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Confessions of a Beachcomber

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among the natural advantages of land offered for close settlement, was catalogued an annual rainfall of 18 inches; in another an official inducement of an average rainfall of 27 inches was offered, in yet another 24 inches, with a not too shrewd note that 15 inches of rain was ample. Some of the denizens of a dry area in Victoria find it hard to credit the simple facts recorded by my rain-gauge. The rainfall for the month of January 1903, on Dunk Island was 26.60 inches, only 0.76 inches short of the mean for the whole year in Victoria, and more than twice the quantity that blessed the thirsty soil in some parts of Queensland. The total rainfall of the wettest locality in Victoria was 42.11 inches. Here the month of March alone gave 44.90 inches. At Thargomindah (South-Western Queensland) 11.37 inches were registered for 1903, and 9.82 inches for 1904. The two driest months of Dunk Island fell short by a trifle more than 2 inches of the total fall for 1904 for that parched area. At Eulolo (Mid-Western Queensland) 13.68 inches represented the sum of the blessing for 1903, while during 24 hours in December that year the Dunk Island gauge registered just 11 inches, and that quantity was 3 inches more than could he spared for Eulolo for the whole of 1904. During 1904 Cape Otway Forest (Victoria), registered 40.92 inches, Townsville (North Queensland) 26.32 inches, and Dunk Island--only 110 miles from Townsville--94.14 inches. That was a dry year with us. What is known in this neighbourhood as "the drought year" gave just 60 inches. Plants unaccustomed to such hardship, and therefore devoid of inherent powers of resistance, then gave way with pitiful lack of resource, and as speedily recovered on the return of normal conditions. Yet the 60 inches of "the drought year" represented more than twice the average rainfall of London. The average annual rainfall for the State of Victoria during the last thirty years has been 26.68 inches. Townsville (considered to be one of the driest places on the coast of North Queensland) averaged 45.54 inches during the period of thirty-four years. Twenty-five miles further north the rainfall for 1904 exceeded that of Dunk Island by 6 inches more than the average rainfall of the upper basin of the Thames Valley, which is given as 28 inches. Australia is big--there is bigness in our differences. Here in the tropics we have the finer weather--no excess of either heat or cold, no sudden, constitution-shattering changes. At Wood's Point (Victoria) rain fell on 185 days in 1903, and on 166 days in 1904. At Dunk Island rain occurred on 107 days in 1903 and On 92 days in 1904. We had many more days of picnic weather, notwithstanding our overwhelming superiority in quantity of rain. Moreover, in the tropics the bulk of the rain falls after sundown. After a really fine day in the wet season the hours of darkness may account for several inches of rain. Here over 12 inches have been collected between sundown and nine o'clock the following morning. Particular references are confined to seasons three or four years past because recent official data, necessary for enlightening comparisons are not available, but in confirmation of statements concerning the meteorological conditions of the coast of tropical Queensland, the record of rainfall at Dunk Island since 1903 may be quoted: 1904 94.41 inches. 1905 89.06 " First nine months of 1906 134.70 " Of the latter total, 56 inches occurred in February, two days (6th and 18th), accounting for 22.95 inches--more than half the average rainfall of the State of Queensland. An illustration--homely but graphic--of climatic differences may be given. During the first five months of 1904 the rainfall of Dunk Island amounted to 75.15 inches, the lowest monthly record being May (5.30 inches) and the highest March (29.05 inches). At the end of May on the Burdekin Delta--150 miles to the south--the sugarcane was beginning to be affected by the hot, dry weather, and irrigation was about to be resorted to. Here in January it became necessary to repair the roof of the boat-shed, and to keep the ridge covering of paper-bark in position, two long saplings were tied parallel with the ridge pole. At the end of May these saplings were taken down in order that the whole of the thatch might be renovated, when it was found that both had started to grow, several of the shoots being 8 and 10 inches long. While sugarcane was languishing for lack of moisture, 150 miles away down the coast, a roughly-cut sapling exposed on the roof of a building found the conditions for the beginning of a new existence so favourable and stimulative that it had budded as freely as Aaron's rod. "Through the scent of water it had budded and brought forth boughs like a plant." Nearly as much misapprehension prevails in the Southern States of the Commonwealth as to the characteristics of North Queensland as seems to prevail among the good old folks "at home" as to Australia generally. If the few facts presented excite even mild surprise, they will not be altogether out of place in these pages. Dunk Island has a mean temperature of about 69 deg.; January is the hottest month with a mean of 87 deg, and July the coolest, mean 57 deg. Taking the official readings of Cardwell (20 miles to the south), I find the greatest extremes on record occurred in one year, when the highest temperature was 103.3 deg. and the lowest 36.2 deg. At Geraldton (25 miles to the north) the extremes were 96 deg. and 43.4 deg. Rainfall and temperature, the proportion of clear to cloudy skies, calms, the direction, strength and the duration of winds, do not wholly comprehend distinctive climatic features. There are other conditions of more or less character and note, some hard to define, yet ever present. Here the air is warm and soothing, seldom is it crisp and never really bracing. Hot dry winds are unknown, but in the height of the wet season--which coincides with the dry season of the Southern States--the moisture-laden air may be likened to the vapour of a steam bath. While the rain thunders on the roof at the rate of an inch per hour, inside the house it may be perspiringly hot. After a fortnight's rain the damp saturates everything. Neglected boots and shoes grow a rich crop of

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