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- W766856876 abstract "Abstract A study was made of sedimentary structures in the Hardangerfjord in western Norway using the Continuous Seismic Profiler. This paper is concerned with an area less than 500 m deep lying between Xorheimsund and the main channel of the fjord. An accompanying paper by Cone, Neidell, and Kenyon (1963) discusses the deeper part of the fjord. Geological interpretation of the sub-bottom echoes is discussed, and data are presented for the thickness and volume of recent sediment in the region. Attempts to measure the velocity of sound in the sediments by refraction techniques were only partially.successful, but velocities were measured in some core- and Van Veen samples. The velocities ranged from 1.5 to 2.7 km/sec in the sediments, and a value of 4.2 km/sec was observed in the underlying material. Photographic evidence for water currents of 1 to 2cm/sec on the bottom of the fjord is presented." @default.
- W766856876 created "2016-06-24" @default.
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- W766856876 date "1963-12-30" @default.
- W766856876 modified "2023-09-27" @default.
- W766856876 title "The natural history of the Hardangerfjord 6. Studies of the sediments of parts of the Ytre samla-fjord with the continuous seismic profiler" @default.
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- W766856876 doi "https://doi.org/10.1080/00364827.1963.10409520" @default.
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