Travel Reference
In-Depth Information
Mr. Motley,
*
who visited the mountain in the dry season, and paid much attention to bot-
any, gives the following list of genera of European plants found on or near the sum-
mit:—Two species of Violet, three of Ranunculus, three of Impatiens, eight or ten of Rubus,
and species of Primula, Hypericum, Swertia, Convallaria (Lily of the Valley), Vaccinium
(Cranberry), Rhododendron, Gnaphalium, Polygonum, Digitalis (Foxglove), Lonicera
(Honeysuckle), Plantago (Rib-grass), Artemisia (Wormwood), Lobelia, Oxalis (Wood-sor-
rel), Quercus (Oak), and Taxus (Yew). A few of the smaller plants (Plantago major and
lanceolata, Sonchus oleraceus, and Artemisia vulgaris) are identical with European species.
The fact of a vegetation so closely allied to that of Europe occurring on isolated mountain
peaks, in an island south of the Equator, while all the lowlands for thousands of miles
around are occupied by a flora of a totally different character, is very extraordinary; and has
only recently received an intelligible explanation. The Peak of Teneriffe, which rises to a
greater height and is much nearer to Europe, contains no such Alpine flora; neither do the
mountains of Bourbon and Mauritius. The case of the volcanic peaks of Java is therefore
somewhat exceptional, but there are several analogous, if not exactly parallel cases, that will
enable us better to understand in what way the phenomena may possibly have been brought
about. The higher peaks of the Alps, and even of the Pyrenees, contain a number of plants
absolutely identical with those of Lapland, but nowhere found in the intervening plains. On
the summit of the White Mountains, in the United States, every plant is identical with spe-
cies growing in Labrador. In these cases all ordinary means of transport fail. Most of the
plants have heavy seeds, which could not possibly be carried such immense distances by the
wind; and the agency of birds in so effectually stocking these Alpine heights is equally out
of the question. The difficulty was so great, that some naturalists were driven to believe that
these species were all separately created twice over on these distant peaks. The determina-
tion of a recent glacial epoch, however, soon offered a much more satisfactory solution, and
one that is now universally accepted by men of science. At this period, when the mountains
of Wales were full of glaciers, and the mountainous parts of Central Europe, and much of
America north of the great lakes, were covered with snow and ice, and had a climate resem-
bling that of Labrador and Greenland at the present day, an Arctic flora covered all these re-
gions. As this epoch of cold passed away, and the snowy mantle of the country, with the gla-
ciers that descended from every mountain summit, receded up their slopes and towards the
North Pole, the plants receded also, always clinging as now to the margins of the perpetual
snow line. Thus it is that the same species are now found on the summits of the mountains
of temperate Europe and America, and in the barren north-polar regions.
