In some places, Earth`s crust thins enough to see mantle.
In some places, Earth`s crust thins enough to see mantle.
The destructive force in the earths mantle is melted metals. The melted metal or molten lava is able to burn anything it touches.
crust
The soft layer of rock in the Earth's mantle is called the asthenoshere. The asthenoshere is a solid but able to flow slowly.
- By using seismic waves .
I dnt know that's why im asking you Dnt u know wat the answere is
The deepest scientist have been able to study earths interior depth is 12,262 meters
The destructive force in the earths mantle is melted metals. The melted metal or molten lava is able to burn anything it touches.
No we would over heat and die!
crust
The soft layer of rock in the Earth's mantle is called the asthenoshere. The asthenoshere is a solid but able to flow slowly.
Genetics is the study of inherited characteristics Geneticists study genes and DNA. Scientists who study genes may soon be able to prevent inherited diseases. .
Scientists are able to study specific genes.
making inferences based on data from seismic waves.
Scientists aren't able to dig any deeper because the the temperatures, and there's a risk of digging into the mantle, which could be very dangerous. Scientists aren't able to dig any deeper because the the temperatures, and there's a risk of digging into the mantle, which could be very dangerous.
- By using seismic waves .
Since we're not (yet?) able to drill a hole down there and find out, we're reduced to indirect measurements. Things like the mass of our planet and its gravity. (That's why we're pretty sure that the core is primarily iron.) The speed of earthquake vibrations in the mantle. The material that comes out of the Earth in volcanoes. Stuff like that.
Scientists learn about the Earth's interior through the use of seismographs. Since seismic waves travel at various speeds when passing through different types of material, scientists will be able to formulate the conditions of the Earth's interior.