News Releases

Earth’s Tidal Forces Linked to Shrinking Moon

Smithsonian Scientist Cites Newly Discovered Lunar Faults as Evidence

September 15, 2015

Images taken by NASA’s Lunar Reconnaissance Orbiter show that tidal forces from Earth are influencing the formation of thousands of young faults on the moon related to its shrinking. The findings are reported in a paper—“Global Thrust Faulting on the Moon and the Influence of Tidal Stresses”—published online and in the October issue of the journal Geology. Tom Watters, Smithsonian senior scientist in the National Air and Space Museum’s Center for Earth and Planetary Studies, is the lead author.

The shrinking of the moon was initially reported in 2010, based on images captured by the Lunar Reconnaissance Orbiter (LRO), which was launched by NASA to orbit the moon in June 2009. At that time, the high-resolution images taken by the LRO’s Camera (LROC) covered only about 10 percent of the lunar surface—enough for the camera team to identify 14 fault scarps, or cliffs, in addition to a small number of scarps photographed years earlier by the Apollo Panoramic Camera during the Apollo space missions.

Now, after more than six years in orbit, the orbiter has imaged nearly three-quarters of the lunar surface at pixel scales of 0.5 to 2 meters, or about 2-by-6 feet. More than 3,000 lobate (lobe-shaped) fault scarps have been discovered, with a strong likelihood of finding more as coverage increases. These faults, which have emerged as the most common tectonic landform on the moon, are created when crust materials are pushed together, break and are thrust upward. They are small, typically less than 10 kilometers long (about six miles) and 10s of meters in height, and are widely distributed over the lunar surface.

An already established and major cause of scarp formation is global contraction resulting from cooling of the still hot interior of the moon. As the interior cools and portions of its liquid outer core solidify, the moon’s volume decreases, and it shrinks. If the sole cause of fault scarp formation was the cooling of the moon’s interior, scarp orientations would be random, because contracting forces have equal magnitude in all directions. But, according to Watters, “this is not what we found.” It is the non-random orientation of the scarps that suggested to Watters and his co-authors that the Earth has played a role in the formation of the fault scarps.

“There is a pattern in the orientations of the thousands of faults, and it suggests something else is influencing their formation, something that’s also acting on a global scale,” Watters said. “That something is the Earth’s gravitational pull.”

The moon is a tidally locked satellite that is slowly moving away from Earth. This movement causes stresses in the lunar crust that build up over time. Unlike tides that occur on Earth, tides on the moon created by Earth’s gravity cause the lunar crust to rise and fall, and generate stresses. Though relatively small compared to those resulting from global contraction, which are equal in magnitude in all directions, the tidal forces generated by Earth are not equal. When these tidal forces are superimposed on forces resulting from global contraction, the combined stresses should cause predictable orientation of the fault scarps from region to region. “The agreement between the mapped fault orientations and the fault orientations predicted by the modeled tidal and contractional forces is pretty striking,” said Watters. Identifying the similarity between the actual and modeled formations would not have been possible without the volume of data amassed in the past five years.

“The discovery of so many previously undetected tectonic features as our LROC high-resolution image coverage continues to grow is truly remarkable,” said Mark Robinson of the School of Earth and Space Exploration at Arizona State University, coauthor and principal investigator of LROC. “Early on in the mission we suspected that tidal forces played a role in the formation of tectonic features, but we just did not have enough coverage to make any conclusive statements.”

The fault scarps are very young, and it is likely they are actively forming today. Based on current modeling, peak crustal stresses are reached when the moon is furthest from the Earth in its orbit (at apogee). If the faults are still active, the occurrence of shallow moonquakes related to movement on the faults may be most frequent when the moon is at apogee. This hypothesis could be tested with a lunar seismic network.

“The discovery of thousands of young fault scarps, influenced by tidal forces from Earth, is an exciting new dimension to our understanding of the close relationship between our planet and the Moon,” Watters said.  

In addition to Watters, co-authors include: Maria Banks, Katie Daud and Michelle Selvans, Center for Earth and Planetary Studies at the National Air and Space Museum; Mark Robinson and Nathan Williams, School of Earth and Space Exploration at Arizona State University Tempe, Ariz.; and Geoffrey Collins, Physics and Astronomy Department at Wheaton College, Norton, Mass.

The Center for Earth and Planetary Studies is the scientific research unit within the Smithsonian’s National Air and Space Museum. Its scientists perform original research and outreach activities on topics covering planetary science, terrestrial geophysics and the remote sensing of environmental change.

The National Air and Space Museum building on the National Mall in Washington, D.C., is located at Sixth Street and Independence Avenue S.W. The museum’s Steven F. Udvar-Hazy Center is located in Chantilly, Va., near Washington Dulles International Airport. Attendance at both buildings combined exceeded 8 million in 2014, making it the most visited museum in America. The museum’s research, collections, exhibitions and programs focus on aeronautical history, space history and planetary studies. Both buildings are open from 10 a.m. until 5:30 p.m. every day (closed Dec. 25).

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SI-418-2015

 

Media only 
Claire Brown 
(202) 633-2371 
brownch@si.edu

Alison Mitchell 
(202) 633-2376 
mitchellac@si.edu

Related photos: 

Image of prominent lobate fault scarp on the Moon

Smithsonian Institution

A nadir (top) and perspective view (bottom) of a prominent lobate fault scarp in the Vitello Cluster, one of thousands discovered in Lunar Reconnaissance Orbiter Camera images (LROC). In the perspective view, the Narrow Angle Camera (NAC) image is draped over topography derived from NAC stereo images. A degraded crater has been uplift as the fault scarp has formed.

Related photos: 

Lobate thrust fault scarps on the Moon

Smithsonian Institution

Thousands of young, lobate thrust fault scarps have been revealed in Reconnaissance Orbiter Camera images (LROC). Lobate scarps like the one shown here are like stair-steps in the landscape formed when crustal materials are pushed together, break and are thrust upward along a fault forming a cliff.

Related photos: 

Map of lobate thrust fault scarps on the Moon

Smithsonian Institution

The map shows the locations of over 3,200 lobate thrust fault scarps (red lines) on the Moon. The black double arrows show the average orientations of the lobate scarps sampled in areas with dimensions of 40° longitude by 20° latitude and scaled by the total length of the fault scarps in the sampled areas.

Related photos: 

Prominent lobate fault scarp in Vitello Cluster

Smithsonian Institution

A prominent lobate fault scarp in the Vitello Cluster is one of thousands discovered in Lunar Reconnaissance Orbiter Camera images (LROC). Topography derived from the LROC Narrow Angle Camera (NAC) stereo images shows a degraded crater has been uplift as the fault scarp has formed (blues are lower elevations and reds are higher elevations).



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