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In groups of five, pupils were engaged with the task of unravelling some particularly intriguing landscape puzzles.
The tectonic puzzle centred on the site of the Viking parliament at Thingvellir and the nearby Nesjavellir geothermal power station. Both are within an impressive section of the Mid Atlantic rift valley between the Eurasian and North American plates.
The Solheimajokull was our glacial puzzle; Iceland’s most active volcano, the subglacial volcano Katla, periodically supplies basalt and water in untold quantities to a tongue of ice now retreating 100m every year. Katla conspires to compete with the discharge of the Amazon and boasts the world’s largest lava field (which we also visited).
Our fluvial puzzles were the great waterfalls, Gullfoss and Seljandsfoss: these are regrading cliff lines abandoned by combinations of isostatic readjustments and Jokulhaup (glacier burst) aggradation. If you had landed on Iceland 5,000 years ago there would have been no ice at all.
The black basalt beach and sand dunes of Vik, Iceland’s most southerly point, hosted our coastal puzzle. The Arctic terns were not happy to be left off the risk assessment and, in their hundreds, proceeded to dive bomb our psammosere explorers. The Marburian response: to charge! |