Is a foft and rofy light befprent; And out to the dark rush waves of flame, The fun is coming. Hans looks around, Gracefully fwirling from bank to bank Wildly he ftruck, but forward fell, And under the clofing waters fank. When Hans the miller opens his eyes Flat on his back with his limbs outspread, Like a toad when crushed by a ploughman's tread ; But how he was fifhed up from the well, Or how sent spinning through the air, Is more than Hans the miller can tell While choking and coughing and gasping there. And now, And then it spreads like a fummer cloud A fhadowy form there Hans can see, "Lo! I go, Henceforth I cease to be thy friend, So low I may not bend, And covetous thou art, In the waters clear Of the well, Many a year Did I dwell, For nothing of evil came it near : It has polluted been by thee; Under the spreading tree The grafs is green – The cloud floats flowly over the mill For his bones are aching every one, "There was truth after all in Frau Grethel's old fong; I wish I had left the WELL alone!" The Hill-Man. "The avalanche, the thunderbolt of fnow." The Hill-men or Dwarfs of Switzerland lived among the inacceffible peaks of the upper Alps, pafturing and tending their flocks-not of sheep or goats, but of wild chamois, a cup of whose milk received from the hands of a Hill-man, its rightful owner, like the widow's crufe of oil, "failed not." Although thus living remote from the dwellings of men, they not unfrequently came to the folitary chalets on the lower Alps, bringing to the disconsolate herdsman stray lambs or goats; and on occafions they also descended into the valleys, to give to the inhabitants of the villages timely warning of coming ftorms, floods, avalanches and landflips: for the Hill-men, from their great knowledge of the conditions and changes of the elements, and from their living in the upper regions of the earth, where all primary elemental changes are wrought, knew the time, the force, the direction and the duration of was forming, when it would be diflodged from its giddy ledge, and upon what part of the terrified valley it would be precipitated. “The natives of the Alps distinguish between several kinds of avalanches. The ftaub-lawinen (duft avalanches) are formed of loose fresh-fallen fnow, heaped up by the wind early in the winter, before it has begun to melt or combine together. Such a mass, when it reaches the edge of a cliff or declivity, tumbles from point to point, increasing in quantity as well as in impetus every instant, and spreading itself over a wide extent of furface. It defcends with the rapidity of lightning, and has been known to rush down a distance of ten miles from the point whence it was first detached, not only descending one fide of a valley, but also ascending the oppofite hill, by the velocity acquired in its fall, overwhelming and laying proftrate a whole forest of firs in its descent, and breaking down another foreft up the oppofite fide, fo as to lay the heads of the trees up the hill in its ascent. "Another kind of avalanche, the grund-lawinen (ground avalanche) occurs in fpring, during the months of April and May, when the fun becomes powerful, and the fnow thaws rapidly under its influence. * * * * This fpecies is more dangerous in its effects, from the fnow being clammy and adhesive, as well as hard and compact." The legend of "The Dwarf feeking lodging" is variously related, and more than one valley in Switzerland can fhow the tomb of a village, and claims for it the catastrophe of the ballad. THE HILL-MAN. FOR weeks had the fnow, and the fnow alone, But a sturdy wind leaped up at last From a mountain gorge where it long had flept; And as down through the glens it shouting past Came the mifts and the vapours following faft, And out and over the vale they swept; Like the willing vaffals of warrior lord Who follow his foot and who wait his word. The trees are stirred and their branches all Caft their heavy burdens to the ground, And erect upfpring, like men from thrall And the setting fun disdains to throw |