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Which statement provides evidence that the seafloor is spreading out from both sides of the Mid-Atlantic Ridge?
The presence of alternating magnetic stripes on either side of the Mid-Atlantic Ridge provides evidence that the seafloor is spreading out. As magma solidifies to form new oceanic crust, it records the Earth's magnetic field. These magnetic stripes mirror each other on either side of the ridge, indicating a symmetric pattern of seafloor spreading.
What is used as evidence for sea-floor spreading-?
The rocks on either side of a mid-ocean ridge record the direction of the Earth's magnetic field at the time they were formed, and form a pattern of 'magnetic stripes' on either side of the ridge which are symmetrical. It is also now possible to measure ocean widths with sufficient accuracy to show yearly changes.
How do rocks that formed at mid-ocean ridges show that magnetic reversal have occurred?
Rocks formed at mid-ocean ridges exhibit patterns of magnetic stripes that record Earth's magnetic reversals. As magma rises and solidifies at the ridge, iron-rich minerals align with the Earth's magnetic field, locking in a record of the magnetic orientation at that time. When a magnetic reversal occurs, new rocks forming at the ridge will display the opposite magnetic alignment, creating a symmetrical pattern of alternating magnetic orientations on either side of the ridge. This evidence supports the theory of seafloor spreading and provides a timeline of Earth's magnetic history.
How does the ocean floor keep track of magnetic fields?
The ocean floor records magnetic fields through a process called seafloor spreading. As magma rises at mid-ocean ridges and solidifies, it creates new oceanic crust that aligns with the Earth's magnetic field at the time of its formation. This alignment is preserved in the rock, resulting in a pattern of magnetic stripes on either side of the ridge that reflects reversals in the Earth's magnetic field over geological time. These magnetic patterns serve as a historical record, allowing scientists to study tectonic plate movements and the Earth's magnetic history.
How do records of magnetic reversals show that plates move apart?
As the molten material rises and cools, some magnetic minerals line up with the Earth's magnetic field. When the material hardens, the minerals are permanently fixed like tiny compass needles pointing north and south. Whenever the magnetic field reverses, the cooling minerals record the change.
How do magnetic stripes show the history of Earth's magnetic field?
as you move away from an ocean ridge the rocks get older
Which statement provides evidence that the seafloor is spreading out from both sides of the Mid-Atlantic Ridge?
The presence of alternating magnetic stripes on either side of the Mid-Atlantic Ridge provides evidence that the seafloor is spreading out. As magma solidifies to form new oceanic crust, it records the Earth's magnetic field. These magnetic stripes mirror each other on either side of the ridge, indicating a symmetric pattern of seafloor spreading.
How do earths magnetic pole reversals provide evidence for plate tectonics?
Magnetic stripes can be seen as you move away from ocean ridges.
What is used as evidence for sea-floor spreading-?
The rocks on either side of a mid-ocean ridge record the direction of the Earth's magnetic field at the time they were formed, and form a pattern of 'magnetic stripes' on either side of the ridge which are symmetrical. It is also now possible to measure ocean widths with sufficient accuracy to show yearly changes.
What causes Magnetic stripes on the seafloor are caused by?
These "stripes" formed the pattern known as magnetic striping. ... They hypothesized that the magnetic striping was produced from the generation of magma at mid-ocean ridges during alternating periods of normal and reversed magnetism by the magnetic reversals of the Earth's magnetic field.
How do records of magnetic reversals show that plates move apart?
As the molten material rises and cools, some magnetic minerals line up with the Earth's magnetic field. When the material hardens, the minerals are permanently fixed like tiny compass needles pointing north and south. Whenever the magnetic field reverses, the cooling minerals record the change.
What are pole reversals?
The direction of the Earth's magnetic field has reversed several times during its history. This causes the North magnetic pole to become a South magnetic pole and vice versa. We know this because of the direction of magnetism in the rocks on the ocean floor, which alternates in 'stripes' on either side of the mid-ocean ridges.
When new rock is added to an oceanic ridge the magnetized strips on side of the ridge are evidence of sea floor spreading this is because the rock the two sides of the ridge?
are equal in width and polarity
Which observation about the mid atlantic ridge region probides the best evidence that the seafloor has been spreading for millions of years?
The fact that there is a series of magnetic 'stripes' on either side of the ridge. They show that the earth's magnetic field has reversed several times during the formation of the rocks, and this only happened about every 5 million years. (There is some evidence that this is speeding up).
How an isochron map of the ocean floor supports the theory of seafoor spreading?
An isochron is a line on a map that connects points that have the same age. An isochron map of the ocean floor supports the theory of seafloor spreading because it shows the older rock near the deep sea trenches and the younger rocks near ocean ridges.
How do magnetic bands provide evidence that tectonic plates are moving apart at mid-oceanic ridges?
Through seafloor-spreading as iron rich minerals cool they become magnetized in the direction parallel to the existing magnetic field. As the magnetic fields change direction so will the magnetized minerals, allowing scientists to record each change in the seafloor as it spreads.
What do strips of alternating magnetic polarities found in rocks in the ocean basins provide?
Strips of alternating magnetic polarities found in ocean basin rocks provide evidence for seafloor spreading and plate tectonics. These magnetic anomalies are formed as magma cools and solidifies at mid-ocean ridges, recording the Earth's magnetic field at that time. The symmetrical pattern of these stripes on either side of the ridge indicates that new oceanic crust is created and pushes older crust away, supporting the theory of continental drift. This contributes to our understanding of the dynamic nature of the Earth's lithosphere.
