146 RDINBURGH PAST AND PRESENT.
very nature of the materials on which the history is founded, imperfection of
this kind cannot but prevail. These materials consist mainly of the sand, mud,
and gravel of ancient sea-floors, lake-bottoms, and river-beds, which have been
buried under later accumulations, and have been subsequently elevated into
land. Seldom did these sediments enclose a tolerably complete record of
the plants and animals and the physical changes of the time. Seldom, too,
have they remained without suffering much from the forces which have broken
them up from below and worn them away above.
It is the task of the geologist to put together the fragmentary evidence to
the best of his ability, not attempting to supply blanks where he can find no
information, but leaving them to be filled in, if possible, from subsequent research.
He is in the habit of arranging the order of events in the past
history of the earth under three great divisions of geological time-(r.) Primary
or Pakozoic; (2:) Secondary or Mesozoic j (3.) Tertiary or Cainozoic; to which
latter a subsidiary section, (4.) Post-Tertiary or Recent, is appended. The
fragmentary nature of the materials for unravelling the geological history
of the.district around the Scottish metropolis may be inferred from the fact
that they relate only to some of the later parts of the first, and (with trifling
fragments of the third) to some of the more marked events in the fourth of
these sections. The Engraving fronting the first page of this paper shows
the order and relation of the rocks of the neighbourhood of Edinburgh,
as they would appear if we could form a huge pillar of them, having the
oldest at the bottom and the youngest at the top.
Let us throw the scattered facts into the form of a narrative, and trace as
succinctly as may be the successive changes of which this part of the country
has been the scene. ’
The first picture we can draw is that of the bottom of a sea which seems
to have stretched not bnly over the site of Britain, but over most of Europe,
and to have covered alqo much of what is now land in both hemispheres.
The sand, mud, and gravel deposits of that ancient ocean, laid down continuously
above each other, layer upon layer, to a depth of many thousand
feet, form the materials of which the pastoral hills of the south of Scotland
and the mountains and glens of the Highlands are mainly composed, When
the visitor to Edinburgh looks south-eastward, he sees as the boundary of the
landscape, the blue outline of the chain of heights which stretch from Lammermuir
into Peeblesshire. These distant bounding hills are portions of the
hardened and upraised sediments of this early sea-bottom. Wandering among
them, we observe how the bare rock come to the surface. We split them open,
