What is the mystery mass on the moon?

Far side of the full moon with red oval around lower part of picture.
The South Pole-Aitken Basin (outlined) on the far side of the moon. The unusual mass is beneath the surface in this area. Image via NASA.

What is hiding beneath the largest crater on Earth’s moon (in fact, the largest crater in our solar system)? That’s what scientists said they’d like to find out after an unusual large mass of material was discovered lurking underneath the lunar South Pole-Aitken Basin. It’s a lot of mass, too, according to Peter B. James, assistant professor of planetary geophysics in Baylor University’s College of Arts & Sciences:

Imagine taking a pile of metal five times larger than the Big Island of Hawaii and burying it underground. That’s roughly how much unexpected mass we detected.

The intriguing peer-reviewed findings were first published in the April 15, 2019, issue of the journal Geophysical Research Letters. From the abstract:

The South Pole-Aitken Basin is a gigantic impact structure on the far side of the moon, with an inner rim extending approximately 2,000 kilometers [1,200 miles] in the long-axis dimension. The structure and history of this basin are illuminated by gravity and topography data, which constrain the subsurface distribution of mass. These data point to the existence of a large excess of mass in the moon’s mantle under the South Pole-Aitken Basin. This anomaly … likely extends to depths of more than 300 km [about 200 miles].

Moon with large blue patch in center, white dotted line in middle of blue area.
False-color map of the far side of the moon, showing the location of the unusual massive subsurface deposit beneath the South Pole-Aitken Basin. Image via NASA Goddard Space Flight Center/ University of Arizona/ Baylor University.

So what is this mysterious mass?

It is most likely metal of some kind, given its density and the fact that it is weighing the crater basin floor down by more than half a mile (0.8 km). An ancient asteroid impact would be a logical solution. Computer simulations of large asteroid impacts suggest that, under the right conditions, an iron-nickel core of an asteroid might be lodged into the upper mantle of the moon (the layer between the moon’s crust and core) during an impact, in this case the impact that created the South Pole-Aitken Basin.

Researchers analyzed data from spacecraft used for NASA’s Gravity Recovery and Interior Laboratory (GRAIL) mission to measure very small changes in gravity around the moon. As James explained:

When we combined that with lunar topography data from the Lunar Reconnaissance Orbiter (LRO), we discovered the unexpectedly large amount of mass hundreds of miles underneath the South Pole-Aitken basin. One of the explanations of this extra mass is that the metal from the asteroid that formed this crater is still embedded in the moon’s mantle. We did the math and showed that a sufficiently dispersed core of the asteroid that made the impact could remain suspended in the moon’s mantle until the present day, rather than sinking to the moon’s core.

The South Pole-Aitken Basin is estimated to have been formed about 4 billion years ago. The solar system was a very chaotic place back then, with collisions occurring between rocky and metallic bodies such as asteroids and young protoplanets – planetary embryos – on a pretty much regular basis. It seems quite feasible, then, that this is how the dense subsurface mass on the moon got there.

One other plausible theory, however, is that the mass might be a concentration of dense oxides associated with the last stage of lunar magma ocean solidification. It is theorized that the moon once had an ocean of sorts – not of water, but of magma, or molten rock – which then cooled and solidified. In the process, the oxides could have been deposited in this region, forming the large mass. 

These scientists say an asteroid impact is still the leading hypothesis, however, and James referred to the South Pole-Aitken Basin as one of the best natural laboratories for studying catastrophic impacts in the early solar system.

Closeup of blue patch with irregular concentric lines and labeled surface materials.
Topographic map of the South Pole-Aitken Basin on the moon. Image via Goddard Space Flight Center.

The South Pole-Aitken Basis is the largest known crater in the solar system. Measured from outer rim to outer rim, it’s about 1,600 miles (2,500 km) in diameter and 8.1 miles (13 km) deep. It was named for two features on opposite sides of the basin: Aitken Crater on the northern end and the lunar south pole at the other end. The basin’s existence had been suspected since 1962, based on data from the Luna 3 and Zond 3 orbiters, but was not confirmed until the mid-1960s by the Lunar Orbiter program.

On January 3, 2019, China’s Chang’e 4 spacecraft landed within this basin, in the smaller and younger Von Kármán Crater. This was the first time that any spacecraft has landed on the far side of the moon. It has studied samples of material thought to have come from deeper within the moon’s mantle, excavated during the impact that created the crater. This is a unique opportunity to explore in detail not only the crater, but a small portion of the larger basin as well.

Smiling man seated in front of computer monitor with same picture as above displayed on it.
Peter B. James via Baylor University.

Bottom line: The massive dense deposit below the largest crater on the moon is a very interesting discovery, and may be metal left over from a huge asteroid impact 4 billion years ago.

Source: Deep Structure of the Lunar South Pole-Aitken Basin

Via Baylor University

June 19, 2019

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