The town of Gwâlior extends along the foot of the hill on one side, and consists of a single street above a mile long. There is a very beautiful mosque, with one end built by a Muhammad Khan, A.D. 1665, of the white sandstone of the rock above it. It looks as fresh as if it had not been finished a month; and struck, as I passed it, with so noble a work, apparently new, and under such a government, I alighted from my horse, went in, and read the inscription, which told me the date of the building and the name of the founder. There is no stucco- work over any part of it, nor is any required on such beautiful materials; and the stones are all so nicely cut that cement seems to have been considered useless. It has the usual two minarets or towers, and over the arches and alcoves are carved, as customary, passages from the Korân, in the beautiful Kufic characters.[14] The court and camp of the chief extends out from the southern end of the hill for several miles. The whole of the hill on which the fort of Gwâlior stands had evidently, at no very distant period, been covered by a mass of basalt, surmounted by a crust of indurated brown and red iron clay, with lithomarge, which often assumes the appearance of common laterite. The boulders of basalt, which still cap some part of the hill, and form the greater part of the glacis at the bottom, are for the most part in a state of rapid decomposition; but some of them are still so hard and fresh that the hammer rings upon them as upon a bell, and their fracture is brilliantly crystalline. The basalt is the same as that which caps the sandstone hills of the Vindhya range throughout Mâlwâ. The sandstone hills around Gwâlior all rise in the same abrupt manner from the plain as those through Mâlwâ generally; and they have almost all of them the same basaltic glacis at their base, with boulders of that rock scattered over the top, all indicating that they were at one time buried, in the same manner under one great mass of volcanic matter, thrown out from their submarine craters in streams of lava, or diffused through the ocean or lakes in ashes, and deposited in strata. The geological character of the country about Gwâlior is very similar to that of the country about Sâgar; and I may say the same of the Vindhya range generally, as far as I have seen it, from Mirzapore on the Ganges to Bhopâl in Mâlwâ--hills of sandstone rising suddenly from alluvial plain, and capped, or bearing signs of having been capped, by basalt reposing immediately upon it, and partly covered in its turn by beds of indurated iron clay.[15]