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Age of the Earth
4.6 billion years old
Plate Tectonics
The theory that explains the movement of Earth's lithospheric plates driven by mantle convection.
Earth Formation
4.6 billion years ago.
Moon Formation
4.5 billion years ago.
First Bacteria
3.8 billion years ago.
First Oxygen Accumulation
About 2 billion years ago.
Nebular Hypothesis
The widely accepted theory that explains the formation of the solar system from a rotating cloud of gas and dust.
Solar Nebula
The cloud of gas and dust from which our solar system formed, consisting primarily of hydrogen and helium.
Accretion
The process by which particles clump together to form larger bodies, eventually leading to planet formation.
Protoplanets
Larger bodies that formed from the collision and merging of planetesimals, leading to the formation of planets.
Tidal Forces
Forces exerted by gravity from large bodies, influencing the shapes and orbits of smaller bodies in the solar system.
Solar Wind
A stream of charged particles ejected from the sun that affects the atmospheres of celestial bodies, including planets.
Van Allen Belts
Two doughnut-shaped regions of charged particles trapped by Earth's magnetic field, located above the atmosphere.
Planetesimals
Small celestial bodies that formed from dust and gas in the solar nebula, coalescing to create planets.
Lithospheric Plates
Rigid segments of the Earth's lithosphere that move on the semi-fluid asthenosphere, driving plate tectonics.
Asthenosphere
The semi-fluid layer of the Earth's mantle located beneath the lithosphere, responsible for enabling plate tectonics.
The driving force for plate tectonics
Convection
Ring of Fire
A horseshoe-shaped area in the Pacific Ocean known for a high frequency of earthquakes and volcanic eruptions, resulting from tectonic plate boundaries.
Tectonic Plate Movement Speed
1 to 10 centimeters per year, similar to the rate at which human fingernails grow.
Silicate Minerals
The most abundant group of minerals in the Earth's crust, composed primarily of silicon and oxygen tetrahedra.
Carbonate Minerals
The second most abundant group of minerals in the Earth's crust, primarily composed of CO3.
Extrusive Igneous Rocks
Rocks formed from the cooling and solidification of lava that erupts onto the Earth's surface.
Intrusive Igneous Rocks
Rocks formed from the cooling and solidification of magma within the Earth's crust.
Weathering
The process by which rocks, including igneous rocks, are broken down into smaller particles or sediments through physical and chemical means.
Stages of the Rock Cycle
Melting, crystallization, erosion, sedimentation, compaction, and metamorphism.
Melting
The process where rocks turn into magma due to high temperatures.
Crystallization
The solidification of magma into igneous rocks as it cools.
Erosion
The wearing away and transport of rock and soil by wind, water, or ice.
Sedimentation
The accumulation of sediments that can form sedimentary rocks over time.
Compaction
The process of layers of sediments being pressed together under pressure.
Metamorphism
The alteration of existing rocks due to heat, pressure, and chemical processes, leading to the formation of metamorphic rocks.
Clastic Sedimentary Rocks
Rocks formed from the accumulation and cementation of fragments, or clasts, of pre-existing rocks.
Non-Clastic Rocks
Rocks formed by chemical precipitation, including limestone and evaporites, resulting from the evaporation of water or the precipitation of minerals from solution.
Number of Discovered Exoplanets
Over 5000
Neptune-like
35% of exoplanets are
Earth-like
3% of exoplanets are
Gas Giants
30% of exoplanets are
Terrestrial
4% of exoplanets are