Jökull


Jökull - 01.12.1968, Blaðsíða 59

Jökull - 01.12.1968, Blaðsíða 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
Blaðsíða 1
Blaðsíða 2
Blaðsíða 3
Blaðsíða 4
Blaðsíða 5
Blaðsíða 6
Blaðsíða 7
Blaðsíða 8
Blaðsíða 9
Blaðsíða 10
Blaðsíða 11
Blaðsíða 12
Blaðsíða 13
Blaðsíða 14
Blaðsíða 15
Blaðsíða 16
Blaðsíða 17
Blaðsíða 18
Blaðsíða 19
Blaðsíða 20
Blaðsíða 21
Blaðsíða 22
Blaðsíða 23
Blaðsíða 24
Blaðsíða 25
Blaðsíða 26
Blaðsíða 27
Blaðsíða 28
Blaðsíða 29
Blaðsíða 30
Blaðsíða 31
Blaðsíða 32
Blaðsíða 33
Blaðsíða 34
Blaðsíða 35
Blaðsíða 36
Blaðsíða 37
Blaðsíða 38
Blaðsíða 39
Blaðsíða 40
Blaðsíða 41
Blaðsíða 42
Blaðsíða 43
Blaðsíða 44
Blaðsíða 45
Blaðsíða 46
Blaðsíða 47
Blaðsíða 48
Blaðsíða 49
Blaðsíða 50
Blaðsíða 51
Blaðsíða 52
Blaðsíða 53
Blaðsíða 54
Blaðsíða 55
Blaðsíða 56
Blaðsíða 57
Blaðsíða 58
Blaðsíða 59
Blaðsíða 60
Blaðsíða 61
Blaðsíða 62
Blaðsíða 63
Blaðsíða 64
Blaðsíða 65
Blaðsíða 66
Blaðsíða 67
Blaðsíða 68
Blaðsíða 69
Blaðsíða 70
Blaðsíða 71
Blaðsíða 72
Blaðsíða 73
Blaðsíða 74
Blaðsíða 75
Blaðsíða 76
Blaðsíða 77
Blaðsíða 78
Blaðsíða 79
Blaðsíða 80
Blaðsíða 81
Blaðsíða 82
Blaðsíða 83
Blaðsíða 84

x

Jökull

Beinir tenglar

Ef þú vilt tengja á þennan titil, vinsamlegast notaðu þessa tengla:

Tengja á þennan titil: Jökull
https://timarit.is/publication/1155

Tengja á þetta tölublað:

Tengja á þessa síðu:

Tengja á þessa grein:

Vinsamlegast ekki tengja beint á myndir eða PDF skjöl á Tímarit.is þar sem slíkar slóðir geta breyst án fyrirvara. Notið slóðirnar hér fyrir ofan til að tengja á vefinn.