Chapter 1 Vocab Flashcards
Asthenosphere
A weak and perhaps partly molten weak layer of Earth’s mantle below the lithosphere.
Conduction
Process of transferring heat by contact between two surfaces of different temperatures; head transfers without motion of water
Convection
Process of simultaneously transferring heat and matter by movement of fluid or plastically deforming rock because of density contrast; denser and typically colder material sinks while less dense and typically warmer material rises.
Convergent Plate Boundary
Curving zone where plates collide nearly head on into one another, compressing the lithosphere and causing subduction of one plate beneath the other.
Core
The central region of Earth composed primarily of iron metal and consisting of a molten liquid outer part and a solid inner part.
Crust
Outermost concentric layer of Earth composed of mostly silicate minerals and containing more silicon and aluminum than the underlying mantle.
Divergent Plate Boundary
Linear or curving zones where plates move apart from one another and new lithosphere forms.
Energy
A measure of the ability to do work.
Geology
The science of the origin, composition, structure and history of the Earth
Hot Spots
An area of intense volcanic activity not explained by plate boundary process. Hot Spots form where asthenosphere rises beneath lithospheric plates.
Hypothesis
Testable prediction about a natural process that can be checked using data.
Laws
Scientific description of how nature is observed to behave.
Lithosphere
Outer strong shell of earths consisting crust and uppermost mantle.
Mantle
The mostly solid but generically weak silicate zone of Earth below the crust and above the core.
Plates
One of several discrete, ridged to semi- ridged, roughly 100km thick slabs that make up earths lithosphere.
Plate Tectonics
Theory that Earths out shell is not seamlessly continuous but is broken into discrete pieces that move slowly relative to one another and change in size over geologic time.
Potential Energy
Energy that an object possesses because of its elevation. The potential energy that causes objects to move is greater for objects at high elevation that for objects at low elevation. Objects move from areas where the possess high potential energy to areas where they possess low potential energy.