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pertschachtricht, a long cavern of the extent of five hundred and sixty feet, through which we toiled with a growing sense of weariness. We had now come to the top of the last and longest "slide" in the whole Durrnberg. It is called the Wolfdietrichberg-rolle, and is four hundred and sixty-eight feet long, carrying us two hundred and forty feet lower down into the mountain. We went down this "slide" with the alacrity of school-boys, one after another keeping the pot boiling, and all regulating our movements with great circumspection, for we knew that we had far to go and we could never see more than a few yards before us. Having gained the ground beneath in safety, our attention was drawn to a fresh water well or spring, sunk in this spot at great cost by order of the Archduke, and blessed among miners. Amid all the stone and salt and brine, a gush of pure fresh water at our feet was very welcome to us all. The well was sunk, however, to get water that was necessary for the mining operations. We did not see any of those operations underground, for they are not exhibited; the show-trip underground is only among the ventilating shafts and galleries. Through the dark openings by which we had passed, we should have found our way (had we been permitted) to the miners. I have seen them working in the Tyrol, and their labours are extremely simple. Some of the rock-salt is quarried in transparent crystals, which undergo only the process of crushing before they are sent into the market as an article of commerce. Very little of this grain salt is seen in England, but on the continent it may be found in some of the first hotels, and on the table of most families. It is cheaper than the loaf salt, and is known in Germany under the title of _salzkorn_, and in France, as _selle de cuisine_. In order to obtain a finer grained and better salt, it is necessary that the original salt-crystals should be dissolved, and for this purpose parallel galleries are run into the rock, and there is dug in each of them a dyke or cistern. These dykes are then flushed with water, which is allowed to remain in them undisturbed for the space of from five to twelve months, according to the richness of the soil; and, being then thoroughly saturated with the salt that it has taken up, the brine is drawn off through wooden pipes from Hallein over hill and dale into the evaporating pans. We had traversed the last level, and had reached what is
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