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Practice flashcards covering key topics, scientists, processes, and concepts for the upcoming oceanography and Earth science exam.
Ocean
A vast, continuous body of saline water that occupies major basins on Earth's crust, with an average depth of about 3682m.
Sea
A smaller, shallower body of saline water that is partially enclosed by land and directly connected to an ocean.
Ocean vs. Sea (Comparison)
Oceans are immense, deep, open water reservoirs bounded by continents, whereas seas are smaller, shallower, and partially bordered by land.
Deepest region in the ocean
Challenger Deep in the Mariana Trench, reaching approximately 11034m (36201ft) below sea level.
Lowest dry land elevation on Earth
The shore of the Dead Sea, located at approximately 430m (1410ft) below sea level.
Deepest ocean region vs. lowest dry land (Comparison)
Challenger Deep plunges over 25 times deeper below sea level (11034m) than the lowest exposed land at the Dead Sea (430m).
Pacific Navigators
Indigenous explorers who traveled across open ocean island chains without instruments by reading waves, stars, clouds, and winds.
European Navigators
Explorers driven by global trade routes who mapped ocean paths using navigational tools like the compass, astrolabe, and sextant.
Types of Ocean Explorers
Pacific navigators who used indigenous wayfinding, European navigators who charted trade routes with navigational tools, and modern scientific explorers who systematically measure ocean properties.
Ocean Exploration
The practical and scientific investigation of the ocean's physical, chemical, geological, and biological features using ships, diving equipment, and submersibles.
James Cook's Expedition
The first ocean voyage dedicated to systematic scientific research, accurately charting the Pacific using a marine chronometer.
Physical conditions measured by James Cook
Ocean depth soundings, water temperatures at varying depths, wind conditions, and current speeds and directions.
Submersible
A small specialized watercraft built to operate underwater and withstand high hydrostatic pressure for deep-sea exploration and research.
Human-Occupied Vehicle (HOV)
A deep-sea submersible that carries a crew of scientists directly to the ocean floor to make direct visual observations and collect samples.
Remotely Operated Vehicle (ROV)
An unmanned, tethered submersible controlled by operators on a surface ship to capture video and collect samples from the deep sea.
Autonomous Underwater Vehicle (AUV)
An untethered, programmable robotic submersible that independently navigates and collects ocean data without real-time human control.
Geological Oceanography
The study of the seafloor, ocean basin structure, marine sediments, and plate tectonics.
Chemical Oceanography
The study of the chemical composition, salinity, dissolved gases, and nutrients of seawater.
Physical Oceanography
The study of water motion, including currents, waves, tides, and thermal energy exchange with the atmosphere.
Biological Oceanography
The study of marine plants, animals, microbes, and their ecological interactions in oceanic environments.
Scientific Hypothesis
A tentative, testable, and falsifiable proposed explanation for an observed phenomenon.
Scientific Theory
A comprehensive, highly substantiated explanation of a natural phenomenon supported by a large body of empirical evidence.
Hypothesis vs. Theory (Comparison)
A hypothesis is a proposed, untested explanation, whereas a theory is thoroughly tested, verified, and widely supported by evidence.
Nebular Hypothesis
The model proposing that our solar system condensed from a giant rotating cloud of interstellar gas and dust roughly 4.6×109years ago.
Proto-Earth Accretion
The process where colliding dust particles, rocks, and meteoroids coalesced through gravity to build the early planet.
Density Stratification
The gravitational separation of early molten Earth into layers: dense iron and nickel sank to form the core, while lighter silicates floated to form the mantle and crust.
Earth's Compositional Layers
The silicate crust, the silicate mantle (largest by volume), and the dense metallic iron-nickel core.
Lithosphere
The cool, rigid, brittle outermost physical layer composed of the crust and uppermost mantle, divided into tectonic plates.
Asthenosphere
The hot, plastic, ductile layer in the upper mantle beneath the lithosphere that can slowly deform and flow.
Lithosphere vs. Asthenosphere (Comparison)
The lithosphere is rigid and brittle, floating atop the deeper asthenosphere, which is ductile and semi-plastic.
Oceanic Crust
A thin (5km to 10km), dense (≈3.0g/cm3) crust made primarily of dark volcanic rock called basalt.
Continental Crust
A thick (30km to 50km), lower-density (≈2.7g/cm3) crust made primarily of light-colored rock called granite.
Oceanic Crust vs. Continental Crust (Comparison)
Oceanic crust is thinner, denser, and basaltic; continental crust is thicker, lighter, and granitic.
Isostatic Adjustment
The vertical rising or sinking of Earth's crust to maintain buoyant equilibrium within the underlying plastic mantle.
Origin of Earth's atmosphere
Volcanic outgassing emitted water vapor, carbon dioxide, methane, and ammonia, creating an early atmosphere with virtually no free oxygen.
Origin of Earth's oceans
Cooling of the planet allowed outgassed water vapor to condense, producing torrential rains over millions of years that accumulated in low basins.
Stanley Miller Experiment
A laboratory apparatus simulating prebiotic Earth that used electric sparks on basic gases to synthesize organic amino acids.
Evolution by Natural Selection
The process where individuals with favorable inherited traits are more likely to survive, reproduce, and pass those traits to offspring.
Photosynthesis
The process using sunlight, carbon dioxide, and water to produce sugar and oxygen: 6CO2+6H2O→C6H12O6+6O2.
Cellular Respiration
The process breaking down glucose in the presence of oxygen to release usable cellular energy (ATP), carbon dioxide, and water: C6H12O6+6O2→6CO2+6H2O+ATP.
Great Oxidation Event
The sudden rise in atmospheric oxygen caused by early photosynthetic cyanobacteria around 2.4×109years ago.
Oxygen and Mass Extinctions
Rapid depletion of dissolved oxygen (oceanic anoxia) suffocates marine life, causing widespread global die-offs in Earth's history.
Radiometric Dating
A technique that determines the numerical age of rocks by measuring the ratio of radioactive parent isotopes to stable daughter products.
Half-Life
The time required for half of the radioactive atoms in a sample to decay into daughter atoms.
Geologic Time Scale
A calendar dividing Earth's 4.6×109year history into eons, eras, periods, and epochs based on rock strata and fossil records.