Thinning of the Earth's crust is caused by the Earth's mantle heating up and expanding. As the mantle expands, large areas of the crust fall in, where they are melted.
crust
When mass is added to Earth's crust, it causes the crust to subside and sink due to the increased weight. Conversely, when mass is removed from the crust, it can rebound and rise due to the decreased load. This process is known as isostatic adjustment and can result in changes in the Earth's topography.
One special feature of Earth's crust is that it is divided into tectonic plates that float and move on the semi-fluid upper mantle. This movement causes earthquakes, volcanoes, and the formation of mountain ranges.
Another word for Earth's outer surface is "crust."
The crust, more specifically the lithosphere.
The sudden vibration in the plates inside the crust causes the earths crust to rise & fall.
Compression and tension can indeed affect the thickness of the Earth's crust. Compression can thicken the crust by folding and faulting, while tension can cause stretching and thinning of the crust through processes like rifting and faulting. These tectonic forces play a significant role in shaping the Earth's crust over geological time scales.
The movement in earths plates create powerful forces that pull or squeeze the rock in the crust.
Thinning of ozone causes UV to enter the earth. These UV are fatal for life on earth.
Tension
It causes it to deform - this deformation is called "strain".
Pressure from the earths core
Simple- Convection in the mantle causes mantle to slowly move, and it pushes against the crust. As it does this, the tectonic plates move.
Because the density of the force increases.
The Earths crust is approximately 650 km deep.
A divergent boundary causes tensional stress, where tectonic plates are moving away from each other. This stress results in the stretching and thinning of the Earth's crust, leading to the formation of new crust through volcanic activity and seafloor spreading.
No. Earth's crust does not convect. Convection in the mantle, however can create hot spots and rifting, which can lead tot he formation of volcanoes.