The Continental Monthly, Vol. 5, No. 4, April, 1864 — John Shaqi
The Continental Monthly, Vol. 5, No. 4, April, 1864Various
Religion
The Continental Monthly, Vol. 5, No. 4, April, 1864
Various
Literature, Modern -- 19th century -- Periodicals; United States -- Politics and government -- 19th century -- Periodicals
The main stream of the geological evidence of the antiquity of man tends
to one point, viz., _that man coexisted with the extinct animals_. There
are collateral branches of proof, but this is the main channel. The
remains of man and of man's works and the remains of extinct races of
animals lie side by side, and claim from the geologist the same meed of
antiquity. This is the burden of the book before us. We offer the reader
a brief outline of this evidence. In doing so, we will follow the order
of Sir Charles Lyell's work, and merely state the leading facts which
geological investigations have brought to light.
In the Danish islands there are deposits of peat from ten to thirty feet
thick, formed in the hollows or depressions of the northern drift or
bowlder formation. These beds of peat have been examined to the bottom,
and they reveal the history of vegetation in those localities, and the
contemporaneous history of human progress. Beginning at the top, the
explorer finds the first layers to contain principally the trunks of the
beech tree, along with implements and tools of wood and iron. Below
these is a deposit of oak trunks, with implements mainly of bronze.
Farther down still he finds the trunks of the _Pinus sylvestris_, or
Scotch fir, together with implements of stone. This clearly indicates
that in the lapse of centuries the pine was supplanted by the oak, and
the oak by the beech, and that man advanced contemporaneously from the
knowledge and use of stone implements to those of bronze and iron. Now
the known fact is that in the time of the Romans, as now, the Danish
isles were covered by magnificent beech forests, and that eighteen
centuries have done little or nothing toward changing the character of
the vegetation. How many centuries must have elapsed to enable the oak
to supplant the pine, and the beech to supplant the oak, can only be
vaguely conjectured. Yet the evidence is clear that man lived in those
old pine forests--leaving his implements of stone behind him, as he did
his tools of bronze and iron in the succeeding periods. Along the coast
of Denmark, also, are found shell mounds mixed with flint knives,
hatchets, etc., but never any tools of bronze or iron, showing that the
rude hunters and fishers who fed on the oyster, cockle, and other
mollusks, lived in the period of the Scotch fir, or, as it has been
called, the 'age of stone.'
In many of the Swiss lakes are found ancient piles driven into the
bottom, on which were once erected huts or villages, the lacustrine
abodes of man. This use of them is proved by the abundance of flint
implements and fragments of rude pottery, together with bones of
animals, which have been dredged up from among the piles. The implements
found belong to the 'age of stone,' or the period of the Scotch fir in
Denmark, and the bones of animals are all, with one exception, those of
living species.
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