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Assuming there is no Earth magnetic field, and no other significant magnetic fields, they will not allign in any preferred direction.

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13y ago

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How do rocks get magnetized?

They may contain naturally occurring magnetic minerals.


How does the magnetic orientation of lava layers demonstrate reversals of earths magnetic field?

When lava cools and solidifies, magnetic minerals within it align themselves with Earth's magnetic field. By studying the orientation of these minerals in lava layers, scientists can track changes in the Earth's magnetic field over time. Reversals of the Earth's magnetic field are reflected in lava layers as bands of alternating magnetic orientation.


Where is Earths magnetic reversals recorded?

Earth's magnetic reversals are recorded in rocks that contain magnetized minerals, such as iron-bearing minerals like magnetite. When these minerals solidify and align with Earth's magnetic field, they preserve a record of the magnetic field at that time. Scientists can study these rocks to determine the timing and duration of past magnetic reversals.


What on the ocean floor is evidence that earths magnetic field changes?

Evidence that Earth's magnetic field changes can be found in the alignment of magnetic minerals in rocks on the ocean floor. As magma solidifies into new rock, the magnetic minerals within it align with the current magnetic field direction. By studying the alignment of these minerals in rocks of different ages along the ocean floor, scientists can track changes in the Earth's magnetic field over time.


When does paleomagnetism happens?

Paleomagnetism occurs during the formation of rocks when magnetic minerals align with the Earth's magnetic field. This alignment helps to preserve a record of the Earth's past magnetic field direction. Scientists study paleomagnetism to understand the movement of tectonic plates and the history of Earth's magnetic field reversals.


What happens to minerals in rocks that cool in the presence of the Earth's magnetic field?

Minerals in rocks that cool in the presence of Earth's magnetic field can become magnetized and align with the magnetic field. This phenomenon is known as paleomagnetism, and it provides valuable information about the Earth's magnetic history and the movement of tectonic plates.


When molten material hardens into the rock on the ocean floor the domains of the iron it contains?

align with Earth's magnetic field, freezing the magnetic orientation of those minerals. This creates a record of the Earth's magnetic field at the time of cooling, which scientists can study to understand past changes in the planet's magnetic field.


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.


Magnetic striping of evidence of?

Magnetic reversals and sea floor spreading.


How could an old magnetic field be preserved in rocks?

Because lava can melt iron (demagnetizing it) and when it solidifies, it will pick up whatever magnet field it is currently subject to, thus locking in a record of the magnet field at the time in history.


Do magnetic domains of iron naturally align with earth's axis?

Magnetic domains have the tendency to align with magnetic fields. The Earth's magnetic field is relatively weak, but I would expect SOME alignment.


What is fossil magnetism?

In hot Iron bearing rocks or magmas the iron minerals they contain align themselves parallel to the Earth's magnetic field. When they cool below about 500 degrees Celsius the the iron minerals 'freeze' in this magnetic orientation and are no longer able to adapt to any changes in the Earth's field (which occasionally reverses polarity and wanders). This frozen magnetic alignment is a fossil of the ancient magnetic field and can be 'read' to find out what the Earth's magnetic field has been doing in the past.