Lecture 6 Flashcards
What caused the size increase of the proto-earth?
Accretion of particles of molten matter-atmosphere was cold, surface formed a crust of solid material.
What caused an increase in temperature of the proto-earth?
Collisions from asteroids, debris, protoplanets etc, and the decay of radio active elements trying to find stable state. Heat was trapped inside the core and turned liquid.
What is the gravitational differentiation process?
Different elements moved to different parts of the Earth due to the gravitational field-As Iron and Nickel reached their melting points, they moved towards the centre and silicate moved upwards.
How did we first attempt to investigate Earths interior?
Wells (can’t go past 5000m). Miners (cant go past 2500 metres).
What is seismic investigation?
Looks at the surfaces of discontinuity (boundaries of layers). Behaves differently at the seismic activity. Place Geophones at the surface and detonate-energy propagates through Earths interior. Measures waves that are reflected back by the surfaces of discontinuity.
What are Earthquakes?
Natural phenomena generated by the rearrangement of Earth’s layers.
What is the hypocentre?
Underneath the epicentre-distance between the two makes the earthquakes depth. Used to localize.
What are body waves and the two types?
Waves which travel throughout the Earth. P-Waves: The first waves to get to the seismic observatories (very fast). S-Waves: Slower, produce damage.
What are surface waves?
Last to reach seismic observatories. Extremely destructive.
What is the chemical composition of the Earth?
Core (iron dominated, nickel 2nd). Mantle (silicates with low diversity. Crust (silicates with high diversity)
What is the Guttenberg discontinuity (chemical)?
Boundary between the core and the mantle.
What is the Mohorovich discontinuity (chemical)
Boundary between the mantle and the crust.
What are the physical compositions of the Earth? (from outermost to innermost).
Lithosphere (solid), Athenosphere (exists solely on Earth, mobility of surface and existence of lifeforms, continents float on it, plastic surface), Mesosphere (solid, most of the volume of the earth (like the mantle), Outercore (Guttenburg discontinuity-only shared thing with chemical. Liquid Iron state due to temperature), Inner core (same chemical composition as outer, but is SOLID, due to very high pressures.
How do we know the outer core is liquid?
S-waves can’t travel through it
Where is the Moho discontinuity at a lower depth?
Continents