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Updated: May 3, 2025
He took my hand and encouraged me, and I heard him murmur, "Oh! if I could only not breathe, so as to leave more air for my master!" Tears came into my eyes on hearing him speak thus. If our situation to all was intolerable in the interior, with what haste and gladness would we put on our cork-jackets to work in our turn! Pickaxes sounded on the frozen ice-beds.
Considered in connection with their subsequent work together in the ancient ice-beds and moraines of England, Scotland, Ireland, and Wales, it is curious to find Buckland answering: "I am sorry that I cannot entirely adopt the new theory you advocate to explain transported blocks by moraines; for supposing it adequate to explain the phenomena of Switzerland, it would not apply to the granite blocks and transported gravel of England, which I can only explain by referring to currents of water."
Lay minds conceive of these great ice-beds of transformed snow as inert, immovable bodies. They think the snow lies upon the surface of the rocks or earth. The scientific observer knows better. By the very inertia of its own vast and almost inconceivable weight the glacier is compelled to move.
Snow thus packed together soon changes its character. From the light airy flake, it becomes, in masses, what the geologists term névé. This is a granular snow, intermediate between snow and ice. A little lower down this névé is converted into true glacial ice-beds, which grow longer, broader, deeper and thicker as the névé presses down from above.
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