because diamond and other minerals found in kimberlites can form only under very high pressures
surface
Mantle Is The Below Layer Of The Crust In Earth.
Convection currents in the mantle drive plate movements.
is the temperature if the stiffer mantle above or below its melting point
If we're talking layers of the earth, that would be the upper mantle, below the crust.
Scientists used detectors which determined the mantle existed. As well, scientists must hypothesize and theorize what cannot be readily seen, and make determinations based on the evidence that does exist.
Why do scientists look to the ocean floor to research the mantle? Because magma from the mantle flows out of active volcanoes on the ocean floor. These underwater volcanoes have given scientists many clues about the composition of the mantle.
Why do scientists look to the ocean floor to research the mantle? Because magma from the mantle flows out of active volcanoes on the ocean floor. These underwater volcanoes have given scientists many clues about the composition of the mantle.
Scientists predict the mantle is about 2,900 km (1,800 mi) thick.
Why do scientists look to the ocean floor to research the mantle? Because magma from the mantle flows out of active volcanoes on the ocean floor. These underwater volcanoes have given scientists many clues about the composition of the mantle.
They can do this by how and how quickly seismic waves can move through the mantle.
Scientists study the mantle indirectly by analyzing seismic waves from earthquakes, studying volcanic eruptions, and examining rock samples brought to the surface by volcanic activity. By combining these methods, scientists can gain valuable insights into the composition, temperature, and behavior of the Earth's mantle.
seismometers
In some places, Earth`s crust thins enough to see mantle.
the mantle
Convection currents in the mantle.
The mantle was not discovered by a single individual, but its composition and properties were studied and understood through the work of multiple scientists over time. Scientists such as Alfred Wegener, Arthur Holmes, and Inge Lehmann made significant contributions to our understanding of the Earth's mantle.