Image caption The Grail satellites hit the flank of the mountain about 30 seconds apart

Media playback is unsupported on your device Media caption Nasa engineer Glen Havens describes the final radio signals from the Grail twins

The US space agency's (Nasa) Ebb and Flow gravity mapping satellites have ended their mission to the Moon.

The duo were commanded to slam into a 2km-high mountain in the far lunar north.

The deliberate ditching avoids the possibility of an uncontrolled descent on to locations of historic importance, such as the Apollo landing sites.

Nasa's deep-space radio-tracking system confirmed the loss of signal from the satellites just before 22:30 GMT.

Afterwards, it was announced the impact site would be named for Sally Ride, the first female American astronaut who died earlier this year. Ms Ride's educational programme had run the outreach cameras on the spacecraft.

The satellite twins returned some remarkable data during their operational mission, which got under way in March. Their maps of the subtle variations in gravity across the Moon's surface are expected to transform many areas of planetary science.

"Ebb and Flow have removed a veil from the Moon and removing this veil will enable discoveries about the way the Moon formed and evolved for many years to come," said principal investigator Prof Maria Zuber from the Massachusetts Institute of Technology, US.

Together known as Grail (Gravity Recovery and Interior Laboratory), the pair hit the flank of the lunar-nearside mountain about 3km and 30 seconds apart.

The peak - located at 75 degrees North latitude close to a crater named Goldschmidt - was in darkness at the time.

Image caption The Sally Ride Science organisation ran the "Moonkams" on the Grail satellites

Being only the size of washer-driers, and having completely depleted their fuel tanks, the pair were not expected to produce any sort of impact flash visible to Earth observers.

That said, another of Nasa's missions at the Moon, its Lunar Reconnaissance Orbiter (LRO), was looking out for the crashes.

If it was lucky, LRO's ultraviolet imager might have seen some volatile materials being driven off the surface by the heat from the impacts. The orbiter will also image the site in a couple of weeks to see if it can discern any new craters.

Deep views

The Grail mission has produced the highest resolution, highest quality global gravity maps for any planetary body in the Solar System, including Earth.

Image caption The mountain (red) represents the partially buried rim of an old impact basin

The gravity differences the satellites have measured are the result of an uneven distribution of mass across the Moon.

Obvious examples at the surface include big mountain ranges or deep impact basins, but even inside the lunar body the rock is arranged in an irregular fashion, with some regions being denser than others.

Much of the twins' data has yet to be analysed but already scientists are getting some tantalising new insights into the Moon's structure and history.

"One of the major results that we've found is that the lunar crust is much thinner than we had believed before, and that a couple of the large impact basins probably excavated the Moon's mantle, which is very useful in terms of trying to understand the composition of the Moon as well as the Earth, because we actually think that the Earth's mantle has a similar composition to the Moon's mantle," said principal investigator Prof Maria Zuber from the Massachusetts Institute of Technology, US.

The gravity data also shows the lunar body's top-most layers to be far more fractured than anyone had previously suspected. These pulverised and porous materials that coat the surface bear witness to the brutal battering the Moon received in the first few hundred million years of its existence.

In addition, Ebb and Flow found evidence for great lava-filled fissures just under all this impact debris.

Image caption Scientists have really only just begun to delve into the Grail gravity data

These dykes, some hundreds of km long, appear to reach deep into the Moon, and may hint at an early expansion phase in its history when the hot body expanded outwards, before eventually cooling and contracting.

Grail data will be critical in tying down ideas for how the Moon came into existence. The dominant theory calls for a giant impact billions of years ago between the Earth and a Mars-sized object which threw material into space that ultimately coalesced into the familiar body we recognise in the sky today.

Some scientists have argued that Earth may once even have had two moons which later merged - although the Grail data could have sunk this idea.

"We have looked for evidence of the second moon and we have not seen any of the suggested characteristics of the internal structure of the Moon that would be consistent with the idea of a second companion," said Prof Zuber.

"That in itself does not rule out that idea at this point. We and others can look at this in more detail, but nothing jumps out in that regard."

Jonathan.Amos-INTERNET@bbc.co.uk and follow me on Twitter: @BBCAmos