H. P by Sabine Baring-Gould — Read

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The river Vézère leaps to life among the granite of the Limousin, forms a fine cascade, the Saut de la Virolle, then after a rapid descent over mica-schist, it passes into the region of red sandstone at Brive, and swelled with affluents it suddenly penetrates a chalk district, where it has scooped out for itself a valley between precipices some two to three hundred feet high.

These precipices are not perpendicular, but overhang, because the upper crust is harder than the stone it caps; and atmospheric influences, rain and frost, have gnawed into the chalk below, so that the cliffs hang forward as penthouse roofs, forming shelters beneath them. And these shelters have been utilised by man from the period when the first occupants of the district arrived at a vastly remote period, almost uninterruptedly to the present day. When peasants live beneath these roofs of nature's providing, they simply wall up the face and ends to form houses of the cheapest description of construction, with the earth as the floor, and one wall and the roof of living rock, into which they burrow to form cupboards, bedplaces, and cellars.

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