1.3 Magnetic striping Flashcards
1
Q
Magnetic Striping
A
- Earth has a geographic North and a geographic South as well as a magnetic North and magnetic South.
- The geographic North and geographic South do not change.
- However, the magnetic North and magnetic South can shift, and they have reversed multiple times over geological time.
- Currently, the magnetic North points roughly towards the geographic North and the magnetic South points roughly towards the geographic South - this is known as normal polarity.
- Reverse polarity happens when the magnetic North points roughly towards the geographic South, and the magnetic South points roughly towards the geographic North.
- Over geological time, the Earth’s polarity has flipped multiple times, alternating between normal and reverse polarity
2
Q
Evidence from rock patterns
A
- rocks created along the spreading oceanic ridges preserve pattern of polarity reversal as they cool
- pattern can be used to determine the rate of ocean ridge
- alternating polarity forms a striped patterns
- with each reversal of the earth’s polarity, magnetic minerals in the rocks align themselves with the magnetic North and South, forming a striped pattern
- when poles reverse, Earth’s magnetic north and south poles swap locations
- this zebra-like pattern is symmetrical on either side of mid-ocean ridges, showing that this is not a random or isolated occurrence
3
Q
Why magnetic striping occurs
A
- Basaltic rocks from the oceanic crust are volcanic rocks formed from iron-rich lava.
- They contain magnetic materials.
- When the iron-rich lava erupts, it cools and solidifies.
- Its magnetic materials point towards Earth’s magnetic North, recording evidence of Earth’s polarity at that time.
4
Q
How it works
A
- Oceanic plate move away from each other
- Iron-rich lava erupts, cools, solidifies, forms new oceanic crust at crest of ridge
- Crust is pushed in both directions away from the ridge when new lava is solidifies as plates moves apart
- Earth’s polarity will reverse, rocks records reversals
- as more lava moves away from the ridge due to plate divergence, a symmetrical zebra-like pattern forms