Geological maps are of vital importance for documenting and advancing geological knowledge and they are a prerequisite for any meaningful evaluation of economic resources. In Greenland, mapping is taking place on the mainland – that for two centuries has been the traditional exploration target – and offshore, where only in the last decades has h

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NOTE: This article was published in a former series of GEUS Bulletin. Please use the original series name when citing this article, for example: Dawes, P. R., Frisch, T., Garde, A. A., Iannelli, T. R., Ineson, J. R., Jensen, S. M., Pirajno, F., Sønderholm, M., Stemmerik, L., Stouge, S., Thomassen, B., & van Gool, J. A. (2000). Kane Basin 1999: mapping, stratigraphic studies and economic assessment of Precambrian and Lower Palaeozoic provinces in north-western Greenland. Geology of Greenland Survey Bulletin, 186, 11-28. https://doi.org/10.34194/ggub.v186.5211 _______________ The geological map coverage of Greenland at scale 1:500 000 is nearing completion, with the Kane Basin sheet of north-western Greenland the last to be compiled (sheet 6 between 78°–81°N; Fig. 1). Sporadic work by the Survey since the 1970s identified the main geological provinces and structure of the region but the lithologies of the Precambrian shield were not sufficiently mapped inland to warrant final compilation. Project Kane Basin 1999 was designed to provide this knowledge; the optimal use of logistics enabled a range of geological activities to be undertaken, as well as other scientific disciplines.

In the past few decades, little information on the wolf (Canis lupus) in Greenland has been published. The decline of the species and its extirpation in the late 1930s from East Greenland is well documented. Since then, there has been a tendency for wolves sighted in the North and East Greenland National Park to be classified as temporary visitors wandering afar from adjacent Canada, with no prospect of survival in Greenland for anything but a short period. In view of the virtual absence of human population in this vast region, that assumption may not be accurate.There is now abundant evidence to indicate that a renewed immigration and dispersal of wolves has been taking place during the last years, with a migration route from Ellesmere Island eastward across North Greenland into Peary Land, and then southward into the fjord region of central East Greenland. The wolf is reoccupying its former range and by the winter of 1983 wolves had reached the Scoresby Sund region the species' southernmost temtory of the 1930s.Examination of the published records and all available unpublished data provides a historical picture of the status of the wolf in Greenland, from which some conclusions can be made regarding populations, pack size, migration routes, feeding habits and travelling distances.