Temperature
The density increases
The density increases
Outgassing is the release of trapped gases from within the earths interior to the earths atmosphere. It also includes outgassing at the smaller scale, such as the mostly porous pumice.
As elements decay within the Earth's interior, they release energy. This energy creates movement within the magma (along with the rotation of the Earth and heat) and this movement causes the plates of the Earth to move, hence the geography of the planet is different to thousands and millions of years ago.
Uneven heating of the Earths atmosphere and oceans by the sun
The density increases
The density increases
Tectonic Plate Movement
tectonic plate motion
tectonic plate motion
Beneath the surface of the earth temperature remains the same. Within the Earth, irregular convection cells within the mantle transfer heat from the core to the surface of the planet. Volcanoes and earthquakes are two examples of heat transferring from the interior to the surface.
Outgassing is the release of trapped gases from within the earths interior to the earths atmosphere. It also includes outgassing at the smaller scale, such as the mostly porous pumice.
The mantle lies between the crust and the outer core of Earth's interior, and is not within the crust.
heat.
An intrusive igneous rock is formed by the gradual cooling, solidification, and crystallization of magma within the earths crust/interior.
It shows that the rock is a plutonic rock and was formed as a result of slow cooling within the earths crust/interior.
Convection currents are agents of heat transfer within Earth's interior. And could also serve as mechnism for heat generation in the earth crust.