The Romance of Modern Geology: Describing in simple but exact language the making of the earth with some account of prehistoric animal life — John Shaqi
The Romance of Modern Geology: Describing in simple but exact language the making of the earth with some account of prehistoric animal lifeGrew, Edwin Sharpe
Science
The Romance of Modern Geology: Describing in simple but exact language the making of the earth with some account of prehistoric animal life
Grew, Edwin Sharpe
Geology; Paleontology
In dry countries, especially in the large tracts of Central Asia
and of Africa, the air is often so thick with a fine yellow dust
that the sun's light struggles through it as through a London fog.
The dust settles on everything, and after many centuries a deposit,
which may be hundreds of feet deep, is thus accumulated on the
surface of the land. Some of the ancient cities of the old world,
Nineveh and Babylon for example, after being long abandoned by man,
have gradually been buried under the fine soil which the wind blew
over them. Even in England the Roman town of Silchester, not far
from Reading, after falling into decay when its inhabitants left it,
has been buried under the accumulations of two thousand years, and
its walls and floors now lie underground and have to be carefully
unearthed in order to lay them bare. But we need not seek these
exceptional cases in order to perceive what the wind is doing with
sand and the fine dust of the earth's uppermost layers. At many
places round the coast are sand-dunes. On sandy shores, exposed
to the winds that blow off the sea, the sand is dried and carried
away from the beach, gathering into long mounds or ridges which run
parallel to the coast-line. These ridges are often fifty or sixty
feet, sometimes even more than 250 feet high, with deep troughs and
irregular hollows between them, and they sometimes form a strip
several miles broad bordering the sea. These sand-hills creep
farther inland, till their progress is stopped by the fields or woods
they encounter, or till, by seeds finding a root, vegetation springs
up on them and they harden and consolidate under the influence of
their own vegetation and move inland no farther. But in many parts of
Western Europe and Eastern America the dunes are marching inland at
the rate of twenty feet a year. Off the coast of Friesland and North
Germany the danger has grown so threatening that scientific attention
has been given to the problem; and the German scientific men have
employed ingenious devices of planting wind-stakes--something like
the wooden breakwaters that are to be found along every seaside
beach, but arranged at different angles,--of forcing the sand-dune
to heap itself up so as to form an obstruction to further arrivals;
or of sowing those plants in the sand that will bind its particles
together, in order to preserve the land from further invasion.
[Illustration:
_Stereo Copyright, Underwood & U._ _London and New York_
A Curious Rock greatly revered by the Natives
This is the Dance Rock of the Walpi Indians of Arizona. Its curious
shape is the result of weathering.]
Public-domain text, read in full here on John Shaqi.
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