1/100
A set of vocabulary flashcards covering planets, Earth systems, rock science, geologic processes, dating methods, hazards, hydrometeorology, and coastal management for exam review.
Name | Mastery | Learn | Test | Matching | Spaced |
---|
No study sessions yet.
Exoplanet
A planet that orbits a star outside our solar system.
Dwarf Planet
A nearly round body that orbits the Sun but has not cleared its orbital path of other debris.
Kuiper Belt
Distant, doughnut-shaped region beyond Neptune that hosts many dwarf planets and icy bodies.
Gas Giant
Large outer-solar-system planet composed mainly of hydrogen and helium (e.g., Jupiter, Saturn).
Ice Giant
Outer planet rich in water, ammonia and methane ices (Uranus and Neptune).
Great Red Spot
Centuries-old storm on Jupiter larger than Earth.
Runaway Greenhouse Effect
Process on Venus where thick CO₂ atmosphere traps extreme heat.
Great Dark Spot
Giant storm once observed on Neptune.
Hydrosphere
All Earth’s water in liquid, solid, and vapor forms, including oceans, lakes, ice, groundwater and moisture.
Geosphere
Solid Earth—crust, mantle, and core—composed of rock and minerals.
Biosphere
All living organisms and the environments they inhabit.
Atmosphere
Gaseous envelope surrounding Earth, ~78 % N₂ and 21 % O₂, regulating climate and supporting life.
Igneous Rock
Rock formed by cooling and crystallization of magma or lava.
Plutonic (Intrusive) Rock
Igneous rock that cools slowly beneath Earth’s surface (e.g., granite).
Volcanic (Extrusive) Rock
Igneous rock that cools quickly at or near the surface (e.g., basalt, pumice).
Sedimentary Rock
Rock formed by compaction and cementation of sediments.
Compaction
Weight of overlying layers squeezes sediments, reducing pore space.
Cementation
Minerals precipitate from groundwater and “glue” sediments together.
Metamorphic Rock
Rock altered by heat, pressure, or chemically active fluids without melting.
Rock Cycle
Continuous processes that transform rocks among igneous, sedimentary, and metamorphic types.
Mechanical Weathering
Physical breakup of rocks (e.g., frost wedging, root growth).
Chemical Weathering
Breakdown of rock through chemical reactions, such as oxidation or carbonation.
Erosion
Transport of weathered material by water, wind, ice, or gravity.
Deposition
Dropping of sediments when transporting agents lose energy.
Conduction (Earth)
Heat transfer through molecular contact, dominant in lithosphere.
Convection (Mantle)
Heat transfer by movement of molten or plastic material, driving plate tectonics.
Radiation (Heat)
Transfer of energy by electromagnetic waves; controls surface temperature exchange with space.
Crust
Earth’s outermost solid layer, 5–70 km thick, composed of continental and oceanic varieties.
Mantle
Layer from crust base to 2,900 km depth, behaving as viscous solid; 84 % of Earth’s volume.
Outer Core
Liquid iron-nickel layer that generates Earth’s magnetic field.
Inner Core
Solid iron-nickel sphere under immense pressure at Earth’s center.
Magma
Molten rock beneath Earth’s surface, containing minerals and volatiles.
Lava
Magma that reaches Earth’s surface.
Partial Melting
Process where only some minerals in a rock melt, generating magma of different composition.
Decompression Melting
Magma formation as hot mantle rock rises and pressure decreases (mid-ocean ridges).
Flux (Wet) Melting
Lowering of rock melting point by adding volatiles like water (subduction zones).
Folding
Plastic bending of layered rocks under compressive stress.
Anticline
Up-arched fold with oldest rocks at its core.
Syncline
Down-curved fold with youngest rocks at its center.
Monocline
Simple one-sided bend in otherwise horizontal strata.
Fault
Fracture where blocks of rock move relative to each other.
Normal Fault
Hanging wall moves down relative to footwall due to extension.
Reverse Fault
Hanging wall moves up relative to footwall due to compression.
Strike-Slip Fault
Blocks move horizontally past each other due to shear (e.g., San Andreas).
Law of Superposition
In undisturbed strata, oldest layers lie at the bottom and youngest at the top.
Law of Inclusions
Fragments enclosed in a rock must be older than the host rock.
Cross-Cutting Relationship
Geologic feature that cuts another is younger than what it cuts.
Original Horizontality
Sediments are initially deposited in nearly horizontal layers.
Unconformity
Surface representing a gap in the geologic record due to erosion or non-deposition.
Faunal Succession
Fossil assemblages succeed one another in a recognizable order through time.
Relative Dating
Placing rocks and events in sequence without assigning exact ages.
Absolute (Radiometric) Dating
Determining numerical ages using radioactive decay of isotopes.
Half-Life
Time required for half of a radioactive parent isotope to decay to daughter isotope.
Radiocarbon Dating
Method using decay of carbon-14 to date organic remains up to ~45,000 yrs old.
Potassium-Argon Dating
Radiometric technique for igneous rocks 100 kyr to billions of years old.
Uranium-Lead Dating
Radiometric method measuring lead-206 in zircon; dates rocks >100 Myr.
Rubidium-Strontium Dating
Technique using decay of 87Rb to 87Sr for rocks older than 10 Myr.
Hadean Eon
Oldest eon (4.6–4 Ga) marked by formation of Earth’s crust and oceans.
Archean Eon
3.8–2.5 Ga; early continents form; first life emerges in methane-rich atmosphere.
Proterozoic Eon
2.5 Ga–541 Ma; atmospheric oxygen rises, eukaryotes appear, supercontinents assemble.
Paleozoic Era
541–252 Ma; explosion of marine life, amphibians, reptiles, and formation of Pangaea.
Mesozoic Era
252–66 Ma; “Age of Dinosaurs” comprising Triassic, Jurassic, Cretaceous periods.
Cenozoic Era
66 Ma–present; mammals diversify, humans evolve, several ice ages occur.
Earthquake
Sudden release of energy along faults producing ground shaking.
Ground Shaking
Vibration of the ground during an earthquake; can trigger other hazards.
Liquefaction
Loss of soil strength during shaking when water-saturated sediments behave like liquid.
Landslide
Downslope movement of rock, earth, or debris; often earthquake-triggered.
Surface Faulting
Displacement that breaks through to Earth’s surface during fault slip.
Tsunami
Long-wavelength sea wave generated by seafloor disturbance such as an earthquake or landslide.
Tephra Fall
Volcanic ash and larger fragments ejected and deposited from eruption plume.
Pyroclastic Flow
Fast, dense avalanche of hot ash, lava fragments, and gases down volcano slopes.
Lahar
Volcanic mudflow of water and debris rushing down river valleys.
Lava Dome
Bulbous mound formed by viscous lava piling over a volcanic vent.
Hydrometeorology
Science of water in the atmosphere and its interaction with land and oceans.
Hydrometeorological Hazard
Atmospheric, hydrologic, or oceanographic process causing potential harm (e.g., typhoon, flood).
Tropical Cyclone
Warm-core, rotating low-pressure system forming over ≥26 °C oceans.
Typhoon
Tropical cyclone in the Northwest Pacific (Philippines, Japan, China).
Hurricane
Tropical cyclone in the North Atlantic or Eastern Pacific.
Cyclone (Indian Ocean)
Regional term for tropical cyclone over South Pacific or Indian Ocean.
Monsoon
Seasonal reversal of wind and rain pattern (e.g., Habagat and Amihan in Philippines).
Flood
Overflow of water onto normally dry land.
Tornado
Violently rotating column of air extending from a thunderstorm to the ground.
Hazard Map
Spatial representation identifying areas susceptible to specific natural hazards.
Wave (Ocean)
Rhythmic movement of water generated by wind friction on the surface.
Swash
Up-rush of water on a beach after a wave breaks, carrying sediment landward.
Backwash
Water flowing back to sea after swash, moving sediment seaward.
Longshore Drift
Zig-zag transport of sediment along coast by angled wave action.
Spring Tide
Large tidal range occurring at full and new moons when Sun, Earth, and Moon align.
Neap Tide
Small tidal range occurring at quarter moons when Sun and Moon forces act at right angles.
Sea Level Rise
Global or local increase in ocean height, currently ~2 mm/yr.
Storm Surge
Abnormal rise of sea level during a storm from wind and low pressure.
Coastal Erosion
Removal of shoreline material by wave action, currents, or sea level rise.
Saltwater Intrusion
Landward movement of seawater into freshwater aquifers.
Sea Wall
Concrete or stone barrier built parallel to shore to reflect wave energy.
Groynes
Structures built perpendicular to shoreline to trap sand and widen beaches.
Riprap (Rock Armour)
Large boulders placed at foot of cliffs or seawalls to absorb wave energy.
Beach Nourishment
Addition of sand to an eroding beach for protection and recreation.
Managed Retreat
Planned abandonment of low-value coastal land to allow natural processes.
Cliff Stabilization
Techniques (e.g., vegetation, netting) to reduce cliff erosion and slope failure.
Hard Engineering
Use of built structures to defend coasts against erosion and flooding.