To learn about the temperature inside the Earth's crust, scientists study geothermal gradients, which measure the increase in temperature with depth. They often use data from wells, boreholes, and geothermal energy sites, as well as seismic studies to infer temperature distributions. Additionally, they analyze rock samples and mineral compositions, which can provide insights into thermal conditions at various depths. These methods help to create models of the Earth's thermal structure and understand geological processes.
The sudden vibration in the plates inside the crust causes the earths crust to rise & fall.
Well that will be intrusive igneous rocks, extrusive forms inside the earths crust
The earth's crust is not stress
Metamorphic rocks are formed by the effects of high temperature, pressure, and/or chemically active fluids. These forces cause existing rocks to recrystallize and change their mineral composition without melting.
continental crust
it depends on the deepth
The sudden vibration in the plates inside the crust causes the earths crust to rise & fall.
because of the metamorphism when temperature and pressure inside earths crust change that were present in the rock when it formed
it depends on the deepth
it depends on the deepth
Scientists study seismic waves to learn about the temperature inside the Earth's crust. By analyzing the speed and direction of these waves as they travel through different layers of the Earth, scientists can infer information about the temperature and composition of the Earth's crust.
The earths crust varies. There is no temperature because it varies from cold to hot.
sills
by heat and pressure
igneous rocks come from inside the earths crust. Usually through volcanoes, or fissures
volcano
The Earths crust is approximately 650 km deep.