ORIGINS: Creation and Composition of the Earth Flashcards
creation of the new solar system
- derived from the death of the previous one
- star becomes supernova, destroying itself, simultaneously creating new solar system (w elements)
nebula to solar system
- gravitational energy is converted to heat (the cold cloud warms up)
- vapourizes all of the elements
- heat at the center lights up the sun
- gas/vapour blown away cools and recondenses as dust
Condensation of planetesimals from dust and gas
- first by electrostatic forces, then by gravity
- elements interact, sharing and donating electrons
rocky vs gas vs ice rich planets
- planets forming close to the sun are rocky
- planets condensing far from the sun are gas & ice rich
- the planets comprised of heavier elements (rocks) are (terrestrial planets) did not travel as far
half-finished Earth (10-100MYA)
- Earth bombarded by millions of smaller bodies (meteors and comets)
- bombardment heated the Earth (collisions)
- heating increased by gravitational contraction
- melting of Earth creating magma ocean. Iron-rich fraction of this liquid was heavier and it settled to Earth’s centre
* this melting drove off H, He- rich primordial atmosphere
Earth 4.4 Ga (billion years)
- solid core (iron-rich)
- ‘outer core’ of liquid iron
- partly molten ‘mantle’
- thin skin of solid rock at its surface
- too hot for liquid water
Jupiter and Saturn atmosphere
-close to the frost line
- gas giants as a result of no hot melting event
- retain a “primordial” atmosphere
uranus and neptune
- light gases turned to ice
- made of mostly ice
- same composition as Jupiter and Saturn but at much lower temperature
ontology of Earth’s Moon
- collision between large body and Earth
- moon grew from ejected material of this collision
- initially closer to the Earth
on a moonless Earth:
- tides would be solar and less powerful
- days would be shorter
- faster winds
Igneous Rocks
- “fire formed:” cooled from liquid
- the most accurate to date
- basalt, granite
sedimentary rocks
- tell us about relative order in which events occurred
- formed from chemical precipitates or fragments of earlier formed rocks
metamorphic rocks
-formed by application of heat and pressure to either igneous or sedimentary rocks
radioactive decay
- useful until about 6 half lives
- measures proportions of parent and daughter isotopes of an element in SEVERAL samples
age of the moon
- Earth’s major structures were established prior to the birth of the Moon
- BC an impact on Earth that did not have a separate Fe-rich core would have contributed more Fe to the moon
- by 4.4 Ga Earth and Moon were already a pair