (mid-oceanic ridge/spreading center), sea floor grows and spreads at divergent plate boundary
- 2. colliding plates- convergent plate boundary (subduction zone), sinking plate (subducts), volcanic arc
- 3. plates sideswipe- transform plate boundary
-
Earth's atmosphere
CO2 and H2O to 80% N2 and 20% O2
-
Photosynthesis
plants combine CO2 + sunlight + H2O
|
|