The way the convection cell might affect the crust above it is that it can cause the earths surface to turn into a volcano. If there is already a volcano there then it will erupt,
Well, honey, that convection cell is like a little dance party under the Earth's crust. It's heating up and rising, then cooling down and sinking, causing all sorts of chaos above. The crust material above it is gonna feel the heat, quite literally, and might start shifting and cracking like a bad break-up. Just keep an eye on it, darling, and maybe grab some popcorn for the show.
There is no true answer to this question. But scientists believe Mercury's crust is anywhere from 100km-300km. They get an estimated measurement by taking the circumfrance of the earth and the estimated circumfrance of Mercury and adding them together then they take an approximate amount of earths crust and subtract the crust by the difference of the earths and mercurys crust
answer Mantle: Convection here leads to earthquakes Crust: Ranges from 6 km to 70 km thick Core: Has a liquid and solid layer Moho Barrier: Separates the crust and mantle The core has a liquid layer and a solid layer. The mantle has convection cells that lead to earthquakes. The Moho Barrier separates the mantle and the crust. The crust is the thinnest layer, ranging from about 6 km to 70 km in thickness
The plasticity of the mantle allows convection currents to occur, which drive the movement of Earth's lithospheric plates. As the hot mantle material rises and the cooler material sinks, it creates a cyclic motion that drags the overlying brittle lithosphere along, causing the plates to move. This movement can lead to plate tectonics, including the formation of new crust at mid-ocean ridges and the subduction of old crust at convergent boundaries.
Heating from the Earth's core drives convection in the upper mantle. This convection is extremely slow; the speed with which material in the Earth's crust spreads from the mid-ocean ridges is of the order of several cm per year. Nevertheless, it is evident that the same forces which drive convection in the atmosphere and in the ocean are present in the "solid" earth as well. Mantle convection is the slow creeping motion of Earth's solid silicate mantle caused by convection currents carrying heat from the interior of the Earth to the surface. Mantle convection is the slow creeping motion of Earth's solid silicate mantle caused by convection currents carrying heat from the interior of the Earth to the surface.
I think the convection cell might affect the crust because the convection cell is bigger than the crust.
I think the convection cell might affect the crust because the convection cell is bigger than the crust.
I think the convection cell might affect the crust because the convection cell is bigger than the crust.
Well, honey, that convection cell is like a little dance party under the Earth's crust. It's heating up and rising, then cooling down and sinking, causing all sorts of chaos above. The crust material above it is gonna feel the heat, quite literally, and might start shifting and cracking like a bad break-up. Just keep an eye on it, darling, and maybe grab some popcorn for the show.
No. As the word "core" might imply, it is the innermost part of Earth. The outermost layer is the crust.
it will make the earth hotter
Well what cools it is the atmosphere and the air that we breathe from. The earth's crust is very rocky and it also could be smooth, so when it rains or snows of course the earths land is cold. It is also just like how the matter rises from the center and goes to the top then the matter packs in and then it drops then rises again then comes back up. These are called convection currents.
Metal comes from Earths crust ,so if we dont reuse it ,we might run out of it some day
No, at the deepest part of the ocean, their is crack that with any interference, monsters from a parralel universe might come out and destroy the Earth.
they give it a slight wobble
It would have to be melted into the earths magma and cool down as either intrusive (inside the earth) or extrusive (on the Earth's crust) igneous rock.
It would have to be melted into the earths magma and cool down as either intrusive (inside the earth) or extrusive (on the Earth's crust) igneous rock.