Moon’s Early Magnetic Field Made Human Existence Possible

Is it significant that Earth and the Moon shared a magnetic field about 4 billion years ago? Research shows that it is. Scientists have learned that a coupled magnetosphere (shared magnetic field) between Earth and the Moon helped shield our planet from the young Sun’s radiation that would have been catastrophic for life.

Textbooks used to describe the Moon as having no magnetic field now and never having had one of any consequence. However, the magnetometer delivered to the Moon by the Apollo 12 astronauts in 1969, revealed that the Moon does have a magnetic field, albeit a thousand times weaker than Earth’s present magnetic field. This lunar magnetic field is a leftover magnetic memory of the earliest lunar eras preserved in the Moon’s surface rocks. Laboratory analysis of lunar rocks brought to Earth by Apollo astronauts revealed that the Moon must have possessed a substantial magnetic field during the several hundred million years after its formation.

Below I provide scientific details about a previous analysis and a new discovery in the next two sections. If they seem too technical, feel free to skim and begin again at “Implications.”

Moon’s Early Magnetic and Dynamic History Laboratory analysis of the lunar rocks established that, 4.25–3.50 billion years ago, the Moon’s maximum magnetic field strength ranged from 20–100 microtesla (0.2–1.0 gauss). 1 From 3.50 to 3.20 billion years ago, the Moon’s maximum magnetic field strength dropped to about 5 microtesla (0.05 gauss). These measurements compare with Earth’s present maximum magnetic field strength of 65 microtesla (0.65 gauss).

For both Earth and the Moon the magnetic field strength varies according to where one is located on the surface. Earth’s present surface magnetic field strength ranges from 23 microtesla (0.23 gauss) in Paraguay to 65 microtesla (0.65 gauss) between Tasmania and Antarctica.

Previous to 3 billion years ago, the Moon was much closer to Earth. The Earth-Moon separation was only about 21 Earth radii (133,800 kilometers or 83,100 miles) 3.9 billion years ago and only about 18 Earth radii (114,700 kilometers or 71,300 miles) 4.0 billion years ago.2 (The present Earth-Moon separation is 384,400 kilometers or 239,000 miles.)

For the Moon to possess a strong magnetic field, there would need to be strong, enduring convection currents circulating in its liquid iron core. Internal heat remaining from the Moon formation event kept the Moon’s iron core liquid previous to 3.5 billion years ago. Scientists are convinced that the formation event was brought about by the collision-merger of Theia, a planet 11–15% of Earth’s present mass, with the proto-Earth.3 The Moon’s proximity to Earth previous to 3.5 billion years ago provided the required convection currents. Earth’s gravity on the Moon’s side nearest Earth would have been significantly stronger than Earth’s gravity on the Moon’s far side. The difference in the gravitational strengths caused the Moon to experience a substantial wobble. (A much smaller wobble persists to this day.) This wobbling stirred up the liquid iron in the lunar core, which produced the convection currents that generated the Moon’s strong magnetic field.

Previous to 3.5 billion years ago, the Moon exerted a substantially stronger gravitational pull on Earth’s near side than it did on Earth’s far side. The difference in gravitational pulls generated convection currents in Earth’s liquid iron core. Today, the lunar contribution to convection in Earth’s liquid iron core is several hundred times weaker. It has been replaced by convection driven by the transformation of Earth’s core from entirely liquid to an inner solid and an outer liquid core.

Neither Earth nor the Moon would have possessed a strong, enduring magnetic field previous to 3.5 billion years ago if it were not for their close proximity to one another. This proximity at that time also made possible the coupling of their magnetospheres with profound implications for life on Earth.

Earth-Moon System’s Magnetosphere History Now, a team of four planetary astronomers led by James Green has shed light on this early coupling of magnetic fields. The team used the known lunar magnetic field strengths and lunar distances from Earth previous to 3 billion years ago along with the known solar wind intensities at the time to determine the magnetospheres for both the Earth and Moon and how the two magnetospheres were coupled.4 Figures 1–4 show what they achieved.

Figure 1: Coupled Magnetospheres (showing magnetic field lines) for the Earth-Moon System 4 Billion Years Ago When the Moon Is between the Sun and Earth and the Magnetic Dipoles Are Aligned. Body sizes and separations are to scale. Image credit: adapted from James Green et al., eabc0865. 

Figure 2: Coupled Magnetospheres for the Earth-Moon System 4 Billion Years Ago When Earth Is between the Sun and the Moon and the Magnetic Dipoles Are Aligned. Image credit: adapted from James Green et al., eabc0865.

Figure 3: Coupled Magnetospheres for the Earth-Moon System 4 Billion Years Ago When the Moon Is between the Sun and Earth and the Magnetic Dipoles Are Antialigned. Image credit: adapted from James Green et al., eabc0865.

Figure 4: Coupled Magnetospheres for the Earth-Moon System 4 Billion Years Ago When Earth Is between the Sun and the Moon and the Magnetic Dipoles Are Antialigned. Image credit: adapted from James Green et al., eabc0865.

Implications of Earth-Moon System’s Coupled Magnetosphere History
Green’s team showed that regardless of the orientations of Earth’s and Moon’s magnets, the coupled magnetosphere of the Earth-Moon system previous to 4 billion years ago was sufficiently strong and stable to prevent the intense solar wind from sputtering away or seriously degrading either Earth’s atmosphere or its hydrosphere. It also was strong and stable enough to protect the microbes on Earth’s surface at that time from deadly solar radiation.

Then 3.2 billion years ago, the Moon’s magnetic field became too weak and the Moon too distant from Earth for the Moon’s magnetic field to provide any significant magnetospheric protection for Earth’s atmosphere, hydrosphere, and life. However, by this time it was no longer necessary. The Sun’s flaring activity and intensity of x-ray and gamma-ray emission had decreased to levels where Earth’s magnetosphere, by itself, would be sufficient to protect Earth’s atmosphere, hydrosphere, and life (see figure 5).

Figure 5: Sun’s Flaring Activity Level throughout Its History
The y-axis is logarithmic. The Sun’s flaring activity level was more than 100,000 times greater shortly after its formation than it is now. The Sun’s intensity of x-ray and gamma-ray emission is strongly correlated with the its flaring activity level. The blue dotted line indicates the present time.
Diagram credit: Hugh Ross 

I have written previously that our Moon is like no other known moon.5 A small rocky planet as close to its host star as Earth is to the Sun being orbited closely by a single enormous Moon requires the most extraordinarily fine-tuned collision event known to astronomers.

A planet 11–15% Earth’s present mass of a just-right composition and internal structure must merge with the proto-Earth at a just-right time in the solar system’s history in a just-right manner (just-right velocity, just-right merge angle, just-right rotation direction and rate, etc.) for a moon like our Moon to form. The required fine-tuned designs are so mind-boggling that one lunar-formation modeler, Tim Elliott, wrote in Nature that it was causing him and his colleagues “philosophical disquiet.”6 Now more layers of fine-tuned designs must be added—the early strong magnetic fields of both Earth and the Moon resulting from their proximity to one another and the coupled magnetosphere history of the Earth-Moon system.

Green and his colleagues close their paper by explaining that they have uncovered yet another habitability requirement. For a planet other than Earth to host anything more than a few microbial species for more than a brief time period it must host a moon virtually identical to ours. Such a planet-moon system must possess both a coupled dynamical history and a coupled magnetosphere history virtually identical to the Earth-Moon system. I would add that such a planet-moon system must orbit a star virtually identical to the Sun since stars more massive or less massive than the Sun pose an even greater risk to the planet’s atmosphere, hydrosphere, and life.7

The four planetary astronomers do not comment any further, but as an astronomer I would also observe the additional habitability requirements they uncovered demand such exceptional fine-tuning as to rule out any reasonable naturalistic explanation for how any planet in the universe could become a home for long-term life or for any conceivable multicellular life. The only reasonable explanation for such a planet and Earth-Moon system is that it is the product of a super-intelligent, supernatural Being who created a home where humans can exist, thrive, and enter into a personal relationship with the cosmic Creator.

Featured image: Moon and Earth
Image credit: Chinese National Space Administration, Xinhuanet


  1. Saied Mighani et al., “The End of the Lunar Dynamo,” Science Advances 6, no.1 (January 1, 2020): id. eaax0883, doi:10.1126/sciadv.aax0883.
  2. V. N. Zharkov, “On the History of the Lunar Orbit,” Solar System Research 34, no. 1 ( January 2000): 1.
  3. Hugh Ross, “Lunar Coincidences Lead to ‘Philosophical Disquiet,'” Today’s New Reason to Believe (blog) March 3, 2014,; Hugh Ross, Improbable Planet (Grand Rapids: Baker, 2016), 48–60,
  4. James Green et al., “When the Moon Had a Magnetosphere,” Science Advances 6, no. 42 (October 14, 2020): id. eabc0865, doi:10.1126/sciadv.abc0865.
  5. Ross, “Lunar Coincidences”; Hugh Ross, “Update on Our Miraculous Moon,” Today’s New Reason to Believe (blog) August 31, 2020,; Hugh Ross, “Why the Moon Lost Its Magnetism and Earth Did Not,” Today’s New Reason to Believe (blog) January 27, 2020,; Ross, Improbable Planet, 48–60.
  6. Tim Elliott, “A Chip Off the Old Block,” in “Shadows Cast on the Moon’s Origin,” Nature 504 (December 5, 2013): 90, doi:10.1038/504090a.
  7. Hugh Ross, Weathering Climate Change (Covina, CA: RTB Press, 2020), 117–26,