In the immediate neighbourhood of these relics of antiquity is the recently-erected statue to the great Lord Clive, the Townhall, the Working Man's Hall, the Music Hall, the public news-room, and a group of other handsome buildings. A passage near the Music Hall leads to the Museum of the Shropshire and North Wales Natural History and Antiquarian Society, which no visitor with time on his hands should neglect to visit. In addition to objects of natural history, it contains others of interest obtained from Wroxeter, and is open daily from ten to four to visitors upon payment of twopence. Portions of the town walls, erected in the reign of Henry III., with one of the ancient towers, are still standing, and form a pleasant walk. But the grand promenade is the Quarry Avenue, which, with Kingsland on the opposite side, is the common property of the inhabitants. The former is a sloping piece of meadow land, intersected by limes, whose intertwining branches make a fretted archway of living green, whilst the latter is the spot where the trade pageant, called Shrewsbury Show, is held. In addition to objects of interest which we have enumerated, our readers will find materials for observation and study for themselves; as a further aid to which, we would commend them to "Sandford's Guide to Shrewsbury." APPENDIX. GEOLOGY OF THE DISTRICT. We glanced in passing at some few features which could scarcely fail to attract the attention of the tourist, and a brief notice only of others will be needed for the geologist. In ascending the river we descend, geologically speaking, from an upper to a lower series of rocks, which rocks, in many instances, are covered over by fluviatile and marine deposits of sand and gravel, containing shells of fish inhabiting our modern seas. These show how recently the sea must have retired from a surface so covered with its remains; whilst their position low down in the valley, and but a little way above the present bed of the Severn, proves how much more recently the arm of the sea, known as the Severn Sraits, must have been succeeded by the river. The best places for collecting these remains along the railway will be found to be in embankments and cuttings near Buildwas and Coalbrookdale, the latter having yielded as many as twenty-two distinct species. In cuttings along the railway, and in their immediate vicinity, will also be found sections of rocks, from the variegated marls of the New Red Sandstone, of the Mesozoic, to the silurians, of the Palaeozoic, or Primary Formations. The coal measures of Coalbrookdale, with their alternating beds of coal, clay, and iron ore, are rich in specimens of the fauna and flora of the carboniferous age; the best places for discovering them being the spoil banks of the mines, where shale, and ironstone nodules, will be found the most productive. One of the richest beds yielding fossils is the Penneystone, which may be seen on the surface near Coalbrookdale and