Why Do Scientists Estimate The Density Of The Inner Core
Scientists can estimate the density of the inner core to be 12.7 – 13.0 g/cm3, because our best evidence comes from iron meteorites, because they are composed of iron and nickel. Scientists also use seismic waves to find important information about the density of the inner core by looking at the sizes of the waves.
The inner cores density is based on the way seismic pressure waves move through the Earth to arrive at locations remote from the earthquake source. Scientists estimate that the inner cores density is 12.7 to 13.0 g/cm3, because the pressure deep in Earth’s core increases density by forcing liquids to turn into a solid state, and then as the pressure increases, solids turn into new tightly packed crystal structures. This shows
The inner cores density is based on the way seismic pressure waves move through the Earth to arrive at locations remote from the earthquake source. Scientists estimate that the inner cores density is 12.7 to 13.0 g/cm3, because the pressure deep in Earth’s core increases density by forcing liquids to turn into a solid state, and then as the pressure increases, solids turn into new tightly packed crystal structures. This shows