Jökull


Jökull - 01.12.1953, Síða 3

Jökull - 01.12.1953, Síða 3
I HAVE been asked to contribute to this issue of JOKULL. I will do it by the following lines. Ever since Landnámstid (the time of colon- ization 870—930) the glaciers have received more attention and have been better understood in Iceland than in any other country, not even excluding the Alpine districts or Norway. The reasons for this are many. ln the first place the glaciers in lceland are so large and they are so located that their influence on culti- vated areas and settlements has been import- ant. 1 need only to refer to Sigurdur Thorar- insson’s papers on the oscillations of the sou- thern outlet glaciers of Vatnajökull and their influence on the settlements in Austur-Skafta- fellssýsla. Secondly the Icelanders have a realistic interest for nature phenomena which is greater than that of most other peoples. Not even dur- ing the Middle Ages was this interest darkened by superstition and theology. This is evident i. a. from Konungsskuggsjá (Speculum Regale), JOKULL ÁRSRIT JÖKLÁRANNSÓKNAFÉLAGS ÍSLANDS 3. ÁR REYKJAVÍK 1953 the Norwegian manuscript from about the middle of the I3th century; Thórdur Vídalín (1662—1742) and Sveinn Pálsson (1762—1840) were pioneers in the field of glaciology. The interest in glaciers shown at present in Iceland is admirable. Her own contributions to sucli knowledge are important and well knoxan. This periodical, JOKULL, is a proof of this. While the rest of the world has trouble in maintaining a journal solely on glaciology, Ice- land has started her own publication. It shows the ambition and capacity not only of the few Icelandic scientists but also of the whole peop- le in a way which has no paralell elsewhere. I would like to mention especially Jón Ey- thórsson, who has by self-sacrificing work main- tained the measurements of Icelandic glaciers and who is the initiator and editor of JOKULL. Iceland is situated in a centre faction of the general atmospheric circulation and lier glaciers have an exceptionally rich and interesting for- mation. It is of greatest importance that in- vestigations will be maintained in Iceland whose particular purpose is to clarify the connection betiueen the glacial regime and climatic fluctuations. Iceland has in this respect a key position. Therefore I express the hope that internati- onal cooperation in the field of glaciology will be able to support the Icelandic effort to make use of her unique natural advantages. Z'haVT G/LW i

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Jökull

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