Flows Sentence Examples

Nevertheless, under some of these flows remains of plants and insects of species now living in the islands have been found - a proof that the formation as well as the denudation of the country is, geologically speaking, recent.

Thence the river flows S.E.

The river flows in exquisite wooded reaches, navigable only for small boats.

On this view the water flows upwards under the influence of variations of pressure and tension in the vessels.

The Chu rises in the Tian-shan Mountains and flows north-westwards through Akmolinsk; and the Naryn flows south-westwards along a longitudinal valley of the Tian-shan, and enters Ferghana to join the Syr-darya.

The Guaira river, a branch of the Tuy, traverses the plain from west to east, and flows past the city on the south.

The Chi Tandui, also rising here, flows south-east to the Indian Ocean, and alone of all the rivers in this province is navigable.

The Serchio (anc. Auser), which joined the Arno at Pisa in ancient times, now flows into the sea independently.

The Chambal is by far the largest river in Rajputana, through which it flows for about one-third of its course, while it forms its boundary for another third.

Suppose the key to be depressed, then a current flows through one winding of the differential relay to line and through the other winding and rheostat to earth.

In this case no current flows from the battery through the line or instruments, the whole action being inductive.

To the sending currents, however, the bridge offers only apparent ohmic resistance due to the fact that the current entering the mid-point of the winding flows through the two halves or arms in opposite direction, and, owing to the winding being on the same iron core, the mutual inductive effect of the two arms on one another neutralizes the self-induction to the sending currents.

The river, which flows between the castle-hill and the powerfully armed fort of San Cristobal, is crossed by a magnificent granite bridge, originally built in 1460.

A current then flows and in passing round the circuit operates the line relay, with the result that the calling-lamp is lighted.

Of these the Dora (called for distinctions sake Dora Riparia), which unites with the greater river just below Turin, has its source in the Mont Genèvre, and flows past Susa at the foot of the Mont Cenis.

The next great affluent of the Po, the Adda, forms the outflow of the Lake of Como, and has also its sources in the Alps, above Bormio, whence it flows through the broad and fertile valley of the Valtellina for more than 65 m.

The Adda flows out of the lake at its south-eastern extremity at Lecco, and has thence a course through the plain of above 70 m.

It flows by Lodi and Pizzighettone, and receives the waters of the Brembo, descending from the Val Brembana, and the Serio from the Val Seriana above Bergamo.

The Arno, which has its source in the Monte Falterona, one of the most elevated summits of the main chain of the Tuscan Apennines, flows nearly south till in the neighborhood of Arezzo it turns abruptly north-west, and pursues that course as far as Pontassieve, where it again makes a sudden bend to the west, and pursues a westerly course thence to the sea, passing through Florence and Pisa.

The Elsa and the Era, which join it on its left bank, descending from the hills near Siena and Volterra, are inconsiderable streams; and the Serchio, which flows from the territory of Lucca and the Alpi Apuani, and formerly joined the Arno a few miles from its mouth, now enters the sea by a separate channel.

The most considerable rivers of Tuscany south of the Arno are the Cecina, which flows through the plain below Volterra, and the Ombrone, which rises in the hills near Siena, and enters the sea about 12 m.

In its lower course it flows near Canosa and traverses the celebrated battlefield of Cannae.

The united stream breaks through the mountains to the south, and, receiving on its way the Patnotz Su (left) and the Khinis Su (right), flows south-west, west and south, through the rich plain of Bulanik to the plain of Mush.

Below the junction of the two arms the Euphrates flows south-west past the lead mines of Keban Maden, where it is 120 yds.

At the ferry on the Malatia-Kharput road (cuneiform inscription) it flows eastwards in a valley about a quarter of a mile wide, but soon afterwards enters a remarkable gorge, and forces its way through Mount Taurus in a succession of rapids and cataracts.

Hirmas) flows south through the land of Gozan in which Sargon settled the deported Israelites in 721 B.C. At the mouth of the Khabur stood the Roman frontier fortress of Circesium (Assyrian, Sirki; Arab.

Under the Arabs the old designation again prevailed and the Euphrates is always described by the Arabian geographers as the river which flows direct to Kufa, while the present stream, passing along the ruins of Babylon to Hillah and Diwanieh, has been universally known as the Nahr Sura.

The important river Lofa flows nearly parallel with the St Paul's river and enters the sea about 40 m.

The Duobe rises at the back of the Satro Mountains and flows nearly parallel with the Cavalla, which it joins.

Ethnologically the Bulgarians ought perhaps to come here; but, as a large admixture of Slav blood flows in their veins and they speak a distinctly Slav language, they have in this table been grouped with the Slays.

The latter, although it flows over a great number of rapids, is navigable throughout its length (330 m.); it is connected.

Dvina flows with a very slight gradient through a broad valley, and reaches the White Sea at Archangel.

The Onega, which flows into Onega Bay, has rapids; but timber is floated down in spring, and fishing and some navigation are carried on in the lower portion.

The Neva (40 m.) flows from Lake Ladoga into the Gulf of Finland.

The Volkhov, discharging into Lake Ladoga, and forming part of the Vyshniy-Volochok system of canals, is an important channel for navigation; it flows from Lake Ilmen, which receives the Msta, connected with the Volga, and the Lovat.

The Svir, also discharging into Lake Ladoga, flows from Lake Onega, and, being part of the Mariinsk canal system, is of great importance for navigation.

The Pruth rises in Austrian Bukovina, and separates Russia from Rumania; it enters the Danube, which flows along the Russian frontier for 100 m.

Below Ekaterinoslav the Dnieper flows for 46 m.

Some rivers, notably the Kur (Kyros, Araxes) which flows into the Bakhtegan lake east of Shiraz, drain into inland depressions or lakes.

The Amur proper flows at first in a south-easterly direction for about Boo m., as far as long.

The largest river is the Kan Kiang, which rises in the mountains in the south of the province and flows north-east to the Po-yang Lake.

Another river of note is the Chang Kiang, which has its source in the province of Ngan-hui and flows into the Po-yang Lake, connecting in its course the Wuyuen district, whence come the celebrated "Moyune" green teas, and the city of King-to-chen, celebrated for its pottery, with Jao-chow Fu on the lake.

Rising in the N.E., it flows in a tortuous channel in a general S.W.

The latter stream flows for 150 m.

It flows east and south in a wide curve, through a broad upper valley past Chippenham and Melksham, after which it turns abruptly west to Bradford-on-Avon, receives the waters of the Frome from the south, and enters the beautiful narrow valley in which lie Bath and Bristol.

Its general direction thereafter remains south-westerly, and it flows past Stratfordon-Avon, receives the Stour on the south and the Arrow on the north and thence past Evesham and Pershore to Tewkesbury.

It flows at first through rather monotonous country, but the latter portion of its course, from the village of Altenahr, over which tower the ruins of the castle of Ahr, or Are (10th century), is full of romantic beauty.

It would seem that the greater part of the rest flows away to be lost in space.

The small torrent of Rothwein, which flows into the Wurzener Save, forms near Veldes the splendid series of cascades known as the Rothwein Fall.

The San Miguel river, which flows near, affords a means of transportation, and the town has considerable commerce.

The smaller plain, or rather slope, adjoining Canea and the valley of Alikianu, through which the Platanos (ancient Iardanos) flows, are of great beauty and fertility.

The state contains deposits of iron, gypsum, marl, phosphate, lignite, ochre, glass-sand, tripoli, fuller's earth, limestones and sandstones; and there are small gas flows in the Yazoo Delta.

It rises near the peak of Itatiaya, on the northern slopes of the Mantiqueira, and flows north-west and west across the Minas plateau, receiving several large tributaries from the south.

From it the Oxus, or Amu, flows off to the west, and the Jaxartes, or Syr, to the north, through the Turki state of Khokand, while to the east the waters run down past Kashgar to the central desert of the Gobi, uniting with the streams from the northern slope of the Tibetan plateau that traverse the principalities of Yarkand and Khotan, which are also Turki.

In the southern region of unfolded beds are found the lavas of the " harras " of Arabia, and in India the extensive flows of the Deccan Trap. In the central folded belt lie the great volcanoes, now mostly extinct, of Asia Minor, Armenia, Persia and Baluchistan.

In the northern unfolded region great flows of basic lava lie directly upon the Cambrian and Ordovician beds of Siberia, but are certainly in part of Tertiary age.

This stream flows north-westward from the last lake and vanishes underground within 3 m.

It is now known that the Guadiana Alto has no such course, but flows underground to the Zancara itself, which is the true "Upper Guadiana."

The Zancara rises near the source of the Jucar, in the east of the tableland of La Mancha; thence it flows westward, assuming the name of Guadiana near Ciudad Real, and reaching the Portuguese frontier 6 m.

Its northern boundary is the Kuma-Manych depression, a succession of narrow, halfdesiccated lakes and river-beds, only temporarily filled with water and connecting the Manych, a tributary of the Don, with the Kuma, which flows into the Caspian.

After the Trent the most important river is the Derwent, one of its tributaries, which, taking its rise in the lofty ridges of the High Peak, flows southward through a beautiful valley, receiving a number of minor streams in its course, including the Wye, which, rising near Buxton, traverses the fine Millersdale and Monsal Dale.

The Dove rises on the southern slope, and flows as the boundary stream between Derbyshire and Staffordshire for nearly its entire course.

The Rother rises about Baslow, and flows into Yorkshire, with a northerly course, joining the Don.

Volcanic rocks, locally called "Toadstone," are represented in the limestones by intrusive sills and flows of dolerite and by necks of agglomerate, notably near Tideswell, Millersdale and Matlock.

The united river flows north to Grimma and thence past Wurzen, Eilenburg and Bitterfeld to Dessau, where it joins the Elbe.

The Boz-dagh and another ridge run between the four Koisu rivers, the head-streams of the Sulak, which flows into the Caspian.

The Ohio river flows for 436 m.

Two large rivers, which numerous tributaries, drain the government - the Dniester, which forms its boundary with Bessarabia and is navigable throughout its length, and the Bug, which flows almost parallel to the former in a higher, sometimes swampy, valley, and is interrupted at several places by rapids.

The principal river is the Drave, which flows from west to east through the length of the duchy, and receives in its course the waters of all the other streams, except the Fella, which reaches the Adriatic by its junction with the Tagliamento.

The others, which terminate streams, are the Bahr el-Ateiba, which receives the waters of Damascus; the Mat, into which the Kuwaik flows below Kinnesrin; and the Ak Deniz, or Bahrat Antakia, the ancient Lake of Antioch, which collects the waters of the Kara Su and Afrin, the southward from the watershed which shuts off Commagene.

From the inner sides of that mountain descend the Caledon and the Senku, whilst from its seaward face the Tugela flows through Natal to the Indian Ocean.

The upper part of the Maluti range consists of flows of melaphyres and diabases belonging to the volcanic beds.

For the greater part of its course it flows in a south-westerly direction, but near Pertuis gradually bends N.W.

At the foot of the fortress of Mont Dauphin it receives (left) the Guil, which flows through the Queyras valley from near the foot of Monte Viso.

Separated from Lycabettus by a depression to the south-west, through which flows a brook, now a covered drain (probably to be identified with the Eridanus), stands the remarkable oblong rocky mass of the Acropolis (512 ft.), rising precipitously on all sides except the western; its summit was partially levelled in prehistoric times, and the flat area was subsequently enlarged by further cutting and by means of retaining walls.

The river Derwent, rising in the tarns and "gills" or "ghylls" (small streams running in deeply-grooved clefts) north of Sty Head Pass and the Scafell mass flows north through the wooded Borrowdale and forms Derwentwater and Bassenthwaite.

The principal river of the district is the Jumna, which flows from north-west to south-east, along the N.E.

This watershed slopes gently to the south, to the valley of the Dnieper, which enters the government from the north-east and flows due south.

Water of less salinity flows outwards from the Black Sea as an upper current, and water of greater salinity from the Sea of Marmora flows into the Black Sea as an under-current.

This under-current flows towards Cape Tarhangut,where it divides into a left and right branch.

The principal rivers are the Mississippi, which flows nearly 600 m.

In its upper course it flows over a rocky bed with a swift current and many rapids.

Bosnia belongs wholly to the watershed of the Save, and its rivers to the Danubian system, no large stream finding a way to the Adriatic. The Save flows eastward along the northern frontier for 237 m.

Rising on the Montenegrin border, under the Lebrsnik mountains, it flows north-westwards at the foot of the Dinaric Alps; and, near Konjica, sweeps round suddenly to the south, and falls into the Adriatic near Metkovic, after traversing 125 m.

The city is in an elevated valley opening southward on the narrow ravine through which flows the Cachimayo, the principal northern tributary of the Pilcomayo.

The ice-cap of Greenland must to some extent be considered as a viscous mass, which, by the vertical pressure in its interior, is pressed outwards and slowly flows towards the coasts, just as a mass of pitch placed on a table and left to itself will in the course of time flow outwards towards all sides.

Nathorst has suggested that the whole of Greenland is a "horst," in the subordinate folds of which, as well as in the deeper " graben," the younger rocks are preserved, often with a covering of Tertiary or later lava flows.'

The whole of Cambodia lies in the basin of the lower Mekong, which, entering this territory on the north, flows south for some distance, then inclines south-west as far as Pnom-penh, where it spreads into a delta and resumes a southerly course.

The Mississippi river, which flows for about 800 m.

It still flows on, however, as a deep current and it then becomes a factor of immense importance with regard to the fisheries in the regions into which it penetrates.

It flows in a south-easterly direction for 170 m., and then adheres closely to a nearly easterly course for 500 m.

At Shigatse it flows in a wide extended bed with many channels, but contracts again at Chushul, where it is no wider than it is at Janglache, i.e.

When an electric current flows round a circuit, there is no accumulation of electricity anywhere in the circuit, hence the current strength is everywhere the same, and we may picture the current as analogous to the flow of an incompressible fluid.

In accordance with the principles of energetics, any change which involves a decrease in the total available energy of the system will tend to occur, and thus the necessary and sufficient condition for the production of electromotive force is that the available energy of the system should decrease when the current flows.

When the zinc and copper plates are connected through a wire, a current flows, the conventionally positive electricity passing from copper to zinc in the wire and from zinc to copper in the cell.

Thus as long as a moderate current flows, the only variation in the cell is the appearance of zinc sulphate in the liquid on the copper side of the porous wall.

But, on the other hand, if a few drops of acid be placed in the vessel with the platinum, bubbles of hydrogen appear, and a current flows, zinc dissolving at the anode, and hydrogen being liberated at the cathode.

If the external electromotive force exceed that of the cell by ever so little, a current flows in the opposite direction, and all the former chemical changes are reversed, copper dissolving from the copper plate, while zinc is deposited on the zinc plate.

If, instead of using a single Daniell's cell, we employ some source of electromotive force which can be varied as we please, and gradually raise its intensity, we shall find that, when it exceeds a certain value, about 1.7 volt, a permanent current of considerable strength flows through the solution, and, after the initial period, shows no signs of decrease.

But the ions of an electrolytic solution can move independently through the liquid, even when no current flows, as the consequences of Ohm's law indicate.

The latex is usually obtained from the bark or stem by making an incision reaching almost to the wood when the milky fluid flows more or less readily from the laticiferous vessels.

The latex of this tree flows less freely than that of Hevea brasiliensis, and the collection of large quantities of the latex is attended with considerable difficulty.

The latex flows fairly well, but is usually allowed to dry on the tree.

Upper Austria belongs to the watershed of the Danube, which flows through it from west to east, and receives here on the right the Inn with the Salzach, the Traun, the Enns with the Steyr and on its left the Great and Little Mühl rivers.

Passing Richmond (16) and Kew the river flows through London and its suburbs for a distance of about 25 m., till it has passed Woolwich.

When the magnetic induction flows through a piece of iron or other magnetizable substance placed near the magnet, a south pole is developed where the flux enters and a north pole where it leaves the substance.

Novibazar is a mountainous region, watered by the Lim, which flows north into Bosnia, and by several small tributaries of the Servian Ibar.

Forty miles lower down the Orange is joined by the first of its large tributaries, the Caledon (230 m.), which, rising on the western side of the Mont aux Sources, flows, first west and then south, through a broad and fertile valley north of the Maluti Mountains.

Throughout the greater part of its course in Tibet, where it is called the Dza-Chu, it flows south-eastwards to Chiamdo, on the great east and west caravan route from China to Lhasa.

From here it flows southwards through little-known mountain wastes.

The river flows beneath bare and rocky walls.

Little is known of the country through which it flows, and its channel is broken by rapids and waterfalls where it descends to the coastal plain.

It rises on an elevated tableland in the state of Sao Paulo and flows across the state of Rio de Janeiro from west to east, through a broad fertile valley producing coffee in its most elevated districts and sugar on its alluvial bottom-lands nearer the sea.

The Banganga is the only river which flows through the state.

Though it makes no large sweeps it has so tortuous a course that its length (some 200 m.) is twice that of the valley through which it flows.

It flows alternately through mountainous and pastoral country, and is known for two magnificent waterfalls, both within 12 m.

The only river communication with foreign countries is furnished by the Danube, on the one hand towards Austria and Germany, and on the other towards the Black Sea, All the rivers belong to the watershed of the Danube, with the exception of the Poprad in the north, which as an affluent of the Dunajec flows into the Vistula, and of a few small streams near the Adriatic. The Danube enters Hungary through the narrow defile called the Porta Hungarica at Deveny near Pressburg, and after a course of 585'.m.

The Bega canal runs from Temesvar to Nagy-Becskerek, and thence to Titel, where it flows into the Theiss.

Hence it may be considered to terminate where the Rio Cojedes, which drains the elevated valley in which Barquisimeto stands, after rising on its western slopes flows eastwards into the basin of the Orinoco.

The large towns through which the river flows have vied with one another in building harbours, providing shipping accommodation, and furnishing other facilities for the efficient navigation of the Elbe.

At that time, recent from a geological standpoint, the valley to the north, through which now flows the Semliki river, was blocked.

In its upper and in its lower course the river flows either through high alluvial plains, in which it has scored a deep channel, or across swamp land.

The Rhine rises in the mountains of the Swiss canton of the Grisons, and flows for 233 m.

Gotthard Pass, and then flows N.E.

On issuing from the Lake of Constance at Constance, the Rhine flows nearly due west to Basel, where it leaves Swiss territory, the south bank during this portion of the river being entirely Swiss, save the town of Constance, but the north shore belongs to Baden, save in the case of the Swiss town of Stein-am-Rhein and the Swiss canton of Schaffhausen.

From Basel to Mainz the Rhine flows through a wide and shallow valley, bordered on the east and west by the parallel ranges of the Black Forest and the Vosges.

The clear effluent flows into the Thames, and the sludge is taken 50 m.

Drainage channels are provided, usually along the main haulage roads, by which the water flows to a sump excavated at the pump shaft.

From the Khawak to the head of the Ghorband (a river of the Hindu Kush which, rising to the north-west of Kabul, flows north-east to meet the Panjshir near Charikar, whence they run united into the plains of Kohistan) the Hindu Kush is intersected by passes at intervals, all of which were surveyed, and several utilized, during the return of the Russo-Afghan boundary commission from the Oxus to Kabul in 1886.

The Chindwin, called in its upper reaches the Tanai, rises in the hills south-west of Thama, and flows due north till it enters the southeast corner of the Hukawng valley, where it turns north-west and continues in that direction cutting the valley into two almost equal parts until it reaches its north-west range, when it turns almost due south and takes the name of the Chindwin.

It is a swift clear river, fed in its upper reaches by numerous mountain streams. The Mogaung river, rising in the watershed which divides the Irrawaddy and the Chindwin drainages, flows south and south-east for 180 m.

There is, however, one true river of some size, the Hlaing, which rises near Prome, flows southwards and meets the Pegu river and the Pazundaung creek near Rangoon, and thus forms the estuary which is known as the Rangoon river and constitutes the harbour of Rangoon.

This river, rising in the Sham-Karen hills, flows first due north and then southward through the Kyaukse, Yamethin and Toungoo districts, its line being followed by the Mandalay-Rangoon railway as far south as Nyaunglebin in the Pegu district.

The former flows partly round its walls, the latter through the town; and it has canal communication with the lagoons.

At first the Ghazal flows north with lagoon-like expansions having great breadth and little depth - nowhere more than 13 ft.

A fluid, as the name implies, is a substance which flows, or is capable of flowing; water and air are the two fluids distributed most universally over the surface of the earth.

It rises in the Caucasus, on the slopes of Mount Kasbek, in several head-streams, and flows north as far as Vladikavkaz, just above which it emerges from the mountains.

Then it flows N.W.

One and a half mile from Altdorf by the Klausen road is the village of Burglen, where by tradition Tell was born; while he is also said to have lost his life, while saving that of a child, in the Schachen torrent that flows past the village.

It is situated in a narrow valley between two hills called West Mountain and Skene's Mountain, and Wood Creek flows through the village and empties into the lake with a fall, from which valuable water-power is derived; there are various manufactures, and the village owns and operates the water works.

The clear juice when it arrives at the top of the separator flows slowly over the level edges of, a cross canal and passes in a continuous stream to the service tanks of the evaporators or vacuum pan.

The clear juice in the meantime flows over the edge of the cylindrical vessel without disturbance and finds its way out by the short leg of the siphon, and so passes to the canal for collecting the defecated juice.

They consist of tanks or cisterns fitted with " heads " from which a number of bags of specially woven cloth are suspended in a suitable manner, and into which the melted sugar or liquor to be filtered flows from the melting pans.

The philosophers from whom Croce learned most are Vico, the author of the Scienza nuova, and Hegel, but the thought of all other thinkers flows in his writings, in conformity with its historical character, and for this reason may, for instance, be found in it traces of some of Hegel's most active opponents, such as Herbart.

By a system of carefully laid channels the water flows gently over the land, and deposits its warp with an even level surface.

At the ebb of the tide the more or less clear water flows back again from the land into the main river with sufficient force to clean out any deposit which may have accumulated in the drain leading to the warped area, thus allowing free access of more warpladen water at the next tide.

As soon as the outlet pipe has become sufficiently hot the zinc flows through it and collects in conveniently placed receptacles.

Volcanic cones still exist in large numbers, and the sheets of lava appear as fresh as any recent flows of Etna or Vesuvius.

Into the Danube Canal flows the small stream, called Wien, now arched over almost in its entirety.

Cedria, or cedar resin, is a substance similar to mastic, that flows from incisions in the tree; and cedar manna is a sweet exudation from its branches.

His main contention has met with some acceptance,' but the great current of ethnographical speculation still flows in the direction indicated by Humboldt.

The Huallaga rises north of Cerro Pasco, and, passing Huanuco, flows northwards on the other side of the Central Cordillera for 300 m.

The Vilcamayu rises on the Knot of Vilcanota, flows north through a lovely valley, received the Yanatilde and Paucartambo on its right hank, and, uniting with the Tambo, forms the Ucayali.

The condensing water enters at the top and is conducted to the bottom of the inner tube, which it fills and then flows over the outside of the outer tube; it collects in the bottom funnel and is then led off.

The river Adonis is the Nahr alIbrahim, which flows near the town.

The most plausible hypothesis is that men of this type are descendants of Korean colonists who, in prehistoric times, settled in the province of Izumo, on the west coast of Japan, having made their way thither from the Korean peninsula by the island of Oki, being carried by the cold current which flows along the eastern coast of Korea.

Her language is graceful and natural, her sentiments are refined and sober; and, as Mr Aston well says, her story flows on easily from one scene of real life to another, giving us a varied and minutely detailed picture of life and society in KiOto, such as we possess for no other country at the same period.

During the greater part of the year it is either dry or occupied in part by a string of saline lakes (limans or ilmens); but in spring when the streams swell which empty into it, the water flows in two opposite directions from the highest point (near Shara-Khulusun).

The western stream flows westwards, with an inclination northwards, until it reaches the Don, though when the latter river is running high, its water penetrates some 60 miles up the Manych.

A number of valleys run to the north and north-east, among them that of the Nahr el-Kebir, the Eleutherus of the ancients, which rises in the Jebel el-Abiaei on the eastern slope of Lebanon, and afterwards, skirting the district, flows westward to the sea.

The Aconcagua river rises on the southern slope of the volcano Aconcagua, flows eastward through a broad valley, or bay in the mountains, and enters the Pacific 12 m.

It flows generally east by south through a tortuous valley as far as Miranda de Ebro, passing through the celebrated Roman bridge known as La Horadada ("the perforated"), near Ona in Burgos.

The Moselle, which is here joined by the Seille, flows through it in several arms, and is crossed by fourteen bridges.

When the leaves are cut the juice flows out, and is collected and evaporated.

Three miles to the south of the city the river flows from east to west, spanned by the Pal-i-Malun, a bridge possessing grand proportions, but which was in 1885 in a state of grievous disrepair and practically useless.

An under-current flows out from the Red Sea through the Strait of Bab-el-Mandeb, and from the Mediterranean through the Strait of Gibraltar, raising the salinity as well as the temperature of the part of the ocean outside the gates of the respective seas.

Hence a strong surface current sets inwards through the Straits of Bab-el-Mandeb and Gibraltar, while an undercurrent flows outwards, raising the temperature and salinity of the ocean for a long distance beyond the straits.

Still farther to the east flows the Ken, followed in succession by the Baighin, Paisuni and Tons.

The city is solidly and regularly built, the houses being of stone and the stream that flows through the town being spanned by several stone bridges.

The basin is comparatively narrow, and the Tagus, like the other rivers of the Iberian tableland, generally flows in a rather confined valley, often at the bottom of a rocky gorge below the general level of the adjacent country.

Thence the Tagus flows at first northwestwards, but, after receiving the Gallo on the right, it flows west, and then south-west or west-south-west, which is its general direction for the rest of its course.

The principal exception is the Zatas or Sorraia, which, rising in the Serra d'Ossa, flows westwards across the plateau of Alemtejo, and joins the Mar de Pedro.

Into Tanganyika flows the Malagarasi, a considerable river with many affluents, draining the west-central part of the plateau.

The Kalambo river, a comparatively small stream near the southern end of Tanganyika, flows in a south-westerly direction.

Between Nimule and Fort Berkeley the river flows through a deep gorge and falls nearly woo ft.

To the west of this ridge the water collects to form the Asan, a tributary of the Jumna; whilst to the east the Suswa receives the drainage and flows into the Ganges.

The Pregel, spanned by many bridges, flows through the town in two branches, which unite below the Griine Briicke.

It flows at first towards the south-east, but on quitting Austria turns towards the north-west, maintaining this direction as far as Frankfort-onOder, beyond which its general course is nearly due north.

As far as the frontier the Oder flows through a well-defined valley,.

Aragon is divided by the river Ebro, which flows through it in a south-easterly direction, into two nearly equal parts, known as Trans-ibero and Cis-ibero.

A small stream which flows through the town is lined on both sides by pleasuregrounds.

The chief river is the Pennar, which enters the district from Bellary on the west, and flows eastwards into Nellore.

The plateau of Odenpah, drained by tributaries of the Embach river, which flows for 93 m.

Of the numerous rivers, the Dvina, which flows for 90 m.

The object of the test is to discover the resistance of the insulator I, that is, to determine how much current flows through this insulator by leakage under a certain electromotive force or voltage which must not be less than that which will be employed in practice when the electric lights supplied through these wires are in operation.

If any sensible current flows through this insulator the galvanometer will show a deflection.

The government is drained by the Dnieper, which flows along the frontier for 180 m., and by two minor streams, the Molochnaya and Berda.

The Silurian system is represented by the Baton river beds to the west of the Aorere beds, occurring in the basin of the Motueka river, which flows into Tasman Bay.

When the velocity of the jet is gradually increased there is a certain range of velocity for which the jet is unstable, so that any deviation from the straight rush-out tends to increase as the jet moves up. If then the jet is just on the point of instability, and is subjected as its base to alternations of motion, the sinuosities impressed on the jet become larger and larger as it flows out, and the flame is as it were folded on itself.

It was situated on the lower southern slopes of the Sultan Dagh, in the Konia vilayet of Asia Minor, on the right bank of a stream, the ancient Anthius, which flows into the Hoiran Geul.

From the Klip river confluence it flows west and south-west, entering Griqualand West above Kimberley.

It flows first east-north-east and then nearly east until it passes into North Dakota.

The Big Sioux river rises in the Coteau des Prairies in the north-east and flows almost directly south for a distance of 300 m., in the lower part of its course forming the boundary between South Dakota and Iowa.

It pursues a winding course in a northerly direction, and after passing the manufacturing town of Hof, flows amid well-wooded hills until it reaches the pleasant vale of Saalberg.

From Saalberg the Saale enters the dreary limestone formation of Thuringia, sweeps beneath the barren, conical hills lying opposite to the university town of Jena, passes the pleasant watering-place of Kosen, washes numerous vine-clad hills and, after receiving at Naumburg the deep and navigable Unstrut, flows past Weissenfels, Merseburg, Halle, Bernburg and Kalbe, and joins the Elbe just above Barby, after traversing a distance of 226 m.

The easternmost penetration of the Downs is that effected by the Stour (Great Stour) which rises on their southern face, flows S.E.

The Edison electric meter, like those of Sprague and Lane-Fox, was based upon the principle that when an electric current flows through an electrolyte, such as sulphate of copper or sulphate of zinc, the electrodes being plates of copper or zinc, metal is dissolved off one plate (the anode) and deposited on the other plate (the cathode).

The whole current supplied to the house flows through an electrolytic cell consisting of a glass tube containing two platinum electrodes; the electrolyte is dilute sulphuric acid covered with a thin layer of oil to prevent evaporation.

As the current flows it decomposes the liquid and liberates oxygen and hydrogen gases, which escape.

The current to be measured is passed through the coils of the electromagnet, then enters the mercury disk at the centre, flows through it radially in all directions, and emerges at the periphery.

The Red river flows in a winding channel along the eastern boundary and empties into Lake Winnipeg in Canada, thence reaching Hudson Bay through the Nelson river.

The ordinary process before 1906 was to dam small streams and " coulees "(deep gulches in which water flows intermittently) and flood the surrounding country.

It flows N., then W., then S., describing a semicircle through the fertile district of Pachim, and falls into the sea at the north-east corner of the inner gulf.

The Senne, a small tributary of the Scheldt, flows through the lower town, but since 1868 it has been covered in, and some of the finest boulevards in the lower town have been constructed over the course of the little river.

The latter flows to Belfast Lough, the former drains Lough Neagh, which is fed by a number of smaller streams, among them the Crumlin, whose waters have petrifying powers.

The Rhone flows through it from east to west, and then along its south-west edge, the total length of the river in or within the canton being about 13 m., as it is very sinuous.

The turbid Arve is by far its largest tributary (left), and flows from the snows of the chain of Mont Blanc, the only other affluent of any size being the London (right).

The city of Geneva is situated at the south-western extremity of the beautiful lake of the same name, whence the "arrowy Rhone" flows westwards under the seven bridges by which the two halves of the town communicate with each other.

Through the city flows Mill Creek, which empties into the Ohio.

The branches as well as the upper parts of the main streams flow through broad and shallow valleys; the middle courses of the main streams wind their way through reed-covered marshes, the water ebbing and flowing with the tide; in their lower courses they become estuarine and the water flows between low banks.

To the west of Parr's Ridge the surface for the most part slopes gently down to the east bank of the Monocacy river (which flows nearly at a right angle with the streams east of the Ridge), and then from the opposite bank rises rapidly toward the Catoctin Mountain; but just above the mouth of the Monocacy on the east side of the valley is Sugar Loaf Mountain, which makes a steep ascent of 1250 ft.

It rises on the northern slopes of the Amur mountains and flows N.E.

The Kebir or Rummel - the river is known by both names - is formed by the union of several small streams south of Constantine, and flows past that town N.W.

The Tafna (about ioo m.) rises in a large cavern in the mountains south of Tlemcen and flows N.E.

From Toulouse the Garonne flows to the north-west, now skirting the northern border of the plateau of Lannemezan which here drains into it, the principal streams being the Save, the Gers and the Baise.

From here it flows with ever increasing width between two flat shores to the Bec d'Ambes (151 m.), where, after a course of 357 m., it unites with the Dordogne to form the vast estuary known as the Gironde.

The Tekez flows in the mountains, and pierces narrow gorges.

The Reventazon, or Parismina, flows from the central plateau to the Caribbean Sea; despite the shortness of its valley, its volume is considerable, owing to the prevalence of moist trade-winds near its sources.

The chief river of Bokhara is the Oxus or Amu-darya, which separates it from Afghanistan on the south, and then flows along its south-west border.

The Kashka-darya, which flows westwards out of the glaciers of Hazret-sultan (west of the Hissar range), supplies the Shahri-sabs (properly Shaarsabiz) oasis with water, but is lost in the desert to the west of Karshi.

The river flows out of Loch Earn, pursues an eastward course with a gentle inclination towards the south, and reaches the Firth of Tay, 62 m.

Though small, the harbour is one of the best and safest on the coast, as no river flows into it to fill its anchorage with silt.

Dana introduced the term "as" for this rough kind of lava-stream, whilst he applied the term "pahoehoe" to those flows which have a smooth surface, or are simply wrinkled and ropy; these terms being used in this sense in Hawaii, in relation to the local lavas.

Meanwhile Thorfinn, with the rest of the venturers, sailed south "for a long time," till they reached a spot they called Hop, at the mouth of a river which flows from a lake into the sea (several estuaries near the southern extremity of Nova Scotia would do equally well here).

The lacustrine system of the St Lawrence flows eastward from a relatively narrow drainage area.

It is in association with this field of extinct volcanic activity that a remarkable group of geysers and hot springs has been developed, from which the Yellowstone river, a branch of the Missouri, flows northeastward, and the Snake river, a branch of the Columbia, flows south-westward.

Some of the high plateaus in the north are capped with remnants of heavy lava flows of early eruption.

A group of large volcanoes occurs on the limestone platform s6uth of the Grand Canyon, culminating in Mt San Francisco (12,794 ft.), a moderately dissected cone, and associated with many more recent smaller cones and freshlooking lava flows.

The earlier supposition that these vast lava flows came chiefly from fissure eruptions has been made doubtful by the later discovery of flat-sloping volcanic cones from which much lava seems to have been poured out in a very liquid state.

Some of the flows are still so young as to preserve their scoriaceous surface; here the shore-line of the lava contours evenly around the spurs and enters, bay-like, into the valleys of the enclosing mountains, occasionally isolating an outlying mass.

Many streams descend from the ravines only to wither away on the desert basin floors before uniting in a trunk river along the axis of a depression; others succeed in uniting in the winter season, when evaporation is much reduced, and then their trunk flows for a few score miles, only to disappear by sinking (evaporating) farther on.

Some of the chief valleys are not cut in the floors of the old valleys of the former cycle, because the rivers were displaced from their former courses by lava flows, which now stand up as table mountains.

Other auriferous gravels are buried under the upland lava flows, and are now reached by tunnels driven in beneath the rim of the table mountains.

The lower part of the Keweenawan system consists of a great succession of lava flows, of prodigious thickness.- This portion of the system is overlain by thick beds of sedimentary rock, mostly conglomerate and sandstone, derived from the igneous rocks beneath.

In the western part of the country there are, in addition, very extensive flows of lava covering in the aggregate some 200,000 sq.

The amount of volcanic material, consisting of both pyroclastic material and lava flows, is great.

Igneous rocks, whether lava flows or pyroclastic ejections, are less important in the Quaternary than in the Tertiary, though volcanic activity is known to have continued into the Quaternary.

The united river flows north through an undulating vine-clad country, past Erlangen, Baiersdorf and Forchheim, from which point it is navigable, and falls into the Main at Bischberg, just below Bamberg, after a course of 126 m.

The precise limits were the river Silarus on the north-west, which separated it from Campania, and the Bradanus, which flows into the Gulf of Tarentum, on the north-east; while the two little rivers Laus and Crathis, flowing from the ridge of the Apennines to the sea on the west and east, marked the limits of the district on the side of the Bruttii.

It flows first to the north, then to the north-west, passing out of the Yukon territory into Alaska, and then south-west, ending in Bering Sea, the northward projection of the Pacific, 2000 m.

At Canyon City it passes out of the Rockies through the Grand Canyon of the Arkansas; then turning eastward, and soon a turbid, shallow stream, depositing its mountain detritus, it flows with steadily lessening gradient and velocity in a broad, meandering bed across the prairies and lowlands of eastern Colorado, Kansas, Oklahoma and Arkansas, shifting its direction sharply to the south-east in central Kansas.

In the north-eastern portion the Budorus flows into the Aegean, being formed by two streams which unite their waters in a small plain, and were perhaps the Cereus and Neleus concerning which the story was told that sheep drinking the water of the one became white, of the other black.

The sap which flows in the spring is drawn off and boiled down to an agreeable spirit, or fermented with a birch-wine of considerable alcoholic strength.

The upper Savannah river first flows S.W., then turns abruptly S.E., while the Chattahoochee river rises near this point and continues S.W.

Old trees are selected, from the bark of which it is observed to ooze in the early summer; holes are bored in the trunk, somewhat inclined upward towards the centre of the stem, in which, between the layers of wood, the turpentine is said to collect in small lacunae; wooden gutters placed in these holes convey the viscous fluid into little wooden pails hung on the end of each gutter; the secretion flows slowly all through the summer months, and a tree in proper condition yields from 6 to 8 Ib a year, and will continue to give an annual supply for thirty or forty years, being, however, rendered quite useless for timber by subjection to this process.

The best month for larch planting, whether for poles or timber, is November; larches are sometimes planted in the spring, but the practice cannot be commended, as the sap flows early, and, if a dry period follows, the growth is sure to be checked.

The department is intersected by torrents belonging to the Garonne basin - the Salat, the Arize, which, near Mas d'Azil, flows through a subterranean gallery, the Ariege and the Hers.

Still farther west is the Vecht, which, rising in Westphalia, flows to the Zuider Zee.

With the exception of the Kunhar river, which flows down the Kagan valley to the Jhelum, the whole drainage of the province eventually finds its way into the Indus.

After leaving Hazara it flows in a southerly direction between the Punjab and the North-West Frontier Province, till it enters Mianwali district of the Punjab, from which it emerges to form again the eastern boundary of the province.

The Sind, with its tributaries the Kuwari, Asar and Sankh, flows through the northern division.

The river Moy flows northwards, forming part of the boundary of the county with Sligo, and falls into Killala Bay.

The New River flows through the parish, and Sir Hugh Myddleton, its projector, was for some time resident here.

The most considerable are the Wei, which flows into the Gulf of Chih-li; the I-ho, which empties into a lake lying east of the Grand Canal; and the Ta-wen, which rises at the southern foot of the I-sham Mountains and terminates in the Grand Canal.

The Guadalquivir rises among the mountains of Jaen and flows in a south-westerly direction to the Gulf of Cadiz, receiving many considerable tributaries on its way.

They are distributed along both banks of the Kerwan, a brook which flows south through the Wadi-ed-Der to join the Zerka or Jabbok; but all the principal buildings are situated on the level ground to the right of the stream.

Nearly the whole of Silesia lies within the basin of the Oder, which flows through it from south-east to north-west, dividing the province into two approximately equal parts.

The Rio Quinto has its sources in these ranges; the Desaguadero, or Salado, forms its western boundary; and the Conlara flows northward among its broken ranges to the great salinas of western Cordoba.

The present course of the Upper Allegheny river is the result of the glacier which blocked the northward drainage of the region through which it flows and turned it southward.

Thence, after crossing the upper Yalung, which flows by the town of Kanze, she pursued her journey to the upper course of the Yangtse-kiang (Dre chu), crossing that river somewhere near where A.-K.

This Yarlung, which borrowed its name from the Yalung of the state of Fanni Tu-bat, is a river which flows into the Yaro-tsangpo (Brahmaputra).

In its upper reaches it flows through a rich gold-bearing district to which it gives name, and nearer its mouth it traverses a vast tract of fine pastoral country.

It is situated on a height above the glen through which the Gairie flows, 64 m.

At this point a small stream, the ancient Cladeus, flows from the north into the Alpheus.

It has two sources, the Weisse Main (White Main), which rises in the Fichtelgebirge on the east side of the Ochsenkopf, and the Rote Main (Red Main), which, rising on the eastern slope of the Frankish Jura, flows past Bayreuth.

The Balu stream flows out of the Inle lake, and is navigable from that point to close on Lawpita, where it sinks into the ground in a marsh or succession of funnel holes.

The Wadi Tiaret flows through the town in a series of cascades.

They are then pressed in a large powerful screw-press, and the oily matter which flows out is caught, mixed with an equal proportion of water, and boiled to purify it from mucilaginous and albuminous matter.

Except on the south-east, where the Asahan flows away to the east coast, Toba Lake is surrounded by steep shores.

The southernmost longitudinal valley of Sumatra is that of the Semangka, which flows into the bay of the same name.

The main stream joining the Waal at Gorinchem flows on to Dordrecht as the Merwede, and is continued thence to the sea by the Old Maas, the North, and the New Maas, the New Maas being formed by the junction of the Lek and the North.

It lies on the right (east) bank of the river Parret, near the point where that river debouches from the hills on to the plain through which it flows to the Bristol Channel.

His name is now borne by a larger watercourse which flows some distance from the scene of his death.

The large massive plates of cementite which form the network or skeleton in hyper-eutectoid steels should, under distortion, naturally tend to cut, in the softer pearlite, chasms too serious to be healed by the inflowing of the plastic ferrite, though this ferrite flows around and Steel White Cast Iron 100 75 K 0 ?

For attire the skins manufactured in Europe are generally dyed black or brown, in which state it has a similar appearance to dyed fox, but having less thick underwool, and finer hair flows freely.

The remarkable stability of the mountain appears to be due to the innumerable dikes which penetrate the lava flows and tuff beds in all directions and thus bind the whole mass together.

On entering, the water flows at first in a radial direction, and then gradually, as it passes through the wheel, it receives a downward component which becomes more and more important.

The Memel flows along the north-east frontier of Poland, from Grodno to Yurburg, separating it from Lithuania.

The water which has found its way through the granitic sand flows over the surface of the mica schist and settles in the hollows, and by sinking wells to the solid rock a supply of water can generally be obtained.

It rises in the Slieve Bloom mountains, and flows at first easterly and then almost due south, until, on joining the Suir, it forms the estuary of the south coast known as Waterford Harbour.

It rises at the upper or eastern extremity of the Swiss canton of the Valais, flows between the Bernese Alps (N.) and the Lepontine and Pennine Alps (S.) till it expands into the Lake of Geneva, winds round the southernmost spurs of the Jura range, receives at Lyons its principal tributary, the Saline, and then turns southward through France till, by many mouths, it enters that part of the Mediterranean which is rightly called the Golfe du Lion (sometimes wrongly the Gulf of Lyons).

It issues as a torrent, at the height of 5909 ft., from the great Rhone glacier at the head of the Valais, the recent retreat of this glacier having proved that the river really flows from beneath it, and does not take its rise from the warm springs that are now at some distance from its shrunken snout.

It is almost immediately joined on the left by the Mutt torrent, coming from a small glacier to the S.E., and then flows S.W.

At Bellegarde the Valserine flows in (right), and then the river resumes its southerly direction, from which the great gorge had deflected it for a while.

It flows past Yenne (left) and beneath the picturesque fortress (formerly a Carthusian monastery) of Pierre Chatel (right) before it attains the foot of the extreme southern spur of the Jura, at a height of 696 ft., not far from the village of Cordon, and just where the Guiers flows in (left) from the mountains of the Grande Chartreuse.

Where a river crosses a desert at a level near that of the general surface, irrigation can be carried on with extremely profitable results, as has been done in the valley of the Nile and in parts of the Great Basin of North America; in cases, however, where the river has cut deeply and flows far below the general surface, irrigation is too expensive.

Skirting the forests of Compiegne, Halatte and Chantilly, all on its left bank, and receiving near Creil the Therain and the Breche, the river flows past Pontoise and debouches into the Seine 39 m.

Kairawan is built in an open plain a little west of a stream which flows south to the Sidi-el-Hani lake.

At Aire, in that province, there is a well from which the water has continued steadily to flow to a height of II feet above the ground for more than a century; and there is, within the old Carthusian convent at Lillers, another which dates from the 12th century, and which still flows.

Into this swamp on its east side flows the Chambezi, the most remote head stream of the Congo.

The Luapula flows south through the swamp some 50 m.

The water flows from the ditches as conductors into built conduits formed at right angles to them in parallel lines through the fields; it rises upwards in them as high as the surface of the ground, and again subsides through the soil and the conduits into the ditches as main drains, and thence it passes at a lower level either into a stream or other suitable outfall.

The water is admitted by valved sluices, which open as the tide flows into the field and shut by the pressure of the confined water when the tide recedes.

To water the valley, therefore, it is necessary to construct canals having bed-slopes less than that of the river, along which the water flows until its surface is higher than that of the fields.

This canal flows through land that in 1889 was practically desert.

The Ganges enters the province near the town of Buxar, flows eastward and, passing the towns of Dinajpur, Patna, Monghyr and Colgong, leaves the province at Rajmahal.

Thence it flows first S.W., then due W., through the fertile Valtellina, passing Tirano, where the Poschiavino falls in on the right, and Sondrio, where is the junction with the Malero, right.

The Pommersche or Oder Haff is separated from the sea by two islands, so that the river flows out by three mouths, the middle one (Swine) being the most considerable.

This group of mountains, occupying what may be regarded as ethnologically the centre of Germany, forms a hydrographical centre, whence the Naab flows southward to the Danube, the Main westward to the Rhine, the Eger eastward to the Elbe, and the Saale northward, also into the Elbe.

The Kapitel-Stadt, sometimes called the Bishop's Town, with the palace of the Roman Catholic archbishop, and his late Gothic cathedral, dating from the 15th century, lies eastward of the 1Vledvescak, a brook which flows into the Save.

The latter lake with Rainy Lake and other connected bodies of water belong to the Hudson Bay system of waters, their outlet being by Winnipeg river to Lake Winnipeg, from which flows Nelson river.

From it issues the Kebbi (Mao Kebi) a tributary of the Benue, and through it flows a tributary of the Logone, the chief affluent of the Shari.

Tributaries of the Niger traverse the western portion of the country, the most noteworthy being the Gulbin Kebbi or Sokoto river and the Kaduna, which flows through a valley not more than 500 ft.

But it flows less smoothly and easily than that of the dialogue of Latin comedy.

Hermon in Syria, overlooking a deep amphitheatre from which a brook flows to the Hasbani.

The principal river in the district is the Palar, which rises in Mysore, and flows through North Arcot from west to east past the towns of,Vellore and Arcot, into the neighbouring district of Chingleput, eventually falling into the sea at Sadras.

It rises in the north of the province of Cuenca, at the foot of the Cerro de San Felipe (59 06 ft.), and flows south past Cuenca to the borders of Albacete; here it bends towards the east, and maintains this direction for the greater part of its remaining course.

The thin watery "slip" or slurry flows into large settling tanks ("backs") where the solids in suspension are deposited; the water is drawn off, leaving behind an intimate mixture of chalk and clay in the form of a wet paste.

The Poronai flows south-south-east to the Gulf of Patience or Shichiro Bay, on the south-east coast.

It at first flows south by east, and at the village of Napo is 1450 ft.

The Aguarico also rises on the eastern slopes of the Andes north of Cayambe and flows southeastward to a junction with the Napo in about long.

Little is known of its course, or of the country through which it flows, which is provisionally occupied by Colombia.

The Curaray has its sources in the defiles of the Cerros de Llanganati, and flows south-eastward to the Napo, its length being estimated at 490 m.

It rises in the Chillo valley in the vicinity of Cayambe, and flows across the northern end of the central plateau, breaking through the Western Cordillera between Cotocachi and Pichincha.

The Babahoyo, which is the main stream, has its sources on the slopes of Chimborazo, the Daule on the Sandomo ridge in the latitude of Pichincha, the Yaguachi on the south-eastern slopes of Chimborazo, whence it flows southward for a considerable distance before breaking through the Cordillera to the western plain.

It then flows through a wide but shallow channel, joining the Sioule some distance above Moulins, the chief town on its banks.

East of the watershed are a number of valleys running to the Ghor; the most remarkable of these are the Wadi el-Bireh and the Wadi Jalud, the latter containing the river that flows from the fine spring called 'Ain Jalud.

The rocky gorges through which it flows, with a distant view of the Hindu Kush, form some of the finest scenery in the world.

Lake Placid is the principal source of the Ausable river, which for a part of its course flows through a rocky chasm from 500 to 175 ft.