Zemlya Georga seasonal research station which can shelter up to 10 persons. The "Nightingale Channel" (Proliv Neytingeyl) runs east of Zemlya Georga, separating it from Bruce Island. Most of the land lies under large glaciers and ice domes, such as the Brusilov Ice Dome, Gretton Ice Dome, Dzegudze Ice Dome (Купол Дзегудзе), Zander Ice Dome, Foggy Ice Dome (Купол туманный), Arctic Geology Research Institute Ice Dome (Купол Научно-исследовательский институт геологии Арктики) and the Peary Ice Dome, although there is a large, mostly unglacierized peninsula at its northern end, "Poluostrov Armitidzh". Zemlya Georga Zemlya Georga, or Prince George Land (; "Zemlya Georga", "George
Baltica belt of the Timanide orogeny and overlain by Mesoproterozoic sediments. The margin became a passive margin facing an Ural Ocean in the Cambrian-Ordovician. The eastern margin stretches south through the Ural Mountains from the northern end of the Novaya Zemlya archipelago. The margin follows the bent shape of Novaya Zemlya which was caused in the Late Permian by the Siberian Traps. It is clear from Baltic endemic fossils in Novaya Zemlya that the islands have been part of Baltica since Early Palaeozoic, whereas the Taymyr Peninsula farther east was part of the passive margin of Siberia in the Early Palaeozoic.