Heath and pressure manage to move the material between the bottom and top part of the mantle, causing currents, and affecting the surface of Earth.
Explanation:
The heat and the pressure are crucial for the cycling of matter on our planet. This process happens in the mantle layer. The lower part of the mantle is hotter because of the higher influence by the core, while the upper part is not as hot (though very hot for surface standards). This causes the material in the upper part to be more solid and denser, which in turn causes it to sink toward the bottom. As this material sinks the hotter and less dense one from the bottom is pushed upward. This creates the convection currents.
As the material from the bottom moves upward it comes in contact with the lithosphere. It puts a lot of pressure on it and supported by the heat manages to crack it, which created the tectonic plates. Because of the constant pressure the tectonic plates are pushed and moved on the surface of Earth. On some places (subduction zones) the crust from the surface sinks into the mantle, while from the mantle we have rise of magma toward the surface, so the material is constantly circling and being recycled.
To see it cleared and everyone coming together to take all of it and recycle
Answer:
A tour guide is a person who goes with you on a tour and answers questions and provides information about the area or site you are visiting. This can include information about culture, history, historical sites, museums, and many others. Tour guides usually should be warm, pleasant, have a good memory, good knowledge about the tour, humor.
Answer:
Measurements are made from these images to make maps.
Explanation:
Satellite images are remotely sensed data that are often times used to generate maps.
- Satellites are part of the geographic information systems that are used to obtain information by proxy.
- Satellites images can often by used to obtain information about our solar system.
- Maps can be generated from the images.
Streams flowing from mountainous terrain commonly flow across alluvial fans at the edges of the valleys. ... In arid and semiarid regions, seepage of water<span> from the stream can be the principal </span>source<span> of aquifer recharge.</span>
