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Updated: April 30, 2025


On the shores of Lake Lagoda have been found some implements of argillaceous schist, in Carelia and in Finland tools made of slate and schist, often adorned with clumsy figures of men or of animals.

Both of these had accompanied Hugi in his ascension of the Finsteraarhorn in 1828, and both were therefore thoroughly familiar with all the dangers of Alpine climbing. The lower Aar glacier was to be the scene of their continuous work, and the centre from which their ascents of the neighboring summits would be made. Here, on the great median moraine, stood a huge boulder of micaceous schist.

He soon reached the rocky gate, where the vast ridge of schist, alternating with the limestone, and running north and south in high serrated ridges, was cut through by a deep fissure, formed by the never idle waters of a little creek, that in the course of ages had mined away the softer portions of the slate, and made a practicable pass toward the mountains.

Excavations conducted here by Schliemann in 1880-81 brought to light the broken fragments of a ceiling of greenish schist with which this lateral chamber was once covered. The beautiful sculptured decoration consists of elements which recur in almost the same combination on a fragment of painted stucco from the palace of Tiryns. The pattern is derived from Egypt.

In treating hereafter of the great number of warm springs which we have seen issuing from granite, gneiss, and micaceous schist, we shall have occasion to return to this subject, which is one of the most important of the physical history of the globe. We re-embarked at sunset, and hoisted sail, but the breeze was too feeble to permit us to continue our course to Teneriffe.

Beneath one, for instance, were found fifteen beautiful darts of variegated flint, four polished boars' tusks, some schist pendants, some shells cut into the shape of teeth, some bone and stone necklace beads, and, lastly, two small bronze beads.

At Los Arenales, low down on the eastern flank, the mica-slate is traversed by several closely adjoining, broad dikes, parallel to each other and to the foliation of the schist. The dikes are formed of three different varieties of rock, of which a pale brown feldspathic porphyry with grains of quartz was much the most abundant.

With these arrow-heads were found flint knives, large sloped scrapers, polishers, and bone stilettos, the femora of a ruminant with a pig's tooth fixed on to each end, hoes made of stag horn, beads and pendants made of bone, shell, schist, quartz, and aragonite, with the teeth of bears, boars, wolves, and foxes, all pierced with holes.

The rock formation of the hills upon its right continued of that chlorite schist which prevailed near Mr. Whaby's, which I have already noticed, and quartz still appeared in large masses, on the loftier ranges opposite, so that the geology of the neighbourhood could not be said to have undergone any material change.

The sides of these ranges are generally very precipitous, and there are rivulets between which are not perennial. Many of the hills have been raised by granite, exactly like that of the Kalomo. Dikes of this granite may be seen thrusting up immense masses of mica schist and quartz or sandstone schist, and making the strata fold over them on each side, as clothes hung upon a line.

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