Jökull


Jökull - 01.12.1968, Síða 59

Jökull - 01.12.1968, Síða 59
(see bibliography). At the time of writing two 4 colour maps (1:30000) based on the 1945 and 1965 aerial photography are in the final stages of production. These maps clearly indicate the rapid wastage of Breidamerkurjokull over this period of time and some dramatic changes in the morphology and drainage systems of the proglacial area. The choice of a very large glacier as the subject of study in this project had some major disadvantages. It was not possible to carry out a study of the mass-balance of such a large glacier (15 km wide and over 20 km long), but since the emphasis of the project was on the frontal zone of the glacier ancl the pro- cesses at work in the proglacial area, this clis- advantage was counterbalanced by the great variety of landforms and deposits existing along the wide glacier front. The glaciological studies were limited to an attempt to link the factors of ice movement and ice wastage to the morphological and sedimentalogical pro- cesses at work in the frontal zone. The project has proved to be a very stimu- lating one from the point of view of the re- search workers involved and an excellent op- portunity to teach research methods to both post-graduate and undergraduate stuclents. The total investment of over £ 4000 obtained from various sources listed earlier in this paper has been supplemented by a great deal of labour and equipment which it has not been possible to cost. The photogrammetric plotting machin- es of the Department of Geography have been used on this project for at least 1000 hours and departmental cartographers have been employed for over 2000 hours in producing maps and diagrams. This investment of money, time ancl labour has allowed both research and teaching to be carried out in Iceland. This approacli will be continued during the summer of 1968 when a field course will be given by the author and Mr. Howarth, for sixteen members of the British Quaternary Field Study Group. In a sense this field course is the cul- mination of the project because the initial purpose of the project was to obtain informa- tion about processes in an area of existing glaciers so that areas formerly glaciated in Britain could be more satisfactorily interpret- ed. During this field-course 16 scientists actively engaged in research in geomorphology, geology and pedology in Britain will be able to see for themselves a glacial environment. A CKNO WLEDGEMENTS The author is pleased to acknowledge the support and co-operation of his co-supervisor in this project, Mr. G. Petrie. Without the devotion of Messrs. Welch and Howarth to what was often rigorous and boring ivork this project would not have been possible. Other colleagues who gave advice and assistance were: Mr. J. Keates, Mr. B. D. F. Methley and Mr. H. Williams, Mr. S. Santa and Mr. A. Kelly. All members of the project are indebted t.o Prof. II. Miller for his continuous support and io the following persons in Iceland xuho gave advice and material assistance: Mr. A. Bodvarsson (Landmaelingar Islancls), the fíjorns- son brothers of Kvisker, Mr. S. Johannson (Vegagerd rikisins), and Dr. S. Thorarinsson. The following organisations provided finan- cial support for the project: The Nalural Environment Research Council (formerly D.S.I.R.) The Carnegie Trust for the University of Scotland Tlie Court of the Universily of Glasgow The Royal Geographical Society The Gino Wathkins Memorial Fund BIBLIOGRAPHY Howarth, P. J. 1966: An Esker, Breidamerkur- jokull, Iceland. Occ. Paper No. 3, British Geomorphological Research Group, 6—9. — 1968: Geomorphological and Glaciological Studies. Eastern Breidamerkurjokull, Ice- land. Ph. D. thesis, University of Glasgow — in press. Petrie, G. and Pri.ce, R. J. 1966: Photogram- metric Measurements of the Ice Wastage and Morphological Changes Near the Case- ment Glacier, Alaska. Canadian Journ. Earth Sc„ 3, 827-840. Price, R. J. 1966: Eskers Near the Casement Glacier, Alaska. Geogr. Annal,48, Ser. A, 111-125. — 1969: Moraines, Sandar, Kames ancl Eskers JÖKULL 18. ÁR 393
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