The Cambridge natural history, Vol. 09 (of 10)Evans, A. H. (Arthur Humble)
Science
The Cambridge natural history, Vol. 09 (of 10)
Evans, A. H. (Arthur Humble)
Animals; Birds
It would at first seem from the above that the annual migratory movement
would be in a direction due north and south, or south and north, according
to season, and so in a general way it is; but there is no doubt that this
simple movement is disturbed by many causes, chief among which is possibly
the configuration of the land, which is found to give rise to considerable
deviations, and that to an extent which is at present very imperfectly
understood. It may be considered proved that the trend of a coast-line, the
course of a great river, or the intervention of a chain of mountains, has a
very appreciable effect on the direction taken by migrating Birds; but not
one of these, nor all in combination, affords a sufficient explanation of
all the deflexions, and will certainly not account for at least one
remarkable fact, as it may now be regarded–the tendency of many Birds in
Eastern Europe and part of Siberia to travel westward towards the close of
summer or in autumn. This is shewn in several ways, but in none better than
by the almost yearly occurrence in Britain at that season of examples of
species which breed only in the Russian Empire. For, admitting that such
examples are stray wanderers, which have lost their course, their
appearance here is still useful in indicating the existence of the westward
movement; and, with the evidence they furnish before us, we may judge
whence come vast numbers of others–Starlings, Crows, Rooks, Jays, Larks,
and what not, whose origin and starting-point it would be otherwise hard to
trace or even surmise. Much has been written, especially in Europe, on
so-called Lines of Flight, but as yet to little purpose, and indeed
{19}scarcely any writers on the subject have had sufficient _data_ to form
an hypothesis, so that it is not surprising that hardly any two agree in
theory.[10] In other parts of the world there is still less ground for
theorising, though in North America many valuable observations have been
made; and these, in conjunction with those carried on in Europe, will no
doubt in due time lead to satisfactory results as regards the Northern
Hemisphere. Concerning the Southern our ignorance is almost complete.
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