Scientists have revealed an incredibly detailed image of the lunar surface showing objects up to five meters in diameter, captured with reflected radar signals.
The image, published by the National Radio Astronomy Observatory of America, shows the landing site of NASA’s Apollo 15 mission in 1971 and the toothed grooves and craters surrounding it.
To obtain the image, the researchers used satellites that fired a powerful radar signal to the moon, which was then reflected back into a system of 10 radio telescopes in North America, called the Very Long Baseline Array.
The end result marks a successful preliminary test of the highly complex radio telescope system.
Now, scientists want to develop it even further to capture more detailed images from much deeper of our solar system, including the surfaces of Neptune and Uranus.

New radar image of the landing site of the Apollo 15, located with respect to the outstanding lunar characteristics. Apollo 15 landed in Hadley-Apennine, a region on the near side of the moon, on July 30, 1971.
“The planned system will be a leap forward in radar science, which will provide access to features of the solar system never seen from here on Earth,” said Karen O’Neil, site director of the Green Bank Observatory West Virginia.
The project combines the efforts of the Green Bank Observatory (GBO) of the National Science Foundation, the National Radio Astronomy Observatory (NRAO) and Raytheon Intelligence & Space.
GBO’s Green Bank Telescope in West Virginia, the world’s largest fully orientable radio telescope, was equipped with a new transmitter developed by Raytheon Intelligence & Space, which allowed it to transmit the radar signal into space.
The very long base matrix (VLBA) of the entire NRAO continent received the signal once reflected from the lunar surface and produced the image.
The image was captured in November last year, but has only been published by the National Radio Astronomy Observatory.

GBT-VLBA radar image of the region where Apollo 15 landed in 1971. The characteristic snake is Hadley Rille, a remnant of ancient volcanic activity, probably a collapsed lava tube.

Apollo 15 – NASA, 1971. Apollo 15 astronaut James Irwin uses a ball to dig into the lunar soil in front of Mount Hadley, 1971

Apollo 15 commander Dave Scott greets the American flag at the Hadley-Apennine lunar landing site. The lunar module ‘Falcon’ is partially visible on the right, 1971
The new image shows the Apollo 15 landing site right next to a bleed named Hadley Rille, a remnant of ancient volcanic activity, probably a collapsed lava tube.
The crater at the top, next to the rille, is called Hadley C and is about 6 kilometers in diameter.
Apollo 15 landed in Hadley-Apennine, a region on the near side of the lunar surface, on July 30, 1971.
It was the ninth manned mission on NASA’s Apollo program and the fourth to land on the moon.

The Green Bank Telescope in West Virginia, the most fully orientable radio telescope in the world. This telescope is equipped with a new planetary radar transmitter to study objects in the solar system.

Antenna locations of the set of very long baselines across the continent. These antennas serve as locations for receiving the radar signal reflected from the Green Bank telescope
Using the information gathered from this latest test, the scientists will finalize a plan to develop a 500-kilowatt high-power radar system that can imagine objects in the solar system “with unprecedented detail and sensitivity.”
This will allow astronomers to use radar signals as far away as the orbits of Uranus and Neptune, the two outermost planets in our solar system, which reside about 1.6 billion and 2.7 billion kilometers away from our planet, respectively.
“The concept test drive, which culminates a two-year effort, paves the way for designing a more powerful transmitter for the telescope,” NRAO said in a statement.
“More power will allow better detection and imaging of small objects passing through the Earth, moons orbiting other planets and other debris in the solar system.”