The Strange Adventures of a PebbleHawksworth, Hallam
Science
The Strange Adventures of a Pebble
Hawksworth, Hallam
Geology -- Juvenile literature; Physical geography -- Juvenile literature
[Footnote 19: Did you suspect the giants of this chapter were our old
friends the glaciers of the Ice Age, when I first began talking about
them?]
When the geologists first began digging into these hills they not only
found them as full of pebbles as a Christmas pudding is full of plums,
but the pebbles were of all kinds--sandstone, limestone, slate, granite.
JACK FROST DIDN'T DO IT!
"These different pieces of stone didn't come from the breaking up by
frost of the rock beds on which we now find them," said Some Wise Man,
"for then they would all have been of the same kind of rock."
"And besides," said Some Wise Man No. 2, "they would not have been
shaped into pebbles with the edges rounded off, as all pebbles are by
the waves of lakes or the sea or the water of flowing streams. So these
pebbles must have come from somewhere else."
"Yes, and a long way off," remarked Some Wise Man No. 3; "for look,
there aren't any rock beds anywhere around here from which some of
these pebbles could have been made."
"True enough," said Wise Man No. 4, "and I know what brought these
little foreigners. It was a great flood; for water moves not only
pebbles and clay, but, in times of flood, good-sized cobblestones."
WHAT IS MEANT BY THE "DRIFT" THEORY
So, for a long time, it was believed that the material in these hills
was drifted in by the waters. This was called the "drift" theory, and,
although it is now known that this theory was not the true one, such
heaps of clay and stones are still called "drift."
But the learned men kept on digging into the question and into the
hills, and finally more things were observed.
"Did you notice this?" said one. "The material is not separated into
layers and divided up into coarse, finer, finest as the sediment of
pebbles, sand, and mud is separated and divided when it settles along
shores. These pebbles, this sand and clay, are all mixed up."
"Look at this, will you?" (Here imagine a Learned Somebody picking
up a pebble with a scratched face like mine.) "Water never scratched
anything like that. Here are a lot more of these pebbles, all with
their faces scratched."
"And just see how all these scratched pebbles have flat faces," cried
another of these famous grown-up boys in these great field excursions.
"It looks to me as if they had been ground against something
hard--another rock, say; and for a long time."
HOW THE QUESTION WAS FINALLY SETTLED
Well, to make a long story short, they found that the glaciers of
the Ice Age, those great bodies of flowing ice, were the only things
that could have brought all this material together from such widely
separated regions (as shown by the different kinds of pebbles), and
left them all mixed up as they were; and the faces of many pebbles
scratched and flattened where they had been ground along.
Public-domain text, read in full here on John Shaqi.
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