Week 4 Flashcards
Are the properties of earths atmosphere the same wherever you are?
No, the Properties of atmosphere depend on height you are at becasue different energies will be absorbed at different heights
Electromagnetic field
Molten Metallic core is electrically conducting, and the earth spinning on its axis activated convective currents in the core cause a magnetic field.
Ozone layer
created by UV breaking apart oxygen molecules
Atmosphere effects
Create pressure (determines presence of liquid water on surface), absorb/scatter light, create weather, protects from solar wind, warm through greenhouse effect.
Lithosphere
Ridgid part of interior, that is part of crust and mantle
Dissociation
Distruction of a molecule (UV/xray)
Impact cratering
Something smashes into the surface (asteroid/comet)
Planetary temperature
depends on energy in/energy out
Conduction
Energy can transfer through material
Stratosphere
UV absrobed due to ozone layer
Moon interior
Small core, large Lithosphere
Why is the earths core hot?
After planet accretion and differentiation, it Lost potential energy = gain kinetic energy (heat)
Mercury interior
Almost all metalic core
Why are sunsets red
Red light scatters less
Weather
Day by day variations
Affect of distance from sun
Too close to sun:
- less erosion (as no wind, ice snow rain)
- to hot for atmosphere
Why is the core denser than the crust?
differentiation, i.e. gravity pulls high density stuff to core, light material rises to surface
Why are mercury and the moon geologically dead?
They had a large surface area to volume ratio, so they cooled more quickly
Lunar maria
Highlands =higher, cratered regions
Maria = lower, smoother less cratered regions (formed latter on)
Surface age based on crattering
Highly cratered surface = surface formed early
Minimal craters = surface formed latter on