Grain size distribution in surface sediments samples of the continental shelf and slope of southeast Greenland

• Main Author: Sommerhoff, G
• Format: Dataset
• Language: English
• Published: PANGAEA 1973
• Subjects: BCR; Box corer (Reineck); M6; M6_001; M6_002; M6_003; M6_004; M6_006; M6_007; M6_009; M6_011; M6_012; M6_013; M6_014; Meteor (1964); RUS_EXP_1; RUS_EXP_10; RUS_EXP_11; RUS_EXP_12; RUS_EXP_13; RUS_EXP_3; RUS_EXP_5; RUS_EXP_6; RUS_EXP_7; RUS_EXP_8; RUS_EXP_9; Southeast coast of Greenland; US_EXP_14; US_EXP_15; US_EXP_16; Greenland; Northwest Atlantic
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.604852; https://doi.org/10.1594/PANGAEA.604852

During "Meteor" Cruise 6/1966 in the northwest Atlantic a systematic survey of the bottom topography of the southeast Greenland continental margin was undertaken. Eighty-seven profiles transverse to the shelf edge at distances of 3-4 nautical miles and two longitudinal profiles parallel to the coast were carried out with the ELAC Narrow Beam Echo-Sounder giving a reliable record of even steep slopes. On the basis of the echo soundings the topography and morphology of the continental shelf and slope are evaluated. A detailed bathymetric chart and a serial profile chart were designed as working material for the morphological research. These maps along with the original echograms are morphometrically evaluated. The analysis of the sea bottom features is the basis of a subsequent morphogenetical interpretation, verified and extended by means of interpretation of magnetic data and sediment analysis (grain size, roundness, lithology). The results of the research are expressed in a geomorphological map. The primary findings can be summarized as follows: 1) The southeast Greenland shelf by its bottom topography can be clearly designated as a glacially formed area. The glacial features of the shelf can be classified into two zones nearly parallel to the coast: glacial erosion forms on the inner shelf and glacial accumulation forms on the outer shelf. The inner shelf is characterized by the rugged and hummocky topography of ice scoured plains with clear west/east slope asymmetry. On the outer shelf three types of glacial accumulation forms can be recognized: ice margin deposits with clearly expressed terminal moraines, glacial till plains and glaciomarine outwash fans. Both zones of the shelf can be subdivided into two levels of relief. The ice scoured plains, with average depths of 240 meters (m), are dissected to a maximum depth of 1060 m (Gyldenloves Trough) by trough valleys, which are the prolongations of the Greenland fjords. The banks of the outer shelf, with an average depth of 180 m, surround glacial basins with ...