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Meteorites which are sometimes remnants of exploded planets reveal what the inner layers may consist of. Also of use in inferring the structure of Earth are the responses of seismic waves as they travel through the Earth and are recorded by scientific instruments. Mathematical calculations of Earth's density and its relation to our gravitational effects on the surrounding celestial bodies also plays a part in determing composition. And finally, the study of the magnetosphere, the magnetic field around the Earth which blocks harmful solar radiation, reveals the structure and interplay of the inner and outer core.
The structure of the Earth relates to plate tectonics as in the Earth structure there is the mantle layer, crust layer, inner and outer layer etc. The crust layer on top of the Earth is not a solid layer, the layer the broke up into big chunks which are now called tectonic plates.
solid can be found on the inner core of the earth
The inner and outer core are made mostly of molten rock and lead, as the very center is solid because of the constant force. The thick mantle is liquid towards the center and is primarily considered to be solid. The outer core is what I would say to be the "only" liquid layer in Earth's structure as the inner core has too much pressure and the mantle had too little heat.
Scientists use the difference in density between the inner and outer core as evidence that the inner core is solid. This was proven using seismic waves traveling through the earth.
Meteorites
It is Because one can't go inside earth since it is too hot. Hence, one has to use their evidence from rock samples and seismic waves.
It got its inner structure by sucking your granpa's wrinkly dick
the mantle the outer core and the inner core
core, mantle, inner crust, outer crust
Meteorites which are sometimes remnants of exploded planets reveal what the inner layers may consist of. Also of use in inferring the structure of Earth are the responses of seismic waves as they travel through the Earth and are recorded by scientific instruments. Mathematical calculations of Earth's density and its relation to our gravitational effects on the surrounding celestial bodies also plays a part in determing composition. And finally, the study of the magnetosphere, the magnetic field around the Earth which blocks harmful solar radiation, reveals the structure and interplay of the inner and outer core.
Meteorites which are sometimes remnants of exploded planets reveal what the inner layers may consist of. Also of use in inferring the structure of Earth are the responses of seismic waves as they travel through the Earth and are recorded by scientific instruments. Mathematical calculations of Earth's density and its relation to our gravitational effects on the surrounding celestial bodies also plays a part in determing composition. And finally, the study of the magnetosphere, the magnetic field around the Earth which blocks harmful solar radiation, reveals the structure and interplay of the inner and outer core.
Lots of evidence comes from seismology. The magnitude, direction and speed of transverse and compression waves from earthquakes and sub surface explosions can divulge a lot of information about the structure of the Earth.
Meteorites which are sometimes remnants of exploded planets reveal what the inner layers may consist of. Also of use in inferring the structure of Earth are the responses of seismic waves as they travel through the Earth and are recorded by scientific instruments. Mathematical calculations of Earth's density and its relation to our gravitational effects on the surrounding celestial bodies also plays a part in determing composition. And finally, the study of the magnetosphere, the magnetic field around the Earth which blocks harmful solar radiation, reveals the structure and interplay of the inner and outer core.
Meteorites which are sometimes remnants of exploded planets reveal what the inner layers may consist of. Also of use in inferring the structure of Earth are the responses of seismic waves as they travel through the Earth and are recorded by scientific instruments. Mathematical calculations of Earth's density and its relation to our gravitational effects on the surrounding celestial bodies also plays a part in determing composition. And finally, the study of the magnetosphere, the magnetic field around the Earth which blocks harmful solar radiation, reveals the structure and interplay of the inner and outer core.
Meteorites which are sometimes remnants of exploded planets reveal what the inner layers may consist of. Also of use in inferring the structure of Earth are the responses of seismic waves as they travel through the Earth and are recorded by scientific instruments. Mathematical calculations of Earth's density and its relation to our gravitational effects on the surrounding celestial bodies also plays a part in determing composition. And finally, the study of the magnetosphere, the magnetic field around the Earth which blocks harmful solar radiation, reveals the structure and interplay of the inner and outer core.
Meteorites which are sometimes remnants of exploded planets reveal what the inner layers may consist of. Also of use in inferring the structure of Earth are the responses of seismic waves as they travel through the Earth and are recorded by scientific instruments. Mathematical calculations of Earth's density and its relation to our gravitational effects on the surrounding celestial bodies also plays a part in determing composition. And finally, the study of the magnetosphere, the magnetic field around the Earth which blocks harmful solar radiation, reveals the structure and interplay of the inner and outer core.