Tree rings can tell us a great deal about a tree’s life and the environment it grew in. The field of dendrochronology focuses on analyzing these rings, which can reveal the tree’s age, the occurrence of fires, insect infestations, and even provide clues about past climate conditions. By studying these rings, researchers can trace how Earth’s climate has evolved over time. Recently, scientists discovered an ancient tree that lived during a period when Earth’s magnetic field nearly reversed, offering new insights into this fascinating chapter of history.

Ngāwhā kauri
The ancient tree, an Agathis australis, commonly known as kauri in Māori, was discovered in Ngāwhā on New Zealand’s North Island, buried 26 feet underground. With a diameter of eight feet and a length of 65 feet, this remarkable tree is believed to have lived for 1,500 years, roughly between 41,000 and 42,500 years ago. Alan Hogg from the University of Waikato described the discovery as unparalleled, stating, “There’s nothing like this anywhere in the world. This Ngāwhā kauri is unique.”
What Is Earth’s Magnetic Field?
Earth’s magnetic field is generated by its inner and outer core. The solid inner core transfers heat to the liquid iron in the outer core, causing convection, or movement, of the iron. Because iron is a conductor of electricity, this motion generates a magnetic field.
This field is similar to the one produced by a bar magnet, with two poles at opposite ends, known as the magnetic north and south poles. The magnetic field lines arch out from the north pole and curve into the south pole. While it aligns with the Earth’s axis of rotation, the field is not constant over time. Periodically, the field weakens and re-establishes itself, sometimes switching directions, flipping the north and south poles. These reversals have occurred throughout Earth’s history, with some lasting thousands of years and others for more than thirty million years.
Why Does Earth Have a Magnetic Field?
Earth’s magnetic field is crucial for protecting the planet from harmful solar radiation. The Sun releases vast amounts of radioactive particles, and Earth’s magnetic field deflects these particles, shielding us from potential damage.
What Happens When the Magnetic Field Weakens?
Approximately 565 million years ago, Earth’s magnetic field weakened to the point of nearly collapsing. It became about ten times weaker than it is today, lasting around 75,000 years. If the magnetic field had completely collapsed, Earth would have lost its protection from the solar wind, which could have eroded the atmosphere and even stripped away the planet’s water supply, as explained by John Tarduno of the University of Rochester.
The Laschamp Event
The most recent near-reversal of Earth’s magnetic field occurred about 41,000 years ago, an event known as the Laschamp Excursion. By studying tree rings, scientists can now investigate this period in greater detail. “The Earth’s magnetic field influences the amount of radiocarbon formed in the upper atmosphere, and by analyzing these ancient tree rings, we can examine the scale and pace of the magnetic field’s reversal during the Laschamp,” said Chris Turney, the lead scientist of the study. This research is crucial, particularly with the recent changes in Earth’s magnetic field.
The Shifting of Earth’s Magnetic Field
The Earth’s magnetic poles are not stationary. Since the first recorded position of the North Pole in 1831, its movement has been tracked at an average speed of six miles per year. Recently, however, this rate has increased to 25 miles per year. This change is notable because it affects systems reliant on the Earth’s magnetic field, such as the World Magnetic Model (WMM), used by the US and UK defense departments as well as civilian applications.
Currently, the northern magnetic pole is drifting away from the Canadian Arctic and toward Siberia. The WMM, which is typically updated every five years, was last revised in 2018 after it was found to be inaccurate in the Arctic region. Some scientists are concerned that this erratic behavior signals another potential pole flip. However, Peter Olsen, a geophysicist at Johns Hopkins University, views this as more of a “correction” rather than an impending collapse. “It’s like a stock market correction, not a crash,” he said.
The Role of the Ngāwhā Kauri Tree in Understanding the Past and Future
The Ngāwhā kauri tree, discovered in New Zealand, holds valuable data for scientists to better understand past magnetic field reversals. By analyzing its ancient rings, scientists can uncover details about past geomagnetic events like the Laschamp Excursion. This research helps us understand how Earth’s magnetic field has behaved in the past and prepares us for the potential shifts that may come in the future.

