In shape, the Great Landes may be compared to an immense rectangular
triangle, having for its base the coast, which, from the mouth of the
Gironde to Bayonne, or for a length of more than sixty leagues, is
almost rectilineal. But they are separated from the sea by a long
parallel chain of lakes and water-courses--a waste of shallow pools--a
labyrinth of gulfs and morasses, and then by the continuous chain of the
Dunes, of which we shall speak in the following chapter.
That which is commonly called the Great Lande is bounded on the north by
the _étang_, or lake, of Cazau. It is a sandy, treeless plain, and upon
which, for a traject of several leagues from east to west, not one
habitation worthy of the name is perceptible until the traveller arrives
at Mimizan, near the southern point of the lake of Aureilhan. This lake
on the south-west pours its waters into the sea. To the north it
communicates, through the canal of St. Eulalie, with the lake of
Biscarosse, which is itself connected with that of Cazau. East of this
chain of lakes lies the Lande; west of it stretches the range of
_Dunes_, or sand-hills.
The lake or pool of Cazau is a small sea of fresh water, perfectly
clear, profoundly deep, and fourteen to fifteen thousand acres in
extent. It has its whirlwinds and its tempests, so that in certain
seasons it is perilous to embark on its surface. And were its banks
clothed with rich woods, or raised aloft in irregular or precipitous
cliffs, it would surely attract as great a throng of tourists as the
mountain-tarns and lochs of Scotland or Cumberland, or the Arcadian
waters of Northern Italy. The lake of Biscarosse, in form a triangle,
with one side formed by the Dunes, covers about twelve thousand acres.
It derives its name from a village situated at its northern angle, on
the bank of the canal which connects it with the lake of Cazau. The lake
of Aureilhan is the smallest of the three; the St. Eulalie canal, which
links it to the preceding, traverses a series of peat-bogs bounded
eastward by gloomy pine-forests, and westward by the interminable Dunes,
which, by arresting the flow of the rain-waters, have really created
these so-called lakes and extensive swamps. Enormous quantities of rain
fall every year in the Landes,--which district the Romans would
certainly have dedicated to Jupiter Pluvius,--and find beneath the thin
superficial stratum or crust of sand and earth, a sub-soil of _tufa_ and
_allios_--in other words, of compact chalk and sand agglutinated by a
ferruginous sediment. Frequently this _tufa_ possesses all the hardness
of stone, and its imperviousness is its fundamental property. Hence it
follows, that a portion of the heavy annual rainfall remains in the
receptacles provided by the hollows and depressions of the soil, and in
due time accumulates into marshes and lagoons, until gradually
evaporated by the heat of spring.
Public-domain text, read in full here on John Shaqi.
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