Near Ilulissat on Greenland’s west coast, immense icebergs gather where the Sermeq Kujalleq glacier pours into the sea. The Ilulissat Icefjord is a protected natural landscape, not a town attraction with roads through the wilderness. Its scale is difficult to grasp from a photograph: the glacier advances rapidly, calves huge volumes of ice and sends them into a fjord that carries them toward Disko Bay. A visit combines dramatic scenery with a reminder that this is both a scientific site and a place shaped by generations of Greenlandic life.
The fjord lies about 250 kilometres north of the Arctic Circle and was inscribed on the UNESCO World Heritage List in 2004. At its head, Sermeq Kujalleq drains part of the Greenland ice sheet. UNESCO describes it as one of the world’s fastest and most active glaciers, moving around 40 metres per day. Its annual calving is estimated at more than 46 cubic kilometres of ice, about a tenth of Greenland’s total iceberg production. These figures explain why the fjord is scientifically important, but the view offers a more immediate lesson: ice is not a still surface but a moving system that shapes rock, sea and habitat.