GEL 001 Midterm 1 Flashcards
Solar nebula hypothesis
Plants form from discs of gas and dust that surrounded the sun as it formed.
Planets are byproduct of star formation from nebula.
Nebula
Clouds of gas and dust in space that Mark birthplace of stars
Solar system
Begin with slow, spinning cloud of gas, nebular cloud begins in collapse and toward center, because of gravity
As it collapse It heats up and compresses the center (proto-sun) revolving gas and dust become trapped and stable orbits (rings)
When’s sons internal fusion? Reactor turns on a become real son, and rings matter, clumps as temps drop, planetestimals become planets.
Planetestimals
Constant collisions caused Boulder
Astreoid size particles coalesce because of Gravity
Accretion
Collision growth of planets by constant bombardment
4.6 b.y age of Earth
Formation of sun, 8 planets, over 130 mins, and assorted space debris —> Determined by dating of radioactive elements within meteorites found on earth
Meteorites
Chunks of rock metal that fall to earth from space
Differentiation
Planets, evolved by progressive differentiation (separation) of materials, according to
density,
under the influence of internal heating,
heavy moved to core
Core
Dense interior, in planets
Mantle
Surrounds core, less dense
Crust
Thin, least dense
Hydrosphere
Surface water on earth, along with ground water
Atmosphere
Develops from for volcanic gas
Heat of formation
Frictional heating through constant collision, (kinetic energy of informing matter converts to heat energy)
radioactive heat
Accumulation of U, Th, K, that spontaneously Decay to form heat
Magma ocean
Young earth was hot enough for the uppermost several tens of kilometers to covered by magma ocean
Hadean Era
Magma rock existing in cooling off,
unlivable period,
First 600–700 million years of earth history
Volcanic outgassing
Volcanoes emenate copious quantities of water, paper, CO2, SO2, NO2, and other gases
Rules of comets
“Dirty snowball”
Contributed huge amounts of water to interior of planet,
outgasesand contributed to early atmosphere and hydrosphere
Main elements in the Earth
Fe, O, Si, and Mg
Silica & Silicates
Si and O Create silica (SiO2) Which is the main component of silicates. Silicates doninates the rocky mantle and crust
Geothermal gradient
Rate of change in temperature with depth
Temperature increases towards the center of the Earth
Iron inner core
(s), Very hot and dense, made of metallic Fe With small amounts of Ni and S
Iron outer core
(l), Very hot in tents, made out of metallic Fe with small amounts of Ni and S