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The Locomotive - Lighthouse Survival Blog

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158 THE LOCOMOTIVE. [October,<br />

is 122.29°. This shows that the quantity of heat required to raise the temperature of a<br />

pound of water one degree is not the same at all points of the thermometer scale, but it<br />

indicates, at the same time, that the total variation between the freezing point and the<br />

boiling point is very slight. Similar experiments, made by mixing water at other tem-<br />

peratures, give this same result; and hence we conclude that although a " heat unit " is<br />

not the same at all temperatures, the variation in its value is so slight that for most pur-<br />

poses it can be neglected. In calculating tables of the properties of steam and water,<br />

allowance is made for the fact that the " specific heat " of water is not the same at all<br />

temperatures; but in all the ordinary work of testing boilers and engines, and laying<br />

out steam-plants and heating-systems, it is customary to consider the specific heat of<br />

water to be constant; and the "heat unit " is defined simply as "the quantity of heat<br />

that will raise the temperature of one pound of water one degree."<br />

When we say that a pound of steam, in condensing, gives out 967 heat units, we<br />

merely mean that it gives out an amount of heat that would be sufficient to raise the<br />

temperature of 967 pounds of water 1°, or 96.7 pounds of water 10", or 9.67 pounds<br />

100°, etc. Similarly, when we say that a pound of good coal gives out 14,000 heat<br />

units when burned, we mean that each pound of the coal can heat 14,000 pounds of<br />

water 1°, or 1,400 pounds 10°, or 140 pounds 100°, etc. And finally, when we say<br />

that the "mechanical equivalent of heat" is 779 foot-pounds, we only mean if a weight<br />

of 779 pounds should fall one foot, the work it would do would be just sufficient to<br />

raise the temperature of a pound of water 1°; and, conversely, if we could utilize (by<br />

means of a steam engine or otherwise) all the heat that a pound of water gives out<br />

when it cools 1°, this heat would be just sufficient to raise a weight of 779 pounds<br />

through, a height of one foot.<br />

<strong>The</strong> Recent Eruption of Kilauea.<br />

This great volcano has been active for several months past, the principal character-<br />

istic being a remarkable rise and fall of melted lava within the crater. L. A. Thurston<br />

gives the following among other, particulars in the Pacific Commercial Advertiser. In<br />

March, 1894, the lava had risen almost to the top of the crater, the rise being 447 feet<br />

in 19 months.<br />

On the evening of July 6th a party of tourists found the lake in a state of moderate<br />

activity, the surface of the lava being about twelve feet below the banks. On Satur-<br />

day, the 7th, the surface of the lake raised so that the entire surface was visible from<br />

the Volcano House. That night it overflowed into the main crater, and a blow hole<br />

was thrown up some 200 yards outside and to the north of the lake, from which a flow<br />

issued. <strong>The</strong>re were two other hot cones in the immediate vicinity which were thrown<br />

up about three weeks before. On Sunday, Monday, and Tuesday. July 8th. 9th, and<br />

10th, the surface of the lake rose and fell several times, varying from full to the brim to<br />

15 feet below the edge of the banks.<br />

On the morning of the 11th the hill was found to have sunk down to the level of<br />

the other banks, and frequent columns of rising dust indicated that the banks were<br />

falling in. <strong>The</strong> lake had fallen some 50 feet, through the escape of the lava by some<br />

subterranean passage, and the wall of the lake formed by the hill was falling in at fre-<br />

quent intervals. <strong>The</strong> lava in the lake continued to fall steadily, at the rate of about 20<br />

feet an hour from 10 o'clock in the morning until 8 in the evening. <strong>The</strong>re was scarcely<br />

a moment when the crash of the falling banks was not going on. As the level of the

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