The forest of Chiltern was infested by wolves and wild bulls in the time of Edward the Confessor. William the Conqueror granted the lordship of Riddesdale, in Northumberland, to Robert de Umfraville, on condition of defending that part of the country against enemies and wolves. King John gave a premium of ten shillings for catching two wolves.
In the reign of King Henry the Third Vitalis de Engaine held the manors of Laxton and Pitchley, in the county of Northampton, by the service of hunting the wolf, whenever the king should command him. In the reign of Edward the First, it was found by inquisition that John de Engaine held the manor of Great Gidding, in the county of Huntingdon, by the service of hunting the hare, fox, wild cat, and wolf, within the counties of Huntingdon, Northampton, Buckingham, Oxford, and Rutland. In the reign of Edward the Third, Thomas de Engaine held certain manors by the service of finding, at his own proper cost, certain dogs for the destruction of wolves, foxes, martins, and wild cats in the counties of Northampton, Rutland, Oxford, Essex, and Buckingham.
TEMPLES OF BRAMBANAM.
In the island of Java, and not far from the ruins of Boro Buddor, are situated the Buddhist temples of Brambanam; certainly one of the most extraordinary groups of buildings of its class, and very unlike anything we now find in India; though there can scarcely be a doubt but that the whole is derived from an Indian original now lost.
The great temple is a square building above 45 ft. square, and 75 ft. high, terminating upwards in an octagonal straight-lined pyramid. On each face of this is a smaller temple of similar design joined to the great one by corridors; the whole five thus constituting a cruciform building. It is raised upon a richly ornamented square base. One of the smaller temples serves as an entrance-porch. The building itself is very curiously and richly ornamented with sculpture; but the most remarkable feature of the whole group is the multitude of smaller temples which surround the central one, 239 in number. Immediately beyond the square terrace which supports the central temple stand 28 of these, forming a square of 8 on each side, counting the angular ones both ways. Beyond these, at a distance of 35 ft., is the second square, 44 in number; between this and the next row is a wide space of above 80 ft., in which only 6 temples are situated, two in the centre of the north and south faces, and one on each of the others. The two outer rows of temples are situated close to one another, back to back, and are 160 in number, each face of the square they form being about 525 ft. All these 239 temples are similar to one another, about 12 ft. square at the base, and 22 ft. high, all richly carved and ornamented, and in every one is a small square cell, in which was originally placed a cross-legged figure, probably of one of the Jaina saints, though the drawings which have been hitherto published do not enable us to determine whom they represent—the persons who made them not being aware of the distinction between Buddhist and Jaina images.
The date given to these monuments by the natives is about the 9th or 10th century, at which time the Jains were making great progress at Guzerat and the western parts of India; and if the traditions are to be relied upon, which bring the Hindu colonists of Java from that quarter, it is almost certain that they would have brought that religion with them. If the age, however, that is assigned to them be correct, they are specimens of an earlier date and form than anything we now find in India, and less removed from the old Buddhist type than anything that now remains there.
GRAHAM ISLAND.
The most recent instance of subaqueous eruption, with which we are acquainted is that which produced Hotham or Graham Island, in the year 1831. This island was thrown up in the Mediterranean, between the south-west coast of Sicily and the African coast, in latitude 37° 8' 30" north, and longitude 12° 42' 15" east. The eruption seems to have been first observed by John Corrao, the captain of a Sicilian vessel, who passing near to the spot on the 10th of July, observed an immense column of water ejected from the sea to the height of sixty feet, and about eight hundred yards in circumference.
On the 16th of July, Corrao again passed the same spot, and he found that a small island had been formed, twelve feet high, with a crater in the centre, from which immense columns of vapour and masses of volcanic matter were ejected.
The island was afterwards visited by several scientific gentlemen, and is said to have been two hundred feet high, and three miles in circumference, on the 4th of August. But from this time the island decreased in size; for being composed of loose scoriæ and pumice, it was rapidly acted upon by the water; and on the 3rd of September, when carefully measured by Captain Wodehouse, was only three-fifths of a mile in circumference, and one hundred and seven feet high. At the end of October the island had entirely disappeared, except one small point composed of sand and scoriæ. Captain Swinburne examined the spot in the beginning of the year 1832, and found an extensive shoal to occupy the place where the island had once been. In 1833 there was a dangerous reef, of an oval form, three-fifths of a mile in circumference.