Encyclopædia metropolitana; or, Universal dictionary of knowledge, ed. by E. Smedley, Hugh J. Rose and Henry J. Rose. [With] Plates, Том 51845 |
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Сторінка 12
... quantity would be doubled with. Meteor the impression being conveyed as through a spring . ology . Mr. Daniell illustrates this effect by the beautiful Cry- ophorus of Dr. Wollaston , in which the force of the Illustrated vapour is so ...
... quantity would be doubled with. Meteor the impression being conveyed as through a spring . ology . Mr. Daniell illustrates this effect by the beautiful Cry- ophorus of Dr. Wollaston , in which the force of the Illustrated vapour is so ...
Сторінка 13
Encyclopaedia Edward Smedley. Meteor per minute , that quantity would be doubled with half clogy . the resistance . The changes at the surface affect the whole of the superincumbent column equally , and the temperature of the vapour ...
Encyclopaedia Edward Smedley. Meteor per minute , that quantity would be doubled with half clogy . the resistance . The changes at the surface affect the whole of the superincumbent column equally , and the temperature of the vapour ...
Сторінка 14
... quantity in different with mois- places , but of the same degree of density , would arise , ture and and Clouds of more or less opacity would be formed , at variously corresponding situations , in the planes of deposition . heated ...
... quantity in different with mois- places , but of the same degree of density , would arise , ture and and Clouds of more or less opacity would be formed , at variously corresponding situations , in the planes of deposition . heated ...
Сторінка 15
... quantity took place between the different stages , it would instantly be redissolved by the excess of heat into which it would be naturally inclined to fall . The circulation thus becomes a process of equalization , by which the ...
... quantity took place between the different stages , it would instantly be redissolved by the excess of heat into which it would be naturally inclined to fall . The circulation thus becomes a process of equalization , by which the ...
Сторінка 17
... quantity of aqueous vapour , so , on the other , a rapid increase of the latter may be produced by a fall in the former . The mechanical resistance of the air must of TABLE XIV . Showing the Force of the different Currents in a Mixed ...
... quantity of aqueous vapour , so , on the other , a rapid increase of the latter may be produced by a fall in the former . The mechanical resistance of the air must of TABLE XIV . Showing the Force of the different Currents in a Mixed ...
Загальні терміни та фрази
altitude angle appears architrave atmosphere ature canal Cloud coefficient colour columns Corinthian Order cos² degree density depending depth determined diameter direction distance Ditto diurnal diurnal tide Doric Order Earth effect elastic elevation ellipticity entablature equal equation evaporation expression Fahrenheit feet fluid force formula Gravity heat height high water horizontal Humboldt inches Isothermal latitude length longitude low water mass mean temperature measure meridian Meteor moisture moon moon's motion mountains nearly observations ology parallax parallel particles pendulum perature peripteral peristyle perpetual snows plane Pole produced pronaos proportion quantity radiation Rain regions remarks right ascension side sin² solar spheroid supposed surface syzygies Table temperature Temple theory thermometer tide-wave Tides and Waves tion toises triglyphs upper vapour velocity vertical Vitruvius vt-x walls whole wind
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Сторінка 131 - night, colder than the atmosphere, by radiating their heat to the heavens, I perceived immediately a just reason for the practice, which I had before deemed useless. Being desirous, however, of acquiring some precise information on this subject, I fixed, perpendicularly, in the earth of
Сторінка 147 - discern, Or half-conceal'd some figure at the stern ; Boys who, on shore, to sea the pebble cast, Will hear it strike against the viewless mast ; While the stern boatman growls his fierce disdain, At whom he knows not, whom he threats in vain.
Сторінка 148 - The Rain Cloud. A Cloud, or system of Clouds, from which rain is falling. It is a horizontal sheet, above which the Cirrus spreads, while the Cumulus enters it laterally and from beneath.
Сторінка 27 - At Pékin, also, where the mean temperature of the year is that of the coasts of Brittany, the scorching heats of summer are greater than at Cairo, and the winters as rigorous as at Upsal,
Сторінка 147 - When all you see through densest Fog is seen, When you can hear the fishers near at hand Distinctly speak, yet see not where they stand ; Or sometimes them and not their
Сторінка 292 - When the length of the wave is great in comparison with the depth of the water, (as in the case of tide-waves,) the horizontal motion is sensibly the same from the surface to the bottom, and the vertical motion for different particles varies in the same proportion as their height above the bottom.
Сторінка 143 - of aqueous vapour, and the situation of the ground is such as to permit the cold air from the land to mix with the warmer air above the water, Mist or Fog will be the result. The density of such Mist or Fog will,
Сторінка 132 - whether on hill .. Sometimes, anon on shady vale, each night Under the covert of some ancient oak, Or cedar, to defend him from the Dew.
Сторінка 132 - a hollow cylinder of baked clay, the height of which was 2£ feet, and diameter 1 foot. On the grass, surrounded by the cylinder, were laid 10 grains of wool, which, in this situation, as there was not the least wind, would have received as much rain as a like
Сторінка 131 - in the pride of half knowledge, smiled at the means frequently employed by gardeners, to protect tender plants from cold, as it appeared to me impossible, that