Nature readers : $b Sea-side and way-side. No. 4Wright, Julia McNair
Science
Nature readers : $b Sea-side and way-side. No. 4
Wright, Julia McNair
Nature study -- Juvenile literature; Readers
We now find about us tree-ferns, club-mosses, reeds, calamites,
lichens. There are fishes swarming in the warm seas; a few insects and
spiders crawl among the ferns; here and there are toads, newts, and
scorpions of curious patterns. One, two, three, four, five ages back
we wander, and now the mosses and pines, the fishes and reptiles have
disappeared, and we are in the age of sea-weeds and corals, crabs and
mollusks, such as have few types in the modern world. And here, in the
lower-Silurian, we have arrived at our ancient burial-ground. Have we
not come a long way to find it?
Is there no shorter way to reach it? We have come here by the every-day
style of a carriage over a few miles of plain and hill. We have come
here also by a dash in imagination through three great times and
thirteen busy ages of world-building. We can take yet a third way.
Go yonder to the valley and sink a shaft for seven hundred feet, and
you will pass through these ages and times and reach the era of this
burial-ground. There it is hidden seven hundred feet deep; here it
crops out into the sunshine; here have been tumult and convulsion, and
what in some places might be thousands of feet below the surface, is
here thrust up among modern methods, among apple trees, and bleating
sheep, and white cottages, and little children at their play.
There is still another method of reaching this same burial-ground. Go
into the valley and wander five miles toward the mouth of the little
creek that divides it. As you touch its grassy bank you stand in the
modern age of the present earth-building time. As you travel down
the creek, the successive beds or stages of earth-building are laid
bare, one after another, until at the end of five miles you stand on
the lower-Silurian stratum of this burial-ground. Take a pamphlet,
fold the first leaf over one half, the next a little less, and so on
for thirteen pages, and you have a pattern of the manner in which the
spring and autumn torrents flushing the brook have laid bare the rock
strata, and shown them as they lie here closely crowded upon each other.
This is, however, an unusual case, for each of these ages has in
many places left deposits thousands of feet in thickness. Here the
uncovering has been rapid, deposit light, and we can turn over the
geologic pages in a volume a few hundreds of feet thick.
Public-domain text, read in full here on John Shaqi.
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