Lowest level of geomagnetic field intensity

In summary, a recent study using samples of rock from the Ediacaran period suggests that the Earth's magnetic field was about 10 times weaker than it is today. This has led to speculation about the timing of the Earth's core solidification, with previous estimates ranging from 500 million years to 2.5 billion years ago. However, there is still ongoing debate and uncertainty surrounding this topic, with some suggesting that the Earth's dynamo may have had even weaker episodes before the Ediacaran period.
  • #1
jim mcnamara
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https://www.nature.com/articles/s41561-018-0288-0 (article is behind a paywall).
Popular Science version:
https://motherboard.vice.com/en_us/...-field-collapse-ediacaran-core-solidification

Using samples of rock from the Ediacarian period, 565 million years ago, it was determined that the Earth's magnetic field was about 10 times weaker than it is today.

The Earth’s core is thought to have been entirely liquid at some point, and the question of when it began to solidify has perplexed scientists for decades. Past estimates have ranged from 500 million years to 2.5 billion years ago. Bono’s team now presents evidence that nucleation began after 565 million years ago.
 
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Likes davenn and Wrichik Basu
Earth sciences news on Phys.org
  • #2
After reading popular article, i feel the authors may be jumping to conclusions about relation of iron core solidification and the start of bradichrone/superchron at end of Ediacarian. The knowledge bias is likely - Earth dynamo may had even weaker episodes before Ediacarian, we just do not know exactly due fragmentary paleomagnetic record in pre-Jurassic epoch.
 
  • #3
@trurle If you can read the nature version there is discussion about this topic. There is on-going debate - ~2.0 billion year span of time's worth of hypotheses under discussion. So you are in good company.
 

Related to Lowest level of geomagnetic field intensity

1. What is the lowest level of geomagnetic field intensity?

The lowest level of geomagnetic field intensity is known as the South Atlantic Anomaly (SAA). It is an area of significantly weakened magnetic field strength in the Earth's southern hemisphere.

2. Why is the lowest level of geomagnetic field intensity important?

The SAA is important because it can affect the performance of satellites and spacecraft that pass through it. It can also cause disruptions in communication and navigation systems.

3. How is the lowest level of geomagnetic field intensity measured?

The lowest level of geomagnetic field intensity is measured using a magnetometer, which is a device that detects changes in the Earth's magnetic field. Data from multiple magnetometers around the world is used to create a map of the SAA.

4. Is the lowest level of geomagnetic field intensity constant?

No, the SAA is not constant. It is known to shift and change in intensity over time. In fact, recent studies have shown that the SAA is growing in size and moving towards the west.

5. Can the lowest level of geomagnetic field intensity affect humans?

There is no evidence to suggest that the SAA has any direct effect on human health. However, it is important for scientists to monitor and study the SAA in order to better understand the Earth's magnetic field and its potential impacts on technology and our planet as a whole.

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