1/37
Vocabulary flashcards covering the scope of physical geology, solar system astronomy, comet structures, Earth internal layers and discontinuities, and geologic time concepts.
Name | Mastery | Learn | Test | Matching | Spaced | Call with Kai | Chat |
|---|
No analytics yet
Send a link to your students to track their progress
Geology
The study of Earth, including its interior and exterior surface, rocks and materials, formation processes, surface and underground water, historical changes across geological time, and anticipated future changes.
Physical Geology
A branch of geology examining Earth's materials, processes, and features by focusing on internal (endogenic) and external (exogenic) forces and their dynamic interactions.
Scientific Method in Geology
An ongoing process involving observation of Earth processes, formulation of testable hypotheses, data collection and experimentation, analysis, and theory/model development, often relying on interpreting past physical evidence.
Astronomical Unit (AU)
The average distance between Earth and the Sun, equal to approximately 149.6×106km (93×106miles).
Sun
The central main sequence star of our solar system holding 99.9% of its total mass, generating energy through hydrogen-to-helium fusion, with layers including core, radiative zone, convection zone, photosphere, chromosphere, and corona.

Mercury
The smallest planet in the solar system and closest to the Sun, predominantly composed of iron, featuring surface temperatures from −180∘C to 430∘C, impact craters named after famous artists, and a sodium-sputtered tail extending up to 2.5×106km.
Venus
Known as 'Earth's twin' due to similar size and gravity, this planet features surface temperatures of 460∘C, intense atmospheric pressure, sulfuric acid rain, and surface features named after female figures.
Earth
The third planet from the Sun and fifth largest overall, covered by 70% water and 30% landmass, supporting life through liquid water, a breathable atmosphere, and active plate tectonics.
Mars
The red planet with an axial tilt of 25.1∘ creating four seasons, featuring environments such as dust storms, deserts, ice caps, and sub-surface liquid water evidence at its south pole.
Jupiter
The largest planet in the solar system (1000× Earth's volume) containing a permanent cyclone, 79 moons (including Ganymede, Callisto, Io, and Europa), and an asteroid-retaining gravitational tug-of-war with the Sun.
Saturn
The second-largest yet lightest planet in the solar system, famous for its icy debris ring system, golden-hued atmosphere with swirling ammonia crystals, and 62 moons including Titan.
Uranus
The coldest planet in the solar system (−224∘C) featuring an extreme axial tilt of 98∘, 9 bright rings, a blue methane-rich atmosphere, and 27 moons named after characters created by Shakespeare and Pope.
Neptune
The farthest planet from the Sun (~30AU) with a tilt of 29∘, 14 moons, and the strongest recorded winds of any planet in the solar system.

Comet
An icy solar system body made of frozen gases, rock, and dust that sublimates when near the Sun, forming a glowing coma and distinct tails.
Comet Nucleus
The solid core of a comet composed of ice, dust, and rocky material ranging from hundreds of meters to tens of kilometers across.
Coma
The fuzzy, glowing envelope of gas and dust surrounding a comet's nucleus formed via sublimation as it approaches the Sun.
Dust Tail
A broad, slightly curved comet tail made of small dust particles reflecting sunlight, pointing generally away from the Sun.
Ion Tail
A thin, linear comet tail composed of charged gas particles pushed by solar wind, always pointing directly away from the Sun.
Kuiper Belt
A ring of icy bodies beyond Neptune's orbit spanning approximately 30AU to 55AU from the Sun, serving as the source of short-period comets.
Oort Cloud
A theoretical spherical shell of distant icy bodies surrounding the Solar System from 2,000AU to 100,000AU, serving as the source of long-period comets.
Asteroid Belt
A region located between Mars and Jupiter containing rocky and metallic debris, prevented from forming a planet due to opposing gravitational forces of Jupiter and the Sun.
Aurora
A atmospheric light phenomenon caused when charged particles from solar wind collide with atmospheric gases along Earth's magnetic field lines.
Kp Index
A scale from 0 to 9 measuring geomagnetic activity, where higher values indicate stronger auroras visible farther from the polar regions.
Conrad Discontinuity
The seismic boundary/transition zone located between the upper crust (SIAL) and lower crust (SIMA).
Mohorovičić Discontinuity
The boundary marking the transition zone between Earth's lower crust and upper mantle.
Repetti Discontinuity
The internal seismic transition zone situated between Earth's upper mantle and lower mantle.

Gutenberg Discontinuity
The distinct boundary transition zone separating Earth's mantle and outer core.
Lehmann Discontinuity
The boundary marking the transition zone between Earth's liquid outer core and solid inner core.
Oceanic Crust
Thin (5−10km thick), dense (2.9g/cm3) crustal layer formed by basalt lava flows and gabbro that sinks into the mantle to form ocean basins.
Continental Crust
Thick (10−75km thick), low-density (2.7g/cm3) granitic crustal layer that floats higher on the mantle.
Lithosphere
The rigid, brittle outer layer of the Earth comprising the entire crust and the uppermost solid mantle, approximately 100km thick.
Asthenosphere
A hot, mobile layer of partially molten rock in the upper mantle beneath the rigid lithosphere, approximately 180km thick.
Eon
The largest unit of geologic time, spanning hundreds of millions to billions of years (equivalent to a chronostratigraphic eonothem).
Era
Subdivision of an eon spanning tens to hundreds of millions of years, defined by major changes in Earth's climate, geography, and living organism diversity.
Period
Major subdivision of an era defined by changes in the fossil record and Earth's physical features.
Epoch
Subdivision of a geologic period defined by specific changes in the rock record, lasting hundreds of thousands to millions of years.
Absolute Dating
Geological dating techniques (e.g., radiometric isotopes such as Carbon-14 or Uranium-Lead) providing numerical age estimates in years.
Relative Dating
Determining the chronological order of geological events or rock strata from older to younger relative to one another without numerical age values.