The World of Ice by R. M. (Robert Michael) Ballantyne
page 64 of 284 (22%)
page 64 of 284 (22%)
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preparations for the next--"Mr. Saunders, sir, can you _h_inform me,
sir, 'ow it is that the sea don't freeze at 'ome the same as it does _h_out 'ere?" The countenance of the second mate brightened, for he prided himself not a little on his vast and varied stores of knowledge, and nothing pleased him so much as to be questioned, particularly on knotty subjects. "Hem! yes, Mivins, I can tell 'ee that. Ye must know that before fresh water can freeze on the surface the whole volume of it must be cooled down to 40 degrees, and _salt_ water must be cooled down to 45 degrees. Noo, frost requires to be very long continued and very sharp indeed before it can cool the deep sea from the top to the bottom, and until it is so cooled it canna freeze." "Oh!" remarked Mivins, who only half understood the meaning of the explanation, "'ow very _h_odd. But can you tell me, Mr. Saunders, 'ow it is that them 'ere _h_icebergs is made? Them's wot I don't comprehend no'ow." "Ay," replied Saunders, "there has been many a wiser head than yours, puzzled for a long time about icebergs. But if ye'll use yer eyes you'll see how they are formed. Do you see the high cliffs yonder away to the nor'-east? Weel, there are great masses o' ice that have been formed against them by the melting and freezing of the snows of many years. When these become too heavy to stick to the cliffs, they tumble into the sea and float away as icebergs. But the biggest bergs come from the foot of glaciers. You know what glaciers are, Mivins?" "No, sir, I don't." |
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