The Lake-Dwellings of Europe: Being the Rhind Lectures in Archæology for 1888Munro, Robert
History
The Lake-Dwellings of Europe: Being the Rhind Lectures in Archæology for 1888
Munro, Robert
Lake-dwellers and lake-dwellings -- Bibliography; Lake-dwellers and lake-dwellings -- Europe
Interest in the whole subject now rapidly increased, and extended to
agriculturists and local observers. Yearly excavations were carefully
scanned and even special researches were carried on in the interests
of science. Strobel, a professed naturalist with remarkably precise
and accurate habits, devoted his great energies to the elucidation
of the organic remains, especially the rich and varied products of
the peaty bed (_terra uliginosa_) at Castione, in which the piles
were detected. Pigorini, on the other hand, was an archæologist pure
and simple, but endowed with great ability and much fertility in the
correlation and generalisation of facts--qualities which have since
gained him the chair of archæology at Rome, which he now fills with so
much distinction. Thus associated these two men may be said to have
developed a new school of archæology, especially anent the terremare,
having as its primary and indispensable object the collection of
authenticated data, without which, they asserted, no deductions
however brilliant could be scientific.
In the course of researches conducted by Strobel at Castione, during
the years 1862 and 1863, he observed that the piles were placed in
a sort of basin, either natural or artificial; that they supported
transverse beams over which clay floorings had been placed; and that
they were more thickly set towards the margin, and slanting, as if to
strengthen the inner superstructures. Moreover, he proved that the
supposed peaty formation (_terra uliginosa_) had nothing in common
with true peat, but was simply a subaqueous deposit of ordinary
earth, associated with decomposed organic _débris_. Another terramara
in Parma having similar characteristics to that at Castione was
investigated in the following year by Pigorini, and thus the theory of
an occasional palafitte converted into a land-dwelling seemed to them
to be confirmed. Previous to this the stratification of the beds--one
of the most remarkable features of these deposits--had not excited any
unusual surprise, but now it began to be commented upon.
Public-domain text, read in full here on John Shaqi.
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