Origins of the Universe, Earth Systems, Plate Tectonics, and Marine Geology

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Comprehensive vocabulary flashcards covering the formation of the elements, solar system evolution, Earth's internal structure, plate tectonic mechanics, seafloor geography, and the origins of life and chemosynthetic marine ecosystems.

33 Terms

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The Big Bang

The cosmic expansion event that occurred approximately 13.8 billion13.8\text{ billion} years ago from an extremely hot, dense point of volume, initiating the expansion and cooling of space and the subsequent formation of matter.

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Stellar Nucleosynthesis

The process by which elements heavier than lithium are forged through nuclear fusion reactions inside stars and during explosive stellar events like supernovae.

<p>The process by which elements heavier than lithium are forged through nuclear fusion reactions inside stars and during explosive stellar events like supernovae.</p>
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Molecular Cloud

A cold, dense interstellar gas cloud—composed of approximately 73%73\% hydrogen, 25%25\% helium, and 2%2\% heavier elements—within which stars and planetary systems form.

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Protoplanets

Growing planetary embryos, several hundreds of kilometers in size, formed by the gravitational accretion and collisions of material within a protoplanetary disk.

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Theia

A Mars-sized protoplanet that collided with early Earth in a glancing hit roughly 4.4 to 4.45 billion4.4\text{ to }4.45\text{ billion} years ago, ejecting debris into orbit that eventually coalesced to form the Moon.

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Planetary Migration

The gravitational interaction between forming planets and surrounding disk material that shifts their orbital distances, such as Uranus and Neptune moving outward into lower-density regions.

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Late Heavy Bombardment

A catastrophic period occurring 4.1 to 3.8 billion4.1\text{ to }3.8\text{ billion} years ago where gravitational instability from migrating gas giants sent debris crashing into the rocky planets and moons across the Solar System.

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Planetary Differentiation

The separation of Earth's molten materials according to density, causing heavy metals like iron and nickel to sink into the core while lighter silicate rocks float to form the mantle and crust.

<p>The separation of Earth's molten materials according to density, causing heavy metals like iron and nickel to sink into the core while lighter silicate rocks float to form the mantle and crust.</p>
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Inner Core

The intensely hot (∼5,700 K\sim 5{,}700\text{ K}), densest interior layer of Earth, composed predominantly of iron and nickel kept solid by immense confining pressure.

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Outer Core

The liquid, electrically conductive metallic layer between 3,000 and 4,500 K3{,}000\text{ and }4{,}500\text{ K} composed mainly of molten iron and nickel, situated between the mantle and inner core.

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Earth's Magnetic Field

A protective planetary field generated by the geodynamo mechanism: the motion of electrically conductive liquid iron caused by convection and planetary rotation within the outer core.

<p>A protective planetary field generated by the geodynamo mechanism: the motion of electrically conductive liquid iron caused by convection and planetary rotation within the outer core.</p>
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Asthenosphere

The hot, ductile, plastic-like upper layer of the mantle directly beneath the lithosphere that undergoes convection and allows overlying tectonic plates to move.

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Lithosphere

The rigid outermost mechanical layer of Earth, comprising the entire crust and the uppermost brittle mantle, fragmented into moving tectonic plates.

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Oceanic Crust

A dense (∼3.0 g/cm3\sim 3.0\text{ g/cm}^3), geologically young crust formed of mafic basaltic rock rich in iron and magnesium.

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Continental Crust

A thicker, older, and less dense (∼2.83 g/cm3\sim 2.83\text{ g/cm}^3) crust formed predominantly of felsic granitic rocks rich in silica, aluminum, sodium, and potassium.

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Mantle Convection

The cyclic thermal movement in the mantle driven by heat from the core, where heated lower mantle material expands, rises, cools at the lithosphere, and sinks back down.

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Ridge Push

A gravitational plate-driving mechanism where upwelling magma elevates oceanic lithosphere at mid-ocean ridges, causing the plate to slide downhill away from the ridge crest.

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Slab Pull

The primary tectonic driving force occurring when cold, dense oceanic lithosphere sinks into the subduction zone and pulls the trailing plate into the mantle by its own weight.

<p>The primary tectonic driving force occurring when cold, dense oceanic lithosphere sinks into the subduction zone and pulls the trailing plate into the mantle by its own weight.</p>
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Rift Valley

A low topographic depression created along divergent plate boundaries where tectonic plates pull apart, often occupied by volcanic activity and fractures.

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Convergent Boundary

A tectonic boundary where plates collide, leading to subduction of the denser oceanic slab (oceanic-continental or oceanic-oceanic) or massive crustal uplift (continental-continental).

<p>A tectonic boundary where plates collide, leading to subduction of the denser oceanic slab (oceanic-continental or oceanic-oceanic) or massive crustal uplift (continental-continental).</p>
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Transform Boundary

A plate boundary where tectonic plates slide past one another horizontally without creating or destroying lithosphere.

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Continental Shelf

A shallow, gently sloping region extending from the coast to the shelf break that is geologically part of the continental landmass.

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Turbidity Currents

Dense, fast-flowing underwater avalanches of water and suspended sediment that carve deep submarine canyons into continental margins and deposit sediment onto abyssal plains.

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Abyssal Plains

Vast, extremely flat expanses of deep ocean basin floor covering roughly 40%40\% of the global seafloor, formed by thick sheets of turbidity sediments settling over oceanic crust.

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Guyot

An extinct volcanic seamount whose peak was flattened by surface wave action before being submerged into deeper waters by plate movement and thermal subsidence.

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Trenches

Extremely deep, narrow V-shaped depressions in the ocean floor formed at active convergent margins where subducting tectonic plates plunge into the asthenosphere.

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Atmospheric Evolution of Early Earth

The transition from an early reducing atmosphere rich in CO2\text{CO}_2 and CH4\text{CH}_4 to an oxygenated atmosphere rich in O2\text{O}_2 driven by photosynthetic prokaryotes starting between 4.0 and 3.7 billion4.0\text{ and }3.7\text{ billion} years ago.

<p>The transition from an early reducing atmosphere rich in $$\text{CO}_2$$ and $$\text{CH}_4$$ to an oxygenated atmosphere rich in $$\text{O}_2$$ driven by photosynthetic prokaryotes starting between $$4.0\text{ and }3.7\text{ billion}$$ years ago.</p>
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Electric Spark Theory

The primordial soup hypothesis tested by Miller and Urey demonstrating that electrical discharges simulating lightning could assemble simple atmospheric gases (NH3\text{NH}_3, CO2\text{CO}_2, H2O\text{H}_2\text{O}, H2\text{H}_2, CH4\text{CH}_4) into fundamental organic monomers.

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Hydrothermal Vents

Deep-sea fissures typically located along mid-ocean spreading centers where cold ocean water infiltrates crustal fractures, is superheated by underlying magma, dissolves minerals, and vents back out.

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Black Smokers

High-temperature (>350∘C> 350^\circ\text{C} / >662∘F> 662^\circ\text{F}) hydrothermal vents located nearest to active spreading rifts that spew dark precipitate clouds composed of iron, copper, nickel, and zinc sulfides.

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White Smokers

Intermediate-temperature (30 to 350∘C30\text{ to }350^\circ\text{C} / 86 to 662∘F86\text{ to }662^\circ\text{F}) hydrothermal vents that emit lighter-colored clouds containing precipitated minerals of barium, calcium, and silicon.

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Chemosynthesis

The biological process used by autotrophic bacteria in light-deprived environments to synthesize organic compounds from inorganic molecules, such as hydrogen sulfide and methane, serving as primary producers for deep-sea communities.

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Cold Seeps

Seafloor regions located along continental margins and sediment basins where methane and hydrogen sulfide seep slowly out of decaying sediments, sustaining long-lived chemosynthetic biological communities.