GUERNSEY
GUERNSEY:
CÆSAREA—SARNIA.
Passing between the point of Vale and Herm, we are directly off the harbour of St. Peters Port, its fort of Castle Cornet crowning an isolated granite rock, southward of the pier, which now connects it with the shore, and forms the harbour of refuge. The coup d’œil assumes a perfect Norman aspect, and the costume, dialect, and manners are in just harmony with the scene. The marine quarter of the “town,” as it is par excellence termed (and indeed there is no other in Guernsey), especially the old church, the hotels, and wineshops, of dark grey stone, with which the quay is lined, is perfectly continental. The shops and offices, of more modern aspect, compose the streets; the dwellings of the opulent, among which Castle Carey is conspicuous, are chiefly on terraces along the abrupt escarpment; Elizabeth College, the modern church, and the Victoria Tower, by the cemetery, on the new ground, being the most prominent public objects. The old church on the quay, dating about 1120, is crucial, the interior being darkened by its massive columns and heavy galleries.
The marble slabs of the fish-market are profusely supplied with choice fish—turbot, dorey, and very fine crustacea; and the stalls teem in the season with the treasures of Pomona.
The education at the College is economical, about £12 per annum; the cost for living with the Principal not exceeding £60.
The influence of this facility of learning will enlighten the minds even of the unlettered islanders, among whom there is a prevalent superstition. The belief in witchcraft may still be discerned, although it is now two centuries since women were tortured, hung, and burned under this demoniac creed.
The scenic quality both of the interior and of the eastern and northern coasts of Guernsey is mere prettiness. On the south, however, from Fermains Bay to Rocquaine it is buttressed by some of the most magnificent rocks in the Channel, the land gradually descending from them northward. The coast rocks on the east, south-east, south, and south-west, from Saline to Rocquaine, are of gneiss, those of Rocquaine are of schist, and thence they are granitic.