In today's world, Chumerna Glacier is a very important issue that affects people of all ages, cultures and walks of life. Whether we are talking about Chumerna Glacier in the political, social, scientific or personal context, its relevance is undeniable. This article aims to explore the different facets of Chumerna Glacier and analyze its impact on today's society. Throughout these pages, we will examine the different perspectives on Chumerna Glacier, with the aim of offering our readers a holistic and complete vision of this topic that is so relevant today.
This article includes a list of references, related reading, or external links, but its sources remain unclear because it lacks inline citations. (May 2021) |
Chumerna Glacier | |
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Location of Chumernan Glacier in Antarctica | |
Location | Palmer Archipelago |
Coordinates | 64°08′10″S 62°06′20″W / 64.13611°S 62.10556°W |
Length | 1.1 nmi (2 km; 1 mi) |
Width | 1 nmi (2 km; 1 mi) |
Thickness | unknown |
Terminus | east of Hales Peak |
Status | unknown |
Chumerna Glacier (Bulgarian: ледник Чумерна, romanized: lednik Chumerna, IPA: [ˈlɛdnik t͡ʃoˈmɛrnɐ]) is the 2.2 km long and 1.9 km wide glacier draining the north slopes of Stavertsi Ridge on Albena Peninsula, Brabant Island in the Palmer Archipelago, Antarctica. It flows northeastwards to enter the channel between Brabant Island and Liège Island east of Hales Peak.
The glacier is named after Chumerna Peak in eastern Balkan Mountains, Bulgaria.
Chumerna Glacier is centred at 64°08′10″S 62°06′20″W / 64.13611°S 62.10556°W. British mapping in 1980.
This article includes information from the Antarctic Place-names Commission of Bulgaria which is used with permission.