spacecraft above lunar horizon with Earth in background

10 Cool Things NASA's Lunar Reconnaissance Orbiter is Teaching Us About the Moon

By Natalie Didomenico and Lonnie Shekhtman
NASA’s Goddard Space Flight Center,
Greenbelt, Md.

NEWS | June 24, 2019

Ten years ago, a mission launched that changed how humankind will view its closest neighbor for centuries to come. Ever since, NASA’s Lunar Reconnaissance Orbiter, also known as LRO, has helped us uncover some of the Moon’s deepest secrets. In honor of LRO’s 10th birthday, we reflect on 10 of the many things the intrepid, orbiting explorer has taught us about the Moon.

cliffs on gray lunar surface
This is a wrinkle on the surface of the Moon, called a lobate scarp, caused by shrinking and cooling. This image combines data from two of LRO’s instruments: the Lunar Orbiting Laser Altimeter (LOLA) and the Lunar Reconnaissance Orbiter Camera (LROC) to create a precise digital terrain model. Lobate scarps can tell us about how hot the Moon was when it was born and its ongoing thermal evolution. Image width is about four kilometers. Credit: NASA/GSFC/Arizona State University | › Full image and caption

1. It's shrinking and quaking

LRO observations helped confirm what seismometers placed on the Moon by Apollo astronauts 50 years ago first discovered: The Moon, long thought to be a dead, inactive world, is still losing heat and, as a result, shrinking. As it continues to slowly cool off, the Moon’s crust, or outer layer, is shriveling, like a grape turning into a raisin; the Moon has lost 150 feet (50 meters) of width over hundreds of millions of years, scientists estimate. This shrinking, plus the stress on the Moon’s outer layer produced by the tugging of Earth’s gravitational pull, cracks the Moon’s crust and leads to moonquakes. Some are fairly strong, reaching level 5 on the Richter scale used to measure earthquakes.

lumpy hills
This oblique image of the Ina D region on the Moon was taken by the Lunar Reconnaissance Orbiter Camera (LROC). The smoother areas are elevated and the rougher areas are lower. This volcanic formation could be as young as 33 million years. Credit: NASA/GSFC/Arizona State University | › Full image and caption

2. It had active volcanos more recently than we thought

Scientists thought the Moon volcanoes had extinguished one billion years ago. But LRO has found evidence that volcanoes likely were still erupting within the last 50 million years — a time when mammals were overtaking dinosaurs as dominant lifeforms on Earth. With its high-resolution cameras, LRO photographed old, hardened lava patches on the surface of the Moon’s nearside. Then, scientists determined the approximate ages of these patches by counting the number of craters left on them by meteoroid strikes. Fewer craters implied younger lava. Along with moonquakes, these young lava flows are hinting that the Moon’s interior is warmer than we thought. Other scientists have an alternative explanation for the youthful appearance of the lava patches, though. Some say that they are billions of years old but were formed by foamy lava (the kind responsible for the common volcanic rock called pumice) which responds differently to meteor impacts, making the craters appear much younger.

two hemispheric views of the moon
Each of the above mosaics features roughly 1300 images taken by LRO, pieced together by the camera team. A full global view of the Moon takes about 15,000 images from the wide-angle camera to put together. Credit: NASA/GSFC/Arizona State University | › Full image and caption

3. The far side of the Moon is older than the side we see

Because the Moon is gravitationally locked to Earth, we only see one side of it. But LRO sees both hemispheres, and it has found that the far side has way more craters than the near side. Did the far side get smashed by more asteroids? Likely not. We see fewer craters on the side facing us because they’ve probably been filled in by lava from erstwhile volcanoes. The far side, though, has a much thicker crust (there are theories, but we don’t know why), which may have prevented magma from spewing through the surface there, leaving a well-preserved record of asteroid bombardment for scientists to probe.

crater within a crater
Hawke crater is named after B. Ray Hawke, an LRO scientist who passed away in 2015. Hawke lies on the rim of Grotrian crater and provides an example of how crater formations can tell you the bombardment history of a surface. As we can see, Hawke crater formed after Grotrian crater. Credit: NASA/GSFC/Arizona State University | › Full image and caption

4. Its craters provide a timeline of solar system history

LRO data has allowed scientists to construct a timeline of asteroid bombardment history on the Moon, providing insight not only into the Moon's formation, but of the whole solar system. Since the Moon doesn’t have wind, storms and plate tectonics, its craters don’t get eroded away like Earth’s do. Using tools on LRO, scientists can count and age them. By doing so, we can look back billions of years at the mayhem of the early solar system, when giant collisions (like the one that formed the Moon) were jostling planets and their satellites. One question scientists still have is how these early impacts influenced the building blocks of life that would have been stacking up on Earth and possibly elsewhere.

map of lunar craters with colors indicating temperatures
Temperature measurements from the Diviner instrument on LRO are vital for assisting in future human exploration as well as determining the composition of the Moon. This temperature map of the Moon’s north pole shows chilly Hermite crater, the coldest-measured spot not just on the Moon, but across the entire solar system. Credit: NASA/GSFC/UCLA | › Full image

5. It gets unimaginably cold

Scientists always knew permanently shadowed craters at the Moon’s poles were cold, but LRO measurements surpassed their estimates by a considerable margin. LRO’s Diviner instrument, which measures heat radiating off the Moon’s surface, has recorded some of the coldest temperatures on record at crater bottoms, down to -414.4 degrees Fahrenheit (-248 degrees Celsius). That is about seven times as cold as the lowest temperature ever recorded on Earth! The frigid temperatures on the Moon result from the low angle of sunlight striking the surface at the poles, allowing light to skim the rims of some craters while leaving their deep interiors in shadow. These dark craters are expected to be reservoirs of water, which is why they are a target destination for NASA’s Artemis mission to the Moon.

Frozen water on the Moon! Using several of LRO’s instruments, scientists identified potential water ice at the Moon’s poles. Credit: NASA/GSFC/Scientific Visualization Studio

6. Instead of a dry, dead rock, the Moon is a dynamic and wet world

Over the last decade, LRO and other instruments have returned a pile of evidence of frozen water on the Moon. Although there are still many questions about the amount and locations of water, the substance has huge implications for the astronauts who will work on the Moon and, ultimately, on Mars. Water (H2O) can be split into its components — hydrogen (H) and oxygen (O) — and used separately or in a new combination. Astronauts will need oxygen for breathing and to burn with the hydrogen fuel used in rocket engines. One of the biggest challenges to long-distance space travel is fuel, which is heavy and expensive to bring from Earth, so the goal is to figure out how to make it from water on the Moon.

plain viewed from above with craters, spacecraft and foot trails visible
This image taken by LRO in 2010 depicts the tracks that Apollo 15 astronauts David Scott and James Irwin made 39 years previously. The Moon has no atmosphere, and thus no wind or rain to sweep the footprints away. Credit: NASA/GSFC/Arizona State University | › Full image and caption

7. It preserves footprints for a long time

The Moon doesn’t have an atmosphere. Without it, there is no wind or rain to erode the surface. That’s why LRO is able to spot the tracks of Apollo astronauts and their rovers preserved in the regolith, or Moon soil, decades after those steps were taken. LRO’s orbital path is too far away from the Moon’s surface to resolve individual boot prints.

This animation uses data from LRO to map the permanently shadowed regions at the Moon’s south pole. LRO has several instruments designed to peer into the darkness and measure temperature, reflectivity and neutron absorption, all of which are clues to what chemicals might be hiding there. This animation shows where the permanently shadowed regions are and in what ways LRO can see inside them. Credit: NASA/GSFC/Scientific Visualization Studio

8. The South Pole region is a wondrous land that we want to explore

Instruments on LRO helped NASA identify areas of interest on the Moon for human exploration, with the South Pole rising to the top of the list as a potential hot spot for new discoveries. Since its elliptical, polar orbit is closest to the Moon during passes over the South Pole, the orbiter collects more precise information about this region’s topography, temperatures and locations of frozen water than about any other region. Besides water, we’ve learned that the South Pole has other features that are beneficial to human exploration, such as prolonged periods of sunlight. More than 200 Earth days of constant illumination at the southern pole means ample power for solar panels on rovers and other equipment.

color-coded topographic map of both lunar hemispheres
This false color image depicts elevation on the Moon, with the red and white areas indicating higher elevations and purple indicatingas lower ones. The scale goes from 10 kilometers below and 10 kilometers above the average height of the lunar surface. The data comes from LRO's LOLA instrument, which shoots a laser at the surface of the Moon and measures how long it takes for the light to bounce back. Thanks to LOLA, we know the shape of the Moon better than any other planetary body in the universe, including Earth! Credit: NASA/GSFC/MIT | › Full image

9. We know its surface in more detail than any other celestial body, including our own planet

Thanks to LRO’s super precise laser altimeter — an instrument that determines elevation by shooting a laser at the surface and measuring how long it takes for the light to bounce back — scientists have detailed maps of the shape, or topography, of the Moon’s surface. These will help NASA identify safe landing and exploration sites for commercial landers and future Artemis astronauts. The reason we have better topographic maps of the Moon than of Earth is because our planet is mostly covered by oceans, and laser light cannot penetrate them all the way to their rocky surface.

Learn more about lava tubes, tunnels and caves created by molten lava from NASA’s Acting Chief Exploration Scientist. Credit: NASA360

10. It has underground safe havens that could protect astronauts from radiation

The Moon’s surface is constantly exposed to solar radiation, which poses a threat to astronauts. LRO has helped identify a possible solution: underground caves formed around cooling lava that eventually drained out and left them hollow. High-resolution images taken by the orbiter have shown hundreds of pits across the lunar surface, which scientists believe could be openings to an extensive network. These caves, known as lava tubes, are also found on Earth. Such caves could provide shelter to astronauts during intense radiation events, scientists say, and they could be ideal locations for collecting samples of Moon soil that hasn’t been altered by radiation.