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Global Volcanism Program | Image GVP-05766

Lysuhöll, Iceland's smallest volcanic system, consists of a chain of small cinder cones and vents along a WNW-ESE line cutting diagonally across the Snæfellsnes Peninsula in the center of the photo.  The cones and vents of the Lysuhöll volcanic system, seen here from the ENE, are located between the snow-covered Helgrindur mountains in the foreground and the glacier-covered Snæfellsjökull volcano in the background.  The latest eruptions from Lysuhöll occurred during the Holocene.       Photo by Thorvaldur Bragason, Iceland Geodetic Survey (courtesy of Richie Williams, U.S. Geological Survey).

Lysuhöll, Iceland's smallest volcanic system, consists of a chain of small cinder cones and vents along a WNW-ESE line cutting diagonally across the Snæfellsnes Peninsula in the center of the photo. The cones and vents of the Lysuhöll volcanic system, seen here from the ENE, are located between the snow-covered Helgrindur mountains in the foreground and the glacier-covered Snæfellsjökull volcano in the background. The latest eruptions from Lysuhöll occurred during the Holocene.

Photo by Thorvaldur Bragason, Iceland Geodetic Survey (courtesy of Richie Williams, U.S. Geological Survey).


Helgrindur

Snaefellsjökull