John Edward Lee

Summary

John Edward Lee Excavations at the Kesslerloch… (1876)

Like these the tarns were surrounded by an Alpine flora, the remains of which fell into the mud, and have been preserved to our own days. . . . In the 'Urwelt der Schweiz,' p. 534, &c., I have endeavoured to show that at the Glacial age the Alpine flora very probably occupied the plain land of Switzerland, so far as it was free from glaciers, and that the Alpine plants which we now see insulated on the mountain chains of Northern Switzerland may be the last remains of this ancient flora—the lost children of the Alps surrounded entirely by the inhabitants of the plain.
Source: Wikisource

John Edward Lee Excavations at the Kesslerloch… (1876)

Mr. Nathorst last autumn came to Switzerland, to seek for this northern flora here, and he succeeded in finding it at Schwerzenbach, in the Canton of Zürich, in a bed of loam under a deposit of peat. With the assistance of Dr. Ferdinand Keller, who aided him by his rich fund of experience, masses of this loam under the peat were dug out and brought to Zürich; and in it were found seven species of Arctic plants. They were, Betula nana, Salix polaris, Salix retusa, Salix reticulata, Arctostaphylos uva ursi, Polygonum viviparum, and Dryas octopetala.
Source: Wikisource

John Edward Lee Excavations at the Kesslerloch… (1876)

It cannot, however, be wrong to state one or two facts which in a measure bear on the discoveries of the Kesslerloch. Although the Glacial period after the Tertiary is acknowledged by all thinking persona, yet every additional fact brought to light strengthens the theory—if in fact it can be now called by this name. The evidence of an Arctic or reindeer period in France is given so clearly in the valuable work called 'Reliquiæ Aquitanicæ,' that no one can gainsay it, and it is needless to refer to a volume of such standing
Source: Wikisource

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