mainly the outer core
The solid layer of the Earth that is made mostly of iron and nickel is called the inner core.
The Earth consists of the core, mantle, and crust. The core is composed mostly of iron and nickel and generates the magnetic field. The mantle is a semisolid layer that transfers heat through convection. The crust is the outermost solid layer where we find oceans, continents, and other landforms.
The inner core of the Earth is the oldest layer, estimated to be about 4.5 billion years old. This layer is solid and composed mostly of iron and nickel.
The outer core of the Earth is predominantly composed of liquid iron, along with some nickel. This layer lies beneath the solid inner core and surrounds the Earth's solid mantle and crust. The movement of the liquid iron in the outer core generates the Earth's magnetic field.
The different layers of the Earth are primarily due to differences in density and composition. The outermost layer, the crust, is the lightest and thinnest layer, made mostly of solid rock. The mantle below is more dense, composed of solid but flowing rock. The core, the deepest layer, is the densest and consists mostly of iron and nickel.
The solid layer of the Earth that is made mostly of iron and nickel is called the inner core.
It is believed that the innermost layer of the earth, the inner core, is made mostly of iron and nickel.
The Earth consists of the core, mantle, and crust. The core is composed mostly of iron and nickel and generates the magnetic field. The mantle is a semisolid layer that transfers heat through convection. The crust is the outermost solid layer where we find oceans, continents, and other landforms.
The inner core of the Earth is the oldest layer, estimated to be about 4.5 billion years old. This layer is solid and composed mostly of iron and nickel.
The spherical solid core of the earth. It is an alloy composed mostly of nickel and iron.
The outer core of the Earth is predominantly composed of liquid iron, along with some nickel. This layer lies beneath the solid inner core and surrounds the Earth's solid mantle and crust. The movement of the liquid iron in the outer core generates the Earth's magnetic field.
The different layers of the Earth are primarily due to differences in density and composition. The outermost layer, the crust, is the lightest and thinnest layer, made mostly of solid rock. The mantle below is more dense, composed of solid but flowing rock. The core, the deepest layer, is the densest and consists mostly of iron and nickel.
There is no layer of Earth that is predominantly molten rock. The only layer of Earth that is liquid is the outer core, however this is mainly iron and nickel. The mantle, the thickest layer of the Earth, contains rock that is "ductile" (i.e. very viscous and able to flow very slowly), but not technically "liquid."
The layer of the Earth with the magnetic field is the outer core. This layer consists of molten iron and nickel that generates the planet's magnetic field through a process called the geodynamo effect.
The layer of the Earth that is mostly solid metal is the inner core. The inner core is primarily composed of solid iron and nickel, with temperatures reaching up to 9,000 degrees Fahrenheit.
The Earth's core is mostly made of nickel and iron. It is divided into the outer core, which is liquid, and the inner core, which is solid. These two layers primarily consist of these heavy metals.
A non-example of the ozone layer would be the Earth's core. The ozone layer is a layer of ozone gas in the stratosphere that helps protect the Earth from the sun's harmful ultraviolet rays, while the Earth's core is the innermost layer of the Earth composed of mostly iron and nickel.