Beach Rambles in Search of Seaside Pebbles and Crystals: With Some Observations on the Origin of the Diamond and Other Precious StonesFrancis, John George
Science
Beach Rambles in Search of Seaside Pebbles and Crystals: With Some Observations on the Origin of the Diamond and Other Precious Stones
Thus, between tide-waves and currents, changes are going on continually
both in the volume and the physical constitution of the sea-water.
And this, which might at first on a hasty glance look like casual and
unimportant variation, when we come to consider it attentively, is found
to be an arrangement fraught with wisdom and beneficence; for it insures
continual variations of temperature, it attracts the purifying storms,
restores the elastic spring of the atmosphere, and provides for weary
man a healthy tonic breeze when he rambles along the beach or scales the
face of the cliff. Without the motion imparted by the tides, the sea
would probably become putrid. Now the tides depend upon the MOON; yet
how seldom do we think of her invaluable services, when we gaze upon her
pale face! An Italian once told me that he “loved the moon, adored the
moon, never tired of looking at the moon.” And the Padishah,[4] I have
heard say, prefers “moon-faced” ladies for his soft companions; but I
doubt whether either the pensive Italian or the glittering lord of the
Bosphorus ever bestowed five minutes’ thought on the mighty phenomenon of
the TIDES.
There are other changes in what may be termed the tidal “high-water
mark,” due to the lapse of ages, which the sea has chronicled on the face
of many a shore and cliff. It is well known that the coast-line, in this
and other countries, has experienced many alterations as to its level. In
some places, the ocean has apparently encroached upon the land; in many
others, it has receded. One striking _index_ of this latter, and which
may be implicitly trusted as proving the fact, occurs where the waters
have retired from their former level, and have left exposed to view the
remains of an ancient _beach_. Thus, between Brighton and Ovedean, is
found what goes by the name of the “Elephant-bed,” because such fossil
bones lie among the pebbles in this part of the cliff. The entire stratum
undoubtedly was at one time a beach. Similar phenomena have been traced
along the coast-lines of Arbroath and Cromarty shires.
Elsewhere, the sea has gained upon the land; undermining the friable
sandstone cliffs, and, as it were, melting down the headlands, so as to
change the outline of the coast. But in these latter instances, although
“terra firma” has given way, it may be doubted whether the water itself
has _risen_. Wherever it has indubitably done so, to the extent _e.g._ of
submerging a village, I should apprehend the presence of volcanic agency.
[4] Sultan, “Father of the Faithful.”
CHAPTER IX.
GEOLOGY LIES AT THE BOTTOM OF EARTHLY THINGS.
There seems to be no strong reason for doubting that every elementary
substance of which we have any knowledge was _separated_ at the first
from that crude mass called “the earth,” and which, along with “the
heaven,” God created in the beginning.
Public-domain text, read in full here on John Shaqi.
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