“ The whole Androscoggin River gathers up its strength and plunges through a gorge,—a gateway in the solid rock is regular, as upright, as if man had brought in the whole force of his geometry and gunpowder to the admeasurement and excavation,—plunges, conscious of imprisonment and the insult to its slighted majesty,—plunges with fierce protest and frenzy of rage, breaks against a grim, unyielding rock to dash itself into a thousand whirling waves ”
Androscoggin River
Definition and stakes
Quotes about “Androscoggin River”
Collier's New Encyclopedia (1921)
“ The Androscoggin river, rising in Lake Umbagog, drains the N. E. and the E. mountain district is drained by the Saco. The Piscataqua, with its tributaries, the Salmon Falls, and the Cocheco, forms a S. E. basin. ”
Samuel Adams Drake,
The Heart of the White Mountains…
“ Why did not Nature so order it that mankind might rest like the trees, or shall we, like them, come forth at last strong, vigorous, beautiful, from that long refreshing slumber?Leaving the village, at the end of a mile and a half I took the road turning to the left, where Moose River falls into the Androscoggin, at the point where the latter, making a remarkable bend, turns sharply away to the north. Moose River is a true mountain stream, clear and limpid, foaming along a bed of sand and pebbles. ”
Various, The Continental Monthly, Vol. 2 No 4…
“ We found ourselves surrounded by intelligent people of the country—habitués who gave us all the local information we asked, told us when we came to 'Bryant's Pond,' and that the poor little shrunken stream that still brawled and fretted in its narrowed channel, along which we were gliding, was the Androscoggin. ”
Charles Mair,
Through the Mackenzie Basin
“ Thence the vast stream sweeps boldly into the south, and with a rush discharges down the rapids, and straight over the line of precipice, in a vast tumultuous greyish-drab torrent which speedily emerges into comparatively still water below. The rock here is an exceedingly hard, mottled limestone, resembling the stone at St. Andrew's Rapids on Red River. Where exposed it is pitted or bitten into by the endless action of wind and water, and lies in thick layers, forming an irregular dyke all along the shore, over the surface of which passes the portage, some forty yards in length. ”
Augustus Charles Gregory,
Journals of Australian Explorations
“ The general course of the river during the day was very little to the south of east, its banks still maintaining the same rocky and precipitous character, marks of inundation being frequently observed at the height of thirty feet above the present stream, which now was only running gently in a channel not more than thirty yards wide, but when in flood occupying the whole of the valley, which averages a quarter of a mile in width. The larger pools are lined with flags and reeds, and contain numbers of small fish resembling trout, similar to those found in the Lyons and Gascoyne Rivers. ”
Nathaniel H. Bishop,
Voyage of the Paper Canoe
“ The waters of these baby fountains are swollen by contributions from the streams, ponds, and lakes of the Adirondack wilderness, until along the banks of Fishing Brook, a tributary of the Hudson, the water is utilized at the first saw-mill. A few miles lower down the forests are vexed by the axe of the lumbermen, and logs are floated down the river one hundred miles to Glens Falls, where the State Dam and Great Boom are located. Half a million logs have been gathered there in a single spring. ”
Alexander Jardine, Narrative of the Overland Expedition of the Messrs…
“ November 18.—Cockburn Creek, now an important stream was followed down for four miles, when it formed a junction with the Staaten. The width of the main stream is about 400 yards, in many channels sandy and dry. It now runs generally west and very winding. The country and timber were much as before described, with the exception that a mile back from the river, (a chain of lagoons) generally occurs, some of them being large and deep and covered with lilies. Beyond, a waste of sandy tea-tree levels, thickly covered with triodia or spinifex, and other desert grasses. ”
S. Baring-Gould, A Book of the Cevennes
“ The Ardèche is certainly the most extraordinary river in Europe; after leaping, and burrowing, and sawing its way through basalt, it passes down a cleft of lias disposed in beds completely horizontal, and rising like the walls of houses. In fact, it traverses a long white street, many miles in length, and then enters the great ravine between lofty precipices of Dolomitic limestone, where runs no road, and where one must descend in a boat, shooting rapid after rapid in the midst of scenery only rivalled by the noted gorges of the Tarn. ”
Henry David Thoreau,
A Week on the Concord and Merrimack Rivers
(1849)
“ Unfitted to some extent for the purposes of commerce by the sand-bar at its mouth, see how this river was devoted from the first to the service of manufactures. Issuing from the iron region of Franconia, and flowing through still uncut forests, by inexhaustible ledges of granite, with Squam, and Winnipiseogee, and Newfound, and Massabesic Lakes for its mill-ponds, it falls over a succession of natural dams, where it has been offering its privileges in vain for ages, until at last the Yankee race came to improve them. ”
Richard Le Gallienne,
Pieces of Eight
“ With Charlie gone, and duck-shooting not being one of my passions, there was nothing to detain me in Andros. So we were soon under way, out of the river, and heading north up the western shore of the big monotonous island. We had some fifty miles to make before we reached its northern extremity—and, all the way, we seldom had more than two fathoms of water, and the coast was the same interminable line of mangroves and thatch palms, with occasional clumps of pine trees, and here and there the mouth of a creek, leading into duck-haunted swamps. ”
Various, The National Geographic Magazine…
“ The synclinal streams that entered the Anthracite lakes from the southwest may be named, beginning on the south, the Swatara, S, fig. 21, the Wiconisco, Wo, the Tuscarora-Mahanoy, M, the Juniata-Catawissa, C, and the Wyoming, Wy. One of these, probably the fourth, led the overflow from the Broad Top lake into the Catawissa lake on the middle Anthracite river. The Nittany highland formed a strong divide between the central and northwestern rivers, and on its outer slope there must have been streams descending to the Alleghany lowlands ”
Joel Cook,
America, Volume 6 (of 6)
“ The water-soaked bank shows fissures and help is implored—bells are rung, fleet horsemen arouse the neighborhood, the people assemble and try to stop the break. But the crumbling levee soon gives way, and the swollen and muddy current pours through with a roar like Niagara, the waters spreading afar over the lowlands, and thus by reducing the stream-level bringing relief to the river, but converting the adjacent region 422 for many miles into a turbid lake and ruining the crops. ”
Edward Hart, The silica gel pseudomorph and other stories (1924)
“ Fissure springs, from deep faults in the earth’s crust let out small streams of water from sources far remote; sometimes fit to drink; sometimes loaded with salts in solution and sometimes hot. Such a spring is that which gives rise to Willow Creek which rises among the niter hills of the Great Basin and empties into the Amargosa River a short distance below its source. Alas for the name! The Amargosa “River” turns out on examination to be a stream scarce large enough to turn a mill. After a run of less than 25 miles it sinks into the sands to rise no more. ”
Maturin M. Ballou,
Under the Southern Cross
“ But the truth is that it forms a watercourse dependent at present upon floods, admitting of navigation for hundreds of miles at certain seasons, and at others being as dry as the Arno at Florence or the Manzanares at Madrid. By a series of dams and canals this river might be navigable all the year round. The same remark applies to several of its tributaries, and to rivers generally running toward the inland centres [Pg 236] and flowing into the Murray. The governments of the several colonies have long realized the importance and the necessity of a grand and comprehensive system of irrigation. ”
Intercolonial Railway, Summer Provinces by the Sea
“ The Metabetchouan, an important stream, also flows into Lake St. John; and these rivers with the Chicoutimi, Marguerite, Ha-Ha, and numerous smaller rivers, all unite to swell the great flood of the almost bottomless Saguenay. There are numerous lakes north and south of the river, and, almost needless to state, the whole district abounds in mountain, gorge, and waterfall scenery of the wildest kind. Tumultuous rapids are everywhere ”
Wallace Walter Atwood, The Geography of the Region about Devil's Lake and the Dalles of the Wisconsin
“ At the bottoms of steep slopes, temporary streams build alluvial cones or fans. Along its flood-plain portion, a stream deposits more or less sediment on its flats. The part played by deposition in building a river flat has already been alluded to. A depositing stream often wanders about in an apparently aimless way across its flood plain. At the bends in its course, cutting is often taking place on the outside of a curve while deposition is going on in the inside. The valley of the Baraboo illustrates this process of cutting and building. ”
C. C. Andrews, Minnesota and Dacotah
“ It is seldom that they rise over two hundred feet from the water level, and their height is quite uniform, so that from a distant point of view their summit resembles a huge fortification. Nor, as a general thing, do they present a bold or rocky front. The rise from the river is gradual. Sometimes they rise to a sharp peak, towards the top of which crops out in half circles heavy ridges of limestone. The ravines which seem to divide them into separate elevations, are more thickly wooded, and appear to have been grooved out by the rolling down of deep waters. ”
Henry Rowe Schoolcraft,
Summary Narrative of an Exploratory Expedition to the Sources of the Mississippi River…
“ After passing through this, the river appeared very much in size and volume as it had on the outlet below Cass Lake. It winds its way through the same species of natural meadows, during which there is but little current. On ascending this channel but a short distance, the river is found to display itself in a second lake—which the natives call Pamitascodiac [159] —which, in general appearance and character, may be deemed the twin of Lake Andrúsia. On its upper margin, a tract of prairie land appears, of a sandy character, bearing [229] scattered pines. ”
Joel Cook,
America, Volume 4 (of 6)
“ The main tributaries of Ontario from New York are the Black, Oswego and Genesee Rivers. The Black River gathers various streams draining the western slopes of the Adirondacks, and its name comes from the dark amber hue of the waters. It flows northwest through a forest-covered region, pours down Lyons Falls, a fine cataract of seventy feet, passes the manufacturing towns of Lowville and Watertown, and finally discharges by the broadened estuary of Black River Bay into the east end of Lake Ontario. From Rome, on the Mohawk, a canal is constructed northward to the Black River. ”
Israel C. Russell,
North America
“ This is one of the most beautiful and most instructive examples of consequent drainage—that is, of streams whose direction has been determined by the inclination of the surface over which they flow—thus far discovered. Still another feature of much geographical interest is furnished by the rivers on the adjacent plain, two of which, branches of the Cheyenne River, cross the north and south extensions, respectively, of the Black Hills dome. ”
James Bruce,
Travels to Discover the Source of the Nile…
“ At a quarter past ten, we incamped at Addergey, near a small rivulet called Mai-Lumi, the river of limes, or lemons, in a plain scarce a mile square, surrounded on each side with very thick wood in form of an amphitheatre. Above this wood, are bare, rugged, and barren mountains. Midway in the cliff is a miserable village, that seems rather to hang than to stand there, scarce 166 a yard of level ground being before it to hinder its inhabitants from falling down the precipice. ”
F.C.S. Richard Anderson, Lightning Conductors: Their History…
“ It is especially so as regards the most important of points, that of the underground connection. Of course, wherever there is running water at hand, a river, or even a tiny stream that never dries, the matter is easy enough, but as in the great majority of buildings to be protected such water does not exist, the solution of the question becomes more difficult, and frequently one of the greatest perplexity. It tends even to be more and more so in consequence of the progress of sanitary arrangements under which towns and villages are ‘drained’ until the soil has been made as dry as a rock. ”
Daniel P. Thompson, Gaut Gurley; Or, the Trappers of Umbagog…
“ From the water's edge rose, deeply enshrouded in their bright green, flowing, and furbelowed robes of thickly interwoven pines, the undulating hills, back to the summit level of that long, narrow tongue of forest land, which, for many miles, only separates the Umbagog from the parallel Magalloway, the noble stream that here comes rushing down from the British highlands, to join the scarcely larger Androscoggin, almost at the very outset of its "varied journey to the deep." ”
Lewis Ankeny McArthur, Oregon Geographic Names (1952)
“ For several years federal authorities called the stream East Fork, but it was locally known as Little River. In 1926, at the suggestion of the writer, the USBGN officially named the stream Little Deschutes River, and this name has come into general use. ”
Henry Rowe Schoolcraft,
Summary Narrative of an Exploratory Expedition to the Sources of the Mississippi River…
“ Marie. The Ontonagon River is, with some difficulty, navigable by batteaux 36 miles, at which place, by the union of two smaller streams—one from an easterly and the other from a westerly direction—the main stream is formed. The mass of copper is situated on the western fork, at a distance of six or eight miles from the junction.The face of the country through the upper half of the distance from Lake Superior is uneven, and the irregularity is given it by hills of marly clay, which occasionally rise quite abruptly to the height of one or two hundred feet. ”
Julius Beerbohm, Wanderings in Patagonia; Or, Life Among the Ostrich-Hunters
“ With drooping reins we rode slowly on till we got to the river, now no longer the shallow stream which in summer one can wade over knee-deep, but a broad torrent, which eddied, swirled, and foamed, as it dashed rapidly over its stormy bed through banks which were already growing too narrow for its swollen waters. In the middle we could still see a single tuft of long grass, which was bending with the current, and this, Isidoro told me, grew on a little island, which when the river is fordable, 118 is several feet above the water's level. ”
Various, The National Geographic Magazine…
“ The points of agreement are indeed few and small. Perhaps the most important ones are that the Broad Top region is drained by a stream, the Juniata, which for a short distance follows near the course predicted for it; and that the Nittany district, then a highland, is still a well-marked divide although now a lowland. But there is no Anthracite river, and the region of the ancient coal-basin lakes is now avoided by large streams ”
Gordon Ross, Argentina and Uruguay
“ The huge irrigation scheme now being carried out will utilize an enormous natural hollow formerly known as the Cuenca Vidal, now rechristened Lago Pellegrini (after a once prominent Argentine statesman) as a natural storage reservoir. The surplus water from the lake and river system, which makes a network over the whole of the western part of the territories of Neuquen and the Rio Negro, at the base of the Andes, will be utilized for the irrigation of their eastern plains. ”
M. G. C. Hall, A Lady's Life on a Farm in Manitoba
“ The Government have cut good-sized ditches at right angles to the river, and they are found to be the only practical drainage which is feasible, and, when once cut and the water set running, have no tendency to fill up, but gradually wear deeper and broader, so that in time they almost become small rivers. ”
Joel Cook,
America, Volume 6 (of 6)
“ Whenever land can be reclaimed for agriculture or grazing on the flanks of the mountains and in the protected valleys and parks, it is done, so that the district has extensive irrigation canals, in some parts diverting practically all the available flow of water in the streams. This is particularly the case with the Upper Arkansas River, such diversion of the headwaters 464 in Colorado having robbed the river of its water to such a degree that the people of Kansas, whither it flows on its route to the Mississippi, are greatly annoyed and have protracted litigation about it. ”
