extensive ice field, southeastern Iceland, covering an area of 3,200 sq mi (8,400 sq km) with an average ice thickness of more than 3,000 ft (900 m). Generally about 5,000 ft above sea level, in the Öræfajökull (Öraefa Glacier) in the south it rises to 6,952 ft (2,119 m) on Hvannadalshnúkur, the highest peak in Iceland. There are numerous active volcanoes throughout the ice field, the meltwaters of which feed hundreds of rivers, the largest of which are the Thjórsá, Skjálfandafljót, Jökulsá á Fjöllum, and Jökulsá á Fljótsdal, which further downstream takes on the name of Lagarfljót. Meltwater and moraine deposition at its southern end, aggravated by glacial bursts caused by hot springs under the ice, long prevented road construction on the narrow strip of land between the ice field and the ocean. Thus the coastal road encircling the island was not completed until the mid-1970s.

Periodic eruptions of Grimsvötn, the largest volcano under the ice field, melt the surrounding ice and create a lake that occasionally breaks through its ice walls, causing catastrophic floods called jökulhlaup (“glacier runs”). During the eruptions of 1934 and 1938, the rate of jökulhlaup discharge reached 65,000 cu yd (50,000 cu m) per second. In the 20th century a jökulhlaup broke out of Vatnajökull roughly every 5 or 10 years.