Part 6

The hills are strewn with great boulders left here in the Glacial Age, which rest, poised as monuments of that mystical period. Especially interesting are the dimpled erosions upon one boulder, which rests just northeast of the lakelet, upon the ridges sloping eastward toward the sphagnous swamp. There are visible deep scratches, hollows, arches and miniature pillars, which the whirling eddies of the perilous waves have eroded during the ages unknown. Higher on the summit of the Hoosac rests another immense rock known to students of geology as the “Great Vermonter.” It is said to have been brought from the marble and granite heights of Vermont, imbedded in the ice-drift. Through the melting of the glacial sheet, one of the drifting bergs left this hero of the ages as we may see it now, moored and balanced high on old Hoosac’s brow.

The geological surveys of northern Massachusetts, by President Hitchcock of Amherst in 1838, early identified all of the low, round hills to be seen southward from Aurora’s Lake as the result of glacial action. Mount Greylock’s Brotherhood is a group of giant glacial hills, as it were, and is the highest pile of Taconic formation in this State. The erosions of the great ice-sheet are plainly seen on the rocky summits of these mountains, and only time and the decay of the rock itself will do away with these scars of that mystical age. The name of “Greylock” appears to be derived from the lowering cloud-mist so often capping the whole Brotherhood at early dawn or before a storm.

Vermonters who, from the hills at a great distance to the north, view this group of mountains, depend upon this capping of clouds as a forecast of the weather. Among the old folk, it is known and designated as “Greylock’s Nightcap,” a portent of a coming storm.

Mount Greylock, the highest swell of this range, is 3600 feet above sea level, and commands a variable and extensive view from its bald summit, on which was early erected that first wooden observatory, during President Griffin’s term at Williams College. Here the poet and the philosopher, Hawthorne and Thoreau, have climbed to meditate.

Many a message has gone forth from these heights to bless the busy world. Scarcely is there a son of old Williams who does not recall the mountain-day excursions led by Professor Albert Hopkins, and the glory of old Greylock at dawn and at the sunset hour.

Thoreau writes of it: “It would be no small advantage if every college were thus located at the base of a mountain, as good at least as one well-endowed professorship. It were as well to be educated in the shadow of a mountain as in more classical shades. Some will remember, no doubt, not only that they went to college, but that they went to the mountain. Every visit to its summit would, as it were, generalize the particular information gained below, and subject it to more catholic tests.”

The peak especially designated as Saddleback Mountain is at the junction of the eastern abutments of that huge wall of Taconic Brotherhood which appears south of the old battle-ground where formerly stood the early border Fort Massachusetts, on the Harrison flats, near the flag station of Greylock. The union of Mount Williams, sloping to the east, and Prospect Mountain to the west forms the seat of the saddle.

Mount Hopkins—so named in honor of Professor Albert Hopkins of Williams, the first nature-student of our land, making excursions afield in 1833—lies south of these. Old Greylock, proper, lifts its lofty brow still farther south, being situated about in the centre of this great range as it extends from east to west.

Beyond Greylock stretches a long, misty line of blue peaks against the sky, which if observed from Mount Œta at the north, in Bennington County, Vermont, may be traced to the southwest to Symond’s Peak, the lowest of the group, named in memory of Captain Symond, who led the volunteer forces from our hills and vales to the memorable Battle of Bennington in 1777. Bald Mountain is also in the vicinity, and the closing in of these several peaks has conspired to form what is known as the “Hopper,” and the “Heart of Greylock.” The hollow vale amid these heights has the appearance of the hoppers used by millers years ago.

Surely in the heart of the Taconics we are in one of the oldest rock formations of the earth, and the green terraced stairs lead us slowly down to the deep-set valley of the Hoosac, where once slept that ancient lake. All that now remains of that Lake of Dawn is pocketed in the basin under the Hoosac. The shores of Aurora’s Lake are lonely and still, save for the marsh thrushes which skim low over the waves and whistle shrilly. The groves of pine to the southeast are the haunts of solitude, and those who wander here can well imagine that the Æolian harps among the whispering trees are repeating a music of ages past, when only wind and waves were known to these hills.

Amid these damp and reedy shores and swampy woods are tall brakes and delicate Maiden-Hair Ferns. Here, too, the tall and stately Royal-Fern (Osmunda regalis) flourishes in deep seclusion, sheltered by the low-branching pines along the shore. It grows from two to four feet high in this locality, and is of a deep rich crimson-green tone against the grasses and bushes near. Mounds of moss, marking one of the trees of a primitive forest rotting below the soil, are thickly carpeted with the leaves of the Dog’s-Tooth Lily. Indeed, the picturesque paths which lead through these woods wind through a veritable fairy-land of flowers and ferns. One of these trails runs southward through rocky pastures, swamps and thickets, toward the Tunnel’s western gate.

Along these slopes, among the limestone rocks, I found rows of the Ebony Spleenwort Fern, rather rare in this much-travelled way; and on the brow of this ridge were many species of common fern. The pastures are barren and dry, with few bushes to break the dreary horizon, as one approaches the western portal of the Tunnel.

I came upon one lone Apple-Thorn bush, of genus Cratægus of the Apple Family. Nearly opposite, across the valley of the south branch of the Hoosac, which the Indians named the Ashuilticook, may be distinguished the smoking Limekilns; while still farther southward, the white-spired village of Adams nestles at the base of Greylock, which towers serenely above the shaggy shoulders of Ragged Mountain. I wandered about the edges of the Tunnel cliffs where, in years gone by, had stood the impoverished cabins which sheltered the laborers who tunnelled the Hoosac. I descended into the chasm and seated myself upon the wall of rocks, waiting for the trains to appear and disappear at the portal in the side of the hill. Presently one from the West crept ponderously into the cavern. The echoing roar was smothered, and died slowly away until it became an indistinct murmur. Not long afterward I felt, as well as heard, the low breathings and rumblings of a locomotive coming in the opposite direction. I heard its subterranean groans as of a great spirit, while the smoke poured forth, pushed in volumes before the engine, wreathing and curling about it as it emerged, and partially concealing its grim outlines.

The faithful watchman, a modern Eckhart, sits before the entrance of the Western Gateway of Hoosac Mountain, and warns the people against entering through this portal to the greater world that lies beyond. It is as if he wished to guard these children of the marble highlands from the risks attendant upon the wild whirl of life beyond these quiet hills.

The sun was setting as I left him, calm but alert, at his post of duty, trimming and lighting his colored lanterns for signals of danger or safety to the approaching trains. Climbing up by the path which passes the little red cottage on the crest of the hill on the north bank of the chasm, I returned leisurely homeward, winding over the hillsides, far above Aurora’s Lake, then down along the borders of the swamp-lands. In the crevices of rock were creeping colonies of the Common Polypody (Polypodium vulgare). Along the edges of this bog are still seen the primeval stumps of the pine and hemlock forests, which clothed these hillsides when only the Redmen dwelt and hunted among these wildernesses.

In May and early June these decaying stumps are usually draped with Painted Trillium and the delicate vines of Gaultheria and the Creeping Snowberry, while the Arbutus trails about luxuriantly, covering up the ruins of years.

Ball Brook and the Bogs of Etchowog

Fringing the stream, at every turn Swung low the waving fronds of fern; From stony cleft and mossy sod Pale asters sprang, and golden-rod.

WHITTIER, The Seeking of the Waterfall.

On May 25th I reached Pownal, Bennington County. Upon the following day I explored the great swamps of Etchowog. Prepared with luncheon, vasculum, basket for roots and my hound Major, I started on one of those happy excursions such as Thoreau recommends we should take, “in the spirit of undying adventure, never to return,—prepared to send back our embalmed hearts only as relics to our desolate kingdoms.”

Ball Brook, a sluggish stream flowing northwardly to East Pownal swamps—commonly called the Bogs of Etchowog—has its source in the marshy hillsides northwest of the schoolhouse in District Fourteen. Two streams flow from this valley. One is called Ladd Brook, running southwesterly and following the windings of the shady Ladd Road to Pownal village, where it joins the Hoosac River. The other stream, Ball Brook, flows north and northeast onward through innumerable and unfathomable swamps, to Bennington village, ten miles north, there meeting the Walloomsac River, which is also a tributary of the Hoosac, farther northward in its course. This brook is rich in a continuous chain of peat bogs—rich from an orchid-hunter’s point of view.

Although I have been familiar with this region from childhood, viewing it from the roadside only, I never at any time had ventured to follow Ball Brook through all its meanderings to the Bogs of Etchowog near Pownal Pond, a distance of some three miles. This would not be a long walk on a fair road, but it becomes rather dangerous and formidable when leading through quaking marshes in the soaking currents of a stream.

A short distance to the right, north of the schoolhouse in Number Fourteen, there is an old pathway nearly overgrown with bushy pines and birch and chestnut underbrush. This I followed, entering the hollow under the brow of the hill, and passing along the wood road which skirts the margins of one of the deepest, darkest jungles in these regions. The old people look upon it as akin to “Witch Hollow,” on the Gulf Road near by, and tell strange tales of ghosts, and of some mythological peddler who was swallowed here in the black mud of this ancient tarn, after having been robbed of his fine silks and precious jewels.

Weird, hollow drummings issue and echo through these shaded vales from time to time. Probably they are due, however, to nothing more startling than the alarum of a partridge, or the hoot of the screech-owl; or the creaking and rubbing of partially fallen trees against their supporting brothers, voicing a portent of coming storm. I hear in this woodland seclusion little save the whispering of the winds, the sighing of the pines, and snapping of dead twigs, mingled with the chorus of the thrushes. The first settlers here about interpreted these wood-sounds far differently; then the primeval forests were dense, and the noises were deep and full of mystery, and there was fear of the Redman’s war-whoop. As Burroughs writes: “The ancients, like women and children, were not accurate observers. Just at the critical moment their eyes were unsteady, or their fancy, or their credulity, or their impatience got the better of them, so that their science was half fact and half fable.... They sought to account for such things without stopping to ask, Are they true? Nature was too novel, or else too fearful to them to be deliberately pursued and hunted down.”

I stopped on a corduroy bridge to draw on my high-water boots and rubber gloves, for one feels safer when entering this dense swamp if protected from poisonous roots and foliage, biting insects and things that creep and crawl.

I had started out with small belief that I would find any prime blossoms of the Orchid Family, for nothing of importance had yet unfolded in Aurora’s Swamp in North Adams. But when I penetrated the heart of these rich, warm glooms, I found waiting for me a fragrant company of Dwarf Yellow Lady’s Slipper (Cypripedium parviflorum); and innumerable Stemless Pink Lady’s Slippers, more frequently called the Indian’s Moccasin-Flower (Cypripedium acaule), stood as sentinels on the dryer edges of the swamp.

The Marsh Marigolds were here also in their last stages, fading away, but still sufficiently bright; with the late indigo-blue violets, which rear their faces at least a foot high above the dark pools, to carpet the marsh with gold and purple. Poison Ivy cropped out frequently among these graceful orchids,—a beautiful vine, although unfriendly to man.

It is difficult to describe the dense gloom of this bog, closed in on all sides by high rock-bound hills, which are clothed with pine and yellow birch trees, and which in their turn are but foothills to the higher watershed. It seems to have been a receiving basin for the waste and wear of the heights above for thousands of years. Here are fallen trees of every variety common in southwestern Vermont, and these prostrate giants helped to form a safe footing through the quaking bogs.