No. Liquid iron is found in the outer core. There are distinct layers in the earth.
solid
The layer just below the lower mantle is the outer core. It is composed primarily of liquid iron and nickel and is responsible for generating Earth's magnetic field through the movement of these molten metals. The outer core lies beneath the mantle and above the solid inner core.
Gutenburg Discontinuity
Iron is most commonly found in the Earth's core, particularly in the outer and inner core layers. The outer core is primarily composed of liquid iron and nickel, while the inner core is made up of solid iron. Additionally, smaller amounts of iron can also be found in the mantle and crust, but the majority resides in the core.
The inner mantle comprises of silicon and magnesium sulphides and oxides while the outer mantle consists of tough liquid rock with iron and magnesium silicates.
The layer just below the lower mantle is the outer core. This layer is composed of liquid iron and nickel, and is responsible for generating Earth's magnetic field.
The liquid core of Earth is surrounded by the solid mantle and crust. This liquid outer core is mostly composed of iron and nickel, and it is responsible for generating Earth's magnetic field through convection currents.
The lower mantle is primarily solid, although some areas may experience partial melting to create magma. The solid nature of the lower mantle is due to high pressure, which helps keep the minerals in a solid state despite high temperatures.
solid
core
Gutenburg Discontinuity
The Earth's interior consists of the crust, mantle, outer core, and inner core. The crust is the outermost layer, followed by the mantle which is composed of the lithosphere and asthenosphere. Beneath the mantle is the outer core, made of liquid iron and nickel, and the inner core, composed of solid iron and nickel.
Outer core.
The earth's crust lower mantle is made up of silicate perovskites and ferropericlase. While the silicate perovskites are the names given to calcium silicates and magnesium iron, ferropericlase is an oxide of magnesium/iron. The lower mantle is at a depth that ranges from 650 kilometers to 2,890 kilometers.
its made of a mantle, inner core, outter core and crust.......and a magnetic field. The interior is made up of the # crust # lithosphere (part of crust & upper mantle) # upper mantle # asthenosphere (more liquid-like part of mantle) # lower mantle # outer core (liquid ball) # inner core (solid ball) ...is what im pretty sure of
The layer beneath the mantle and surrounding the inner core is the outer core. The outer core is composed mostly of liquid iron and nickel. Its movement is responsible for generating Earth's magnetic field.
A solid layer made of iron and a nicel