waves, it is said that an old order for the repair of Hanois roads is still extant. That Vazon and the Braye du Valle were the sites of forests is indisputable, though the former is now a sandy bay into which the Atlantic flows without hindrance, and the latter, reclaimed within the present century by an enterprising governor, formed for centuries a channel of the sea by which the Clos du Valle, on which the Vale Church stands, was separated from the mainland. A stratum of peat extends over the whole arm of the Braye, while as regards Vazon there is the remarkable evidence of an occurrence which took place in December, 1847. A strong westerly gale, blowing into the bay concurrently with a low spring tide, broke up the bed of peat and wood underlying the sand and gravel, and lifted it up like an ice-floe; it was then carried landwards by the force of the waves. The inhabitants flocked to the spot, and the phenomenon was carefully inspected by scientific observers. Trunks of full-sized trees were seen, accompanied by meadow plants and roots of rushes and weeds, surrounded by those of grasses and mosses; the perfect state of the trees showed that they had been long buried under the sand. Some of the trees and boughs were at first mistaken for wreckage, but the fishermen soon discovered their error and loaded their carts with the treasure locally known as "gorban." Subsequent researches have shown that acorns and hazel-nuts, teeth of horses and hogs, also pottery and instruments of the same character as those found in the cromlechs, exist among the Vazon peat deposits. There is therefore abundant evidence that the legends relating to the former inhabitants of the forest are based on traditions resting on an historical foundation.

     PREFACE.

     ILLUSTRATIONS

     CHAPTER I

    .—TRADITION

     CHAPTER II

    .—SUPERSTITION

     CHAPTER III

    .—DEVOTION

     CHAPTER IV

 Prev. P 2/44 next