Jökull

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Jökull - 01.11.1998, Qupperneq 31

Jökull - 01.11.1998, Qupperneq 31
Ascent of Oræfajökull Sveinn Pálsson Edited by Richard S. Williams, Jr., U. S. Geological Survey and Oddur Sigurðsson, National Energy Authority, Hydrological Service THE GLACIER BOOK OF SVEINN PÁLSSON Sveinn Pálsson did glaciological research in Ice- land in the years 1792-1794 after academic studies in Copenhagen. In 1795, he sent a manuscript of a trea- tise on Icelandic glaciers in Danish to the Society of Natural History in Copenhagen. For a variety of rea- sons it was not printed in full until 1945 and then only in an Icelandic version (Pálsson, 1945). The “Glacier Book“ is “the culmination of a glaciology which may be called Icelandic in the sense that it was principally based on knowledge of Icelandic glaciers” (Tho- rarinsson, 1960). One of the most noteworthy chapters in the “Glacier Book” is the description of Pálsson's ascent of Öræfajökull where he became convinced that his previous ideas of the plastic motion of glacier ice, were correct, when he observed the regular pattern of ogives on Hrútárjökull or Fjallsjökull. That idea had not been published before, except in the works of the French naturalist A. C. Bordier in 1775 (Bordier, 1775). That piece of writing also lay obscure for al- most a century before being revealed to the glacio- logical community. Flosi Björnsson, farmer at Kvísker, studied the route supposedly taken by Pálsson (Fig. 1) and found a caim and Pálsson's initial “P” engraved on a rock close to the glacier (Bjömsson, 1957, 1965). EXCERPT FROM THE “GLACIER BOOK” Here follows an excerpt from A Physical, Geo- graphical, and Historical Description of Iceland's Glaciers on the Basis ofa Journey to the Most Promi- nent ofThem in 1792-1794 (Including Four Plan and [Eight] Perspective Drawings) by Sveinn Pálsson. Translated into English by Bjöm Netland and edited, with annotations (endnotes), by Richard S. Williams, Jr. and Oddur Sigurðsson. Ascent of Öræfajökull On 11 August [1794] we were already well under- way long before sunrise with our intention of climb- ing Öræfajökull; the weather was quite calm, without a cloud in the sky. Eggert Ólafsson' considered Ör- æfajökull to be the highest mountain in Iceland. Equipped with a barometer, thermometer, pocket compass, pickaxe, glacier cane, and a length of rope measuring eight fathoms, my two companions and I set out from the abandoned Kvísker farmstead at 0545 hr after having indicated our destination on a piece of paper that we fastened to our tent, in case we should get lost on the glacier. We made our way up rather steep foothills and finally reached the margin of the glacier at 0845 hr, where we rested on a hill for a few minutes. At the foot of this hill, we observed a few plants of the beautiful alpine species Ranunculus ni- valis [co/r. Ranunculus glacialis (mountain butter- cup)] growing on the barren gravel; a few of them had even shed their blossoms. The ones that had just bloomed had snowy-white petals, but the large ones had saffron-yellow and later [stage of the blooming cycle] red ones. I had not come across this species of plant before in the mountains of the southem districts. At this location, it grows at a higher altitude than Sta- tice armeria [Armeria maritima (thrift)], which had still not started blossoming here, and even higher up than the little Salix herbacea [least willow], which, however, usually grows in the highest location and is second only to lichens [that grow at the highest eleva- JÖKULL, No. 46, 1998 29
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