<P> The crust ranges from 5--70 kilometres (3.1--43.5 mi) in depth and is the outermost layer . The thin parts are the oceanic crust, which underlie the ocean basins (5--10 km) and are composed of dense (mafic) iron magnesium silicate igneous rocks, like basalt . The thicker crust is continental crust, which is less dense and composed of (felsic) sodium potassium aluminium silicate rocks, like granite . The rocks of the crust fall into two major categories--sial and sima (Suess, 1831--1914). It is estimated that sima starts about 11 km below the Conrad discontinuity (a second order discontinuity). The uppermost mantle together with the crust constitutes the lithosphere . The crust - mantle boundary occurs as two physically different events . First, there is a discontinuity in the seismic velocity, which is most commonly known as the Mohorovičić discontinuity or Moho . The cause of the Moho is thought to be a change in rock composition from rocks containing plagioclase feldspar (above) to rocks that contain no feldspars (below). Second, in oceanic crust, there is a chemical discontinuity between ultramafic cumulates and tectonized harzburgites, which has been observed from deep parts of the oceanic crust that have been obducted onto the continental crust and preserved as ophiolite sequences . </P> <P> Many rocks now making up Earth's crust formed less than 100 million (1 × 10) years ago; however, the oldest known mineral grains are 4.4 billion (4.4 × 10) years old, indicating that Earth has had a solid crust for at least that long . </P> <P> Earth's mantle extends to a depth of 2,890 km, making it the thickest layer of Earth . The mantle is divided into upper and lower mantle . The upper and lower mantle are separated by the transition zone . The lowest part of the mantle next to the core - mantle boundary is known as the D" (pronounced dee - double - prime) layer . The pressure at the bottom of the mantle is ≈ 140 G Pa (1.4 M atm). The mantle is composed of silicate rocks that are rich in iron and magnesium relative to the overlying crust . Although solid, the high temperatures within the mantle cause the silicate material to be sufficiently ductile that it can flow on very long timescales . Convection of the mantle is expressed at the surface through the motions of tectonic plates . As there is intense and increasing pressure as one travels deeper into the mantle, the lower part of the mantle flows less easily than does the upper mantle (chemical changes within the mantle may also be important). The viscosity of the mantle ranges between 10 and 10 Pa s, depending on depth . In comparison, the viscosity of water is approximately 10 Pa s and that of pitch is 10 Pa s . The source of heat that drives plate tectonics is the primordial heat left over from the planet's formation as well as the radioactive decay of uranium, thorium, and potassium in Earth's crust and mantle . </P> <P> The average density of Earth is 5,515 kg / m . Because the average density of surface material is only around 3,000 kg / m, we must conclude that denser materials exist within Earth's core . Seismic measurements show that the core is divided into two parts, a "solid" inner core with a radius of ≈ 1,220 km and a liquid outer core extending beyond it to a radius of ≈ 3,400 km . The densities are between 9,900 and 12,200 kg / m in the outer core and 12,600--13,000 kg / m in the inner core . </P>

Enlist and explain the different layers of the interior of the earth along with diagram