The temperature is highest in the inner core of Earth, reaching up to 6000°C (10,800°F). This intense heat is primarily generated by the radioactive decay of elements and the residual heat from Earth's formation.
The mantle is the largest layer in the Earth's interior.
The temperature is highest in the thermosphere, the outermost layer of the Earth's atmosphere. This is where solar radiation is absorbed, leading to high temperatures.
The temperature zone layer of Earth's atmosphere shown in the cross-section is the stratosphere. This layer is characterized by an increase in temperature with altitude due to the presence of the ozone layer, which absorbs and scatters UV radiation from the sun.
The Earth's crust is the thinnest layer, ranging from about 5-70 km thick. The average density of the Earth's crust is around 2.7-3.0 g/cm³.
The temperature of the Earth's layers increases from the crust towards the core. The outermost layer, the crust, has the lowest temperature, while the inner core has the highest temperature. This gradient is due to the heat generated by radioactive decay in the core and the residual heat from the Earth's formation.
Rock cycle
the mantle
inner core
Thermosphere, it is also the atmosphere with the highest temperatures.
The mantle
The mantle is the largest layer in the Earth's interior.
troposphere
thermosphere
The temperature is highest in the thermosphere, the outermost layer of the Earth's atmosphere. This is where solar radiation is absorbed, leading to high temperatures.
Thermosphere, it is also the atmosphere with the highest temperatures.
the material is hotter & denser
the mantle, which contains the lithosphere, asthenosphere and the mesosphere