Start Date: End Date: Published Date Data Date
Data acquired April 27, 2006 337 x 284 65 KB - JPEG
Data acquired April 27, 2006 605 x 444 260 KB - JPEG
Data acquired April 27, 2006 1210 x 888 797 KB - JPEG
Data acquired April 27, 2006 2420 x 1776 2 MB - JPEG
Most spring floods are triggered by rain or melting snow, but when the Skafta River of southern Iceland flooded in late April 2006, geologic activity may have been the driver. The river flows out from under the Vatnajokull Ice Cap, a large permanent field of snow and ice that covers more than 8,000 square kilometers of southeastern Iceland, including a number of volcanoes and other regions of geothermal activity. Over these hotspots, the lower layer of the ice cap melts to form glacier lakes, some of which drain into the Atlantic Ocean through rivers such as the Skafta. Other lakes are dammed by walls of ice from the overlying glacier. Catastrophic floods can occur when water breaks through the ice dams and bursts into the rivers, or when geologic activity increases and melts more water.
Jesse Allen, Earth Observatory
Published May 2, 2006 Data acquired April 27, 2006