Image copyright NATURAL HISTORY MUSEUM OF DENMARK Image caption Space view: The semi-circular margin of the ice sheet traces the outline of the crater

What looks to be a large impact crater has been identified beneath the Greenland ice sheet.

The 31km-wide depression came to light when scientists examined radar images of the island's bedrock.

Investigations suggest the feature was probably dug out by a 1.5km-wide iron asteroid sometime between about 12,000 and three million years ago.

But without drilling through nearly 1km of ice to sample the bed directly, scientists can't be more specific.

"We will endeavour to do this; it would certainly be the best way to get the 'dead fish on the table' (acknowledge the issue, rather than leaving it), so to speak," Prof Kurt Kjær, from the Danish Museum of Natural History, told BBC News.

If confirmed, the crater would be the first of any size that has been observed under one of Earth's continental ice sheets.

The discovery is reported in the journal Science Advances.

Image copyright Svend Funder Image caption Kurt Kjær collects sand transported from under the glacier

What does the crater look like?

The putative impact crater is located right on the northwest margin of the Greenland Ice Sheet, underneath what is known as Hiawatha Glacier.

Additional high-resolution radar imagery gathered by Prof Kjær's team clearly shows a circular structure that is elevated at its rim and at its centre - both classic traits. But because the depression is covered by up to 980m of ice, the scientists have so far had to rely on indirect studies.

Image copyright Natural History Museum of Denmark Image caption A map of the bedrock topography beneath the ice sheet

What is the supporting evidence?

Meltwaters running out from under Hiawatha Glacier into the Nares Strait carry sediments from the depression. In these sediments are quartz grains which have been subjected to enormous shock pressures, of the type that would be experienced in an impact.

Image copyright Natural History Museum of Denmark/NASA Image caption Quartz grains show evidence of having experienced shock pressures

Other river sediments have revealed unusual ratios in the concentrations of different metals.

"The profile we saw was an enrichment of rhodium, a depletion of platinum, and an enrichment of palladium," explained team-member Dr Iain McDonald, from Cardiff University, UK.

"We got very excited about this because we realised we weren't looking at a stony meteorite, but an iron meteorite - and not just any old iron meteorite; it had to be quite an unusual composition."

Such metal objects that fall to Earth are thought to be the smashed up innards of bodies that almost became planets at the start of the Solar System.

The signatures identified by Dr McDonald are relatively close to those in iron meteorite fragments collected at Cape York not far from the Hiawatha site. It's not inconceivable, the team argues, that the Cape York material represents pieces that came away from the main asteroid object as it moved towards its collision with Earth.

Image copyright NASA/John Sonntag Image caption The Hiawatha Glacier cuts across the rim of the crater

What are the doubts?

One concerns the absence of any trace of the impact in several cores that have been drilled through the ice sheet to the south. At the very least, these might have been expected to incorporate the dust that fell out of the sky after the event.

The other head-scratcher is the absence in the vicinity of the Hiawatha site of any rocky material that would have been ejected outwards from the crater on impact.

Prof Kjær says these missing signatures might be explained by a very shallow angle of impact that took most of the ejecta to the north. And if the fall-out area was covered in ice, it's possible any debris was later transported away.

"We know that at one time the Greenland Ice Sheet was joined to the Canadian Ice Sheet, and flowed out into the Nares Strait. If you wanted to find this material today, you'd have to do deep drilling in the ocean," Prof Kjær explained.

Media playback is unsupported on your device Media caption Dr Iain McDonald: "The Cape York meteorite could be linked to this impact"

What are the age constraints?

The team knows the crater must be older than roughly 12,000 years because the undisturbed ice layers above the depression can be lined up with the layers in drill cores that have been directly dated.

And they estimate an age younger than three million years based on an assessment of likely rock erosion rates, both within the crater and on nearby terrains. But the only way to get a definitive age for the crater would be to drill down and collect rocks for laboratory dating.

Image copyright Natural History Museum of Denmark/NASA Image caption An artist's depiction of an iron asteroid hurtling through space

How does this connect with other ideas?

If the impact was right at near-end of the age window then it will surely re-ignite interest in the so-called Younger Dryas impact hypothesis.

The Younger Dryas was a period of strong cooling in the middle of the climatic warming that occurred as the Earth emerged from the height of last ice age.

Some have argued that an asteroid impact could have been responsible for this cooling blip - and the accompanying extinction of many animal groups that occurred at the same time across North America.

Others, though, have been critical of the hypothesis, not least because no crater could be associated with such an event. The Hiawatha depression is likely now to fan the dying embers of this old debate.

Dr Mathieu Morlighem, a team-member from the University of California, Irvine, US, commented: "When you think about it, the bed below the ice sheets has to have impact craters that have not been explored yet, and there may even be some in Antarctica as well, but more radar measurements are necessary to locate them, and dating them is extremely challenging."

Image copyright BEDMACHINE Image caption A map of the bedrock of Greenland. It would be the most northerly crater on Earth

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