Answer:
The correct answer is "Divergent boundary in the ocean
".
Explanation:
- The so-called divergent limits when two oceanic plates move apart. Ultimately, divergent borders between hemispheres or continentals generate rifts that eventually generate rift valleys.
- Alongside oceanic flats seem to be the dynamic or energetic divergent bounds as well as they are frequently dubbed midfield furrows.
So the preceding solution is the right one.
Answer:
Heat from the mantle forms convection currents causing the tectonic plates to diverge and form ocean basins.
Explanation:
Ocean basins form as a result of convection in the mantle along divergent margins.
- At a divergent margin, new crusts are being formed.
- It is said to be a constructive margin because new materials reaches through to the earth surface from there.
- The mantle convection pushes materials up and down away from heating centers and to cold regions and back and forth.
- This leads to the creation of cells which moves the overlying plate.
- The mantle materials are then able to reach the surface to form new ocean basin.
An Egyptian pylon can best be described as a massive gateway with sloped sides. The two structures on each side are usually rectangular in size. The first pylon was constructed in ancient Egypt and is believed to be called Philae.
