- Which is the first step in the seafloor spreading process?
- What are the 4 steps of seafloor spreading?
- What causes the plate to move?
- Why is seafloor spreading important?
- What are the three types of seafloor spreading?
- What is the theory of seafloor spreading?
- Who discovered seafloor spreading?
- What discovery about the ocean floor is associated with seafloor spreading?
- What is the first step of seafloor spreading?
- What is the average speed of seafloor spreading?
- Is seafloor spreading beneficial or harmful for Earth?
- Do earthquakes cause seafloor spreading?
Which is the first step in the seafloor spreading process?
A crack forms in oceanic crust.
Molten rock rises up through oceanic crust.
Molten rock solidifies at the center of the ridge..
What are the 4 steps of seafloor spreading?
What are the 4 steps of seafloor spreading?Magma comes out of the rift valley.Magma cools to rock and hardens.Rock is pushed away as new rock is formed at MOR.Oceanic crust and continental crust meet at the trench.Oceanic crust bends down under the continental crust.Gravity pulls rock towards mantle.Rock melts to mantle.
What causes the plate to move?
The plates can be thought of like pieces of a cracked shell that rest on the hot, molten rock of Earth’s mantle and fit snugly against one another. The heat from radioactive processes within the planet’s interior causes the plates to move, sometimes toward and sometimes away from each other.
Why is seafloor spreading important?
Significance. Seafloor spreading helps explain continental drift in the theory of plate tectonics. … At a spreading center, basaltic magma rises up the fractures and cools on the ocean floor to form new seabed. Hydrothermal vents are common at spreading centers.
What are the three types of seafloor spreading?
There are three types of plate-plate interactions based upon relative motion: convergent, where plates collide, divergent, where plates separate, and transform motion, where plates simply slide past each other.
What is the theory of seafloor spreading?
Seafloor spreading, theory that oceanic crust forms along submarine mountain zones, known collectively as the mid-ocean ridge system, and spreads out laterally away from them. …
Who discovered seafloor spreading?
Harry HessHarry Hess: One of the Discoverers of Seafloor Spreading main content.
What discovery about the ocean floor is associated with seafloor spreading?
The magnetic history of the earth is thus recorded in the spreading ocean floors as in a very slow magnetic tape recording, forming a continuous record of the movement of the ocean floors. Other supportive evidence has emerged from study of the fracture zones that offset the sections of the ridge.
What is the first step of seafloor spreading?
Also Know, what is the first step of seafloor spreading quizlet? Sea-Floor Spreading begins at a mid-ocean ridge, which forms along a crack in the oceanic crust. along the ridge, molten material that forms several kilometers beneath the surface rises and erupts.
What is the average speed of seafloor spreading?
approximately 5 centimeters a yearThe average speed of seafloor spreading is approximately 5 centimeters a year. This growth rate can be compared to the growth rate of human fingernails (Krupicka). The global ridge system consists of oceanic ridges. Seafloor spreading occurs at these elevated oceanic ridges and has high heat flow and volcanism.
Is seafloor spreading beneficial or harmful for Earth?
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. This increases the volume of the ocean basin and decreases the sea level.
Do earthquakes cause seafloor spreading?
Scientists in Japan study stress released by oceanic earthquakes in newborn sections of seafloor. … Volcanic activity causes the seafloor to spread along oceanic ridges, forming new areas of crust and mantle. After being generated, this new oceanic lithosphere cools down and contracts by up to 3% of its own volume.