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The seafloor spreads apart, creating new rocks that record magnetic orientation. Small grains of magnetite on the volcanic basalt (ocean floor) have magnetic properties.
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Why do magnetic strips appear on the sea floor?
Magnetic stripes on the sea floor form as a result of the movement of tectonic plates. When magma rises to the surface at mid-ocean ridges and solidifies into new rock, it records the Earth's magnetic field at the time. This creates alternating stripes of normal and reversed polarity as the Earth's magnetic field has flipped multiple times throughout history.
How magnetic reversals provide evidence for sea floor spreading?
Because of the stripes at the sea floor which are magnetic minerals
What are Magnetic stripes on the sea floor caused by?
Magnetic stripes on the sea floor are caused by the alternating polarities of Earth's magnetic field. As magma rises and solidifies at mid-ocean ridges, it locks in the magnetic orientation of the Earth's field at that time. Over time, as the Earth's magnetic field reverses, these magnetic stripes are preserved, providing a record of past magnetic field variations.
How does magnetic reversals provide evidence for seafloor spreading?
Because of the stripes at the sea floor which are magnetic minerals
Why do magnetic stripes appear on the seefloor?
The seafloor spreads apart, creating new rocks that record magnetic orientation. Small grains of magnetite on the volcanic basalt (ocean floor) have magnetic properties.
What three forms of evidence do geologists have of sea floor spreading?
Magnetic Stripes, Drilling Samples, and Molten Material.
What is the relationship between the ages of magnetic stripes and their distance from the ridge crest?
Magnetic stripes that are closer to the ridge crest tend to be younger, while those further away are older. This is because new crust is continually formed at the ridge crest through sea floor spreading, with magnetic minerals aligning themselves with Earth's magnetic field as they solidify, creating the alternating pattern of magnetic striping.
Bands of magnetic material in the sea floor that have opposite poles or exhibit magnetic reversal can provide evidence for sea floor spreading true or false?
True. Bands of magnetic material in the sea floor that have opposite poles or exhibit magnetic reversal provide evidence for sea floor spreading. This is because as new oceanic crust forms at mid-ocean ridges, Earth's magnetic field periodically reverses, creating magnetic stripes on the ocean floor that align with the direction of the magnetic field at that time.
Strips of alternating magnetic polarities found in rocks in the ocean basins?
They are known as magnetic stripes and are formed as new sea floor is created at mid-ocean ridges. When molten rock solidifies, it preserves the direction of Earth's magnetic field at that time, creating a record of magnetic reversals in the oceanic crust. The alternating stripes of normal and reversed polarity provide evidence for seafloor spreading and plate tectonics.
What do magnetic stripes confirm?
Magnetic stripes confirm the authenticity of a credit or debit card and store essential account information that is required for transactions.
Describe how the polarity of earth's magnetic field is recorded in the sea-floor?
Magnetic minerals in the Earth's crust align with the planet's magnetic field at the time of their formation. When new oceanic crust is created at mid-ocean ridges, these minerals record the direction of the Earth's magnetic field on the sea-floor. This creates alternating stripes of normal and reversed polarity as the sea-floor spreads.
Why magnetic stripes on the sea floor are parellel to mid-ocean ridge?
Magnetic stripes on the sea floor are parallel to mid-ocean ridges because they form as molten rock at the ridge cools and solidifies, capturing the Earth's magnetic field at that time. As tectonic plates slowly diverge at the ridge, new magma rises and creates new oceanic crust, leading to symmetrical patterns of magnetic reversals on either side of the ridge. This phenomenon is a result of seafloor spreading, which helps scientists understand the history of Earth's magnetic field and plate tectonics.
