A crack in Larsen C, one of Antarctica's largest ice shelves, could shed a block of ice twice the size of Rhode Island.

The crack recently split in two and forked northward.

When the ice calves, more ice behind the block could destabilize and push into the sea.

A slab of ice nearly twice the size of Rhode Island is breaking off a massive Antarctic glacier, and new satellite images do not bode well for the block's survival.

The giant ice block is part of the Larsen C ice shelf, which is the leading edge of one of the world's largest glacier systems. A single large crack in the ice shelf has rapidly developed since 2010, lengthening to about 120 miles.

Now scientists say that a 6-mile fork in the rift has formed at its leading edge. While the main part of the rift doesn't seem to have grown over the past couple of months, the new branch points northward, toward the Southern Ocean — making it seem more likely the ice block will break off.

"When it calves, the Larsen C ice shelf will lose more than 10% of its area to leave the ice front at its most retreated position ever recorded," scientists Adrian Luckman and Martin O'Leary, both with Swansea University in the UK, wrote in a blog post. The post, published Monday, said that when the slab breaks off, it "will fundamentally change the landscape of the Antarctic Peninsula."

Other satellite data shows the block moving toward the Southern Ocean faster than the rest of Larsen C, widening the rift.

"Although the rift length has been static for several months, it has been steadily widening, at rates in excess of a meter per day," Luckman and O'Leary wrote for the Melt on Ice Shelf Dynamics and Stability project, or MIDAS. "This widening has increased noticeably since the development of the new branch."

The Larsen C ice shelf is located off Antarctica's prominent peninsula and is called a shelf because it floats on the ocean. It's normal for ice shelves to calve big icebergs as snow accumulation gradually pushes old glacier ice out to sea. But the consequences of this ice block splitting off could be huge.

A growing rift

A map of Antarctica's biggest ice shelf systems. Larsen C was the fourth-largest — now the fifth-largest — until iceberg A68's calving between July 10 and July 12, 2017. Diti Torterat/Wikipedia (CC BY 2.0)

The piece of floating ice in question is colossal — it's at least 1,100 feet thick at the edge (it grows thicker inland) and roughly 2,000 square miles in area. It's destabilizing quickly, a process likely accelerated by human-caused climate change.

Previous satellite images suggest the crack in Larsen C opened around 2010 and had lengthened by dozens of miles by June 2016. In November 2016, a team of scientists in NASA's Operation IceBridge survey flew over the rift and confirmed that it was at least 80 miles long, 300 feet wide, and one-third of a mile deep.

Then in January 2017, another group of researchers — the MIDAS group, based out of Swansea University — revealed that the entire block of ice was hanging on by 12 miles of unfractured ice. Luckman, a glaciologist with MIDAS at Swansea, began sounding the alarms.

"If it doesn't go in the next few months, I'll be amazed," Luckman said in a January 6 press release. "It's so close to calving that I think it's inevitable."

This graphic shows the crack's progression until Monday using data from the US Geological Survey's Landsat-1 satellite and the European Space Agency's Sentinel-1 InSAR satellite:

Satellite imagery of a giant crack in Antarctica's Larsen C ice shelf, as of May 1. MIDAS/ESA/USGS

In the Sentinel-1 satellite data depicted below, the white, hot pink, and magenta colors show the places where the ice's surface is moving the fastest — and where the ice block is threatening to break off.

Red and orange show relatively quick speeds, while the slowest speeds are shown in yellow, green, and blue.

Adrian Luckman/MIDAS/Swansea University; Business Insider

Luckman and O'Leary say it's difficult to get an exact read on the crack's progress because it's currently winter in Antarctica, making it tough to see.

NASA's Ice, Cloud, and Land Elevation Satellite, or ICESat, used to provide more current, year-round views of Antarctic ice. But that mission ended in 2009, so researchers now have to fly over the region to confirm estimates of the crack.

The next similar satellite, ICESat-2, isn't scheduled for launch until 2018. President Donald Trump's transition team in December 2016 suggested the administration might strip NASA of funding for such earth science missions, which date back to the formation of the space agency 59 years ago. However, Trump's signing of a new NASA law may mean the program will continue.

"Rifting of this magnitude doesn't happen so often, so we don't often get a chance to study it up close," Joe MacGregor, a glaciologist and geophysicist at NASA's Goddard Space Flight Center, previously told Business Insider in an email. "The more we study these rifts, the better we'll be able to predict their evolution and influence upon the ice sheets and oceans at large."

NASA's program to fly over the ice with airplanes is funded through 2019 and is (poetically) called IceBridge.

The big breakup

The Larsen C ice shelf rift snaking into the distance, as seen from an IceBridge flight. John Sonntag/IceBridge/NASA Goddard Space Flight Center When the block breaks off, it could be the third-largest in recorded history.

MacGregor said it would then "drift out into the Weddell Sea and then the Southern Ocean and be caught up in the broader clockwise ... ocean circulation and then melt, which will take at least several months, given its size."

Computer modeling by some researchers suggests the calving of Larsen C's big ice block might destabilize the entire ice shelf, which is about 19,300 square miles — roughly two times as large as Massachusetts — via a kind of ripple effect.

But MacGregor and Luckman have both downplayed this possibility.

"We would expect in the ensuing months to years further calving events, and maybe an eventual collapse — but it's a very hard thing to predict, and our models say it will be less stable," Luckman said in the release, adding that it wouldn't "immediately collapse or anything like that."

However, a rapid ice-shelf collapse would not be unprecedented.

In 2002, a large piece of the nearby Larsen B ice shelf snapped off, but within a month — and quite unexpectedly — an even larger swath of the 10,000-year-old feature behind it rapidly disintegrated. The rest of Larsen B may splinter by 2020.

If there's any good news about the rift in Larsen C, it's that the ice shelf "is already floating in the ocean, so it has already displaced an equivalent water mass and minutely raised sea level as a result," MacGregor previously said. In other words, when the iceberg melts, it won't cause the sea level to rise any further.

The bad news is that if all of Larsen C collapses, the ice it holds back might add another 4 inches to sea levels over the years — and that it's just one of many major ice systems around the world affected by climate change.