ALiquid
BSolid
CGas
DPlasma
Answer:
A. Liquid
Read Explanation:
Spheres of the earth
Based on the analysis of the structure & composition generated during earthquakes, the Earth has been divided into different layers.
Crust
Mantle
Outer core
Inner core
Crust
The comparatively thin outer shell of the earth.
Approximately 10 km thick
Two parts – Continental crust, oceanic crust.
The continental crust is made of granitic, metamorphic, and sedimentary rocks. It's sometimes called sial because it's rich in aluminum silicates (Al-Si)
Oceanic crust differs from continental crust in several ways: it is thinner, denser, younger, and of different chemical composition.
Mantle
Located beneath the curst.
Extended upto 2900km from the crust
Two parts - upper mantle, lower mantle.
Upper mantle
This layer is made up of solid and molten rock, and extends from the Earth's crust to a depth of 255 miles. It contains two parts: the asthenosphere, which is a transition zone of semi-molten rock, and the lithosphere, which contains the tectonic plates
Lower mantle
This layer is located directly above the outer core, and is made up of solid rock that's around 7,000° F in temperature. It's hotter and denser than the upper mantle, and is less ductile. The intense pressure in the lower mantle keeps it solid, despite the high temperatures
Core
Central part of the earth
From 2900km to 6371 km
Two parts - outer core, inner core
Inner core - Solid, with a radius of 1,216 km. The inner core is under intense pressure, which keeps it solid despite its high temperature
Outer core - Liquid, with a thickness of about 1,300 miles (2,092 km). The outer core is liquid because there isn't enough pressure to keep it solid.