A seismograph is used to sense seismic waves in the earth. The seismic waves are sent down by scientist and how fast and how straight the line is when the seismograph reads them is how they tell which mineral or if its a liquid or solid.
Which is how they know about the inner and outter core, and the mantel.
Back in the early 1900s, two seismologists, Sir Harold Jeffreys and Keith Edward Bullen, made a series of travel-time curves that show how long it takes for different seismic waves to travel certain distances in through the earth. These curves show a general velocity through the earth. Seismic waves from an earthquake go through the earth in a push-pull, or sine wave motion (vertically and horizontally). These seismic waves reflect off of, refract off of, or speed up through different layers in the earth that have large changes in density. These velocities are used to determine approximate thicknesses of layers within the Earth, as distance (or thickness) = velocity*time.
Only one segment of inner earth is theorized to be liquid. This segment is known as the outer core. Scientists suspect that the outer core is liquid because of its interaction with seismic waves. A type of seismic wave known as an "S" wave or Shear wave moves side-to-side in a shearing motion and does not propagate through liquid only through solid.
Reflection and refraction seismology.
IDK find it out yourself you cheater I'm kidding it is the crust,inner core,and the lithosphere
Through Seismology, or through studying earthquakes, we have been able to find that the Earth's interior is composed of three layers: Crust, Mantle and Core. The core is further divided into outer core and inner core.
atmosphere/hydrospherelithosphereasthenospheremantleouter coreinner core(you could divide these further, but the above are the main 6 layers)
The mantle is the hot rock.
You cn find Mudrock in caves, and on beaches. It is most commonly found on the inner core of our perpendicular earth. If Mudrock reaches 5000 degrees it becomes igneous formations into crystals
To be precise, there is actually an outer core and an inner core. You can find the details in the Wikipedia article "Structure of the Earth".
Earth's core is made primarily of iron and nickel.
They measure how waves from earthquakes travel through the earth, and they test how waves travel through liquid and solid and goo, and they compare the results to find the consistency of the inner core and other layers of the earth.
The answer is we know what it is because if you Google it up you will find it says the heatness of the earth's inner core is why.
Scientists find out information on the core by using special tools to dig out samples from deep inside the earth. Special instruments "look inside" parts of the earth we cannot see.
The center of the planet. The Inner Core.
You can find the most Iron and nickel in the earth's inner and outer core.
IDK find it out yourself you cheater I'm kidding it is the crust,inner core,and the lithosphere
Through Seismology, or through studying earthquakes, we have been able to find that the Earth's interior is composed of three layers: Crust, Mantle and Core. The core is further divided into outer core and inner core.
It's approximately (3,963)miles down to the earths core.
atmosphere/hydrospherelithosphereasthenospheremantleouter coreinner core(you could divide these further, but the above are the main 6 layers)
The mantle is the hot rock.