SOURCES OF THE HUDSON.

The noble Hudson River, which we have ascended to Glen's Falls, flows

out of the great Adirondack wilderness of Northern New York, the

headwaters draining its extensive southern declivity. Among these

virgin Adirondack woods and mountains, near the Long Lake, is the

remote source of the western branch of the Hudson, the "Hendrick

Spring." Surrounded by forest and swamp, this cool and shallow pool,

about five feet in diameter, fringed by delicate ferns, and overhung

with vines and shrubbery, is the beginning of the great river, and

named in honor of its discoverer and first explorer:

"Far up in the dim mountain glade,

Wrapped in the myst'ry of its shade,

On a cold rock, a dewdrop fell,

And slumbered in its stony shell,

Till brewed within its rocky bed,

There trickled out a silver thread,

A little, shy, lost waterling,

That marks the cradled mountain spring."

The Hendrick Spring is within a half-mile of Long Lake and upon the

same summit, the latter discharging its waters northward into the St.

Lawrence. The little stream from this source gathers force, and flows

through a chain of brooks and ponds to the lovely Catlin Lake. High

peaks environ them, and their swelling waters make much of the river

on coming to the confluence with the northern branch of the Hudson at

the outlet of Harris Lake. Here there blooms, all about, the splendid

cardinal plant, its showy flower glowing like a flame.

The most elevated fountain head of the Hudson is upon the northern

branch. Within the inmost recesses of the mountain wilderness, in a

ravine between two of the highest peaks, the river has its spring

nearest the sky, known as "The Tear of the Clouds," a lofty pool,

adjacent to one of the noted Adirondack portages, the Indian Pass, at

about forty-three hundred feet elevation above the sea. From this pool

the water flows out through the Feldspar Brook into the Opalescent

River, which does not go far before it tumbles down the picturesque

cascade of the Hanging Spear, leaping fifty feet into a narrow abyss

between perpendicular walls, and emerging among a mass of huge

boulders. All these rocks, like the greater part of the Aganus-chion,

or Black Mountains, as the Indians often called the Adirondacks, are

composed largely of the labradorite or opalescent feldspar, which

fills the stream-bed with beautiful pebbles of blue or green or gold,

many of them having all the colors. Thus glittering with the splendors

of its rich coloring under the sunlight, the Opalescent River falls

into Sandford Lake. A visitor to the Indian Pass says the explorers

entered the rocky gorge between the steep slopes of Mount McIntyre and

the cliffs of Wallface Mountain to the westward. Clambering high above

the bottom of the canyon, they could see the famous Indian Pass

between these mountains in all its wild grandeur. Before them rose a

perpendicular cliff nearly twelve hundred feet from base to summit,

its face being apparently as raw as if only just cleft. Above sloped

Mount McIntyre, still more lofty than the cliff of Wallface, and in

the gorge between lay piles of rocks, grand in dimensions and awful in

aspect, as if hurled there by some terrible convulsion. Through these

came the little stream going to the Hudson, bubbling along from its

source close by a fountain of the Ausable. In spring freshets their

waters commingle, part finding their way to the ocean at New York and

part at Newfoundland.

Still another spring of clear cold water is a source of the Hudson,

sending down the mountain side a vigorous rivulet, falling into the

Opalescent. This fountain bubbles from a mass of loose rocks, some

weighing a thousand tons apiece, about a hundred feet from the summit

of the noble Mount Marcy, which the Indians called Tahawus, the

"Sky-piercer." From these sources among the Adirondacks flows the

most important river of New York, uniting the waters of myriads of

lakes and springs to form the noble stream which is picturesque and

attractive throughout the whole of its course of three hundred miles

to the sea. The main branches of the upper Hudson unite almost under

the shadow of Tahawus, and flowing a tortuous course, it receives the

outlet of Schroon Lake, the largest in the Adirondacks, covering about

twenty square miles, the junction-point being but a short distance

west of Lake George. Then flowing southward and turning eastward, it

emerges from the mountain wilderness, and in about a hundred miles

reaches its great cataract at Glen's Falls. Sweeping around the grand

bend below, and tumbling down Baker's Falls, past Fort Edward and the

rapids of Fort Miller, it receives the largest tributary from the

eastward, the Battenkill, a rapid shallow stream flowing from the

Green Mountains of Vermont. Thence its course is southward, every mile

from the wilderness to the sea being replete with historic and scenic

attractions:

"Queen of all lovely rivers, lustrous queen

Of flowing waters in our sweet new lands,

Rippling through sunlight to the ocean sands,

Within a smiling valley, and between

Romantic shores of silvery summer green;

Memorial of wild days and savage bands,

Singing the patient deeds of patriot hands,

Crooning of golden glorious years foreseen."

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