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Geothermal Gradient
The rate at which the Earth's temperature increases with depth, estimated at about 2.5 degrees per 100 meters.
Kola Super Deep Borehole
The deepest borehole in the world, located in Siberia, measuring more than 12 kilometers deep.
Peridotite
A dense, ultramafic rock that is lower in silica and rich in metals like magnesium and iron, often found in volcanic eruptions.
P Waves
Primary waves that are compression waves traveling faster than S waves and can move through solids and liquids.
S Waves
Secondary waves that are shear waves, slower than P waves, and cannot travel through liquids.
Moho Discontinuity
The boundary between the Earth's crust and the underlying mantle.
Lithosphere
The rigid outer part of the Earth, consisting of the crust and uppermost mantle, which makes up tectonic plates.
Asthenosphere
The upper part of the mantle, situated beneath the lithosphere, that behaves plastically and allows for movement over geological time.
Gutenberg Discontinuity
The boundary between the Earth's mantle and outer core.
Curie Point
The temperature above which certain materials lose their permanent magnetic properties, relevant to understanding the Earth's magnetic field.
Chondrite Meteorites
Meteorites that are rich in iron, carbon, and water, believed to be primordial material from which the Earth formed.
Iron Meteorites
Meteorites consisting mostly of iron and nickel, thought to originate from the cores of differentiated bodies in the early solar system.
Seismic Wave
Waves of energy caused by earthquakes that travel through the Earth's layers, providing information about its interior structure.
Seismograph
An instrument that records the motion of the ground during an earthquake, capturing seismic waves.
Shadow Zone
Regions of the Earth where seismic waves do not arrive due to being refracted by different materials.
Density
Mass per unit volume, important for understanding the classification of Earth's layers.
Earth's Core
The innermost part of the Earth, consisting of a liquid outer core and solid inner core, primarily composed of iron and nickel.
Seismic Wave Refraction
The bending of seismic waves as they pass through materials of different densities.
Earthquake
A sudden release of energy in the Earth's crust that causes seismic waves.
Seismic Waves
Energy waves that are produced by the movement of faults during earthquakes, which include P waves, S waves, and surface waves.