Landslide-induced jökulhlaup are an increasingly pertinent glacial hazard with climate change enacting paraglacial landscape responses which are instigating more frequent landslide and proglacial lake interactions, a matter of utmost relevance in areas of ongoing deglaciation like the Himalayas. This study used the 1967 Steinholtshlaup in Iceland as a case study to explore the feasibility of using an Earth observation approach through Structure from Motion (SfM) photogrammetry, establishing geomorphological landscape changes, and providing a better understanding of the mechanisms that control jökulhlaup interactions with the landscape and the enduring geomorphological legacy. Historical aerial photography and a modern Unmanned Aerial Vehicl...