2. What right the Government has to lease out these mines without incurring some obnoxious consequences to the leaseholder, or to other parties concerned.
The sulphur mines that are at the disposal of the Government[202] are those of “Reykjahlid,” “Kráfla-námar” (the mines of the Krafla mountain), and “Fremri-námar” (the mines farthest from the coast), but “Theistareykja-námar” (the mines of Theistareykir) have never been Government property, although they apparently are lying in the tract of which the above-mentioned Mr Lock has wished to take lease.
As it is well known, from the excellent essay by the Right Reverend Hannes Finnson, Bishop of Iceland (see “Rit hins islendska lærdómslista-fèlags”—the Works of the Icelandic Society of Learning and Arts—vol. iv., p. 29), Mr Paul Stigsson, superintendent or governor of Iceland, bought of the Thorsteinssons, so called, in the presence of Mr Hans Nilsson and Mr Hans Lauritsson, on the behalf of his Majesty Frederik II., the mines of which there is no question here, with the exception of the Theistareykja mines, or more properly speaking, the right of digging sulphur in these mines. This bargain was made at Eyjafjord on the 15th of August 1563, and the said Thorsteinssons gave up the sulphur-diggings in “Fremri-námar,” “Kráfla-námar,” and “Heidar-[203] (heath) námar;” but it is nowhere on record, that any land or ground for house-building and road-making has been comprised in this bargain. As it appears, the Government of his Majesty Frederik II. has thought it sufficient to acquire the monopoly of the sulphur that was to be found there, for, as it appears, there has, as a rule, never been lack of persons willing to dig out the sulphur and to carry it, like other merchandise, down to the sea-coast.
In this manner the above-mentioned mines were worked in the time of his Majesty Frederik II., and a great quantity of sulphur was dug up there. It is said that the profit has sometimes, in the said period, amounted to 10,000 rixdollars (or upwards of £1100), and that the total export of sulphur has gone up to about 200 commercial lasts (or 400 tons) a year.
In the time of Christian IV. the working of the mines, which had answered so well in the time of his father, was almost discontinued; and the attempts of this king to let the mines, for a period of fifteen years, to Mr Jorgen Brochenhuus, of Wolderslev, and Mr Svabe, proved a complete failure. Thus, in the time of Christian IV., the mines were of little consequence for the Government and the country. This, the Right Reverend Hannes Finnson says, was a great drawback for the Danes, as it caused the scarcity of powder, which was one of the reasons why the Danes were defeated by the Swedes in Holstein in 1644.
Shortly after the middle of the seventeenth century, or in the year 1665, a certain “assessor,” Gabriel Marsilius by name, acquired a concession of digging sulphur and exporting it from Iceland; and it is said that he has exported from here a very great quantity of sulphur with considerable profit. Since that time, or since 1676, little is said of the sulphur-mining in Iceland until the first part of the eighteenth century; then, in 1724, two foreigners, Mr Sechmann and Mr Holtzmann, acquired a concession of exporting sulphur from Iceland; and it is said that they exported a great quantity of sulphur for a period of five years; but this export was again discontinued, owing to the death of Mr Holtzmann, who was the leader of the business, and to the apparent unwillingness of Mr Sechmann to repair to Iceland.
In the year 1753 the sulphur-mining was recommenced in Iceland by the Government. First it was commenced in the south, and afterwards, or in 1761, in the north (see “Eptirmæli 18 aldar”—“Review of the Events of the Eighteenth Century”). The author of this work, the late Mr Stephensen, says, that both the mines, the southern and northern, have been worked with considerable profit, adding, that the produce of the mines has amounted to 1400 rixdollars (or upwards of £155) a year; and in 1772 the profit of the sulphur mines in the north, according to the same author, was estimated at 1260 rixdollars (or about £140). After 1806 the Danish Government leased out the sulphur mines in the north to some merchants there for a trifling yearly rent, which in no way was a sufficient indemnity for the deterioration of the mines during the time of the lease.
For ten years ago it was a general opinion that the brimstone in the Icelandic sulphur mines for the most part was embedded in the layer that covers the “live mines,” and which must be considered a “sublimate” product of the so-called sulphur pits or caldrons; it had, however, been observed that in the “Fremri-námar,” so called, “dead mines” also existed where the sulphur stratum sometimes was a foot thick. The sulphur digging at Krisuvik last year has proved that these strata can be a good deal thicker, as it has also been ascertained that most sulphur mountains contain a considerable quantity of sulphur earth, clayish and ferruginous sulphur; all of which might yield from twenty-five to fifty per cent. of clean sulphur, if managed in the right manner.
When the three naturalists, Mr Steenstrup, Mr Schythe, and Jonas Hallgrimson, travelled through Iceland in 1840, they calculated that the sulphur mines in the north might yield 10,000 rixdollars a year; but Dr Hjaltalin, who, ten years later, was sent to examine these mines, disavows this statement, adding that the mines, as the matter then stood, could by no means yield so much, for the “live mines” were then in a state of deterioration, and that it would be impossible exactly to say how many “dead mines” were to be found till it is ascertained by successive examinations; on the other hand, he is convinced that the mines of Krisuvik might be able to yield 100 commercial lasts (or 200 tons) of clean sulphur a year, and the experience of the recent time has proved this to be no exaggeration; for during the last winter (1868-69) about 250 commercial lasts (or 500 tons) of raw sulphur have been dug up, which must make a good deal more than 100 lasts of clean sulphur at least; further, Dr Hjaltalin observes, that copper ore of rather a good quality is to be found there, and a more recent experience has rendered it likely that there is a considerable quantity of this mineral.
On the other hand, the sulphur must, no doubt, have accumulated to a considerable degree in the mines of the north for the last twenty years they have not been worked; it is, therefore, pretty certain that they might now yield a considerable quantity of sulphur if they were worked in the right manner; but as it must always be borne in mind that no mines are so liable to deterioration as sulphur mines, it must in consequence be very precarious to make them over to foreigners. A French geologist, Mr Eugène Robert, who travelled here in 1835, and afterwards has written treatises on the geology of Iceland in the French language, has also called attention to this point. He says, that care ought to be taken not to lease out to the Englishmen (who then were applying for the lease) the mines in the north, as they might be of great consequence, the sulphur mines of Sicily having begun to fall off.