from the northern continent into the Mediterranean. It is formed
by the mountain-system of the Apennines branching off in a southern
direction from the western Alps. The Apennines take in the first
instance a south-eastern course between the broader gulf of the
Mediterranean on the west, and the narrow one on the east; and in the
close vicinity of the latter they attain their greatest elevation,
which, however, scarce reaches the line of perpetual snow, in
the Abruzzi. From the Abruzzi the chain continues in a southern
direction, at first undivided and of considerable height; after
a depression which formsa hill-country, it splits into a somewhat
flattened succession of heights towards the south-east and a more
rugged chain towards the south, and in both directions terminates
in the formation of narrow peninsulas.

The flat country on the north, extending between the Alps and the
Apennines as far down as the Abruzzi, does not belong geographically,
nor until a very late period even historically, to the southern land
of mountain and hill, the Italy whose history is here to engage
our attention. It was not till the seventh century of the city
that the coast-district from Sinigaglia to Rimini, and not till the
eighth that the basin of the Po, became incorporated with Italy.
The ancient boundary of Italy on the north was not the Alps but
the Apennines. This mountain-system nowhere rises abruptly into
a precipitous chain, but, spreading broadly over the land and
enclosing many valleys and table-lands connected by easy passes,
presents conditions which well adapt it to become the settlement of
man. Still more suitable in this respect are the adjacent slopes
and the coast-districts on the east, south, and west. On the
east coast the plain of Apulia, shut in towards the north by the
mountain-block of the Abruzzi and only broken by the steep isolated