-Gould
Brittany
PREFACE
Brittany can hardly claim the attention of the tourist as a superlatively beautiful country. The way in which trees are clipped and tortured out of shape disfigures the sylvan landscape; and of mountain scenery there is none. The ranges of the Montaignes Noires and the Monts d'Arrez are insignificant. Yet the valleys are pretty, but never grand. The charm of Brittany is to be found in the people and in the churches. The former with their peculiar costumes, and their customs are full of interest, and the latter are of remarkable beauty and quaintness. The ordinary tourist will hardly see much of the costume unless he attends a pardon, the Patron of the Irish peasant; the patronal feast at some chapel frequented only on the day of the pardon. But the student of men and manners will find much to interest him at such a gathering. The churches are of extraordinary beauty, they are for the most part of granite, but of a fine-grained granite that lends itself to elaborate carving. And the kersanten stone is employed, a dark volcanic product that is undercut and preserves its sharpness through centuries, and is employed for carving of lace-like delicacy. The coast scenery is fine, but not of the finest description, and varies very greatly from the granite cliffs of Finistère to the sandy dunes of the Morbihan. The towns are not comparable to those of Normandy for the number and richness of their mediæval domestic buildings, but are set in far more charming surroundings. The cathedrals are, for the most part small, Quimper and S. Pol de Léon and Tréguier have the finest, but these are of a French type, whereas the village churches possess a stamp peculiar to Brittany, where spared. Unhappily a passion has possessed the people of late to pull down their ancient churches and build new Houses of God in very questionable taste. In the diocese of Vannes the modern architecture is execrable, but the architects of Quimper are of a vastly higher type. They follow the old lines, and imitate what is good, whereas in the Côtes du Nord and in Morbihan, the modern work is insufferably vulgar and bad. The whole country teems with prehistoric antiquities, but these will only interest those who have made such monuments a special study; nevertheless Carnac and Locmariaquer and Gavr' Inis cannot fail to impress the ordinary traveller with a sense of astonishment at the majesty of the rude architecture of a lost and mysterious people of whom almost nothing is known, and whose one religious idea seems to have been, the cult of the dead.
The people are intensely religious. Religion is their passion; and the efforts made by the Republican government to tread it down, and to de-Bretonise the people, have only intensified their religious and national enthusiasm. The Breton peasant is said to have a hard head. He is obstinate and resists outside pressure to alter his creed or his customs. The old Royalist tendency of the Breton is a thing of the past. He is content to be under a republic, if the republic will only leave him alone. Fishing and shooting may be obtained on easy terms, and both are good. The roads are excellent for the cyclist, and the costumes and the architecture present inexhaustible subjects for the camera. The inns are always clean, the charges are moderate, and the fare very passable. No part of Europe is so accessible, and contains so much of interest in varied directions as Brittany. It is a delightful land for a brief visit, it is full of matter for study by one who can make there a prolonged stay. The climate is mild, and not so rainy as the West of England and Wales. The kindly people will always treat a traveller with gracious courtesy. But Brittany, it must be remembered, is divided into two very distinct portions, that in which only French is spoken, and that in which the language is Breton, closely akin to Welsh. And of Brittany, by far the most interesting portion is Finistère, where old costumes and old customs are clung to more tenaciously than elsewhere.
S. B. G.
I. General Features and Geology
Brittany, the extreme Western promontory of the North of France, comprises the five departments of Côtes-du-Nord, Ille-et-Vilaine, Finistère, Morbihan, and Loire-Inférieure. It is distinguished into Upper and Lower Brittany. In the former the French language is spoken, in the latter the Breton, and French is an acquired tongue.
The back-bone of Upper Brittany is the chain of the Menez that runs from East to West, and then branches, forming on the North the Montagnes d'Arrée, and on the South, the Montagnes Noires. The system may be likened to a hay-fork or a pair of tongs, where the prongs of the fork form the above-named ranges. The whole rests on an elevated plateau that slopes to the sea North and West, and on the South dies down into the plain of the Vilaine and the Loire.
On the North this plateau is seamed by the rivers that have cut narrow valleys and ravines through which they make their way to the sea. Such are the Rance, the Gouet, the rivière de Morlaix, with the result that there is no coast-road, and the traveller passes along the main arteries of traffic at some distance from the sea, catching a glimpse of it only once at the Anse d'Iffinac, and has to branch off from it to the coast so as to make acquaintance with the bold and picturesque coast.
The mountain range is nowhere high, and rarely reaches a thousand feet. The highest point is the Mont Saint Michel which attains to slightly over 1200 ft. The freshman arriving at Cambridge asked where was the Gogmagog range, and was told that he might see it when an intervening cart got out of the way. Owing to the ridges rising out of an elevated plateau, they are almost as insignificant as the Gogmagogs. However, the Menez-hom most nearly attains to the dignity of a mountain, as it stands above the Bay of Douarnenez, reaches however only to 990 ft.
Along the Western confines of the department of Ille-et-Vilaine, the Menez spreads out into high tableland sown with lakelets acting as feeders to the Vilaine.
The Monts d'Arrée, starting from the Coat-an-Noz in Côtes-du-Nord, extend to the peninsula of Crozon, they attain their highest point at the Mont S. Michel, and decline as they approach the sea. They rarely rise 300 ft. above the tableland on which they are planted, and this prevents them from having an imposing appearance.
The Montagnes Noires flank the central plain on the South. Their maximum height is 1050 ft. After running S.W., they bend abruptly towards the N.W., and terminate in the Menez-hom in the Crozon peninsula.
In the Morbihan, the Lande de Lanvaux, running from W. to N.E., extends 50 kilometres, and rises to the height of from 240 to 320 ft. between the basins of the Claye and the Arz which unite at Redon to feed the Vilaine.
The North coast of Brittany is eaten into bays from which the sea retreats to considerable distances, and is fringed with reefs and islands. It is a favourite resort of Parisians, throughout its stretch, from Dinard to Plestin.
The West of this peninsula is torn into shreds of promontories with deep inlets between them. The promontories of S. Mathieu, Crozon, Sizun, and Penmarch are bald, but bold. Below the point of Penmarch the coast rapidly trends S.E. and alters in character; it loses its bleak desolation and ragged rocky nature, and forms landlocked seas, as those of Belz and the Morbihan; and the rocks make way for sand-dunes. The island chain that constitutes a natural breakwater to the bay of Quiberon is the wreckage of the barrier of another inland sea, broken up by the Atlantic surges. South of the mouth of the Loire the island of Noirmoutier stretches almost sufficiently far out to enclose another.
The plateau formation of the country is not conducive to beauty, and its lovely sites must be sought in the valleys, and its wildest scenes on the coast. The deep cleft ravine of the Rance, the sweet valley of the Elorn, that of the Aulne, canalised, the Blavet, the Laïta and the Arz, will richly repay tracing upward.
The promontories of Crozon and Sizun till of late years were bare and untilled, and heath-grown; but the use of sardine heads as manure has given a great impetus to agriculture, and the demand for fir balks for the South Welsh mines has caused the planting of vast tracts with the Austrian pine.
The geological structure of Brittany is simple. It consists of an immense upheaval of granite through beds of Silurian and Cambrian schist. Rare deposits of lime occur in the folds of these beds. Dykes of quartz and diorite have traversed the schist and granite, and
