Thus the chalk is no unimportant element in the masonry of the earth's
crust, and it impresses a peculiar stamp, varying with the conditions to
which it is exposed, on the scenery of the districts in which it occurs.
The undulating downs and rounded coombs, covered with sweet-grassed
turf, of our inland chalk country, have a peacefully domestic and
mutton-suggesting prettiness, but can hardly be called either grand
or beautiful. But on our southern coasts, the wall-sided cliffs, many
hundred feet high, with vast needles and pinnacles standing out in
the sea, sharp and solitary enough to serve as perches for the wary
cormorant confer a wonderful beauty and grandeur upon the chalk
headlands. And, in the East, chalk has its share in the formation of
some of the most venerable of mountain ranges, such as the Lebanon.
What is this wide-spread component of the surface of the earth? and
whence did it come?
You may think this no very hopeful inquiry. You may not unnaturally
suppose that the attempt to solve such problems as these can lead to
no result, save that of entangling the inquirer in vague speculations,
incapable of refutation and of verification.
If such were really the case, I should have selected some other subject
than a "piece of chalk" for my discourse. But, in truth, after much
deliberation, I have been unable to think of any topic which would so
well enable me to lead you to see how solid is the foundation upon which
some of the most startling conclusions of physical science rest.
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