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. 2014 Aug 2;301(2):809–832. doi: 10.1007/s00606-014-1118-5

Fig. 3.

Fig. 3

The Aamaruutissaa locality/outcrop in an oblique aerial photograph. The landslide is clearly seen, as well as the Talerua Member lava flows in situ at heights above 200 m a.s.l. North of the landslide the contact between lava flows of the Kanissut Member and the Talerua Member, respectively, has been described by Hald (1977)