when their flow is slackened on entering the still water the materials
they bring down with them sink and are spread out in layers over the
bottom. The structure of the sandstones and shales shows that they were
formed in this way; they often inclose the remains of plants that have
been carried down from land, and occasionally of animals that lived in
the water where they were deposited.

The next we have to consider is limestone, which is mainly made up of a
substance known to chemists as calcium carbonate, or carbonate of lime.

In some districts, especially in volcanic countries, springs occur very
highly charged with carbonate of lime. The warm springs of Matlock are
a case in point; they are probably the last vestige of volcanic action
which was in operation in that neighborhood during carboniferous times.
Limestone is chiefly formed by the agency of small marine creatures of
low organization. By the aid of these animals the carbonate of lime is
brought back to a solid form; at their death their hard parts fall to
the bottom and accumulate in a mass of pure limestone, which afterward
becomes solidified into limestone rock.

The information that limestone gives us is this:

When we find, as is often the case, a mass of limestone hundreds of feet
thick, and composed of little else but carbonate of lime, we know that
the spot where it occurs was, at the time it was formed, far out at sea,
covered by the clear water of mid ocean; and when we find that this
limestone grows in certain directions earthy and impure, and that layers
of shale and sandstone, thin at first, but gradually thickening out in
a wedge-shape form, come in between its beds, we know that in those
directions we are traveling toward the shore lines of that sea whence