What geological feature is most likely to form at a mid ocean ridge?
Answer: The answer is: volcano. Explanation: The mid-ocean ridges are underwater elevations located in the middle part of the Earth’s oceans.
Is ocean ridge a geological feature?
oceanic ridge, continuous submarine mountain chain extending approximately 80,000 km (50,000 miles) through all the world’s oceans. Collectively, the oceanic ridge system is the most prominent feature on Earth’s surface after the continents and the ocean basins themselves. …
What would you expect to see at a mid ocean ridge?
Because mid-ocean ridges are places where tectonic plates are pulling apart, you might expect to find an incredibly deep canyon, but that’s not exactly the case. As the tectonic plates pull apart, molten rock, or magma, comes up from below to fill in the gaps. Mid-ocean ridges can spread slowly or quickly.
What is the role of the mid-ocean ridge in seafloor spreading?
Mid-ocean ridges and seafloor spreading can also influence sea levels. As oceanic crust moves away from the shallow mid-ocean ridges, it cools and sinks as it becomes more dense. Seafloor spreading proves that the ocean itself is a site of tectonic activity.
What are the names of the mid ocean ridges?
Two well-studied mid-ocean ridges within the global system are the Mid-Atlantic Ridge and the East Pacific Rise.
Where does the Mid Atlantic Ridge start and end?
The Mid-Atlantic Ridge The mid ocean ridge systems are the largest geological features on the planet. The Mid-Atlantic Ridge (MAR) is a mostly underwater mountain range in the Atlantic Ocean that runs from 87°N -about 333km south of the North Pole- to subantarctic Bourvet island at 54°S.
What kind of volcanoes are on the Mid Atlantic Ridge?
Where this magma is able to reach the surface, the result is basaltic volcanoes and islands. Where it is still submerged, it produces “pillow lava”. As the plates move further apart, new ocean lithosphere is formed at the ridge and the ocean basin gets wider.
Where does seafloor spreading take place in the mid ocean ridge?
This feature is where seafloor spreading takes place along a divergent plate boundary. The rate of seafloor spreading determines the morphology of the crest of the mid-ocean ridge and its width in an ocean basin.