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A set of vocabulary flashcards derived from the lecture notes on the structure, composition, and properties of Earth's layers.
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Seismic Waves
Waves of energy that travel through the Earth's interior, generated by earthquakes.
Isostasy
The equilibrium between the Earth's crust and upper mantle, where the crust floats on the viscous mantle.
Lithosphere
The rigid outer layer of the Earth, consisting of the crust and the uppermost part of the upper mantle.
Asthenosphere
The partially molten layer of the upper mantle that behaves like a viscous fluid.
Core
The innermost layer of the Earth, primarily composed of iron (Fe) and nickel (Ni).
P Waves
Primary waves, a type of seismic wave that compress and expand material.
S Waves
Secondary waves, a type of seismic wave that shears material and cannot pass through liquids.
Moho Discontinuity
The boundary between the Earth's crust and the underlying mantle.
Convection
The movement caused within a fluid by the tendency of hot material to rise and cool material to sink.
Crust
The outermost layer of the Earth, consisting of oceanic and continental crust.
Mantle
The layer of the Earth between the crust and the core, consisting of solid rock that flows slowly.
Outer Core
The liquid layer of the core, lying beneath the mantle and above the inner core.
Inner Core
The solid innermost layer of the Earth, composed primarily of iron and nickel.
Geodynamo
The process that generates Earth's magnetic field through the motion of conductive fluids in the outer core.
Geotherm
The rate of temperature increase with depth in the Earth.
Shadow Zone
Areas on the Earth's surface where no seismic waves from a given earthquake can be detected.
Density
The mass per unit volume of a substance, significant in geological structures and isostatic calculations.
Gravity
The force of attraction between objects with mass, influencing isostatic balance.
Crustal Root
The deeper part of the crust that extends below mountain ranges, contributing to mountain height.
Compression
A type of stress that occurs when rocks are squeezed together.
Shear
A type of stress that causes layers of rock to slide past one another.
Archimedes Principle
The principle stating that an object immersed in a fluid is buoyed up by a force equal to the weight of the fluid displaced.
Brittle
A property of rocks that indicates they will break or shatter under stress instead of deforming.
Plastic
A property describing materials that can flow or deform under stress without breaking.
Temperature Gradient
The rate at which temperature changes with depth within the Earth.
Basaltic Rocks
Rocks formed from basalt; typically found in oceanic crust and rich in iron and magnesium.
Granitic Rocks
Rocks composed mainly of quartz and feldspar; common in continental crust.
Peridotite
A dense, coarse-grained rock composed mainly of olivine, found in the upper mantle.
Buoyancy
The ability of an object to float in a fluid, related to isostasy.
Rebound
The process by which the Earth's crust rises after being depressed by weight, such as from ice sheets.
Thermal Expansion
The increase in volume of materials as they are heated.
Tectonic Plates
Massive slabs of Earth's crust that move and interact at their boundaries, causing earthquakes and volcanism.
Upper Mantle
The upper layer of the mantle, directly beneath the crust.
Lower Mantle
The portion of the mantle located below the upper mantle, reaching down to the outer core.