Waterspouts exhibit various aspects, but a frequent appearance has been thus described, as it has been observed at sea. Under a dense cloud, a circular area of the ocean, in diameter from 100 to 120 yards, shows great disturbance, the water rushing toward the centre of the agitated mass, from whence it rises in a spiral manner toward the clouds, assuming a trumpet-shape, with the broad end downward. At the same time, the cloud assumes a similar form, but the position of the cone is inverted, and its lower extremity, or apex, gradually unites with the upper extremity of the ascending column of water. At the point of junction, the diameter is not more than two or three feet. There is thus a column of water and vapor formed, extending from the sea to the cloud, thin in the middle, and broad at the two extremities, the sides of which are dark, which gives it the appearance of a hollow tube. It moves with the wind, and even in calm weather, when no wind is perceptible, the position shifts. Sometimes the spout preserves the perpendicular in its motion, but frequently, from the wind not acting with equal force upon its upper and lower extremities, or the one being more susceptible of impulsion than the other, it assumes an inclined position, and the column is speedily ruptured by the unequal velocity of its parts. A few minutes suffices in general for the duration of the phenomenon, but several have been known to continue for near an hour. Instances of repeated disruption and formation have been witnessed, and in the Mediterranean, as many as sixteen waterspouts have been observed at the same time. The mariners of former days were accustomed to discharge artillery at these moving columns, to accelerate their fall, fearful of their ships being crossed by them, and sunk or damaged—a practice alluded to by Falconer in the opening of the second canto of The Shipwreck: but the principal danger arises from the wind blowing in sudden gusts in their vicinity, from all points of the compass, sufficient to capsize small vessels carrying much sail. Waterspouts on land are not uncommon, and in this case there is no ascending column of water, but only a descending inverted cone of vapor. Vivid flashes of lightning frequently issue from them, and deluges of rain attend their disruption. A remarkable spout appeared and burst on Emott Moor, near Coln in Lancashire, in the year 1718, about a mile distant from some laborers digging peat, whose attention was directed to it by hearing an unusual noise in the air. Upon leaving the spot in alarm, they found a small rippling stream converted into a roaring flood, though no rain had fallen on the moor; and at the immediate scene of action, the earth had been swept away to the depth of seven feet, the naked rock appeared, and an excavation had been made in the ground by the force of the water discharged from the spout, upward of half a mile in length.