Chapter 12 Flashcards
The transfer of heat through matter by molecular activity
Conduction
The transfer of heat by the mass movement or circulation of a substance
Convection
The innermost layer of Earth based on composition. It is thought to be largely an iron-nickel alloy with minor amounts of oxygen, silicon, and sulfur
Core
The gradual increase in temperature with depth in the crust. The average is 30 degrees C per kilometer in the upper crust
Geothermal Gradient
The solid innermost layer of earth, about 1216 kilometers in radius
Inner core
The rigid outer layer of Earth, including the crust and upper mantle
Lithosphere
Lies between the transition zone and the liquid core, contains the mineral perovskite, is the earths largest layer occupying 56% of the volume of the planet
Lower mantle
The solid rocky shell that extends from the base of the crust to a depth of 2900 kilometers
Mantle
A field that surrounds the Earth because of Earths convection currents in earths liquid iron core
Magnetic field
A subdivision of the mantle situated below the lithosphere. This zone of weak material exists below a depth of about 100 kilometers and in some regions extends as deep as 700 kilometers. The rock within this zone is easily deformed.
Asthenosphere
The part of the mantle that extends from the core-mantle boundary to a depth of 660 kilometers. Also known as lower mantle
Mesosphere
The boundary separating the crust and the mantle, discernible by an increase in seismic velocity
Moho
A layer beneath the mantle about 2270 kilometers thick, which has the properties of a liquid
Outer core
The zones between 105 and 140 degrees distance from an earthquake epicenter, which direct waves do not penetrate because of refraction by Earth’s core
Shadow zones
When seismic wave hits a boundary between different Earth materials and waves are reflected back toward surface
Seismic reflection