Formation of the Solar System + Earth Flashcards
Lecture 3
Solar Nebular Disk Model Consists of:
Nebula (cosmic dust and gasses) and nearby star which goes Supernova (massive explosion at end of lifecycle)
How is a disk and then protostar formed
supernova releases massive wave of energy –> spins nebula –> flattens into disk shape –> creates a gravitational pull –> mass pulled into center of disk –> pressure and temperature increases –> forms a protostar
How is a star formed
more mass and pressure causes protostar to undergo FUSION –> creates a star
helps in planet formation by preventing loss of nebula material, solar winds, gravity
How are planets formed (accretion and planetesimals)
Accretion (many small pieces brought together)
Planetesimal (objects already formed by accretion that are large enough to generate their own gravity)
these planetesimals accrete together and grow even bigger
Importance of Solar Winds
waves of charged particles interact with other atoms and structures in new solar system
Metals and rocks were not moved very far by solar winds – formed small planets
Light materials pushed very far by solar winds (past frost line) - formed big gas planets
Formation of Earth and when
4.56 - 4.53Ga
gasses to form the atmosphere pulled in by gravity, no oxygen
formation of the metallic core
mantle solidfies (4.53Ga)
Formation of the Moon
4.5 billion years ago
Theia collided with developing Earth
Theia destroyed
debris formed the moon
Slowly moving away from Earth
Important processes after the moon formation (4)
Plate tectonics, magnetic field, outgassing as rock cools, bombardment
Formation of Plate Tectonics
Possible impact that broke up solid crust which began process of recycling and movement
Believed to be essential to life
Formation of Magnetic Field
Interaction between solid metal core and liquid outer core
deflects solar winds, protects atmosphere
Habitable Zone factors
Right mass of star
Right distance from star where liquid water and gaseous CO2 can exist
Gravity - retain atmosphere and ocean
Right planetary mass - for plate tectonics and magnetic field
Jupiter factor - clears out comets
Large Moon - stabilizes tilt, creates tides for life
Plate Tectonics - internal heat bc of big enough
When is carbon-dating used
shorter term dating of mainly organic samples
Outgassing
atmosphere generated by
1) cooling rock releasing gases
2) continued volcanic activity
3) elements from comet impacts (water derived from comets)
When was the Late Heavy Bombardment? - add more
drop in bombardment rates of asteriods and comets 4.4 - 3.8 Ga
Radiometric Dating + Half Life
Radioactive isotopes have half life (time needed for a quantity of a substance to reduce by half)
also, ratio of old parent isotopes to newly formed daughter isotopes