In an article in this Journal Footnote * on the equatorial glaciers of East Africa Lieutenant-Commander Spink described the Ruwenzori range as a non-volcanic chain of peaks extending about 70 miles (112 km.) along the Belgian Congo–Uganda border in a north-north-easterly direction.

I traversed this range in December 1949 as a member of a small party led by Mr. Ashley Greenwood. We followed the route shown in Fig. 1 below. We had but little time to spare for detailed study, but the paucity of information on this area prompts me to offer these few observations in the hope that they may fill in some gaps and initiate a fuller enquiry.

Fig. 1

The largest glaciated area visited was the Stanley Plateau. This caps Mt. Stanley and through it protrude several peaks—Margherita, the highest point of the whole range, rising approximately to 16,794 ft. (5119 m.), Alexandra (16,749 ft.), Elena (16,385 ft.), Savoia (16,421 ft.).

The plateau is about a mile long and falls slightly towards the foot of Margherita. Its mean height is about 16,000 ft. (4877 m.). We ascended to it by the Elena Glacier tongue.

No powder snow lay on the ice although much rain had fallen at lower levels during the previous week. The firn was fairly consolidated, no doubt because of the large diurnal range. A remarkable point is that there was never more than a gentle breeze during our stay and this, I believe, is the normal state of affairs.

I did not see a dirt cone, thrust plane, perched block, pot-hole, surface stream nor any nieve pentente on any glacier. The glaciers are only moderately crevassed and the run-off streams, although examined at all times of day, were almost free of rock flour.

Where cornices were seen they were not of the usual alpine type and suggested no prevalent wind direction. During three nights at Ridge Camp at 15,000 ft. (4571 m.), beside the Elena Glacier the temperature never fell below 28° F. (−2.2° C.) and on the first night only reached freezing point. The snow on the plateau lost crust at about 9.30 a.m.

A close examination was made of a glacier tongue 1000 ft. (305 m.) above the East African Mountaineering Club hut at Bujuku. This flows down from Mt. Speke. Here we were joined by Messrs. O. K. Mather and G. Du Bois of the Geological Survey, who by permission of its Director, Dr. K. A. Davies, were enabled to visit this area and map the tongue (see Fig. 2, p. 511).

Fig. 2

A beacon was set up so that annual measurements may be made. The glacier snout lies at about 14,000 ft. (4267 m.) in a deep gulley whose smooth sides display an obvious and rapid retreat. Vegetation has not yet sprung up in the abandoned area which extends to an altitude of 13,000 ft. (3962 m.).

Large areas were devoid of firn and showed layers of dirty ice, the dirt probably consisting of wind-blown dust and the ash from the innumerable forest fires which are lit in the valleys every hot season. Only a few stones were held in the ice and there is no moraine at the present glacier foot although a fairly large one exists 500 ft. (152 m.) lower down. Still lower very large ancient moraines are in evidence.

I was able to crawl right under and inside the ice at the centre of the snout. There were no signs of plucking of the rock bed. The roof of this ice cave was 5 ft. (1.5 m.) above me with corrugations transverse to the line of flow at 4 ft. intervals. The crystals here measured up to 3.0×0.5 cm. and there seemed to be a tendency for them to lie vertical to the line of flow. At the side of the tongue they were smaller (about 1.0 cm.×2 mm.) and I had the impression that they lay more or less parallel to the line of flow. There were bands of smaller crystals and their significance is obscure. They cannot be annual bands as there is no distinct winter-summer cycle.

Access to, and examination of, the Elena Glacier was difficult because of ice falling from the hanging glacier above it. The snout could not be reached, but beacons were set up for annual measurements. These may be found by bearing 195° from Ridge Camp and walking for fifteen minutes. The snout of this glacier terminates at 14,800 ft. (4511 m.) in a deep unvegetated groove. There is no terminal moraine and its stream is clear of detritus. This is true of all the Ruwenzori glacier streams and one never sees the turbid, opaque water common to alpine streams of similar type.

At some 200 ft. (61 m.) above the snout I entered a cleft by a rock outcrop. I found only dense, consolidated firn. The crystals were of millimetre size. Ablation caused bands to stand out like fins of an air-cooled cylinder. They contained much dirt but again only of such size as could be wind-blown. Again there was no evidence of plucking of the rock bed and no boulders or detritus could be seen in the snout of this glacier.

I could find no true glacier ice above the snout nor any sign of present glacial action, and this would seem to show that the conditions now existing are not quite usual. Investigation should be continued at other times of year and more frequently. Valuable work could be performed by a properly equipped party camping on the Stanley Plateau and working over a much longer period than was possible for us.