In the convection Zone!
Geothermal energy comes from the Earth's mantle, which is located between the crust and the core. Heat from the Earth's interior is transferred to the surface through volcanic activity and geothermal reservoirs, which can be tapped for energy production.
CFC's i.e Chloro Fluorocarbon which are released from deodorants, refrigerants are carried upwards towards the atmosphere where in presence of the high energy ultraviolet rays these break down into molecules of chlorine and fluorine molecules which further deplete ozone.
The outermost layer of Earth's atmosphere is the exosphere. This layer is where the atmosphere is the thinnest, gradually transitioning into space. The exosphere is composed mostly of hydrogen and helium atoms.
The thermosphere is the layer of the atmosphere that contains the fewest gases. Although it is a very low-density layer, it is composed mainly of nitrogen and oxygen atoms.
The layer of the atmosphere closest to the sun is the thermosphere. This layer absorbs the majority of the sun's energy and is where temperatures can reach thousands of degrees Celsius.
The convection zone.
The convection zone
Energy is transformed between atoms in the radiative zone of the sun. In this layer, energy moves through the absorption and re-emission of photons by atoms. This process creates a gradient of temperature and density as energy is slowly transferred from the core to the surface of the sun.
Energy can be transferred by conduction between the Earth's lithosphere (solid outer layer) and the atmosphere (gas layer). Another example is the transfer of energy by conduction between a hot electric stove and a pot placed on it.
The Radiative Zone.
The convection zone.
The Radiative Zone.
the azone layer
The Radiative Zone.
The Radiative Zone.
The Radiative Zone.
The Radiative Zone.