crust
The three primary layers of the Earth's ionosphere are the D layer, which is the lowest layer closest to the surface, the E layer, which is the middle layer, and the F layer, which is the highest layer. Each layer has unique characteristics and plays a role in the reflection and absorption of radio waves in the atmosphere.
The mantle is the second coolest layer of the Earth, located between the crust and the core. It is mainly composed of solid rock and extends about 1,800 miles below the Earth's surface. Temperature in the mantle ranges from about 392°F to 7,230°F.
The Ionosphere is one layer of charged particles above the Earth, and is important for High Frequency radio communication. There are several layers in the ionosphere, and since they weren't certain that the first one identified was not guaranteed to be the lowest, it was given the name of 'the e-layer'. Above it are some f-layers, and below it a d-layer. Some of these are at least in part controlled by the UV from the Sun.
The ionosphere consists of the D layer and F layer. The D layer is located closest to the Earth's surface, while the F layer is situated higher up in the atmosphere. These two layers play a critical role in reflecting radio waves and affecting communication systems.
The inner core of the Earth is the layer that has temperatures reaching up to 11,000°F. It is the hottest part of the Earth, mainly composed of solid iron and nickel, and is under immense pressure from the surrounding layers.
The lower mantle is a solid layer located between the upper mantle and the outer core of the Earth, composed mainly of silicate minerals. In contrast, the inner core is a solid sphere composed primarily of iron and nickel at Earth's center due to extreme pressure. The lower mantle is part of the mantle layer, whereas the inner core is part of the core layer of the Earth.
Mesosphere
The thermosphere is the layer of Earth's atmosphere with the highest temperatures. In this layer, temperatures can reach up to 2,500 degrees Celsius due to the absorption of high-energy solar radiation.
the third layer of earths atmosphere
Is called a fault. By the way, did you need the answer for a school crossword.
Radio and TV signals are reflected back to Earth in the ionosphere, specifically in the F layer. This layer is located approximately 150-500 kilometers above the Earth's surface and is characterized by its ability to reflect high-frequency radio waves.
The ionosphere layer, specifically the upper layers known as the F layer and the E layer, can reflect radio waves back to Earth through a phenomenon called ionospheric reflection. These layers are made up of charged particles that can alter the path of radio waves, allowing them to travel beyond the line of sight and communicate over long distances.