Sermeq Avannarleq glacier, Torsukattak ice fjord, western Greenland late May 2013

27 09 2013

Sermeq-Avannarleq glacier, Greenland

A view of the Sermeq Avannarleq glacier in Western Greenland and its ice front, 29th May 2013. Take out the window during a flight from London to San Francisco. I did not know which glacier it was until late September when I found it on Google Earth at 70° 3’3.24″N, 50°19’1.22″W. Click on the photo for a full size view. According to the Byrd Polar Research Center, the Sermeq Avannarleq glacier lost 2 square miles from its ice front in 2007 and again in 2008. Increasingly rapid movement of this and other glaciers in south west Greenland  is likely caused by surface melt waters percolating into the glacier, warming and lubricating the ice. You can find more scientific details in the AGU press release about  Phillips et al., 2013.

Seismic tremor under Katla

29 04 2010
seismic earthquake Iceland Katla volcano volcanic

The Earth shook directly under Mount Katla in Iceland when a small earthquake (magnitude 1.5) was detected at about 6 km depth on Wed 28th April 2010. Is the giant awakening? UPDATE: Another earthquake occurred under Katla. The original 28th April 2010 earthquake is now being reported as two simultaneous earthquakes, one at 7.1 km (magnitude Ml=1.0) and another at 0.5 km depth (Ml=1.5). Heidi Soosalu writing on Katla seismicity (Journal of Volcanology and Geothermal Research, vol 153 177-186, 2006) states that Katla has seasonal earthquake activity. These tremors usually occur later in the year probably because of changes in glacial melting and groundwater pressure in the roof of the caldera. Seismic shocks shake two distinct areas of Katla, the Goðabunga rise on the west side, and the caldera area in the center of Katla. The latest two earthquakes are associated with the rim of the caldera. A third earthquake occurred today on the southern slopes of Katla (magnitude 1.7 at about 7km depth). Since 2002, seismic activity has been fairly continuous over and above the seasonal effect, particularly on the Goðabunga rise during 2001-2004. However a seasonal effect is still evident - earthquakes are less frequent in winter. The increased seismic activity since 2001-2002 is attributed to acceleration of a rising dome of highly silicic, viscous magma 1.5km down stressing and deforming the roof above it. Inflation of the volcano and increased geothermal activity have accompanied the increased seismicity since 1999. Because of the rising dome under Goðabunga rise, several eruption scenarios are worth considering besides the more "traditional" basaltic eruption from the caldera. These include a more silicic style event, a type that has not occurred in Katla for more than 1700 years, and could be extremely violent. Seismicity preceding silicic eruptions have been noted by Soosalu et al 2006 at Unzen in Japan and in the Soufrière Hills of Montserrat in the context of a silicic Katla eruption. The good news so far is that the current seismicity cannot be easily attributed to anything but ongoing activity started in 1999. Signs of an imminent eruption will include further increases in hydrothermal activity and ground uplift - neither of which have been reported as anomalous so far. The not so good news is that post-1999 earthquakes shout loudly at us to not ignore the slumbering beast, and accept the possibility that an explosive eruption from the Goðabunga rise on the west side of Katla could be more than a little bit bigger than the current Eyjafjallajökull eruption! Image © Robert Corkery 2010.

Frozen 1

7 02 2010

Frozen canal between Långholmen and Södermalm, Lake Mälaren, Stockholm

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