COMPUTER-BASED BATHYMÉTRIC MAP OF LAKE BAIKAL

dc.contributor.author	Sherstyankin P.P.
dc.contributor.author	Alekseev S.P.
dc.contributor.author	Abramov A.M.
dc.contributor.author	Stavrov K.G.
dc.contributor.author	De Batist M.
dc.contributor.author	Hus R.
dc.contributor.author	Canals M.
dc.contributor.author	Casamor J.L.
dc.date.accessioned	2024-10-27T02:28:41Z
dc.date.available	2024-10-27T02:28:41Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13516236
dc.identifier.citation	Doklady Earth Sciences, 2006, 408, 4, 564-569
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46238
dc.description.abstract	The history of deep-water plumbing of the depth in Lake Baikal started in 1789 when Nikita Karelin, Sergei Smetanin, and Egor Kopylov, employees of the Kolyvano–Voskresensk plants, carried out two traverses with 28 measurements between the head of the Angara River and the mouth the Selenga River. One of such measurements yielded a maximum depth of 1238 m. Thus, Lake Baikal was immediately recognized as one of the world’s deepest lakes. Later, according to oceanographic historians, the British captain Fips accidentally discovered an even deeper area when thermometers used for the measurement of water temperature in this lake reached a depth of about 1250 m.
dc.subject	Baikal
dc.title	COMPUTER-BASED BATHYMÉTRIC MAP OF LAKE BAIKAL
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06040131

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