earthquakes and volcanoes
It's mantle with less, then mantle with more as you go deeper into earth.
As you go deeper and deeper the layers will start to get hotter and thicker.
The degree of temperature and exertion of pressure by the molten materials (magma) within the mantle is directly proportional to its depth. This means that, the deeper you go down the mantle the higher the degree of temperature and pressure exerted.
P waves unlike S waves can go through liquid ie. the mantle. When a P waves hits the mantle it is refracted and changes speed.
Because the mantle rock is opaque, most radiation (except for radioactivity from decay of uranium and other radioisotopes) cannot pass through it. Radiation from radioisotopes (e.g. x-rays, gamma rays, beta rays) occurs in earth's mantle and can go significant distances before being absorbed by the rock, helping to keep the mantle hot.
The deeper into the Earth you go it gets hotter and hotter.
It's mantle with less, then mantle with more as you go deeper into earth.
Deeper near the core and mantle. The deeper you go, the hotter it gets.
As you go deeper into the earth the temperature increase. The rate at which the temperature increases is called the geothermal gradient.
As you go deeper and deeper the layers will start to get hotter and thicker.
Temperature and pressure increases.
The deeper you go inside the ground the hotter it gets and the more pressure begins to build. So basicly they both increaese.
The degree of temperature and exertion of pressure by the molten materials (magma) within the mantle is directly proportional to its depth. This means that, the deeper you go down the mantle the higher the degree of temperature and pressure exerted.
Each relationship between each layer is different. Like the mantle and the outer core. Its like the mantle is solid and it starts to soften and turn to liquid the deeper you go. Or like the outer core and the inner core . The outer core starts to get harder and denser and the deeper you go the solider it gets. Like the mantle and the crust too. The mantle gets a little more solid and becomes the crust.
convection currents. the great heat and pressure inside the mantle causes the solid rock to move very slowly.Whoo! Go science!GO MATH >B) SHAM WOW!!!! whoa that was randoom
If a metamorphic rock were to reach the mantle and melt, it would become magma. If that magma were then to recrystallize it would be an igneous rock.
It becomes a solid and gives off heat.