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- ocean lecture 3 chapter 1
ocean lecture 3 chapter 1
Natural Science 1 with Teach at University of California - Riverside
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Created: 2010-10-03
Size: 29 flashcards
Views: 38
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Kathy
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The origin of the Universe (14 billion years ago) 14 000 000 000 years = 14 thousand million aka the big bang theory
Universe = everything that physically exists (matter and energy
A galaxy is a huge rotating aggregation of stars, dust,
gas and other debris
are massive spheres of hot glowing gases
nucleosynthesis
Stars convert hydrogen (H) and helium (He) to heavier elements by nuclear fusion as they age
Our Solar System (Sun & planets) was formed of material made in older massive stars which accreted (stuck together and grew larger)
Hydrogen , Helium
98.6%
Water, Methane, Ammonia
1.1%
Silicates, Oxides
.22%
.08%
attraction of particles causes planet to grow
Gravitational attraction
causes pressure inside, melting rock and light stuff rises, dense stuff sinks.
heating
melting
atmosphere acquisition
Suitable distance from Sun in the Habitable Zone
Sufficient planetary mass
plate tectonics
stabilizing effect of the Moon
to support comples multicellular life, need atmospheric 02
Condensed from a cloud of gas and dust (molecular cloud or solar nebula) including remnants of older exploded stars (Supernovae)
compression, heating , rapid spin
NEBULAE : Clouds of H , He and DUST
Gravitational Collapse Compression
Heating Rotation (spin-up)
Pre-Stellar Spinning Gas + Dust Disk Core Compression
Heating to ~4 million O Ignition of Thermonuclear H to He Fusion
Stellar Wind Clears Remaining Gases but not Solids Solid “seeds” clump and PLANETS form The Sun is in its Main Sequence phase
Molecular cloud of gas + dust etc. collapses (solar nebula)
Spinning disk with hot core (star)
Accretion of particles (seeds) forms planets in disk out from central star
Melting and density separation of planets
Accretion – Growth vs Fragmentation
Heating – Accretionary and Radioactive Heat
Melting – Sphericity + Differentiation (density)
Atmosphere Acquisition PRIMARY ATMOSPHERES
H (hydrogen) + He (Helium) from Pre-Solar Nebula
SECONDARY ATMOSPHERES Accumulate after Nebula has dispersed Gas from Comet Ice – H2O, CO2, CO, CH4, NH3, etc. Erupting Volcanoes – H20, CO2, N2, H2S, SO2, etc. Heavy Molecules held by Gravity of Planets >0.1 Earth Mas
GAS = Low Density ICE = 1 gm/cc ROCK = 3 gm/cc METAL = 7 gm/cc
About this deck
Created: 2010-10-03
Size: 29 flashcards
Views: 38
About StudyBlue
Kathy