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In this way, assemblages of an infralittoral affinity will appear under this zone, and their depths of living at the time of dating are given in the vertical range from their elevation to the curve.Taking a closer look at the data between 40 BP covering most of the Saqqaq and Dorset Culture periods, it appears that the shoreline “fell” more than 10 meters during this time. (1999) “various indications show that after mid-Holocene times the initial glacio isostatic rebound of Greenland was followed by increased subsidence”.
This is generally sparsely vegetated, leaving the rocks beautifully exposed and the geology incredibly easy to see.
Mya truncata: a) foot b) siphon sheath c) exhalant siphon d) inhalant siphon e) umbones or beaks f) anterior g) posterior end of the shell.
Repeated measurements were most kindly taken the following summer by a group of students from the Technical University of Denmark.
Map of the Sisimiut District with the three Saqqaq sites: Asummiut, Akia and Nipisat (marked with large black dots) and the additional sample sites (marked with small red dots) Nipisat – a Saqqaq Culture Site in Sisimiut, Central West Greenland – 2004 Anne Birgitte Gotfredsen, Tinna Møbjerg, Ella Hoch and Kaj Strand Petersen Meddelelser om Grønland – Man and Society 31
eln=202653 The molluscan assemblages – recent and subfossil The sampling activities were concentrated to six localities, however some localities were sampled at several levels.
If you were an alien and wanted to try to piece together the geological story of Planet Earth – but could only visit one area – East Greenland would be the place to go.
The Geology of East Greenland – James Cresswell of East Greenland article by The Geological Survey of Denmark and Greenland (GEUS) has more than 50 years of experience in field work in Greenland.
A total of 33 dates, making this site one of the best dated in the entire Arctic, reveal that Nipisat was occupied continuously for nearly 1,500 years.
Although protruding bedrock disturbed the stratigraphy and several lenses of crushed shells interrupted the layers, three different chronological phases could be identified.
The geology can be studied either in detail or in true “seismic scale”.
Geological Survey of Denmark and Greenland (GEUS) 1989 to 1994, more than 200 m2 were excavated at the Saqqaq site of Nipisat, situated on a small island 15 km south of Sisimiut.
also represents the highest level of the six localities.