the English channel; the Straits of Gibraltar, uniting the Mediterranean sea with the Atlantic ocean; the Straits of Babelmandel, by which the Red sea, or Arabic Gulf, communicates with the Indian ocean. In the northern parts of Europe such a strait is often termed a sound, as the Sound of Mull, on the west coast of Scotland; and the much frequented pass between Denmark and Sweden, connecting the German ocean with the Baltic sea, is, for distinction's sake, called the Sound.

A body of water entirely inclosed by the land is called a lake, in Scotland a loch, and in Ireland a lough, (both words being of the same sound, although differently written); such as the Lake of Geneva in Switzerland, Lake Ladoga in Russia, the Lakes of Cumberland and Westmoreland, (which, with many other pieces of water in England, are commonly called Meres); Loch Lomond, Loch Tay, Loch Leven, &c. in Scotland; Lough Neagh, Killarney Lough, &c. in Ireland. The terms loch and lough are, however, often applied to pieces of salt-water running deep into the land, but having an open communication with the sea; as Loch Fyne on the west coast of Scotland, and Lough Foyle on the north coast of Ireland.

A large stream of water rising in the interior of a country, and flowing to the sea, or into some lake, is called a river; when the stream is small, it is termed a rivulet or brook: the word bourne or burn, so often met with in the names of places over England, and still used in its proper sense in Scotland, also signifies a rivulet or brook.

Although the sea appears to be stable, and confined to one particular situation on the globe, yet in many parts there are motions of the waters resembling the stream of a river: this stream is called a current, and in certain places it flows so rapidly as to require a strong wind to keep a vessel from being hurried along with it. When one current is opposed by another setting in a contrary direction, a circular motion

of the water is produced, which we call a whirlpool, such as the celebrated Charybdis, near Messina in Sicily, and the Maelstrom on the coast of Norway. Besides these partial currents, there are in certain parts near the equator, a continual setting of the waters of the ocean to the westward, as that which bears from the coast of Africa to the coast of South America, where it bends northerly, and enters the Gulf of Mexico, where it receives a contrary direction from the land, and turning towards the north-east, runs up the coast of North America, by the banks of Newfoundland, into the Atlantic ocean.

The sea is subject to another motion, by which it rises and falls twice in about 25 hours, flowing up on the shore, and retiring with great regularity. This motion, which is called the tide, or the flowing and ebbing of the sea, is closely connected with the state of the moon, being most observable when that luminary is new or full but the precise periods of high and low water at any particular spot are so much affected by its local situation, that they can only be ascertained by observation and experience.

The globe of the earth is surrounded by a fine elastic fluid, commonly called the air, but more properly the atmosphere. This air is indispensibly requisite for the existence of all animals and vegetables, for the transmission to us of light from the heavenly bodies, and for the production of vapours, clouds, dews and rain. The atmosphere itself is perfectly colourless, and the bluish or other tints, which we observe in it, are produced by vapours floating in it. Air being elastic, is susceptible of augmentation or diminution of its bulk from various causes: by heat, for instance, it is rarefied and enlarged, and by cold it is condensed and diminished; when by heat the air is rarefied, the colder air in the neighbourhood being heavier, will naturally rush into the place where the air is thin and light, and by its motion create a stream or current, to which we give the name of wind.

In the temperate regions of the earth, where the heats are irregular, currents of air or winds will of course be variable, and proceed from all directions at different times; but some local circumstances may occasion certain winds to be more prevalent in one country than in another; thus, in Britain, the south-west winds are observed to be much more fre quent than those from any other quarter.

In certain parts of the sea, at and on each side of the equator, where the heat of the sun occasions the most sensible and the most uniform changes in the temperature of the air, the rarefaction following the sun's course, the colder air rushes in from the eastward, and hence produces currents in general from east to west, during the whole year; to which, from their great utility to vessels employed in commerce, we have given the name of the trade-winds. It is to gain the assistance of this wind that vessels from Europe, bound for the West India islands, usually run a good way southwards on the coast of Africa, although by this they lengthen their voyage; for when they have come within the range of the trade-winds, they are sure of finding a fair wind to carry then to their desired port. In the Indian ocean the tradewinds blow regularly from east to west between 30° and 10o of south latitude: but to the northward of this line, on both sides of the equator, the wind changes every six months, one half of the year blowing, in a general sense, from east to west, and the other half of the year from west to east. These changing trade-winds are called monsoons.

In warm climates we meet with what are called sea and land breezes; that is, the wind, during a certain portion of the day, blows on shore from the sea, and in the night time off shore from the land. The cause of this phenomenon is supposed to be, that the land being more heated by the sun's rays than the sea, the air upon the land is heated and rarefied; and, consequently, the cooler air from the sea crowds in to fill its place: but in the night time, when the

air on the land is cooled, the equilibrium is restored, and the current of air again returns to the sea.

Besides these motions of the air, by which great masses are observed to change their relative positions, there is another motion of the particles of air among themselves, or a sort of vibration by which they move forwards and backwards for some time, in proportion to the strength of the impulse at first applied. This vibration is occasioned by a stroke on such bodies as we call sonorous, whose parts being elastic, move forwards through a small space, and then return to their original position; but without stopping there, they move backwards nearly as far as they moved forwards, and thus continue this vibratory motion, gradually diminishing in effect until at last they come to be perfectly at rest: such a motion is observed in a weight fixed at the end of a string, and suspended from the finger. This vibration of the parts of a sonorous body must act upon the particles of air in contact with them, by successive, but gradually diminishing impulses, and thus by agitating the membrane called the tympanum, or drum of the ear, occasion in us that sensation to which we give the name of sound. Although these vibrations are produced in succession, yet the intervals between the vibrations are so minute as not to be perceptible, and therefore to our senses they produce only one constant uniform sound.

When these vibrations of the air strike against any fixed immoveable surface or body, they are compelled to change their course and move backwards, thus acting again on the ear, and producing a second sound, which we call an echo.

The nature and process of vibration of the particles of air, may easily be conceived by observing the appearances and effects produced by throwing a stone into a pond of sti!! water. The water suddenly displaced by the stone rises up in a circular wave round it, and then sinks down into a hollow

hollow nearly as much below the surface of the pond as the top of the wave was above it again, another wave is produced and succeeded by another hollow; and in this manner a number of concentric waves and hollows are exhibited, gradually diminishing in elevation and depression, until the force of the impulse communicated by the stone is exhausted, and the circles totally disappear; but, if the impulse has been considerable, these circles are continued to the margin of the pond, where, striking against the banks, a contrary impulse is given to the water, and a fresh series of waves and depressions is produced, returning back towards the centre of the pond, in the same manner as the echo returns to the ear, by the repercussion of the particles of air from the resisting body, by which the vibrations of the air had been interrupted.

Sounds are observed to move with an equable velocity of about 1142 feet in one second of time: but the strength or londness of sounds vary agreeably to the state of the atmosphere. In cold dense air sounds are loudest, and in warm, thin, or rarefied air, they are weakest when all air has been extracted from a vessel, or a vacuum is produced, no sound is perceived.

It was already observed, that the atmosphere is necessary for the transmission of light, which is composed of inconceivably minute particles, proceeding in straight lines, and in all directions, from certain bodies, which are thence said to be luminous, such as the sun and other celestial bodies, a fire, a candle, or any other substance in a state of combustion or burning, from heat in a certain temperature, as red hot iron; when a flint is struck against another flint, or against a steel, luminous sparks are produced.

Light is so generally found united with heat, that we are apt to consider then as inseparable; but light is frequently perceived when there is no sensible heat, as in the appearance of putrescent animal and vegetable substances, of glow

worms