NASA satellite imagery shows 'New' island emerges from melting ice in Alaska
Global warming is having effects all around the world. In some places, it’s transforming once-lush environments into barren deserts; in others, it’s doing essentially the opposite, albeit through an irony-fuelled, monkey’s paw kind of interpretation of “re-green the Earth’s deserts”. NASA's Earth Observatory has announced that Alaska has a "brand new island" after a retreating glacier lost contact with the Prow Knob mountain landmass in Alsek Lake. Alaska is turning into "a new lake district" thanks to melting glaciers. A 'new' island has appeared in the middle of a lake in southeastern Alaska after the landmass lost contact with a melting glacier, NASA satellite images reveal.
A new set of photos from NASA has laid bare a striking example of the latter effect, and it’s right on our doorstep. Alaska, it turns out, has a new island, not thanks to new land rising up through the seas, but because of glacial melt so dramatic that it has surrounded a piece of land previously connected to the mainland. “Along the coastal plain of southeastern Alaska, water is rapidly replacing ice,” NASA announced in an Earth Observatory Image of the Day post. “Glaciers in this area are thinning and retreating, with meltwater forming proglacial lakes off their fronts. In one of these growing watery expanses, a new island has emerged.” The landmass, named Prow Knob, is a small mountain which was formerly surrounded by the Alsek Glacier in Glacier Bay National Park. However, Alsek Glacier has been retreating for decades, slowly separating itself from Prow Knob and leaving a growing freshwater lake in its wake.
“The Alsek Glacier once encircled a small mountain known as Prow Knob near its terminus,” NASA explained. “In summer 2025, the glacier lost contact with Prow Knob, leaving the approximately 2-square-mile (5-square-kilometer) landmass surrounded by the water of Alsek Lake.” A recent satellite image, taken by Landsat 9 in August, reveals that the glacier has now lost all connection to Prow Knob, according to a statement released by NASA's Earth Observatory. Prow Knob provides a clear visual example of how glaciers are thinning and retreating in southeastern Alaska. "Along the coastal plain of southeastern Alaska, water is rapidly replacing ice," Lindsey Doermann, a science writer at the NASA Earth Observatory, wrote. "Glaciers in this area are thinning and retreating, with meltwater forming proglacial lakes off their fronts. In one of these growing watery expanses, a new island has emerged." Alsek Glacier used to split into two channels to wind its way around Prow Knob, which has a landmass of about 2 square miles (5 square km's). In the early 20th century, the glacier extended across the now-exposed Alsek Lake and as far as Gateway Knob, about 3 miles (5 km's) west of Prow Knob.
The melting of the Alsek Glacier happened slowly, until it didn’t. In 1894, the earliest observations of the glacier on record, the ice basically covered what’s now Alsek Lake; reports from 1907 described it as being “anchored to a nunatak,” according to a US Geological Survey review from 2005, the term refers to a rocky island surrounded by flowing glacier ice rather than water, with an iceface “as much as 50 m[eters, 164 feet] high.” The late glaciologist Austin Post, who captured aerial photographs of Alsek in 1960, named Prow Knob after its resemblance to the prow (pointed front end) of a ship. Post and fellow glaciologist Mauri Pelto, a professor of environmental science at Nichols College in Massachusetts, previously predicted that Alsek Glacier would release Prow Knob in 2020, based on the rate it was retreating between 1960 and 1990. The glacier has therefore clung on to its mountain for slightly longer than initially predicted.
But “by 1948, the glacier had retreated 1.5 to 2.5 km,” the survey continues. “By 25 August 1960, retreat was as much as 5 km.” By the late 1970s, the glacier, now much reduced in size and reach, seemed like it was about to separate into two ice tongues; two decades later, it had done precisely that, and “by 2003, the terminus separated into three distinct ice tongues,” the authors writes. Prow Knob completely separated from Alsek Glacier between July 13 and Aug 6. Many of Earth's glaciers are retreating as the planet gets warmer due to climate change. Last year was the hottest year for global average temperatures since records began, while 2025 has been marked by a string of record-breaking and near-record-breaking hot months. All of these changes can be seen in the images published by NASA, but it’s the most recent couple, from 2018 and 2025, which are most striking. In the space of just seven years, a short enough time that you probably think of yourself as not having aged at all throughout it, Alsek Lake has grown from abutting most of Prow Knob to entirely surrounding it.
At the same time, the ice has retreated, melting into the lake and calving away from itself as soaring temperatures make it warmer and less stable. It’s a trend that’s likely to continue, NASA warns, and one that’s becoming all too familiar in the once-icy Arctic state. Along with the Yakutat and Grand Plateau Glaciers, the melting of Alsek has resulted in lakes almost double the sizes they once were, not in times long past, but within living memory. “The lakes that are forming in this region are immense,” Mauri Pelto, a glaciologist at Nichols College, told NASA in November last year. “Starting at the mountains and spreading toward the coast,” the waters coming from these melting glaciers likely represent the fastest lake growth in the US this century, he believes. Alaska now is “a new lake district,” he said. “[One] that is unique in our nation.”