Earth's Composition Flashcards
Density equation
mass / volume
Density of water
1 g/cm^3
Average density of earth
5.52 g/cm^3
Earth’s Atmosphere
Extends 100km above surface, 77% nitrogen, 21% oxygen, 2% argon, water, carbon dioxide
Oblate Spheroid
Earth bulges around equator, slightly squashed sphere, makes gravity weaker at the equator
Crust
Outermost layer of earth, DENSITY 3 g/cm^3, 100km thick, continental crust is thick and less dense, and oceanic crust is thin but more dense,
Mantle
Majority of earth, hot moving rock in upper mantle (taffy like), moves continents, crust to 2900 km, density 3 g/cm^3 at top and 9 g/cm^3 at bottom
Core
Mantle to center of earth, outer core is molten, inner core is solid, creates earth’s magnetic field, density 9 g/cm^3 at top and 13 g/cm^3 at center
Order of Earth’s interior
crust - mantle- liquid core - solid core (will need to be able to draw)
Seismic Waves
earthquakes, helps us understand the internal structure of earth
P waves
Travel through liquid and solids, straight line
S Waves
Can only travel through solids, shows us the upper mantle is molted, bounces, important for understanding interior
Plate Tectonics
Multiple plates make up earth, move over the mantle to form crevasses, faults, or mountains and volcanoes, driven by CONVECTION CURRENT
Pangea
Ancient super continent, we know because continents fit together like a puzzle, fossils match on far away continents, rocks of same ancient types
Earthquake Epicenters
Earthquakes are when stress builds up between plates, this energy is concentrated at the epicenter