The panorama above shows the volcanoes of Southern Iceland highlighted by early Autumn snows. Click the image for a full size version. It was taken near the town of Hella. From left to right, they are Hekla, Torfajökull, Tindfjallajökull, Katla (low, distant glacier in the background) and Eyjafjallajökull.
The image lists the dates of “historic eruptions”. For Iceland, this is since the country was settled in 871+/-2 A.D. The dates are taken from the catalogue of the Global Volcanism Program. The 870 A.D. eruption of Torfajökull produced pale-coloured rhyolite magma and coincided with the eruption of dark-coloured basaltic magma from the Veiðivötn fissure further northeast. The combination of eruptions produced distinctive two-coloured tephra (pumice and ash) marker layer that can be found in soil across the country called the Settlement Layer or Landnám tephra. It can be used to look for environmental changes since people (and their sheeps) arrived in Iceland.
Only Hekla looks like the classic cone-shaped volcano that a child might draw (and even then it is only from this angle, it is actually a SW-NE running ridge). The other volcanoes were mainly constructed by eruptions when Iceland was covered by ice over 1000 m thick. Instead of lava flows, they contain lots of broken rock fragments, shattered when the hot magma hit cold meltwater (called hyaloclastite) and piled up where they erupted. Most of the Hekla cone has formed since the ice melted, around 8,000 years ago. Tindfjallajökull has had no historic eruptions, but it has some lavas that haven’t been affected by glaciers, so has had at least one eruption since then.
The image was stitched using Hugin, a free/open source panorama stitching program, and annotated with Inkscape, a free/open source Adobe Illustrator/Corel Draw. They can be installed on Ubuntu-like Linux systems with the command sudo apt-get install inkscape hugin, and is also available for Windows and Mac. My photos don’t really do the scene justice, so you should probably just go to Iceland and see for yourself.