In 1842, that is, after the interval of seven
years, they mustered only fifty-four individuals; and, while
each family of the interior of New South Wales, uncontaminated
by contact with the whites, swarms with children, those
of Flinders' Island had during eight years an accession of
only fourteen in number!"
The Beagle stayed here ten days, and in this time I made
several pleasant little excursions, chiefly with the object of
examining the geological structure of the immediate
neighbourhood. The main points of interest consist, first in
some highly fossiliferous strata, belonging to the Devonian or
Carboniferous period; secondly, in proofs of a late small rise
of the land; and lastly, in a solitary and superficial patch of
yellowish limestone or travertin, which contains numerous
impressions of leaves of trees, together with land-shells, not
now existing. It is not improbable that this one small quarry
includes the only remaining record of the vegetation of Van
Diemen's Land during one former epoch.
The climate here is damper than in New South Wales,
and hence the land is more fertile. Agriculture flourishes;
the cultivated fields look well, and the gardens abound with
thriving vegetables and fruit-trees. Some of the farm-houses,
situated in retired spots, had a very attractive appearance.
The general aspect of the vegetation is similar to
that of Australia; perhaps it is a little more green and
cheerful; and the pasture between the trees rather more
abundant.