Jökull


Jökull - 01.12.1956, Page 9

Jökull - 01.12.1956, Page 9
jökull at that time. In all probability Stóralda is older than tlie settlement of Iceland and its lack of soil cover at the time of the 1362 erup- tion can be satisfactorily explained by assum- ing that soil erosion, caused by the arrival of man and his livestock, has deprived the rnorai- nes of their soil cover. In olden times a farm, Freysnes, was probably situated not far from Stóralda. Being prehistoric Stóralda must be formed either after or before the Postglacial Warm Periocl and in my opinion is was most likely formed as a result of the climatis deterior- ation during the first centuries of Subatlantic. Time, that began ab. 600 B. C. REDUCTION OF SVÍNAFELLSJÖKULL AND SKAFTAFELLSJÖIvULL IN RECENT TIME ACCORDING TO MAPS AND AERIAL PHOTOS. The oldest topographical map showing the margins and contour lines of the glaciers in question is the Danish General Staff map of 1904, scale 1:50.000 (sheet 87 Öræfajökull SV). A new map in the same scale was made in 1950 by the U. S. Army Map Service (sheets 6019 III and 6018 IV). This map is based on aerial photos taken in Aug. 1945. The height figures on the glaciers are scanty on the 1904 map. However there is reason to believe that on this map and the U. S. Army map the contour lines are exact enough on the lower part of the glacier tongues to enable us to calculate their thinning 1904—1945 with less than 20% error. On the map fig. 4 the contourlines and river courses are according to the 1950 map. The glacier margins 1904 and 1945 are according to corresponcling topographical maps and so are the lines showing the glacier thickness on the longitudinal section fig 5. The dot line showing the glacier fronts in 1954 is according to the excellent aerial photos taken by Á. Bödvarsson Sept. 15, 1954. The dash line showing approxi- rnately the maximum extension of the glaciers in historical time is partly based on fielcl studies and partly on Bödvarssons photos. I emphasize that this line is only approximate, especially as regards Skaftafellsjökull and the northern part of Svínafellsjökull. Nor do we know at what time the glaciers reached their maximum extension but a least Svínafellsjök- ull seems have been very near this stage ab. 1870. At that time the southernmost part of its front extended so far that blocks of ice broke off frorn it and rolled down the southern slope of the outermost moraine ridge N of the Svína- fell farm. The following figures are based on the above mentioned comparison between the 1904 and 1950 maps. The figures for the frontal areal changes are fairly exact but the figures for the total areal changes are not so reliable as the mapping of the upper parts of the glaciers in 1904 can not have been very exact. Because of the steepness of the uppermost part of the ablation areas the changes of the 1100 m contours due to thinning of the glaciers since 1904 are negligible. SKAFTAFELLSJÖKULL. Area below the 1100 m contour (approx. firn line) 1904 .... 38.5 km2 Area below the 1100 m con- tour 1945 ................ 33.0 „ Total areal loss 1904—1945 . . 5.5 „ (14.3%) Frontal areal loss 1904—1945 4.0 „ (10.4%) Max. linear recession 1904— 1945 ...................... 1.0 km 7

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Jökull

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