Glaciers cutting through the 410 million year old Red Devonian sandstones, the Carboniferous and the upper, 260 million years old Permian Carbonates makes Ekmanfjorden unique.
Weathering and erosion of the surrounding mountains supply the fjord with red sands and muds. Sefströmbreen advanced 6km between 1882 and 1896 (See Map). The advance reworked muds of Ekmanfjorden into large red ridges which effectively turned Coraholmen into a Martian looking landscape 👽 (photo 1, 3, 5, 6, 8).
Sefströmbreen Glacier has since then retreated and is actively melting back which and is now exposing fresh ridge landforms (photos 4,7).
Sites were visited during summer 2023 where we investigated and sampled landforms to assist
@mattilakken1 in data collection for her thesis on glacial processes and landform morphology in Ekmanfjorden.
The tidal flat (Photo 9) Holmströmøyra was investigated and sampled for
@curlyswhirlys thesis on holocene Foraminifera fauna.
Drone photos by
@curlyswhirlys 🛸👩🚀
@unisvalbard @geologi_geoscience
Sources:
Dineley, D., & Waters, R. (1960). Notes on the Recent Advance and Retreat of Sefströmbreen in Ekmanfjorden, Vestspitsbergen. Journal of Glaciology, 3(28), 693-697.
doi:10.3189/S0022143000017986
van der Meer, Jaap JM. "De Geer: Early observations on Holmströmbreen, Sefströmbreen and Coraholmen." Developments in Quaternary Sciences. Vol. 4. Elsevier, 2004. 181-197.
/10.1016/S1571-0866(04)80104-0