The peninsula has a similar geology to Ny-Ålesund, Carboniferous and Permian, but is unaffected by coal wastes, which made the peninsula act as a control area.[3] Melting ice since the last glacial period has resulted in the preservation of a superb raised beach sequence. Today, glaciers across the Peninsula have continued to experience a long-term decline in volume of ice and length since monitoring experiments began in the 1960s, a result of warming in the 20th century.[4]
^Bréchignac, F. (2005). Equidosimetry: Ecological Standardization and Equidosimetry for Radioecology and Environmental Ecology. North Atlantic Treaty Organization. p. 436.
^Creed, Ed. "Open Source". Geography.exeter.ac.uk. Retrieved 2 October 2018.