Cleveland Moffett

Cleveland Moffett

Summary

Portrait of Cleveland Moffett Cleveland Moffett Into the Crater of a Volcano (1915)

Why is not the whole mountain melted, if there are wide-spread fires below? And if there are not wide-spread fires below, why does not the long, narrow tube cool off and become plugged with hardened lava and end its activity?
Dr. Day's theory is that the depths of a volcano like Kilauea are not hotter than the surface opening. On the contrary, he believes that they are much cooler than the surface, his idea being that one great source of volcanic heat, perhaps the chief source in most present-day volcanoes, is the reaction between gases set at liberty in the operation of the volcano.
Source: Wikisource

Portrait of Cleveland Moffett Cleveland Moffett Into the Crater of a Volcano (1915)

In other words, the gases must be secured before they had issued from the molten lake and suffered atmospheric contamination.
But how could this be done? How could these virgin gases be captured? What manner of gas-collector could be set up in the hot, poisonous crater two hundred feet below the rim? What metal would withstand the heat? Platinum, possibly, but platinum would let hydrogen filter through it, and would itself be eaten up by sulphur fumes. No wonder this problem of drawing off gases from a volcano's heart had never been solved.
Source: Wikisource

Portrait of Cleveland Moffett Cleveland Moffett Into the Crater of a Volcano (1915)

But why, we ask, are more gases set at liberty in the upper regions of a volcano than in the lower regions? It is a matter of pressure. These volcano gases are held in solution in the molten lava exactly as carbonic-acid gas is held in a siphon of water. They are quite inactive as long as the valve is closed, but let the valve be opened, let the balance of terrestrial forces be disturbed, and straightway with a lessening of pressure comes a bursting and bubbling forth of gases from earth or bottle.
Source: Wikisource

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