If one of these inlets, mere fissures to the eyes of the eider-ducks, is wide enough for the sea not to freeze between the prison-walls of rock against which it surges, the country-people call the little bay a “fiord,”--a word which geographers of every nation have adopted into their respective languages. Though a certain resemblance exists among all these fiords, each has its own characteristics. The sea has everywhere forced its way as through a breach, yet the rocks about each fissure are diversely rent, and their tumultuous precipices defy the rules of geometric law. Here the scarp is dentelled like a saw; there the narrow ledges barely allow the snow to lodge or the noble crests of the Northern pines to spread themselves; farther on, some convulsion of Nature may have rounded a coquettish curve into a lovely valley flanked in rising terraces with black-plumed pines. Truly we are tempted to call this land the Switzerland of Ocean. Midway between Trondhjem and Christiansand lies an inlet called the Strom-fiord. If the Strom-fiord is not the loveliest of these rocky landscapes, it has the merit of displaying the terrestrial grandeurs of Norway, and of enshrining the scenes of a history that is indeed celestial. The general outline of the Strom-fiord seems at first sight to be that of a funnel washed out by the sea. The passage which the waves have forced present to the eye an image of the eternal struggle between old Ocean and the granite rock,--two creations of equal power, one through inertia, the other by ceaseless motion. Reefs of fantastic shape run out on either side, and bar the way of ships and forbid their entrance. The intrepid sons of Norway cross these reefs on foot, springing from rock to rock, undismayed at the abyss--a hundred fathoms deep and only six feet wide--which yawns beneath them. Here a tottering block of gneiss falling athwart two rocks gives an uncertain footway; there the hunters or the fishermen, carrying their loads, have flung the stems of fir-trees in guise of bridges, to join the projecting reefs, around and beneath which the surges roar incessantly. This dangerous entrance to the little bay bears obliquely to the right with a serpentine movement, and there encounters a mountain rising some twenty-five hundred feet above sea-level, the base of which is a vertical palisade of solid rock more than a mile and a half long, the inflexible granite nowhere yielding to clefts or undulations until it reaches a height of two hundred feet above the water. Rushing violently in, the sea is driven back with equal violence by the inert force of the mountain to the opposite shore, gently curved by the spent force of the retreating waves.