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- W2023060168 abstract "The distribution, morphology, fillings, and origin of buried valleys are discussed. The direction of the valleys varies from NW to NE. Within the Viru-Harju Plateau the valleys have a more or less symmetric profile, but asymmetric profiles are dominating in the pre-klint area. They are mainly filled with glacial (till), glaciofluvial (sand, gravel, and pebbles), glaciolacustrine (varved clay), and marine (fine-grained sand) deposits. The Tallinn valley with its tributary valleys (Saku and Sausti) and fore- klint branches (Harku, Lillekula, and Kadriorg) looks like a river system. The fore-klint branches extend over 20 km in the Gulf of Finland. They are probably tributaries of the ancient river Pra-Neva. Most likely, the formation of valleys was continuous, starting from pre-Quaternary river erosion, and was sculptured by variable processes during the ice ages and influenced by flowing water during the interglacial periods." @default.
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- W2023060168 date "2010-01-01" @default.
- W2023060168 modified "2023-10-01" @default.
- W2023060168 title "Ancient buried valleys in the city of Tallinn and adjacent area" @default.
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- W2023060168 doi "https://doi.org/10.3176/earth.2010.1.03" @default.
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