How does it affect the formation of mountains and the temperature in the surface? b. How does convection current affects the movement of tectonic plates?

Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
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a. Figure A shows the process of convection in the earth's mantle. How does it affect the formation of mountains and the temperature in the surface? b. How does convection current affects the movement of tectonic plates? c. How convection in Earth's interior and conduction in the surface affect the temperature in our atmosphere?
Ac
What's More
sobuction
übduelin
ml-ocenn rldge
Muatle
Figure A. Convection
rlalog
warta alr
air caolu
and sinks
Figure B. Conduction
Figure A shows a convection cell, warm material rises (up to the surface of the earth)
and cool material sinks. These cooled materials will eventually turn to land
formation. In mantle convection, the heat source is the core. The core of the earth is
very hot. It is nearly as hot as the surface of the sun - about 6000'C. Convection
current is relevant to the movement of tectonic plate because the heat builds up
pressure underneath the crust (tectonic plates). As they become unstable, they push
against each other (subduction) and rise upwards or one goes under the other.
Pigure B shows the process of conduction on how air molecules come in contact with
the warmer surface of the land or ocean, resulting to the increase of its thermal
energy through conduction. The thermal energy of the core is transferred to the
surface of the earth and the lower levels of ocean by conduction.
co_Q1_ELS S
Modu
9.
2021.10.26 23:33
Transcribed Image Text:Ac What's More sobuction übduelin ml-ocenn rldge Muatle Figure A. Convection rlalog warta alr air caolu and sinks Figure B. Conduction Figure A shows a convection cell, warm material rises (up to the surface of the earth) and cool material sinks. These cooled materials will eventually turn to land formation. In mantle convection, the heat source is the core. The core of the earth is very hot. It is nearly as hot as the surface of the sun - about 6000'C. Convection current is relevant to the movement of tectonic plate because the heat builds up pressure underneath the crust (tectonic plates). As they become unstable, they push against each other (subduction) and rise upwards or one goes under the other. Pigure B shows the process of conduction on how air molecules come in contact with the warmer surface of the land or ocean, resulting to the increase of its thermal energy through conduction. The thermal energy of the core is transferred to the surface of the earth and the lower levels of ocean by conduction. co_Q1_ELS S Modu 9. 2021.10.26 23:33
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