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where modern operations have obliterated them, such they continue to the present time. Beyond the inference of remote antiquity, which we naturally draw from the fact of their presenting no trace of the use of any kind of machinery, or of gunpowder, or the display of any mining skill, we may cite the unanimous opinion of the neighbourhood, that they owe their origin to the predecessors of that peculiar order of operatives known as "the free miners of the Forest of Dean;" a view which is confirmed by the authentic history of the district. But the numerous Roman relics found deeply buried in the prodigious accumulations of iron cinders, once so abundant here as to have formed an important part of the materials supplied to the furnaces of the Forest, afford proof that the iron-mines were in existence as early as the commencement of the Christian era; so that the openings we now see are the results of many centuries of mining operations, with which their extent, number, and size perfectly accord. [Picture: The Devil's Chapel] These mines present the appearance either of spacious caves, as on the Doward Hill, or at the Scowles near Bream, or they consist of precipitous and irregularly shaped passages, left by the removal of the ore or mineral earth wherever it was found, and which was followed in some instances for many hundreds of yards, openings being made to the surface wherever the course of the mine permitted, thus securing an efficient ventilation, so that although they have been so long deserted the air in them is perfectly good. They are also quite dry, owing probably to their being drained by the new workings adjacent to them, and descending to a far greater depth. In the first instance they were no doubt excavated as deep as the water permitted, that is, to about 100 feet, or in dry seasons even lower, as is in fact proved by the water-marks left in some of them. Occasionally they are found adorned with beautiful incrustations of the purest white, formed by springs of carbonate of lime, originating in the rocky walls of limestone around. Sometimes, after proceeding a considerable distance, they suddenly open out into spacious vaults fifteen feet in width, the site probably of some valuable "pocket" or "churn" of ore; and then again, where the supply was less abundant, narrowing into a width hardly sufficient to admit the human body. Occasionally the passage divides and unites again, o
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