Some Salient Points in the Science of the EarthDawson, John William, Sir
Science
Some Salient Points in the Science of the Earth
Dawson, John William, Sir
Geology; Paleontology
crenulated by little rills running into them from the surface.
It is further to be noticed that all these markings and impressions
on tidal shores may, when covered by succeeding deposits, appear
either in intaglio or relief. On the upper surface they are of course
sunken, but on the lower surface of the bed deposited on them they are
in relief. It often happens also that these casts in relief are the
best preserved. This arises from the fact that the original moulds or
impressions are usually made in clay, whereas the filling material
is sandy, and the latter, infiltrated with calcareous or siliceous
matter, may become a hard sandstone, while the clay may remain a
comparatively soft shale. This tendency of casts rather than of moulds
to be preserved sometimes produces puzzling effects. A cylindrical
or branching trail thus often assumes the appearance of a stem, and
any pits or marginal impressions assume the form of projections or
leaves, and thus a trail of a worm or Gastropod or a rill mark may
easily simulate a plant. It is to be observed, however, that these
prominent casts are on the under side of the beds, that their material
is continuous with that of the beds to which they belong, and that
they are destitute of any carbonaceous matter. There are, however,
cases where markings may be in relief, even on the upper surfaces of
beds. The following are illustrations of this. Just as a man walking
in newly fallen snow compresses it under his feet, and if the snow be
afterwards drifted away or melted away by the sun, the compressed part
resists longest, and may appear as a raised footmark, so tracks made on
soft material may consolidate it so that if the soft mud be afterwards
washed away the tracks may remain projecting. Again, worms eject earthy
matter from their burrows, forming mounds, patches or raised ridges of
various forms on the surface, and some animals burrow immediately under
the surface, pushing up the mud over them into a ridge, while others
pile up over their bodies pellets of clay, forming an archway or tunnel
as they go. Zeiller has shown that the mole cricket forms curious
roofed trails of this kind, and it seems certain that Crustaceans and
marine worms of different kinds execute similar works, and that their
roofed burrows, either entire or fallen in, produce curious imitations
of branches of plants.
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