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over a period of twenty years, together with a project for establishing government monopolies of industries. These undertakings, as described by Dr. Goto, include (1) the laying of a trunk-line railway extending over the whole length of the island; (2) the surveying of lands; (3) the construction of harbors, and (4) the building of government offices and residences. To meet the expenditures required for these works, the Formosan government was authorized to raise loans to the amount of 35,000,000 yen, of which the principal and interest was to be paid out of the revenues of the island. It is estimated that the railroad work alone will require 28,810,000 yen, the construction of the harbor of Kelung 2,000,000, the land-surveying 3,000,000, and the building of government offices and residences 1,200,000. It is believed that the railroad will be finished much within the ten years' time originally assigned to the work, and that it will have a remarkable effect in stimulating industries on the island. Revenues accruing from the part of the island now open to traffic are greater than they were expected to


The completion of an accurate land survey will confirm rights over land, will make landed property secure, and will greatly facilitate transfers. This work, by the way, was undertaken by the Chinese governor some years ago, but without success. As to the projected harbor works at Kelung, this is only the beginning of improvements for that port which will involve the expenditure of tens of millions of yen. It is the intention of the government to make this the chief port of Formosa, and it is believed that the growing industry and commerce of the island justify all the expenditures that have been projected. In the erection of public buildings great care has been taken in regard to sanitary arrangements, and the structures already built or in process of completion will serve as models for the whole island.


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700,000 or 800,000 yen, and this commodity is now exported to Japan in considerable quantities. It is produced by permitting salt water to flow into fields, and then causing it to evaporate by the heat of the sun. Almost the whole supply of camphor of the world comes from Formosa. When Japan acquired Formosa a camphor monopoly was established, with a view to protecting the camphor trees, improving the methods of manufacturing, and putting the industry on a secure basis. The production is now regulated according to the demands of the world's market. The revenue yielded by the monopoly is now about 4,000,000 yen. The present governorgeneral has also formed a plan for eventually making the Formosa finances entirely independent of imperial aid. The imperial government began the administration of Formosa with a grant of nearly 6,900,000 yen, and this grant has been annually diminished until the present time. According to Baron Kodama's project, which was adopted by the Diet, the grant will be steadily decreased until it will entirely disappear in 1910.


The possibility of this gain of financial independence may be seen when we consider the recent remarkable increase of the revenue,—from 5,000,000 yen in 1897 to 14,000,000 yen at present, with the probability of an increase to 20,000,000 yen in two or three years, this increase being largely secured as a result of the operation of the monopolies, the adjustment of the land tax, and other financial reforms. the total expenditure incurred by Japan in connection with Formosa up to the end of the last fiscal year, March 31, 1901, amounted to 150,000,000 yen, including the military expenses, while in the same period the revenue amounted to only 40,000,000 yen, the financial burden to be charged to Formosa may be reckoned as 110,000,000 yen in all. As the annual revenue derived from Formosa is now from 14,000,000 to 20,000,000 yen, it may be said, as Dr. Goto points out, that the capital invested by the imperial government is bearing interest at the rate of 15 to 20 per cent. The import of Japanese commodities into Formosa is now about 15,000,000 yen. Supposing the profit of this trade to be at the rate of 20 per cent., the annual gain of Japan is about 3,000,000 yen, which nearly covers the present amount of the grant which the Formosan government receives from the imperial government.


Among the more important products of Formosa named by Dr. Goto are tea, rice, sugar, hemp and flax, indigo, paper, silk, minerals, cattle, and marine produce. Dr. Goto predicts that

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One of the chief difficulties to be contended with is the poor supply of water, which at present is obtained by local storage of rain water, -not a very satisfactory arrangement. Within twenty or twenty-five miles of Johannesburg there are, however, other sources of water supply which will probably be utilized. Of the maps prepared Mr. Hammond says:

"Great attention is given to the preparation of maps of the underground workings, geological sections, and plans upon which assays are plotted. In these respects the Rand practice is far ahead of that of any other country with which I am familiar."


The labor question is always a difficult one. Mr. Hammond says:

"Reference has already been made to the labor question, in statistics of the relative number of whites and blacks employed. The white workmen are predominantly British, though many of the important members of technical staffs are Americans; the mine and mill foremen are usually either Americans, or British subjects who have had mining experience in America. This labor is generally below the American standard, but is rapidly improving. Manual workers on the surface and all miners except those running machine drills, are blacks, and the quality of the black labor is very poor, especially on first arriving at the mines.

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Mr. Hammond looks for a reduction in the present excessive railway rates. He says:

"Generally speaking, the cost of the principal machinery, erected on the ground, will be two and one-half times its home cost. In respect of labor, cost of dynamite, and charges for railway transport, marked improvement is confidently to be expected from the change of governmental conditions."


Mr. Hammond speaks well of the Transvaal laws :

The mining laws of the Transvaal are most excellent in character, and while the claims cover every square foot of land for an area of nearly 40 miles long by from 2 to 3 miles wide, there have been practically no conflicts over extra-lateral rights.

"Notwithstanding the change in the political status of the Transvaal which will follow the recently concluded peace and final establishment of British rule, it may be confidently assumed that the main features of the mining law of the South African Republic will be retained, and certain oppressive features of monopolies, etc., bearing with special weight on the mining industry, will be abolished. The dynamite monopoly was one that bore most heavily on the mining industry: and, according to the reports of the state mining engineer, explosives, including fuse and detonators, amounted to nearly 10 per cent. of the total working costs of the mines.


"It is estimated that for every mile in length along the course of the reefs, down to a vertical depth of 1,000 feet for the dip of the reefs, gold to the value of about £10,000,000 will be extracted. This is a conservative estimate,—at least as applied to the central section of the Rand. If we assume these conditions to obtain to a depth of 6,000 feet vertically, we have the enormous sum of £60,000,000 for each mile in length. It is not unreasonable to suppose that these conditions will be maintained along most of the central section, say, for a distance of ten miles,—in which case we would have an auriferous area. within practicable mining depths, containing upward of £600,000,000 value of gold."

If," says Mr. Hammond, I were called upon to express my opinion, I would estimate the future duration of profitable operations on a large scale in the district at less, rather than more, than twenty-five years. I believe that, as the result of economic reforms, there will be an ultimate saving of 6s. per ton of ore treated."



HERE recently returned from Martinique a party of scientists, artists, and newspaper men, who had hastened to the site of St. Pierre almost as soon as the news of the catastrophe was made known. One of these was Prof. Angelo Heilprin, who has for twenty years been identified with the scientific institutions of Philadelphia. Professor Heilprin writes in the August McClure's of his observation on Mont Pelée, and of the deductions he has drawn from these observations as to the original cause of the great volcanic upheaval.

Professor Heilprin was the first man to ascend the volcano after the great catastrophe. On May 31, he went up the crater to an altitude of about 4,000 feet. He found that the old crater had not been blown out, as was reported. The next day Professor Heilprin made another ascent to the same crater, accompanied by Messrs. Kennan, Jaccaci, and the artist George Varian, who contributes the pictures which illustrate this article. The party arrived at an elevation of 4,025 feet. They found the temperature to be, two or three inches below the surface, 124° to 130°, and at a somewhat greater depth 162°. Puffs of steam were issuing from a number of vents, and from beneath great bowlder masses, whose heated surfaces were scarred with sulphur blotches.


"We waited patiently for a lifting of the clouds, and it came at last. A sudden gust cleared the summit, and sunlight illuminated the near horizon. We dashed to the line above which welled out the huge steam cloud of the volcano, and in a few instants stood upon the rim of the giant rift in whose interior the world was being re-made in miniature.

We were four feet, perhaps less, from a point whence a plummet could be dropped into the seething furnace. Momentary flashes of light permitted us to peer deep into the tempest-tossed caldron, but at no time could we see its floor, for over it roiled the vapors that rose out to mountain heights. Opposite us, at a distance of perhaps 200 feet or more, across the thin steam vapor, trembled the walls of the other face of the crater. Halfway between rose the central core of the burned-out cinder masses, topped by enormous white rocks, whose brilliant incandescence flashed out the beacon lights which were observed from the sea some days after the fatal 8th, and even at our later day illumined the night-crown of the volcano with a glow of fire. From the interior came deep rumbling detonations, the clinking of falling and sliding cinders, the hissing of the emerging steam, and other

sounds which were too feebly defined to be described. We felt no inconvenience from either

gas or steam.

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We found that we were standing on an overhang, and therefore dared not tarry beyond the time needed to make observations. I attempted to locate the axis of the vent as nearly as the direction of its largely obscured walls and the position of the basin of Lac des Palmistes permitted. I found it to be N.-S., slightly S. W. The magnetic needle, which the day before showed a marked deflection, was nearly normal. The form of the crater is that of a caldron, pitching steeply downward toward the Caribbean, and opening in a direction a little west of the line to St. Pierre. At no time could we positively ascertain the extreme boundaries. Its length must have been 500 feet; it may have been much There can be no question that at the downward side of the crater the rift traverses the position of the narrow rift known as the Fente, or the Terre Fendue, which had been a feature of the mountain since the eruption of 1851, and perhaps existed long before that event.


"Any statement regarding the depth of the crater must for the time remain conjectural. I should say that it could hardly be less than from 200 to 250 feet; it might be very much more."


Professor Heilprin says that the death-dealing eruption of May 8 was from the lower crater. He proves that the description of the catastrophe which spoke of moving sheets of flame were erroneous. Instead, there was a luminous, or incandescent, cloud which may easily in that terrible time have given the impression of flame.

This glowing cloud, Professor Heilprin says, was composed of one of the heavier carbonic gases brought under pressure to a condition of extreme incandescence and whose liberation in contact with the oxygen in the atmosphere, assisted by electric discharges, wrought this explosion, or series of explosions, that developed the catastrophe."

The great cloud of incandescent vapor undoubtedly produced a tornado, and Professor Heilprin found evidence of storm paths lying across the city's ruins. He also considers it certain that electric explosions had their share in the phenomena.


"To the inquiry as to what was the source of this carbon gas, -to my mind the main factor of the catastrophe,-the geologist points to those vast bituminous deposits, like those of Venezuela and the island of Trinidad, which lie but little out

of the line of the connected series of volcanoes, of which the Soufrière of St. Vincent and Pelée of Martinique are a part. He also points to the limestone deposits, with their enormous masses of locked-up carbon, forming the foundation upon which these same volcanoes are implanted, which indicate a source of energy far greater than was required for the catastrophe of Pelée. Though no one could have foretold the cataclysm long in advance of its coming, the episode, except in its magnitude and terrible consequences, is no sur prise to the geologist, who knows this region to be in an area of extreme weakness in the earth's crust. This region of terrestrial instability includes the greater part of the Caribbean and Gulf basins, and defines in its eastern contour the line of disappearance and breakage of the South American Andes, whose sunken crest is the pediment of the lesser Antilles. What great dis. turbances, if any, have taken place in the sea bottom as the result of the recent occurrences is a question that will take time to determine; but there is evidence already that some change has taken place west of Martinique, between the depth of 1,500 and 2,000 fathoms. tions of Colima in Mexico, the earthquakes that so recently destroyed the towns of Chilpancingo in Mexico and Quetzaltenango in Guatemala, the minor disturbances in Nicaragua, are but phases of the phenomena which culminated so disastrously in the explosions of the Soufrière of St. Vincent and Mont Pelée of Martinique."

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ORTUNATELY for the cause of science, several unusually competent investigators were able to visit Martinique and St. Vincent before the volcanic eruptions of May had ceased, and their observations have already been reported in detail. The full report of the representatives of the National Geographic Society appears in the July number of the National Geographic Magazine. This report, which was prepared by Dr. Robert T. Hill, of the United States Geological Survey, is interesting not only as a presentation of facts regarding the great catastrophe, but also for the theories that it suggests to account for the enormous fatality at St. Pierre.

Dr. Hill states two such theories, one or the other of which may ultimately be adopted:

1. The heat-blast theory. This hypothesis. assumed that the lapilli, gases, and steam of the ejected cloud were sufficiently hot to have inflamed the city and destroyed the people by singeing, suffocation, and asphyxiation. It does not account for the forces exerted radially and horizontally, nor the flame.

2. The aërial-explosion theory. The explosion of gases within the erupted cloud after their projection into the air would account for all the phenomena observed.

"The aerial explosion, if it occurred, was most probably a combustible gas, but science is still unable to state its nature. The discussion of explosive gases involves a line of scientific specialization which the writer does not possess ; but as sudden and mysterious as was the great secret, it has left its traces and clues which the detectives of science will follow up. Metal surfaces of objects in the ruins will be examined and analyzed for traces of sulphur and chlorides. The deposits from the numerous steaming fumaroles are already within the chemical laboratory. Even the ash and rocks of the island will be submitted to minute investigation.

"And then there were those frightful lightning bolts! What of them and their igniting power?"


Prof. Israel C. Russell, another geologist who represented the Geographic Society in Martinique, says regarding the nature of the blast which swept over St. Pierre from Mont Pelée :


"It has been stated in the newspapers that the inhabitants of St. Pierre were asphyxiated by noxious gases or killed by a gas explosion. own observations and the best interpretation I can place upon the testimony of surviving wit nesses favors the opinion that the general cause of death was a blast of steam charged with hot dust. Gases, probably in part inflammable, were no doubt present, as the odor of sulphurous acid was perceptible at the time of my visit; but the part that such gases played was seemingly secondary. In order to be able to judge of the conditions where everything was destroyed, it is necessary to learn what took place on the outskirts of the storm. The people on the borders of the devastated area who escaped were in some instances injured, and the injuries were inflicted by hot dust, which on touching the skin adhered and burned. These burns resemble scalds, and destroyed only the epidermis. In several such instances the hair on the burned portions was not destroyed, and where the bodies of the sufferers were protected by even light clothing they were uninjured.

"Had the dust which struck the injured people been somewhat hotter, their clothing would have been ignited; and if they had inhaled the hot dust, death would have been almost instantaneous. The condition of the dead in St. Pierre favors the conclusion that this deduction shows what took place there. While the inhalation of

steam charged with burning hot dust may seemingly be accepted as the principal cause of death in the stricken city, it must be admitted that many persons were no doubt killed by falling walls, by nervous shock, etc.

"The blasts which swept St. Pierre on the morning of May 8, and again on May 20, passed through the city with hurricane force. This is demonstrated by the manner in which great trees were uprooted, strong masonry walls thrown down, the lighthouse overturned, etc. The direction in which all these objects were swept was a little west of south, or directly away from Mont Pelée. The most conspicuous evidence of the strength of the blast which wrought the mechanical destruction is furnished by a statue of the Blessed Virgin, referred to above. That statue, composed, I understand, of iron, and measuring over 11 feet in height and nearly 10 feet in circumference at the shoulders, and weighing several tons, was swept from its pedestal and carried southward about 45 feet. All the evidence collected in this connection cannot here be presented, but it indicates that the blast which wrought the havoc referred to passed over the city with full hurricane force."



HE Good Words comes out this July very much enlarged in size and greatly elated in spirit at the response to its coronation ode competition. Prizes of £50, £15, and £10. were offered last Christmas. The final award was given by Stopford Brook, Edmund Gosse, and William Canton. Odes were received from 1,084 competitors, and from almost every part of the empire. The editor is almost swept off his feet by the unexpected number and widely distributed origins of these odes. "The young loyalty has come to its manhood." The empire has found voice as a unit.

To read them, poem after poem, from all parts of the empire, is to become conscious of an imperial force the like of which history holds. no record and the chronicles of the nations show no trace. Turning over ode after ode the beautiful strains of harmonious patriotism blend into a

Protestant, Roman Catholic, Dissenter, Quaker, and Jew. Their pens, some of them, would have run more readily in Tamil or Telugu, Pushtu or Persian or Arabic, but they are all in the language of the ruling race, and cramped of course though they are, they are all of them real and living in thought and sentiment. Of course, the majority of the odes are by writers of our own race. . . . Never have poets sung with such a voice before. Knowledge of the splendid responsibilities of empire with boundaries that encompass the world, and vexed along all their length by the uncharitableness of envious neighbors or the turbulence of tribes that cannot yet understand, give dignity to the singers and noble form to their song."

The first prize falls to Lauchlan MacLean Watt, B.D., minister of Alloa, Scotland; the second to Rev. S. Cornish Watkins, Kingston, Herefordshire; the third is divided between Lucy Eveline Smith, of Dunedin, New Zealand, and F. H. Wood, M.A., Bromley Park, Kent. Perhaps as characterful as any is the passage in Mr. Watt's Ode on the Union Jack:

Ah, 'tis no empty fluttering of a dream,
Our flag's proud gleam:

Many and tired the fingers that have sewn it,

Seam by seam,

Staining it with life's crimson, and the blue

Of northern skies and seas, till winds have blown it Wider than all their wonder and their dream.

Thin red lines of pulsing lives were the thread of it, Pulsing lives that bled away for its sake beneath the spread of it.

Till the wide seas knew it,

And the winds of the wide world blew it.

And the host of England followed the flag till earth trembled under the tread of it.

Up with it into the sky.

Let it blow abroad, let its message fly

Like the gray gull, over the deep,
As glad and free.

The Good Words is so pleased with the success of this experiment as to offer similar prizes for the three best songs of the empire, to be adjudged next Christmas.


single stately imperial anthem until the reader SUCH is the inscription beneath a picture of

pausing as it were to listen, finds almost overpowering the glorious diapason of the song.. Very interesting, indeed, is the mingling of races and creeds, when side by side, upon a table in London, lie some eleven hundred odes, written by Brahmin and Mohammedan and Buddhist and native Christians,-negroes of the West, from the Leeward Isles and the Windward, natives of the East, Indian, Burmese and Cinghalese,—

statuary in Mr. F. D. How's sixth paper on Lord Salisbury, in Good Words. It might fitly head the entire article. "The curious and interesting statue is to be seen in the sculpture gallery of the beautiful reredos of the Chapel of All Souls' College, Oxford. The reredos was erected about forty-two years ago, at the time that Lord Salisbury had just been elected to a fellowship of all Souls', and the artist, having determined to give his saints the faces of actual

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