The Fairy-Land of Science
These stones are being continually, though slowly, conveyed by the glacier, from all the mountains along its sides, down to the place where it melts. Here it lets them fall, and they are gradually piled up till they form great walls of stone, which are called moraines. Some of the moraines left by the larger glaciers of olden time, in the country near Turin, form high hills, rising up even to 1500 feet.
Therefore, if ice did no more than carry these stone blocks, it would alter the face of the country ; but it does much more than this. As the glacier moves along, it often cracks for a considerable way across its surface, and this crack widens and widens, until at last it becomes a great gaping chasm, or crevasse as it is called, so that you can look down it right to the bottom of the glacier. Into these crevasses large blocks of rock fall, and when the chasm is closed again as the ice presses on, these masses are frozen firmly into the bottom of the glacier, much in the same way as a steel cutter is fixed in the bottom of a plane. And they do just the same kind of work ; for as the glacier slides down the valley, they scratch and grind the rocks underneath them, rubbing themselves away, it is true, but also scraping away the ground over which they move. In this way the glacier becomes a cutting instrument, and carves out the valleys deeper and deeper as it passes through them.
You may always know where a glacier has been, even if no trace of ice remains ; for you will see rocks with scratches along them which have been cut by these stones ; and even where the rocks have not been ground away, you will find them rounded like those in the left-hand of the Frontispiece, showing that the glacier-plane has been over them. These rounded rocks are called roches moutonnees," because at the distance they look like sheep lying down.
You have dnly to look at the stream flowing from the mouth of a glacier to see what a quantity of soil it has ground off from the bottom of the valley ; for the water is thick, and coloured a deep yellow by the mud it carries. This mud soon reaches the rivers into which the streams run ; and such rivers as the Rhone and the Rhine are thick wath matter brought down from the Alps. The Rhone leaves this mud in the Lake of Geneva, flowing out at the other end quite clear and pure. A mile and a half of land has been formed at the head of the lake since the time of the Romans by the mud thus brought down from the mountains.
Thus we see that ice, like water, is always busy carving out the surface of the earth, and sending down m.aterial to make new land elsewhere. We know that in past ages the glaciers were much larger than they are in our time ; for we find traces of them over large parts of Switzerland where glaciers do not now exist, and huge blocks which could only have been carried by ice, and which are called erratic blocks," some of them as big as cottages, have been left scattered over all the northern part of Europe. These blocks were a great puzzle to scientific men till, in 1840, Professor Agassiz showed that they must have been brought by ice all the way from Norway and Russia.
In those ancient days, there were even glaciers in England ; for in Cumberland and in Wales you may see their work, in scratched and rounded rocks, and the moraines they have left. Llanberis Pass, so famous for its beauty, is covered with ice-scratches, and blocks are scattered all over the sides of the valley. There is one block high up on the right-hand slope of the valley, as you enter from the Beddgelert side, which is exactly poised upon another block, so that it rocks to and fro. It must have been left thus balanced when the ice melted round it. You may easily see that these blocks were carried by ice, and not by water, because their edges are sharp, whereas, if they had been rolled in water, they would have been smoothed down.
We cannot here go into the history of that great Glacial Period long ago, when large fields of ice covered all the north of England ; but v/hen you read it for yourselves and understand the changes on the earth's surface which we can see being made by ice now, then such grand scenery as the rugged valleys of Wales, with large angular stone blocks scattered over them, will tell you a wonderful story of the ice of bygone times.
And now we have touched lightly on the chief ways in which water and ice carve out the surface of the earth. We have seen that rain, rivers, springs, the waves of the sea, frost, and glaciers all do their part in chiselling out ravines and valleys, and in producing rugged peaks or undulating plains — here
cutting through rocks so as to form precipitous cliffs, there laying down new land to add to the flat country — in one place grinding stones to powder, in others piling them up in gigantic ridges. We cannot go a step into the country without seeing the work of water around us ; every little gully and ravine tells us that the sculpture is going on ; every stream, with its burden of visible or invisible matter, reminds us that some earth is being taken away and carried to a new spot. In our little lives we see indeed but very small changes, but by these we learn how greater ones have been brought about, and how we owe the outline of all our beautiful scenery, with its hills and valleys, its mountains and plains, its cliffs and caverns, its quiet nooks and its grand rugged precipices, to the work of the Two great sculptors, Water and Ice."
<!-- pandi-media-anchor:figure-p137-o40-06a09a07b193dab3 -->Lecture VI. The Voices of Nature and How We Hear Them
We have reached to-day the middle point of our course, and here we will make a new start. All the wonderful histories which we have been studying in the last five lectures have had
<!-- pandi-media-anchor:figure-p138-o41-846464fd2aa36d9c -->little or nothing to do with living creatures. The sunbeams would strike on our earth, the air would move restlessly to and fro, the water-drops would rise and fall, the valleys and ravines would still be cut out by rivers, if there were no such thing as life upon the earth. But without living things there could be none of the beauty which these changes bring about. Without plants, the sunbeams, the air and the water would be quite unable to clothe the bare rocks, and without animals and man they could not produce light, or sound, or feeling of any kind.
In the next five lectures, however, we are going to learn something of the use living creatures make of the earth ; and to-day we will begin by studying one of the ways in which we are affected by the changes of nature, and hear her voice.
We are all so accustomed to trust to our sight to guide us in most of our actions, and to think of things as we see them, that we often forget how very much we owe to sound. And yet Nature speaks to us so much by her gentle, her touching, or her awful sounds, that the life of a deaf person is even more hard to bear than that of a blind one.
Have you ever amused yourself with trying how many different sounds you can distinguish if you listen at an open window in a busy street i You will probably be able to recognize easily the jolting of the heavy waggon or dray, the rumble of the omnibus, the smooth roll of the private carriage and the rattle of the light butcher's cart ; and even while you are listening for these, the crack of the carter's whip, the cry of the costermonger at his stall, and the voices of the passers by will strike upon your ear. Then if you give still more close attention you will hear the doors open and shut along the street, the footsteps of the passengers, the scraping of the shovel of the mud-carts ; nay, if he happen to stand near, you may even hear the jingling of the shoeblack's pence as he plays pitch and toss upon the pavement. If you think for a moment, does it not seem wonderful that you should hear all these sounds so that you can recognize each one distinctly while all the rest are going on around you ?
But suppose you go into the quiet country. Surely there will be silence there. Try some day and prove it for yourself, lie down on the grass in a sheltered nook and listen attentively. If there be ever so little wind stirring you will hear it rustling gently through the trees ; or even if there is not this, it will be strange if you do not hear some wandering gnat buzzing, or some busy bee humming as it moves from flower to flower. Then a grasshopper will set up a chirp within a few yards of you, or, if all living creatures are silent, a brook not far off* may be flowing along with a rippling musical sound. These and a hundred other noises you will hear in the most quiet country spot ; the lowing of cattle, the song of the birds, the squeak of the field-mouse, the croak of the frog, mingling with the sound of the woodman's axe in the distance, or the dash of some river torrent. And besides these quiet sounds, there are still other occasional voices of nature which speak to us from time to time. The howling of the tempestuous wind, the roar of the sea-weaves in a storm, the crash of thunder, and the mighty noise of the falling avalanche ; such sounds as these tell us how great and terrible nature can be.
Now, has it ever occurred to you to think what sound is, and how it is that we hear all these things ? Strange as it may seem, if there were no creature that could hear upon the earth, there would be no such thing as sound, though all these movements in nature were going on just as they are now.
Try and grasp this thoroughly, for it is difficult at first to make people believe it. Suppose you were stone-deaf, there would be no such thing as sound to you. A heavy hammer falling on an anvil would indeed shake the air viv lently, but since this air when it reached your ear would find a useless instrument, it could not play upon it. And it is this play on the djntm of your ear a7td the nerves within it speaking to your brain which makes sound. Therefore, if all creatures on or around the earth were without ears or nerves of hearing, there would be no instruments on which to play, and consequently there would be no such thing as sound. This proves that two things are needed in order that we may hear. First, the outside movement which plays on our hearing instrument ; and, secondly, the hearing instrument itself.
First, then, let us try to understand what happens outside our ears. Take a poker and tie a piece of string to it, and holding the ends of the string to your ears, strike the poker against the fender. You will hear a very loud sound, for the blow will set all the particles of the poker quivering, and this movement will pass right along the string to the drum of your ear and play upon it.