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Vocabulary flashcards covering the structure and chemical composition of the lithosphere, Earth's internal layers, seismic discontinuities, and meteorological scales.
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Lithosphere
The solid, outer part of the Earth, derived from the Greek words lithos ('rocky') and sphaeros ('sphere'), consisting of the crust and the brittle upper portion of the mantle.
Lithosphere-Asthenosphere Boundary (LAB)
The boundary where geologists and rheologists mark the change in ductility between the rigid lithosphere and the underlying viscous asthenosphere.
Ductility
A property measuring a solid material's ability to deform or stretch under stress.
Oceanic Lithosphere
The portion of the lithosphere with a mafic composition (rich in iron and magnesium, mostly basalt and gabbro), a thickness of 5–10km, a density of approximately 3.0g/cm3, and an age typically under 200 million years.
Continental Lithosphere
The portion of the lithosphere with a felsic composition (rich in silica and aluminum, generally granitic), a typical thickness of about 200km, a lower density of approximately 2.7g/cm3, and an age that can reach billions of years.
Crust
The outermost layer of the Earth, making up 0.5–1.0% of Earth's volume and less than 1% of its mass, with an average density of about 2.7g/cm3.
Sial
The group of lighter silicate minerals composed of silica and aluminium that make up the continental crust.
Sima
The group of heavier silicate minerals composed of silica and magnesium that make up the oceanic crust.
Abundance of Elements in Earth's Crust
The elemental abundance order by weight in the Earth's crust: Oxygen > Silicon > Aluminium > Iron > Calcium > Sodium > Potassium > Magnesium.
Abundance of Elements in Whole Earth
The elemental abundance order by weight across the entire Earth: Iron > Oxygen > Silicon > Magnesium > Nickel > Sulphur > Calcium > Aluminium.
Mantle
The layer extending from Moho's discontinuity to a depth of 2,900km, comprising about 83% of the Earth's volume and 67% of its mass.
Asthenosphere
The upper portion of the mantle extending up to 80–200km that is highly viscous, mechanically weak, and ductile, serving as the primary source of magma for volcanic eruptions.
Outer Core
The liquid layer of molten iron and nickel surrounding the inner core, with a thickness of about 2,200–2,300km, whose movement generates Earth's magnetic field.
Inner Core
The solid, innermost layer of Earth with a radius of about 1,220km, composed mainly of iron (Fe) and nickel (Ni) under extreme pressure, reaching temperatures of 5000–6000∘C.
Discontinuities
Transition zones separating internal layers of the Earth that differ in physical and chemical properties such as temperature and density.
Conrad Discontinuity
The seismic discontinuity located between the upper crust and lower crust.
Mohorovičić Discontinuity
The seismic discontinuity located between the lower crust and upper mantle.
Repetti Discontinuity
The seismic discontinuity located between the upper mantle and lower mantle.
Gutenberg Discontinuity
The seismic discontinuity located between the lower mantle and outer core.
Lehmann Discontinuity
The seismic discontinuity located between the outer core and inner core.
Microscale
An atmospheric scale encompassing very small atmospheric processes with horizontal dimensions from a few meters to a few kilometers and lasting from a few seconds to several minutes.
Mesoscale
An atmospheric scale dealing with weather phenomena occurring over areas from several kilometers to a few hundred kilometers and persisting from minutes to a few hours.
Synoptic Scale
An atmospheric scale covering large weather systems extending across hundreds to thousands of kilometers and lasting from several days to about a week.
Planetary Scale
The largest atmospheric scale, involving global systems extending across continents or the entire globe and persisting for weeks, months, or longer.