in Derbyshire, over the top of High Craven and Whernside and Pen-y-
gent and Cross Fell, and to paddle too over the Cheviot Hills, which part
England and Scotland." I know it, my child, I know it. But so it was
once on a time. The high limestone mountains which part Lancashire and
Yorkshire--the very chine and backbone of England--were once coral-reefs
at the bottom of the sea. They are all made up of the carboniferous
limestone, so called, as your little knowledge of Latin ought to tell
you, because it carries the coal; because the coalfields usually lie upon
it. It may be impossible in your eyes: but remember always that nothing
is impossible with God.

But you said that the coal was made from plants and trees, and did plants
and trees grow on this coral-reef?

That I cannot say. Trees may have grown on the dry parts of the reef, as
cocoa-nuts grow now in the Pacific. But the coal was not laid down upon
it till long afterwards, when it had gone through many and strange
changes. For all through the chine of England, and in a part of Ireland
too, there lies upon the top of the limestone a hard gritty rock, in some
places three thousand feet thick, which is commonly called "the
mill-stone grit." And above that again the coal begins. Now to make
that 3000 feet of hard rock, what must have happened? The sea-bottom
must have sunk, slowly no doubt, carrying the coral-reefs down with it,
3000 feet at least. And meanwhile sand and mud, made from the wearing
away of the old lands in the North must have settled down upon it. I say
from the North--for there are no fossils, as far as I know, or sign of
life, in these rocks of mill-stone grit; and therefore it is reasonable
to suppose that they were brought from a cold current at the Pole, too
cold to allow sea-beasts to live,--quite cold enough, certainly, to kill
coral insects, who could only thrive in warm water coming from the South.

Then, to go on with my story, upon the top of these mill-stone grits came
sand and mud, and peat, and trees, and plants, washed out to sea, as far
as we can guess, from the mouths of vast rivers flowing from the West,
rivers as vast as the Amazon, the Mississippi, or the Orinoco are now;
and so in long ages, upon the top of the limestone and upon the top of
the mill-stone grit, were laid down those beds of coal which you see
burnt now in every fire.

But how did the coral-reefs rise till they became cliffs at Bristol and
mountains