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Updated: June 22, 2025


The distribution is not one of seeds, but rather of geographical conditions thermometric, hygrometric, telluric, and possibly chemical. And this is true of all vegetation, whether growing in the same plant zones, in high latitudes, at high altitudes, or under one degree of temperature and moisture or another.

For I feel cheated by casual glimpses of affairs which concern me not; I resent odd scraps of information, not chosen for my palate; I am indignant at news culled from the public prints, and frantic at thermometric and meteorological intelligence. But stay! There is a case when what seems to come under this heading is really intensely personal, and, therefore, most welcome to the letter receiver.

The late Professor Forbes of Edinburgh, whose untimely death the friends of science have had so much reason to deplore, ascertained that the temperature of boiling water varied arithmetically with the height, and at the rate of one degree of the thermometric scale for every 549.05 feet. Multiplying the difference of the boiling-point by this number of feet, we have the elevation.

This excess is the thermometric effect which the solar heat produces at the surface; now, instead of the large numbers adopted by Mairan, Bailly, and Buffon, what has our colleague found? A thirtieth of a degree, not more. The surface of the earth, which originally was perhaps incandescent, has cooled then in the course of ages, so as hardly to preserve any sensible trace of its primitive heat.

These were to him the thermometric readings of the warmth of her heart. Half way down the first page before he had time to turn the leaf he caught his breath in an effort to smother a sudden outburst of joy. Then with a supreme effort he regained his self-control and read the letter to the end. Mrs.

The first seven lectures of the course deal with thermometric heat, expansion, combustion, conduction, specific and latent heat, and the relation of this force to mechanical processes; while the remaining five treat of radiant heat, the law and conditions of its movement, its influence upon matter, its relations to other forces, terrestrial and solar radiation, and the thermal energies of the solar system.

There is a continuous adaptation of means to ends, of causes to effects, of adjustments to re-adjustments, in respect to the characteristics of the earth's surface its physical configuration, the distribution of its fluids and solids, its fauna and flora, its hygrometric and thermometric conditions, its ocean, wind, and electro-magnetic currents, and even its meteorological manifestations all showing a continuous adjustment of interior to exterior conditions or relations.

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