Ocean Sentence Examples
She breathed in the ocean air.
She faced the ocean, the moon dangling low and large in the sky before her.
The sight, sound and scent of the ocean helped her relax.
In fact, he must be struggling to float on the ocean of problems this family represented.
He glared at the ocean and strode up the beach littered with wood, boats, and cars, to the highway.
Kris opened a portal to the Indian Ocean Sanctuary, where Erik had gone to seek out Ully.
She shivered in the chilly ocean breeze.
His gaze went to the ocean.
His eyes were as dark as the ocean depths, his grip around her body unmovable.
The sound of a roaring ocean filled the chamber.
AdvertisementThe ocean breeze did nothing to cool her off.
Chilled by the cold ocean wind, Deidre pressed herself against his warm body.
Rhyn gasped and struggled to sit. Kiki's still body lay a few feet from him, the ocean lapping at his brother's feet. The Caribbean night was humid and warm, and the moon large over head.
The sun had set, and dusk settled over the ocean.
Like a sunken object freed from the ocean floor, Dean began to ascend to the surface of wakefulness.
AdvertisementShe will be as she was before she walked into the ocean.
According to sources at the Ocean Shore Motel, Byrne was last seen on his way to the beach shortly after midnight by Leo Sutter, a waiter at the motel.
The ocean's calming rhythm and flavorful breeze made the beach more bearable.
If an airplane crashes in the middle of the ocean and someone is listed as a passenger on it, it's pretty simple, even if there's never a body.
Hunter and Dean exchanged information during the short drive to the Ocean Shore Motel.
AdvertisementAccompanied by two guards, she mounted her favorite bay horse and pounded through familiar roads and intersections to the southern wall., The chill of the ocean crept into its walls.
Denton was the one who hated to swim in the ocean.
The fleet is divided into the Mediterranean squadron, the Northern squadron, the Atlantic division, the Far Eastern division, the Pacific division, the Indian Ocean division, the Cochin China division.
The Atlantic Ocean contains a relatively small number of islands.
There the Volga, the Ural, the Syr-darya and the Amu-darya discharge their waters without reaching the ocean, but they bring life to the rapidly desiccating Transcaspian steppes, and link together the most remote parts of Russia.
AdvertisementFinally a fifth depression, which descends below the level of the ocean, extends for more than zoo m.
Urals, and enters the ocean by a large estuary at the Gulf of Pechora.
Though thus exhibiting the distinctive features of a continental climate, Russia does not lie altogether outside the reach of the moderating influence of the ocean.
Along the Murman coast of the Arctic Ocean and in the White Sea, where many millions of herrings are caught annually by some 3000 persons, the yearly produce is estimated at the value of £140,000.
Then he annexed its colonies and thereby extended his dominions to the Polar Ocean and the Ural Mountains.
Thus the term Savaii itself, originally Savaiki, is supposed to have been carried by the Samoan wanderers over the ocean to Tahiti, New Zealand, the Marquesas and Sandwich groups, where it still survives in such variant forms as Havaii, Hawaiki, Havaiki and Hawaii.
The ocean tempers the climate considerably on the seaboard.
It was not unlike the Ocean Shore in Norfolk, only smaller and completely deserted.
Sure enough, after ten minutes of silent driving on nearly empty streets, he recognized Ocean View Avenue, and a few minutes later, The Ocean Shore Motel.
The sun peered over the ocean to the north while blooming apple trees sprinkled their flowers into piles in a cool sea breeze.
If we get separated, go toward the ocean.
The ocean was visible; she estimated they were about half a mile from the orchard.
Her gaze assessed their location for a safe path towards the ocean.
The ocean air was fragrant and heavy, and moonlight pierced the forest canopy in patches.
The quiet city smelled of the ocean and the forest.
The heavy scent of fragrant sea swept over him, the chill of the ocean kept out of the city by its thick walls.
I threw my cousin's body from the Cliffs into the ocean, and I told my mate a bandit killed our daughter.
He broke down and cried quietly for his father and their men, wondering how he could make it across the ocean alone.
If Memon succeeds in raising an army of his allies, he will be able to trap us here on the cliffs, against the ocean here.
The night air was crisp and cool and laden by the scents of the ocean.
He remained facing the ocean, resolved to deal with her on his terms.
Moonlight glinted off the swords at his hip, and a cold ocean breeze swept up the Western Cliffs, rolled over them, and rustled the branches of the nearby forest.
Taran's gaze went to where the dark ocean met the sky in the distance.
The moon was too bright for his eyes, and the cold ocean breeze burned his lungs.
You swim in the ocean, don't you ... or do you stay on the beach all the time to avoid the sharks?
My guess is that you accept the slim possibility that a shark might get you, and swim in the ocean anyway.
She was getting used to the water and it felt good, but she would have preferred a swim in the ocean.
The fragrant ocean breeze was chilly as it brushed his skin, and his movements fell into the rhythm of the ebb and flow of waves.
California sunlight and an ocean breeze streamed in through open windows of Xander's spacious condo.
Jessi watched him go, texted her cousins then returned her gaze to the dark sky and ocean.
He imagined the ocean breeze zipping straight through where his living room used to be.
Her gray eyes were almost the color of the moon overhead, her pale features obscured by curls that danced in an ocean breeze.
North of the Senegal the Sahara reaches the coast, and for over moo miles no river enters the ocean.
The Mediterranean is all that remains of a great ocean which at an early geological epoch, before the formation of the Atlantic, encircled half the globe along a line of latitude.
This ocean, already diminished in area, retreated after Oligocene times from the Iranian plateau, Turkestan, Asia Minor and the region of the north-west Alps.
Some of these lake-beds are at or slightly below sea-level, so that a very slight depression of the land to the south of them would connect much of the interior with the Southern Ocean.
Even the White Sea is merely a gulf of that ocean.
It is a remarkable geographical fact that on the rises and in the basins of moderate depth of the open ocean the organic oozes preponderate, but in the abysmal depressions below 2500 or 3000 fathoms, whether these lie in the middle or near the edges of the great ocean spaces, there is found only the red clay, with a minimum of calcium carbonate, though sometimes with a considerable admixture of the siliceous remains of radiolarians.
It is served by the Panama railway, which crosses the Isthmus of Panama from ocean to ocean.
Besides the Belt there are several parks and reserves, including botanical and acclimatization gardens, the so-called Ocean Beach, and two race-courses.
Norfolk is the see of a Protestant Episcopal bishopric. The city has a public park of 110 acres and various smaller ones, and in the vicinity are several summer resorts, notably Virginia Beach, Ocean View, Old Point Comfort, Pine Beach and Willoughby Beach.
The romance of Alexander is found written in the languages of nearly all peoples from the Indian Ocean to the Atlantic, but all these versions are derived, mediately or immediately, from the Greek original which circulated under the false name of Callisthenes.
In the extreme west, which is as yet but slightly explored and settled, there is an extensive depressed area, largely saline in character, which drains into lakes and morasses, having no outlet to the ocean.
It stands up from the ocean depths in three fairly well-marked terraces.
The first ledge rising from the ocean floor has depth averaging 8000 ft.
The vertical relief of the land above the ocean is a very important factor in determining the climate as well as the distribution of the fauna and flora of a continent.
The Southern Ocean system of the Victorian Dividing Range hardly attains to the dignity of high mountains.
Flowing into the Pacific Ocean on the east coast there are some fine rivers, but the majority have short and rapid courses.
Much accumulated evidence, biological and geological, has pointed to a southern extension of India, an eastern extension of South Africa, and a western extension of Australia into the Indian Ocean.
Thus he came at length to stand on the verge of the Indian Ocean; " gazing upon it," a writer has said, " with as much delight as Balboa, when he crossed the Isthmus of Darien from the Atlantic to the Pacific."
The rivers of the province belong to the basins of the Indian Ocean and the Java Sea respectively, the water-parting being formed by the western and eastern ends respectively of the northern and southern lines of mountain peaks.
The Chi Tandui, also rising here, flows south-east to the Indian Ocean, and alone of all the rivers in this province is navigable.
It extends E northward to the Arctic Basin and southward to the Great Southern Ocean.
On both sides of the central ridge deep troughs extend southwards from the Telegraph plateau to the Southern Ocean, the deep water coming close to the land all the way down on both sides.
In the North Atlantic the distribution of pressure and resulting wind circulation are very largely modified by the enormous areas of land and frozen sea which surround the ocean on three sides.
The movements of the northern branch of the Gulf Stream drift have been the object of more careful and more extended study than all the other currents of the ocean put together, except, perhaps, the Gulf Stream itself.
The tides of the Atlantic Ocean are of great complexity.
The tidal wave of the Southern Ocean, which sweeps uninterruptedly round the globe from east to west, generates a secondary wave between Africa and South America, which travels north at a rate dependent only on the depth of the ocean.
When the consolidation of the Dominion by means of railway construction was under discussion in 1872, Grant travelled from the Atlantic to the Pacific with the engineers who surveyed the route of the Canadian Pacific railway, and his book Ocean to Ocean (1873) was one of the first things that opened the eyes of Canadians to the value of the immense heritage they enjoyed.
He was the author of a number of works, of which the most notable besides Ocean to Ocean are, Advantages of Imperial Federation (1889), Our National Objects and Aims (1890), Religions of the World in Relation to Christianity (1894) and volumes of sermons and lectures.
The experience gained in the earlier days of ocean telegraphy, from the failure and abandonment of nearly 50 per cent.
In depths beyond the reach of wave motion, and apart from suspension across a submarine gully, which will sooner or later result in a rupture of the cable, the most frequent cause of interruption is seismic or other shifting of the ocean bed, while in shallower waters and near the shore the dragging of anchors or 40 fishing trawls has been mostly responsible.
The Atlantic Telegraph Company was reconstituted as the AngloAmerican Telegraph Company with a capital of f600,000 and sufficient cable was ordered not only to lay a line across the ocean but also to complete the 1865 cable.
He also repeated the suggestion which Lindsay had already made that it might be possible to signal in this manner by conduction currents through the Atlantic Ocean from the United States to Europe.
He proposed that one ship should be provided with the means of making an interrupted current in a circuit formed partly of an insulated metallic wire connected with the sea at both ends by plates, and partly of the unlimited ocean.
The furrows are the great ocean basins, and these would still persist even if the land surface were enlarged to the 1400 fathoms contour.
It was natural, if not strictly logical, that the ocean river should be extended from a narrow stream to a world-embracing sea, and here again Greek theory, or rather fancy, gave its modern name to the greatest feature of the globe.
From Sidon, and later from its more famous rival Tyre, the merchant adventurers of Phoenicia explored and colonized the coasts of the Mediterranean and fared forth into the ocean beyond.
The great Phoenician colony of Carthage, founded before 800 B.C., perpetuated the commercial enterprise of the parent state, and extended the sphere of practical trade to the ocean shores of Africa and Europe.
The world was henceforth viewed as a very large place stretching far on every side beyond the Midland or Mediterranean Sea, and the land journey of Alexander resulted in a voyage of discovery in the outer ocean from the mouth of the Indus to that of the Tigris, thus opening direct intercourse between Grecian and Hindu civilization.
After two successful voyages, Eudoxus, impressed with the idea that Africa was surrounded by ocean on the south, left the Egyptian service, and proceeded to Cadiz and other Mediterranean centres of trade seeking a patron who would finance an expedition for the purpose of African discovery; and we learn from Strabo that the veteran explorer made at least two voyages southward along the coast of Africa.
Vasco Nunez, the new commander, entered upon a career of conquest in the neighbourhood of Darien, which ended in the discovery of the Pacific Ocean on the 25th of September 1513.
For this purpose Juan Diaz de Solis was despatched in October 1515, and in Pacific January 1516 he discovered the mouth of the Rio de la ocean.
It was long before another British ship entered the Pacific Ocean.
James Lancaster made a voyage to the Indian Ocean from 1591 to 1594; and in 1599 the merchants and adventurers of London resolved to form a company, with the object of establishing a trade with the East Indies.
On the 6th of May 1615 Spilbergen entered the Pacific Ocean, and touched at several places on the coast of Chile and Peru, defeating the Spanish fleet in a naval engagement off Chilca.
In 1772 the French explorer Yves Kerguelen de Tremarec had discovered the land that bears his name in the South Indian Ocean without recognizing it to be an island, and naturally believed it to be part of the southern continent.
The deviation is of importance in the movement of air, of ocean currents, and to some extent of rivers.3 In popular usage the words " physical geography " have come to mean geography viewed from a particular standpoint rather than any special department of the subject.
Granting that the geoid or mean surface of the ocean is a uniform spheroid, the distribution of land and water approximately indicates a division of the surface of the globe into two areas, one of elevation and one of depression.
Actual or projected routes for telegraph cables across the deep sea have also been sounded with extreme accuracy in many cases; but beyond these lines of sounding the vast spaces of the ocean remain unplumbed save for the rare researches of scientific expeditions, such as those of the " Challenger," the " Valdivia," the " Albatross " and the " Scotia."
Thus the best approximation to the average depth of the ocean is little more than an expert guess; yet a fair approximation is probable for the features of sub-oceanic relief are so much more uniform than those of the land that a smaller number of fixed points is required to determine them.
A striking fact in the configuration of the crust is cs 1'000 n that each continent, or elevated mass of the crust, is T diametrically opposite to an ocean basin or great de 5000 0 -5000 -15000 -20 2500 -300 pression; the only partial exception being in the case of southern South America, which is antipodal to eastern Asia.
Taking the Atlantic as our simplest type, we may say that the surface of an ocean basin resembles that of a mighty trough or syncline, buckled up more or less centrally in a medial ridge, which is bounded by two long and deep marginal hollows, in the cores of which still deeper grooves sink to the profoundest depths.
Where the great continental sag sinks below the ocean level, we have our gulfs and our Mediterraneans, seen in our type continent, as the Mexican Gulf and Hudson Bay.
Where the central oceanic buckle attains the water-line we have our oceanic islands, seen in our type ocean, as St Helena and the Azores.
The percentages of the land surface draining to the different oceans are approximately - Atlantic, 34'3%; Arctic sea, 26.5%; Pacific, 14.4%; Indian Ocean, 12.8%.'
Corals and other quick-growing cal- careous marine organisms are the most powerful in this respect by creating new land in the ocean.
Plicatulae have been found attached to these coprolites, showing that they were already hard bodies when lying at the bottom of the Chalk ocean.
In turn other animals took shape, the last being two golden spiders from whose excrement the earth gradually rose above the surrounding ocean.
The Gallic Wars (58-51) of Caesar (q.v.) added all the rest of Gaul, north-west of the Cevennes, to the Rhine and the Ocean, and in 49 also annexed Massilia.
Hills nearly enclose the city, protecting it from the ocean fogs.
These two conquests, wrought in the great island of the Ocean and in the great island of the Mediterranean, were the main works of the Normans after they had fully put on the character of a Christian and French-speaking people, in other words, after they had changed from Northmen into Normans.
It has a seaboard on the Atlantic Ocean of 120 m., a shore-line to the south on the Rio de la Plata of 235 m., and one of 270 m.
In a steam vessel running at high speed on an ocean route, with engines working smoothly and uniformly, a careful officer with correct line and glass can obtain very accurate results with the common log.
Thus it consists of the immense plains and flat lands which extend between the plateau formation and the Arctic Ocean, including the series of parallel chains and hilly spurs which skirt the former region on the N.W.
The picturesque Bureya Mountains above the Amur, the forest-clad Sikhota-alin on the Pacific, and the volcanic chains of Kamchatka belong, however, to quite another orographical construction, being the border-ridges of the terraces by which the great plateau formation descends to the depths of the Pacific Ocean.
The Eocene covers wide tracts from Lithuania to Tsaritsyn, and is represented in the Crimea and Caucasus by thick deposits belonging to the same ocean which left its deposits on the Alps and the Himalayas.
It is a special feature of Russia that she has no free outlet to the open sea except on the ice-bound shores of the Arctic Ocean.
He now " plunged into the ocean of the Augustan history," and " with pen almost always in hand," pored over all the original records, Greek and Latin, between Trajan and the last of the Western Caesars.
At a time when all nationalities, and at the same time all bonds of religion and national customs, were beginning to be broken up in the seeming cosmos and real chaos of the Graeco-Roman Empire, the Jews stood out like a rock in the midst of the ocean.
On the east and north their boundary was the lower Rhine, on the west the ocean.
The harbours along the sounds and in the estuaries of the rivers are well protected from the storms of the ocean by the long chain of narrow islands in front, but navigation by the largest vessels is interrupted by shoals in the sounds, and especially by bars crossing the inlets between islands.
A great circle, drawn through East Cape and the southern point of Arabia, passes nearly along the coast-line of the Arctic Ocean, over the Ural Mountains, through the western part of the Caspian, and nearly along the boundary between Persia and Asiatic Turkey.
Although for the purposes of geographical nomenclature, boundaries formed by a coast-line - that is, by depressions of the earth's solid crust below the ocean level - are most easily recog- Political nized and are of special convenience; and although such divisions.
The portion of Asia which lies between the Arctic Ocean and the mountainous belt bounding Manchuria, Mongolia and Turkestan Siberia.
Thus it appears that from the Arctic Ocean there stretches a broad area as far as the south of China, in which no marine deposits of later date than Carboniferous have yet been found, except in the extreme north.
It was a portion of a great land-mass which probably extended across the Indian Ocean and was at one time united with the south of Africa.
The moderating effect of the proximity of the ocean is felt in an important degree along the southern and eastern parts of Asia, where the land is broken up into islands or peninsulas.
In the summer a great accumulation of solar heat takes place on the dry surface soil, from which it cannot be released upwards by evaporation, as might be the case were the soil moist or covered with vegetation, nor can it be readily conveyed away downwards as happens on the ocean.
Among the more remarkable phenomena of the hotter seas of Asia must be noticed the revolving storms or cyclones, which are of frequent occurrence in the hot months in the Indian Ocean and China Sea, in which last they are known under the name of typhoon.
The heated body of air carried from the Indian Ocean over southern Asia by the south-west monsoon comes up highly charged with watery vapour, and hence in a condition to release a large body of water as rain upon the land, whenever it is brought into circumstances which reduce its temperature in a notable degree.
Of the marine orders of Sirenia and Cetacea the Dugong, Halicore, is exclusively found in the Indian Ocean; and a dolphin, Platanista, peculiar to the Ganges, ascends that river to a great distance from the sea.
The Polynemidae, which range from the Atlantic through the Indian Ocean to the Pacific, supply animals from which isinglass is prepared; one of them, the mango-fish, esteemed a great delicacy, inhabits the seas from the Bay of Bengal to Siam.
The Salmonidae are entirely absent from the waters of southern Asia, though they exist in the rivers that flow into the Arctic Ocean and the neighbouring parts of the northern Pacific, extending perhaps to Formosa; and trout, though unknown in Indian rivers, are found beyond the watershed of the Indus, in the streams flowing into the Caspian.
It would seem from this distribution that the Malays are not continental, but a seafaring race with exceptional powers of dispersal, who have spread over the ocean from some island centre - perhaps Java.
The district forms a narrow strip of land between the Indian Ocean and the mountains which separate it from the independent kingdom of Siam.
Metternich persuaded the tsar and the king of Prussia to make a declaration that the allies would leave to Napoleon the "natural boundaries" of France - the Rhine, Alps, Pyrenees and Ocean.
The fauna, explored by Dybowski and Godlewski, and in 1900-2 by Korotnev, is much richer than it was supposed to be, and has quite an original character; but hypotheses as to a direct communication having existed between Lake Baikal and the Arctic Ocean during the Post-Tertiary or Tertiary ages are not proved.
Generally, while there is a relative poverty of zoological groups, there is a great wealth of species within the group. Of gammarids, there are as many as 300 species, and those living at great depths (33 o to 380 fathoms) tend to assume abyssal characters similar to those displayed by the deep-sea fauna of the ocean.
It is Egypt therefore - to which, it must be remembered, the centre of Mahommedan power had now been virtually shifted, and to which motives of trade impelled the Italian towns (since from it they could easily reach the Red Sea, and the commerce of the Indian Ocean) - it is Egypt which is henceforth the normal goal of the Crusades.
Shut off from the adjacent Indian Ocean by its mountain barrier, the drainage of the country is westward to the distant Atlantic. As its name implies, the chief rivers rise in Mont aux Sources.
The inhabited world thus delineated formed an island of irregular shape, surrounded on all sides by the ocean, the Erythrean Sea freely communicating with the western ocean.
This map of Eratosthenes, notwithstanding its many errors, such as the assumed connexion of the Caspian with a northern ocean and the supposition that Carthage, Sicily and Rome lay on the same meridian, enjoyed a high reputation in his day.
Even Strabo (c. 30 B.C.) adopted its main features, but while he improved the European frontier, he rejected the valuable information secured by Pytheas and retained the connexion between the Caspian and the outer ocean.
In the main he copied Marinus whose work he revised and supplemented in some points, but he failed to realize the peninsular shape of India, erroneously exaggerated the size of Taprobane (Ceylon), and suggested that the Indian Ocean had no connexion with the western ocean, but formed Mare Clausum.
In every instance the inhabited world is surrounded by the ocean.
Beyond this ocean lies another world, which was occupied by man before the Deluge, and within which Cosmas placed the Terrestrial Paradise.
The charts in use of the medieval navigators of the Indian Ocean - Arabs, Persians or Dravidas - were equal in value if not superior to the charts of the Mediterranean.
Nicolaus Germanus, a monk of Reichenbach, in 1466 prepared a set of Ptolemy's maps on a new projection with converging meridians; and Paolo del Pozzo Toscanelli in 1474 compiled a new chart on a rectangular projection, which was to guide the explorer across the western ocean to Cathay and India.
The ocean separating Europe from he was dependent upon dead reckoning, for although various methods for determining a longitude were known, the available astronomical ephemerides were not trustworthy, and errors of 30 in longitude were by no means rare.
It is also known as the " Eastern Horn of Africa," because it projects somewhat sharply eastwards into the Indian Ocean, and is the only section of the continent which can be spoken of as a peninsula.
The water is deep right to the base of the cliff and owing to the winds and the strength of the ocean currents, navigation is dangerous.
Over this line passes an enormous trade from the Atlantic to the Pacific Ocean - the railway with its "Empress" steamers on the Pacific and also on the Atlantic Ocean claiming to have as its termini Liverpool and Yokohama.
Afterward going westward from Lake Athabasca and through the Peace river, he reached the Pacific Ocean, being the first white man to cross the North American continent, north of Mexico.
Nearly allied is Neophocaena phocaenoides, a small species from the Indian Ocean and Japan, with teeth of the same form as those of the porpoise, but fewer in number (eighteen to twenty on each side), of larger size, and more distinctly notched or lobed on the free edge.
There is thus a minimum circulation in the greater depths causing there uniformity of temperature, an absence of the circulation of oxygen by other means than diffusion, and a protection of the sulphuretted hydrogen from the oxidation which takes place in homologous situations in the open ocean.
The tide-generating force is due to the attraction of the waters of the ocean by sun and moon.
The distribution is very interesting and it has been shown that the water of the Antarctic Ocean contains about 0 .
Clearly, however, the vast quantity of living substance in the ocean is built up from materials that are present in the sea-water as an exceedingly dilute solution, and the solution is dilute just because organisms are incessantly utilizing it.
First of all we consider inorganically combined nitrogen (as nitrates and nitrites chiefly), since upon this depends all the life of the ocean.
It would seem that, on the whole, nitrogen compounds in the ocean (whether existing in the organic or inorganic forms) remain constant in amount.
A considerable degree of denitrification must, therefore, take place in the ocean, for the concentration of combined nitrogen is always excessively small.
The Umfolosi, with two main branches, the Black and White Umfolosi, drains the central part of the country and reaches the ocean at St Lucia Bay.
Farther south the Umhlatuzi empties into a lagoon which communicates with the ocean by Richards Bay.
That it is possible to work with safety beneath rivers, lakes and even the ocean has been proved in numerous instances; mines in different parts of the world having been extended long distances under the sea.
At Wheal Cock near St Just in Cornwall the protecting roof was so thin that holes bored for blasting more than once penetrated to the bed of the ocean, and wooden plugs were kept on hand to drive into such holes when this occurred.
The three vessels lost, the' " Irresistible," " Ocean " and " Bouvet," were out of date; but of those put out of action the " Inflexible " was a modern ship, and she and another very nearly foundered before they could be got to a place of safety.
In 1793 peace was concluded between these two powers, the Siamese yielding to the Burmans the entire possession of the coast of Tenasserim on the Indian Ocean, and the two important seaports of Mergui and Tavoy.
The puma has an exceedingly wide range of geographical distribution, extending over a hundred degrees of latitude, from Canada in the north to Patagonia in the south, and formerly was generally diffused in suitable localities from the Atlantic to the Pacific Ocean, but the advances of civilization have curtailed the extent of the districts which it inhabits.
It is visited by the ocean steamers of several lines, and is the centre of a very extensive beche-de-mer and pearl fishery.
Brett controlled the Newfoundland Telegraph Company on the other side of the ocean, Bright organized with them the Atlantic Telegraph Company in 1856 for the purpose of carrying out the idea, himself becoming engineer-in-chief.
Bahrein, Kuwet and Muscat are in steam communication with India, and the Persian Gulf ports; all the great lines of steamships call at Aden on their way between Suez and the East, and regular services are maintained between Suez, Jidda, Hodeda and Aden, as well as to the ports on the African coast, while native coasting craft trade to the smaller ports on the Red Sea and Indian Ocean.
Bering Sea is the northward continuation of the Pacific Ocean, from which it is demarcated by the long chain of the Aleutian Islands.
The sea is connected with the Arctic Ocean northward by Bering Strait, at the narrowest part of which East Cape (Deshnev) in Asia approaches within about 56 m.
Leaving Hampton Roads on the 18th of August 1838, it Mopped at Madeira and Rio de Janeiro; visited Tierra del Fuego, Chile, Peru, the Paumotu group of the Low Archipelago, the Samoan islands and New South Wales; from Sydney sailed into the Antarctic Ocean in December 1839 and reported the discovery of an Antarctic continent west of the Balleny islands; visited the Fiji and the Hawaiian islands in 1840, explored the west coast of the United States, including the Columbia river, San Francisco Bay and the Sacramento river, in 1841, and returned by way of the Philippine islands, the Sulu archipelago, Borneo, Singapore, Polynesia and the Cape of Good Hope, reaching New York on the 10th of June 1842.
The coast, extending from the base of the Western or Maritime Cordillera to the Pacific Ocean, consists of a sandy desert crossed at intervals by rivers flowing through narrow, fertile valleys.
The coast has been upraised from the ocean at no very distant geological epoch, and is nearly as destitute of vegetation as the Coast.
Such a circle, however, runs so near the coast of Antarctica as to make the southern ocean very small.
Others, like Malte Brun (1803) and Supan (1903), take the loxodromes between the three capes and call the ocean to the south the Antarctic Ocean.
Where the ocean touches the continents the margin is in places deeply indented by peninsulas and islands marking off portions of the water surface which from all antiquity have been known as " seas."
These seas are entirely dependent on the ocean for their regime, being filled with ocean water, though subject to influence by the land, and the tides and currents of the ocean affect them to a greater or less extent.
Enclosed seas extend deeply into the land and originate either by the breaking through of the ocean or by the overflowing of a subsiding area.
They are connected with the ocean by narrow straits, the salinity of the water contained in them differs in a marked degree from that of the ocean, and the tidal waves are of small amplitude.
There are also four smaller continental enclosed seas each with a single channel of communication with the ocean, viz.
Hence their tidal conditions are quite oceanic, though their salinity is usually rather lower than that of ocean water.
If the whole globe were covered with a uniformly deep ocean, and if there were no difference of density between one part and another, the surface would form a perfect ellipsoid of revolution, that is to say, all the meridians would be exactly equal ellipses and all parallels perfect circles.
Hecker took the opportunity of a voyage from Hamburg to La Plata, and in 1904 and 1905 of voyages in the Indian and Pacific Oceans to determine the local attraction over the ocean by comparing the atmospheric pressure measured by means of a mercurial barometer and a boiling-point thermometer, and obtained results similar to Scott Hansen's.
At this period an exact knowledge of the depths of the ocean off after the beginning of the south-west monsoon to a minimum assumed an unlooked-for practical importance from the daring in August, the total range being 92 in.
In the region of tropical hurricanes the navies, while in the Mediterranean and in the Indian Ocean converging wind system of a circular storm causes a heaping many soundings were made in connexion with submarine up of water capable of devastating the low coral islands of the cables to the East.
Ingenious devices had indeed been tried in the 17th biological conditions of the ocean as a whole.
American scientific enterprise, mainly in very deep water, though in a few instances he overestimated under the guidance of Professor Alexander Agassiz, has been the depth by failing to detect the moment at which the lead active in the North Atlantic and especially in the Pacific Ocean, touched bottom.
Viewed from the floor of the ocean the continental block would thus appear as a great plateau rising to a height of 14,360 ft.
Nevertheless, the greatest depths of the ocean below sea-level and the greatest heights of the land above it are of the same order of magnitude, the summit of Mount Everest rising to 29,000 ft.
Particularly steep slopes are found in the case of submarine domes, usually incomplete volcanic cones, and there have been cases in which after such a dome has been discovered by the soundings of a surveying ship it could not be found again as its whole area was so small and the deep floor of the ocean from which it rose so flat that an error of 2 or 3 m.
While such steep mountain walls are found in the bed of the ocean it must be remembered that they are very exceptional, and except where there are great dislocations of the submarine crust or volcanic outbursts the forms of the ocean floor are incomparably gentler in their outlines than those of the continents.
Being protected by the water from the rapid subaerial erosion which sharpens the features of the land, and subjected to the regular accumulation of deposits, the whole ocean floor has assumed some approach to uniformity.
Still there are everywhere gentle inequalities on the smoothest ocean floor which give to its greater features a distinct relief.
The seaward edge of the continental shelf often falls steeply to the greatest depths of the ocean, and not infrequently forms the slope of a trench, a form of depression which has usually a steep slope towards a continent or an island-bearing rise on one side and a gentler slope towards the general level of the ocean on the other.
Continuing southwards the rise joins the Azores Plateau, which has in parts a very marked relief, and runs thence southward almost exactly in the middle of the ocean, becoming gradually lower as it goes.
The greater part of the Indian Ocean is occupied by the great Indian Basin, which covers 35,000,000 sq.
The western part of the Indian Ocean has been shown by the surveys of H.M.S.
The Pacific Ocean consists mainly of one enormous basin bounded on the west by New Zealand and the Tonga, Marshall aid Marianne ridges, on the north by the festoons of islands marking off the North Pacific fringing seas, on the east by the coast of North America and the great Easter Island Rise and on the south by the Antarctic Shelf.
This greatest of ocean basins contains also the largest and deepest trenches.
The northern part of the Marianne Trench leads to a wave-like configuration of the ocean floor, the depth to the east of Saipan being over 4300 fathoms, followed by a rise to 1089 fathoms and then a descent to 3167 fathoms.
The south-western part of the Pacific Ocean has a very rich and diversified submarine relief, abounding in small basins separated by ridges and rises.
The borders of the Malay Sea are everywhere shallower on the side of the Indian Ocean than on that of the Pacific, and consequently water from the Pacific preponderates in the depths.
The Mediterranean Sea, the best-known member of the intercontinental class, is separated from the Atlantic Ocean by a ridge running from Cape Spartel to Cape Trafalgar on which the greatest depth is only 175 fathoms. The depth increases so rapidly towards the east that soundings exceeding 500 fathoms occur off Gibraltar.
Towards the continent there is a broad shelf, and just before the chain of islands separating them from the ocean runs a narrow and deep trough.
Oceanic Deposits.-It has long been known that the deposits which carpet the floor of the ocean differ in different places, and coasting sailors have been accustomed from time immemorial to use the lead not only to ascertain the depth of the water but also to obtain samples of the bottom, the appearance of which is often characteristic of the locality.
As so defined the hemipelagic deposits are those which occur in general on the slope from the continental shelves to the ocean depths and also in the deep basins of enclosed and fringing seas.
Blue mud prevails in large areas of the Pacific Ocean from the Galapagos Islands to Acapulco.
In the Indian Ocean it covers the Bay of Bengal, the Arabian Gulf, the Mozambique Channel and the region to the south-west of Madagascar.
The terrigenous ingredients in the deposits become less and less abundant as one goes farther into the deep ocean and away from the continental margins.
Still, according to Murray and Irvine, finely divided colloidal clay is to be found in all parts of the ocean however remote from land, though in very small amount, and there is less in tropical than in cooler waters.
Volcanic dust thrown into the air settles out slowly, and some of the products of submarine and littoral volcanoes, like pumice-stone, possess a remarkable power of floating and may drift into any part of the ocean before they become waterlogged and sink.
To this inconceivably slowly-growing deposit of inorganic material over the ocean floor there is added an overwhelmingly more rapid contribution of the remains of calcareous and siliceous planktonic and benthonic organisms, which tend to bury the slower accumulating material under a blanket of globigerina, pteropod, diatom or radiolarian ooze.
In the Indian Ocean the area covered is 31,000,000 .sq.
This fact, together with the extraordinarily rare occurrence of such remains and meteoric particles in globigerina ooze, although there is no reason to suppose that at any one time they are unequally distributed over the ocean floor, can only be explained on the assumption that the rate of formation of the epilophic deposits through the accumulation of pelagic shells falling from the surface is rapid enough to bury the slowgathering material which remains uncovered on the spaces where the red clay is forming at an almost infinitely slower rate.
There is even some hesitation in accepting the continuity of the chalk with the globigerina ooze of the modern ocean.
If this estimate is correct there exists dissolved in the ocean a quantity of silver equal to T3,300 million metric tons, that is to say 46,700 times as much silver as has been produced from all the mines in the world from the discovery of America down to 1902.
One can look on sea-water as a mixture of very dilute solutions of particular salts, each one of which after the lapse of sufficient time fills the whole space as if the other constituents did not exist, and this interdiffusion accounts easily for the uniformity of composition in the sea-water throughout the whole ocean, the only appreciable difference from point to point being the salinity or degree of concentration of the mixed solutions.
The great similarity between the salts of the ocean and the gaseous products of volcanic eruptions at the present time, rich in chlorides and sulphates of all kinds, is a strong argument for the ocean having been salt from the beginning.
Magnesium sulphate amounts to 4.7% of the total salts of sea-water according to Dittmar, but to 23.6% of the salts of the Caspian according to Lebedinzeff; in the ocean magnesium chloride amounts to 10.9% of the total salts, in the Caspian only to 4.5%; on the other hand calcium sulphate in the ocean amounts to 3.6%, in the Caspian to 6.9 This disparity makes it extremely difficult to view ocean water as merely a watery extract of the salts existing in the rocks of the land.
Such a simple formula is only possible because the salts of sea-water are of such uniform composition throughout the whole ocean that the chlorine bears a constant ratio to the total salinity as newly defined whatever the degree of concentration.
Their experiments show that in similar conditions the evaporation of sea-water amounts to from 70 to 91% of the evaporation of fresh water, a fact of some importance in geophysics on account of the vast expanses of ocean the evaporation from which determines the rainfall and to a large extent the heat-transference in the atmosphere.
Schott gives the following as the result of measurements of transparency by means of a white disk at 23 stations in the open ocean, where quantitative observations of the plankton under i square metre of surface were made at the same time.
The colour of ocean water far from land is an almost pure blue, and all the variations of tint towards green are the result of local disturbances, the usual cause being turbidity of some kind, and this in the high seas is almost always due to swarms of plankton.
The northern seas have an increasing tendency towards green, the Irminger Sea showing 5-9 Forel, while in the North Sea the water is usually a pure green (io-14 Forel), the western Mediterranean shows 5-9 Forel, but the eastern is as blue as the open ocean (0-2 Forel).
There is a distinct relationship between colour and transparency in the ocean; the most transparent water which is the most free from plankton is always the purest blue, while an increasing turbidity is usually associated with an increasing tint of green.
Brown or even blood-red stripes have been observed in the North Atlantic when swarms of the copepod Calanus finmarchicus were present; the brown alga Trichodesmium erythraeum, as its name suggests, can change the blue of the tropical seas to red; swarms of diatoms may produce olive-green patches in the ocean, while some other forms of minute life have at times been observed to give the colour of milk to large stretches of the ocean surface.
In other words, water which has a specific gravity of 1 0280 at the surface would at the same temperature have a specific gravity of 1 0450 at 2000 and I 0540 at 3000 fathoms. If the whole mass of water in the ocean were relieved from pressure its volume would expand from 319 million cub.
The water of the ocean, like any other liquid, absorbs a certain amount of the gases with which it is in contact, and thus sea-water contains dissolved oxygen, nitrogen and carbonic acid absorbed from the atmosphere.
The distribution of dissolved oxygen in the depths of the open ocean is still very imperfectly known.
Carbonic acid passes from the atmosphere into the ocean as soon as its tension in the latter is the smaller; hence in this respect the ocean acts as a regulator.
The amount of carbonic acid in solution may also be increased by submarine exhalations in regions of volcanic disturbance, but it must be remembered that the critical pressure for this gas is 73 atmospheres, which is reached at a depth of 400 fathoms, so that carbonic acid produced at the bottom of the ocean must be in liquid form.
Buchanan on the " Challenger " were vitiated by the incompleteness of the method employed, but they are none the less of value in showing clearly that the waters of the far south of the Indian Ocean are relatively rich in carbonic acid and the tropical areas deficient.
The North Atlantic maximum is the highest with water of 37.9 per mille salinity; the maximum in the South Atlantic is 37.6; in the North Indian Ocean, 36.7; the South Indian Ocean, 36.4; the South Pacific, 36.9; and the North Pacific has the lowest maximum of all, only 35'9.
For the open ocean the only quite trustworthy results are those obtained by the prince of Monaco in the North Atlantic, and by the recent Antarctic expeditions in the South Atlantic and South Indian Oceans.
Buchanan pointed out in 1876, that the great contrasts in surface salinity between the tropical maxima and the equatorial minima give place at the moderate depth of 200 fathoms to a practically uniform salinity in all parts of the ocean.
Our knowledge of the Pacific in this respect is still very imperfect, but it appears to be less salt than the other oceans at depths below 800 fathoms, as on the surface, the salinity at considerable depths being 34.6 to 34.7 in the Western part of the ocean, and about 34.4 to 34.5 in the eastern, so that, although the data are by no means satisfactory, it is impossible to assign a mass-salinity of more than 34.7 per mille for the whole body of Pacific water.
The warming of the ocean is due practically to solar radiation alone; such heat as may be received from the interior of the earth can only produce a small effect and is fairly uniformly distributed.
There are few obseryations available for ascertaining the depth to which warmth from the sun penetrates in the ocean.
The arrangement of the isotherms thus affords a basis for valuable deductions as to the direction of ocean currents.
We are still ignorant of the depth to.which the annual temperature wave penetrates in the open ocean, but observations in the Mediterranean enable us to form some opinion on the matter.
The vertical distribution of temperature ' in the open ocean is much better known than that of salinity.
The whole ocean must thus form but a cold dwelling-place for the organisms of the deep sea.
Thus in the Central American Sea below 93 o fathoms, the depth on the bar, no water is found at a temperature lower than that prevailing in the open ocean at that depth, viz.
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.
The latter often gives birth to prodigious icebergs and ice islands, which are carried northward by ocean currents, nearly as far as the tropical zone before they melt.
The first comprehensive study of the currents of the Atlantic was that carried out by James Rennell (1790-1.830), and since that time Findlay in his Directories, Heinrich Berghaus, Maury and the officials of the various Hydrographic Departments have produced increasingly accurate descriptions of the currents of the whole ocean, largely from material supplied by merchant captains.
The general lines of the currents of the oceans are fairly well understood, and along the most frequented ocean routes the larger seasonal variations have also been ascertained.
The general scheme of ocean currents depends on the prevailing winds taken in conjunction with the configuration of the coast and its submarine approaches.
The trade-wind regions correspond pretty closely with westward-flowing currents, while in the equatorial calm belts there are eastward-running countercurrents, these lying north of the equator in the Atlantic and Pacific, but south of the equator in the Indian Ocean.
A cyclonic circulation of the atmosphere is associated with a cyclonic circulation of the water of the ocean, as is well shown in the Norwegian Sea and North Atlantic between the Azores and Greenland.
The coincidence of wind and current direction is most marked in the region of alternating monsoons in the north of the Indian Ocean and in the Malay Sea.
We must remember that the ocean is a continuous sheet of water of a certain depth, and the conditions of continuity which hold good for all fluids require that there should be no vacant space within it; hence if a single water particle is set in motion, the whole ocean must respond, as Varenius pointed out in 1650.
Thus all the water carried forward by any current must have the place it left immediately occupied by water from another place, so that only a complete system of circulation can exist in the ocean.
When the wind acts on the surface of the sea it drives before it the particles of the surface layer of water, and, as these cannot be parted from those immediately beneath, the internal friction of the fluid causes the propelling impulse to act through a considerable depth, and if the wind continued long enough it would ultimately set the whole mass of the ocean in motion 'right down to the bottom.
Such currents, due to the banking up of water, have a large share in setting the depths of the sea in motion, and so securing the vertical circulation and ventilation of the ocean.
The difference in density which occurs between one part of the ocean and another, shares with the wind in the production of currents.
If there were strong currents at the bottom of the ocean the uniform accumulation of the deposit of minute shells of globigerina and radiolarian ooze would be impossible, the rises and ridges would necessarily be swept clear of them, and the fact that this is not the case shows that from whatever cause the waters of the depths are set in motion, that motion must be of the most deliberate and gentlest kind.
Differences of density between the waters of enclosed seas and of the ocean are brought about in some instances by concentration of the water of the sea on account of active evaporation, and in other instances by dilution on account of the great influx of land water.
A very powerful vertical circulation is thus set up between enclosed seas and the outer ocean.
The very dense water of the Red Sea and the Mediterranean makes the column of water salter and heavier and the level lower than in the ocean beyond the straits.
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.
The determination of the exact relationship of cause and effect in the origin of ocean currents is a matter of great practical importance.
Important current and temperature charts of the ocean and occasional memoirs are published for the Admiralty by the Meteorological Office in London, by the U.S. Hydrographic Office in Washington, the Deutsche Seewarte in Hamburg, and also at intervals by the French, Russian, Dutch and Scandinavian admiralties.
Pilot Charts of the North Atlantic and North Pacific are issued monthly by the U.S. Hydrographic Office, and of the North Atlantic and of the Indian Ocean and Red Sea by the British Meteorological Office, giving a conspectus of the normal conditions of weather and sea.
The town slopes to the ocean, with a background of forest surmounted by the snow-clad volcanic cone of Mount Egmont (8270 ft.).
The Wami and Kingani, smaller streams, have their origin in the mountainous region fringing the central plateau, and reach the ocean opposite the island of Zanzibar.
The warm currents setting landwards from the Indian Ocean bring both moisture and heat, so that the Swahili coast has a higher temperature and heavier rainfall than the Atlantic seaboard under the same parallels of latitude.
The most important and best-known rivers are the Amberno, in the north, discharging by a wide delta at Point d'Urville; the Kaiserin Augusta, which, rising in the Charles Louis range, and entering the Pacific near Cape della Torre, is navigable by ocean steamers for 180 m.; the Ottilien, a river of great length, which discharges into the sea a short distance south of the last named; and the Mambare, navigable by steam-launch for 50 m.
There are various pleasure resorts in the mountains, and among seaside resorts are Santa Monica, Ocean Park, Venice, Playa del Rey, Hermosa, Redondo, Terminal Island, Long Beach, Alamitos Bay, Huntington Beach, Newport, Balboa and Corona del Mar.
Excepting the barren lands of the Antarctic regions, with which Patagonia is somewhat associated by a broken string of islands, the nearest continental lands of a more habitable kind are South Africa and New Zealand., In contrast to the sub-Arctic land ring, here is a sub-Antarctic ocean ring, and as a result the land flora and fauna of South America to-day are strongly unlike the life forms of the other south-ending continents.
But the Greenland colony was obscure, the country was believed to form part of Europe, and the records of the farther explorations were contained in sagas which were only rediscovered by modern scholarship. Throughout the middle ages, legendary tales of mythical lands lying in the western ocean - the Isle of St Brandan, of Brazil and Antilia - had been handed down.
The hope that a passage through to the Spice Islands would be found near existing Spanish settlements was now given up. One was sought farther south, and in November 1520 Ferdinand Magellan passed through the strait which bears his name and sailed across the Pacific. At last the existence of a continent divided by a vast stretch of ocean from Asia, and mostly lying within the sphere of influence assigned to Spain by the pope, was revealed to the world.
While the majority of his researches bear on one or other of the subjects just mentioned, others deal with such widely different topics as the birds of Greenland, ocean temperatures, the Gulf Stream, barometric measurement of heights, arcs of meridian, glacier transport of rocks, the volcanoes of the Hawaiian Islands, and various points of meteorology.
They were, as Milton said, " faithful and freeborn Englishmen and good Christians constrained to forsake their dearest home, their friends, and kindred, whom nothing but the wide ocean and the savage deserts of America could hide and shelter from the fury of the bishops."
The leached guanos and phosphatized rocks, which are grouped with them for commercial purposes, have been obtained in great quantities in many islands of the Pacific Ocean (such as Baker, Howland, Jarvis and McKean Islands) between long.
Christmas Island has been a great source of phosphates of this type; also Jaluit Island in the Maldive Archipelago, Banaba or Ocean Island, and Nauru or Pleasant Island.
Thus New York is pre-eminently a divide region, sending its drainage, by various courses, into widely separated parts of the ocean.
The ocean coast-line, though of limited extent, is by far the most important in the United States.
The harbour entrance is somewhat obstructed by sand bars, so that extensive government work has been necessary to open and maintain a channel for large draft ocean vessels.
About New York City, and on Long Island, the ocean softens the rigours of winter, and through the influence of cold surface waters off the coast, tempers the heat of summer.
The Dutch had long claimed the whole coast from Delaware Bay to Cape Cod, but by the treaty of Hartford (1650), negotiated between himself and the commissioners of the United Colonies of New England, Stuyvesant agreed to a boundary which on the mainland roughly determined the existing boundary between New York and Connecticut and on Long Island extended southward from the west side of Oyster Bay to the Atlantic Ocean.
Along the whole west coast the climate resembles nothing in the British Islands so much as Cork and Kerry, for there are the same wet gales from a western ocean, the same clouds gathering on the dripping sides of wild mountains, an equal absence of severe frosts and hot sunshine, and a rich and evergreen vegetation.
Excluding Coal for Fuel by Ocean Steamers.
In western Washington, where the ocean greatly influences the temperature and the mountains condense the moisture of vapour-bearing winds, the climate is equable and moist.
Eastern Washington, too, usually has a mild temperature, but occasionally some regions in this part of the state are visited by a continental extreme, and as the winds from the ocean lose most of their moisture in passing over the Cascades, the climate is either dry or arid according to elevation.
Just before the purchase of Louisiana, President Jefferson had recommended to Congress (18th January 1803) the sending of an expedition to explore the headwaters of the Missouri, cross the Rockies and follow the streams to the Pacific. In accordance with the recommendation Meriwether Lewis and William Clark, both officers of the United States Army, with a considerable party left St Louis on the 14th of May 1804, ascended the Missouri to the headwaters, crossed the Rockies and, following the Columbia river, reached the ocean in November 1805.
These words are for (I) the swim-bladder of a fish; (2) a narrow stretch of water between an inland sea and the ocean, or between an island and the mainland, &c., cf.
The main range of the Rocky Mountains separates that part which is drained west into the'Columbia river and the Pacific Ocean from that which is drained east into the Missouri and Mississippi rivers and the Gulf of Mexico, and from a very small part which is drained north-east into Hudson Bay; the water-parting which in Montana separates the drainage into Hudson Bay from the drainage into the Gulf of Mexico crosses only the north-west region of Teton county.
In the west the climate is generally delightful, it being there greatly affected by the warm, dry " Chinook " wind which blows from the Pacific Ocean; to some extent the wind modifies the temperature nearly to the eastern border.
Owing to the northern latitude, comparatively high altitudes, and the great distance from the ocean, there are great annual variations of temperature and a very small amount of rainfall.
Before leaving, he led his troops to the coast opposite Britain, and ordered them to pick up shells on the seashore, to be dedicated to the gods at Rome as the spoils of ocean.
The Appalachian belt includes, with the ranges enumerated above, the plateaus sloping southward to the Atlantic Ocean in New England, and south-eastward to the border of the coastal plain through the central and southern Atlantic states; and on the north-west, the Allegheny and Cumberland plateaus declining toward the Great Lakes and the interior plains.
Produced by long-continued subaerial decay and erosion, in later Cretaceous times this lowland extended from the Atlantic Ocean well toward the interior of North America; since then the whole continent has been generally elevated, and by successive steps the Appalachian belt has been raised to form a wide but relatively low arch.
The confinement of the colonies between an ocean and a mountain wall led to the fullest occupation of the coastal border of the continent, which was possible under existing conditions of agriculture, conducing to a community of purpose, a political and commercial solidarity, which would not otherwise have been developed.
Formerly it was the general belief that the herring inhabits the open ocean close to the Arctic Circle, and that it migrates at certain seasons towards the northern coasts of Europe and America.
The object of the work has been described as the glorification of Vespasian's achievements in securing Roman rule in Britain and opening up the ocean to navigation (as the Euxine was opened up by the Argo).
On the 30th of June 1900 the wharves of the North German Lloyd Steamship Company and three of its ocean liners were almost completely destroyed by a fire, which caused a loss of more than 200 lives and over $5,000,000.
The main object of the Portuguese was to obtain a share in the lucrative spice trade carried on by the Malays, Chinese and Japanese; the trade-routes of the archipelago converged upon Malacca, which was the point of departure for spice merchants trading with every country on the shores of the Indian Ocean and Arabian Sea.
But the broad tract which projects towards the west as far as the shores of the Bosporus, though hilly and covered with forests - the Turkish Aghatch Denizi, or "The Ocean of Trees" - is not traversed by any mountain chain.
In 1613 Champlain again crossed the Atlantic and endeavoured to confirm Nicolas de Vignau's alleged discovery of a short route to the ocean by the Ottawa river, a great lake at its source, and another river flowing north therefrom.
It is served by the Pennsylvania, the Philadelphia & Reading, the Northern Central and the Cumberland Valley railways; and the Pennsylvania canal gives it water communication with the ocean.
The conspicuous feature in the view from the ocean is the Borj el Hasan, an unfinished square-built tower, 145 ft.
The climate of Maryland in the south-east is influenced by ocean and bay - perhaps also by the sandy soil - while in the west it is influenced by the mountains.
Mississippi river steamers were armed with heavy guns and protected by armour, boiler-plates, cotton bales, &c., and some fast cruisers were constructed for ocean work, one of them actually reaching the high speed of 17.75 m.
Though he was apt to represent himself as disliked and neglected by the admiralty, and was frequently insolent towards his superiors, he was, as a matter of fact, pretty constantly employed, and he more than justified his appointments by his activity and success as captain of the "Pallas" (32) and "Imperieuse" (38) on the ocean and in the Mediterranean.
It is nearly landlocked to the N., communicating with the Arctic Ocean only by Bering Strait, which is 36 m.
The Asiatic coasts are for the most part low and irregular, and a number of seas are more or less completely enclosed and cut off from communication with the open ocean.
The area and volume of the Pacific Ocean and its seas, with the mean depths calculated therefrom, are given in the article Ocean.
This bank continues southwards to the Antarctic Ocean, expanding into a plateau on which Australia stands, and a branch runs eastwards and then southwards from the north-east of Australia through New Zealand.
In the southern hemisphere there is a transition to the low-pressure belt encircling the Southern Ocean, in which westerly and north-westerly winds continue all the year round.
South of the Tropic of Capricorn the isohalines run nearly east and west, salinity diminishing quickly to the Southern Ocean.
On reaching the western Pacific part of this current passes southwards, east of New Zealand, and again east of Australia, as the East Australian Current, part northwards to join the Equatorial CounterCurrent, and during the north-east monsoon part makes its way through the China Sea towards the Indian Ocean.
The only movement in the depths is the slow creep of ice-cold water northwards along the bottom from the Southern Ocean; but this is more marked, and apparently penetrates farther north, than in the Atlantic.
In the west there is the great looped chain which fringes the east coast of Asia, and with it encloses the series of seas which form parts of the ocean.
As the loop of the Kuriles depends from the southern extremity of Kamchatka, so from the east of the same peninsula another loop extends across the northern part of the ocean to Alaska, and helps to demarcate the Bering Sea; this chain is distinctly broken to the east of the Commander Islands, but is practically continuous thereafter under the name of the Aleutian Islands.
The following paragraphs review the oceanic islands generally, and are therefore concerned almost entirely with the central and mid-western parts of the ocean.
The peaks or sharp cones in which they Islands Of The Pacific Ocean The above figures give a total land area for the whole region of 69,561 sq.
Those plants which are widely distributed are generally found to be propagated from seeds which can easily be carried by the wind or by ocean currents, or form the food of migratory birds.
Not long after the death of Columbus, and when the Portuguese traders, working from the west, had hardly reached the confines of the Malay Archipelago, the Spaniard Vasco Nunez de Balboa crossed America at its narrowest part and discovered the great ocean to the west of it (1513).
Alvaro Mendana de Neyra, after crossing a vast extent of ocean from Peru and sighting only one island, probably in the Ellice group, reached the Solomon Islands.
In September 1650 he came to an agreement with the commissioners of the United Colonies of New England at Hartford upon the boundary between New Netherland and Connecticut, involving the sacrifice of a large amount of territory, the new boundary crossing Long Island from the west side of Oyster Bay to the Atlantic Ocean, and on the mainland north from a point west of Greenwich Bay, 4 m.
It changed thought into an emotional dream; it plunged into the ocean of sentiment; it treated the old world of fable as the reflection of a higher reality, and transformed reality into poetry; and after all these expedients, to borrow a phrase of Augustine's, it only saw afar off the land of its desire.
Medusae thus form an important constituent of the plankton or floating fauna of the ocean, and compete with fish and other animals for the food-supply furnished by minuter forms of life.
In 1909 the ports were ready to receive large ocean steamships, and regular traffic was begun, including cargoes of Hawaiian sugar for New York.
The importance of this is evident when we consider that late in the 19th century Japanese junks still drifted over by the ocean current to California at the rate of about one a year, often with some of the crew still alive.
As is related in the legends, Quetzalcoatl came into the land to teach men to till the soil, to work metals and to rule a well-ordered state; the two gods played their famous match at the ball-game, and Tezcatlipoca persuaded the weary Quetzalcoatl to drink the magic pulque that sent him roaming to the distant ocean, where he embarked in his boat and disappeared from among men.'
That these animals were widely distributed in former times is proved by their occurrence at the present day in palaeozoic fossiliferous strata both of the northern hemisphere and of Australia; and despite the fact that their remains have not been found in rocks of the Mesozoic or Kainozoic epochs, it was conceived to be possible that living specimens might be dredged from the sea-floor during the exploration of the ocean depths undertaken by the "Challenger" expedition.
Dublin lies on the great central limestone district which stretches across the island from the Irish Sea to the Atlantic Ocean, and occupies both banks of the river Liffey.
Along the southern coast are many ponds, all shut off from the ocean by a narrow strip of land, excepting Tisbury Great Pond, which has a small outlet to the sea.
The Syrian goat is met with in various parts of the East, in Lower Egypt, on the shores of the Indian Ocean and in Madagascar.
Between the two mountain systems extends a great central area of plains, stretching from the Gulf of Mexico northward, far beyond the national boundary, to the Arctic Ocean.
The aboriginal occupants of the greater part of North America were comparatively few in number, and except in Mexico were not advanced beyond the savage state, The geological processes that placed a much narrower ocean between North America and western Europe than between North America and eastern Asia secured to the New World the good fortune of being colonized by the leading peoples of the occidental Old World, instead of by the less developed races of the Orient.
The strata are the deposits of an ancient sea, which in the earlier stage of geological investigation was thought to be part of the primeval ocean, while the Laurentian highlands were taken to be the first land that rose from the primeval waters.
Inasmuch, however, as the floor on which the overlapping strata rest is, like the rest of the Laurentian and Superior Oldland, a worn-down mountain region, and as the lowest member of the sedimentary series usually contains pebbles of the oldiand rocks, the better interpretation of the relation between the two is that the visible oldiand area of to-day is but a small part of the primeval continent, the remainder of which is still buried under the Palaeozoic cover; and that the visible oldiand, far from being the first part of the continent to rise from the primeval ocean, was the last part of the primeval continent to sink under the advancing Palaeozoic seas.
The lower coast ranges, nearer the ocean, continue a little farther southward than the Sierra Nevada, before giving way to that part of the Basin Range province which reaches the Pacific in southernmost California.
The distribution of the beds of marine origin shows that the sea crept upon the eastern and southern borders of the continent auring the period, covered the western plains, and formed a great mediterranean sea between the eastern and western lands of the continent, connecting the Gulf of Mexico on the south and the Arctic Ocean on the north.
Closely associated with the effect of continental immobility are the effects dependent on the low specific heat and the opacity of the lands, in contrast with the high specific heat and partial transparence of the ocean waters.
Indeed the contrast between the moderate temperatures of the Pacific coast and the overheated areas of the next interior deserts is so great that the isotherms trend almost parallel to the coast, and are even overturned somewhat in southern California, where the most rapid increase of temperatures in July is found not by moving southward over the ocean toward the equator, but north-eastward over the land to the deserts of Nevada and Arizona.
The equalizing effects of a conservative ocean are brought upon the Pacific coast, where the climate is truly temperate, the mean annual range being only 10 or 12, thus resembling western Europe; while the exaggerating effects of the continental interior are carried eastward to the Atlantic coast, where the mean annual range is 40 or 50.
The Pacific ranges, standing transverse to the course of the prevailing westerlies near the Pacific Ocean, are of the greatest importance in this respect; it is largely by reason of the barrier that they form that the tempering effects of the Pacific winds are felt for so short a distance inland in winter, and that the heat centre is displaced in summer so far towards the western coast.
The rainfall from the stromy westerly winds is largely deposited on the western slopes of the mountains near the Pacific coast, and arid or desert interior plains are thus found close to the great ocean.
The decline of tonnage engaged in ocean traffic was from 2,546,237 net tons in 1860 to 1,352,810 in 1880; and this decline continued in later years.
Thus the country from ocean to ocean is covered by a network of committees1 each having a sphere of action corresponding to some election area, whether a Federal area or a state area.
It was pointed out by Great Britain that this ukase had been the subject of protest both by Great Britain and the United States, and that by treaties similar in their terms, made between Russia and each of the protesting powers, Russia had agreed that their subjects should not be troubled or molested in navigating or fishing in any part of the Pacific Ocean.
The American answer was that the Pacific Ocean did not include Bering Sea.
The great central area of Canada is drained towards Hudson Bay, but its two largest rivers have separate watersheds, the Mackenzie flowing north-west to the Arctic Ocean and the St Lawrence north-east towards the Atlantic, the one to the south-west and the other to the south-east of the Archean protaxis.
The northern part of Alberta and Saskatchewan and much of northern British Columbia are drained through the Athabasca and Peace rivers, first north-eastwards towards Athabasca Lake, then north through Slave river to Great Slave Lake, and finally north-west through Mackenzie river to the Arctic Ocean.
It includes Labrador, Ungava and most of Quebec on the east, northern Ontario on the south; and the western boundary runs from Lake-of-the-Woods north-west to the Arctic Ocean near the mouth of Mackenzie river.
The rocks underlying it have been subjected to successive foldings and crumplings by forces acting chiefly from the direction of the Atlantic Ocean, with alternating prolonged periods of waste and denudation.
The chief seaports from east to west are Halifax, N.S., Sydney, N.S., St John, N.B., Quebec and Montreal on the Atlantic; and Vancouver, Esquimalt and Victoria, B.C.; on the Pacific. Halifax is the ocean terminus of the Intercolonial railway; St John, Halifax and Vancouver of the Canadian Pacific railway.
The coast, both of the ocean and of the Great Lakes, is well lighted and protected.
This has been a means of reducing the ocean freight per ton.
The government offered subventions to those who would provide cold-storage warehouses at various points where these were necessary, and also arranged with the owners of ocean steamships to provide cold-storage chambers on them by means of mechanical refrigerators.
This was distinctly unfavourable to Canada's claims, since it excluded Canadians from all ocean inlets as far south as the Portland Channel, and in that channel gave to Canada only two of the four islands claimed.
The chief features of his administration were the fiscal preference of 333% in favour of goods imported into Canada from Great Britain, the despatch of Canadian contingents to South Africa during the Boer war, the contract with the Grand Trunk railway for the construction of a second transcontinental road from ocean to ocean, the assumption by Canada of the imperial fortresses at Halifax and Esquimault, the appointment of a federal railway commission with power to regulate freight charges, express rates and telephone rates, and the relations between competing companies, the reduction of the postal rate to Great Britain from 5 cents to 2 cents and of the domestic rate from 3 cents to 2 cents, a substantial contribution to the Pacific cable, a practical and courageous policy of settlement and development in the Western territories, the division of the North-West territories into the provinces of Alberta and Saskatchewan and the enactment of the legislation necessary to give them provincial status, and finally (1910), a tariff arrangement with the United States, which, if not all that Canada might claim in the way of reciprocity, showed how entirely the course of events had changed the balance of commercial interests in North America.
Inferior land bearing less than 42 quarters per acre would not be protected to the same extent, and moreover, seeing that a portion of the British wheat crop has to stand a charge as heavy for land carriage across a county as that borne by foreign wheat across a continent or an ocean, the protection is not nearly so substantial as Caird would make out.
The subject of the rates of ocean carriage at different periods requires consideration if a proper understanding of the working of the foreign grain trade is to be obtained.
Comparing these figures with a similar statement for the year 1872, the most remote year for which similar facts are available, it will be found that the actual total cost per quarter for ocean carriage has not much decreased.
The contrast between the case of railway freight and ocean freight is to be explained by the greater length of the present ocean voyage, which now extends to 1 o,000 miles in the case of Europe's importation of white wheat from the Pacific Coast of the United States and Australia, in contrast with the short voyage from the Black Sea or across the English Channel or German Ocean.
Now if we add together all these savings in the rate of rail and ocean freights and incidental expenses, we arrive at an aggregate economy of 8s.
But a people of this name seems to have been mentioned by the early traveller Pytheas as inhabiting the coasts of the northern ocean in his time.
Means of transportation for these products are furnished by the rivers, which are generally navigable as far north as the " fall line " passing through Augusta, Milledgeville, Macon and Columbus; by ocean steamship lines which have piers at St Mary's, Brunswick, Darien and Savannah; and by railways whose mileage in January 1909 was 6,871.8 m.
At sea this circle is well defined, the line being called the sea horizon, which divides the visible surface of the ocean from the sky.
The Dip of the horizon at sea is the angular depression of the apparent sea horizon, or circle bounding the visible ocean, below the apparent celestial horizon as above defined.
For a year he relinquished himself to her endearments, and when he determined to leave, she instructed him how to sail to the land of shades which lay on the verge of the ocean stream, in order to learn his fate from the prophet Teiresias.
In 1817, at the instance of John Quincy Adams, the United States and Great Britain entered into a compact whereby the Great Lakes, and the waterways from them to the ocean by the St Lawrence river, which divide the United States from the Dominion of Canada, were practically excluded from any possible hostilities.
On the land side the Kohala Mountains have been covered with lava from Mauna Kea, and form the broad plains of Kohala, having a maximum elevation of about 3000 ft.; on the ocean side, wherever this lava has not extended, erosion has gone on until bluffs woo ft.
Accordingly Mr Gibson addressed a protest to the great powers, deprecating any further annexation of the islands of the Pacific Ocean, and claiming for Hawaii the exclusive right " to assist them in improving their political and social condition."
Here Claudius himself appeared - the one reigning emperor of the 1st century who crossed the waves of ocean, - and the army, crossing the Thames, moved forward through Essex and captured the native capital, Camulodunum, now Colchester.
In 122 the second reigning emperor who crossed the ocean, Hadrian, came himself to Britain, brought the Sixth Legion to replace the Ninth, and introduced the frontier policy of his age.
He came to the conclusion that the Caspian was a gulf or inlet, and that it was possible to enter it by sea from the Indian Ocean.
The Inguaeones again are defined as being " next to the ocean "; but the name can be traced only in Denmark and Sweden, where we find the eponymous hero Ing and the god Yngvi (Frey) respectively.
He sailed with six missionaries on the 30th of December, but died in the following May in the Indian Ocean.
In short, the workings of all the Western episcopates, from Africa to the ocean, the Rhine and the Danube, lay outside the ordinary influence of the Roman see.
Differences of acceleration due to the attractions of the sun and moon are not important for terrestrial systems on a small scale, and can usually be ignored, but their effect (in combination with the rotation of the earth) is very apparent in the case of the ocean tides.
The temperature is quite mild and equable in the south-east province where the ocean influences it and where the mountains bounding it on the north and north-west are some protection from the colder winds.
From its great distance from the ocean it is extremely arid, and possesses no river outlet.
As a whole the system forms the watershed between rivers flowing to the Indian Ocean - the Indus and its tributaries, Brahmaputra and its tributaries, and Salweenand the streams flowing into the undrained salt lakes to the north.
Grotius maintains that the ocean is free to all nations.
It was defended by Fort Fisher, a heavy earthwork on the peninsula between the ocean and Cape Fear river, manned by 1400 men under Colonel William Lamb.
Unlike Java, Sumatra has a series of considerable islands (Nias Islands, Mentawi Islands, &c.) arranged like outworks in front of the west coast, which faces the open Indian Ocean.
The total number of vessels entering the only two ports of Belgium which carry on ocean commerce, namely Antwerp and Ostend, in 1904 was 7650 of a tonnage of 10,330,127.
In pursuit of historical study, Adam visited the Danish court during the reign of the well-informed monarch Svend Estridsson (1047-1076), and writes that the king "spoke of an island (or country) in that ocean discovered by many, which is called Vinland, because of the wild grapes [vites] that grow there, out of which a very good wine can be made.
Although rivers rising in more favoured regions may traverse deserts on their way to the sea, as in the case of the Nile and the Colorado, the fundamental physical condition of an arid area is that it contributes nothing to the waters of the ocean.
Of the two channels named, the southern, which reaches the sea at Flushing, is the more important and is used for ocean commerce.
The empty fruits (after germination of the seed) are found floating in the Indian Ocean, and were known long before the palm was discovered, giving rise to various stories as to their origin.
In the opinion of Russian geologists the separation of the Caspian from the great ocean must have taken place at a comparatively recent geological epoch.
During the early Tertiary age it belonged to the Sarmatian Ocean, which reached from the middle Danube eastwards through Rumania, South Russia, and along both flanks of the Caucasus to the Aralo-Caspian region, and westwards had open communication with the great ocean, as indeed the ancient geographers Eratosthenes, Strabo and Pliny believed it still had in their day.
This communication began to fail, or close up presumably in the Miocene period; and before the dawn of Pliocene times the Sarmatian Ocean was broken up or divided into sections, one of which was the Aralo-Caspian sea already discussed.
In fact the salinity of the Caspian is only three-eights of that of the ocean.
On most of the country west of the 97th meridian and extending to the Pacific Ocean less than 20 in.
The bulk of its water empties by the Mackenzie river into the Arctic Ocean, but a small portion finds its way by the Ark-i-linik river into Hudson's Bay.
The length of German coast on the North Sea or German Ocean is 293 m., and on the Baltic 927 km., the intervening land boundary on the north of Schleswig being only 47 km.
From Lake Ontario the St Lawrence emerges through the meshes of the Thousand Islands, where it crosses Archaean rocks, after which follow several rapids separated by quieter stretches before Montreal is reached at the head of ocean navigation.
Traversing the central portion of the country is a large river known in its upper course as the Lom, and in its lower as the Sanaga, which enters the ocean just to the south of the Cameroon estuary.
Others believed in a celestial ocean, und sonified under the name of Nun, over which the heavenly myl ies sailed in boats.
First of all living things was Re; rid told how he arose as a naked babe from a lotus-flower floated on the primeval ocean Nun.
The proportion of sodium chloride in the water of the ocean, where it is mixed with small quantities of other salts, is on the average about 3.33%, ranging from 2.9% for the polar seas to 3.55% or more at the equator.
Enclosed seas, such as the Mediterranean, the Red Sea, the Black Sea, the Dead Sea, the Caspian and others, are dependent of course for the proportion and quality of their saline matter on local circumstances (see Ocean) .
In 1817 Ceylon was added to his charge; in 182 3 all British subjects in the East Indies and the islands of the Indian Ocean; and in 1824 "New South Wales and its dependencies"!
The salinity of the water is much less than that of the ocean, containing only 1.05% of salt, and the lake freezes every year for a great distance from its shores.
The extensive water-front is lined with wharves, some of which can accommodate the largest ocean steamers.
When such plants are detached they are enabled to float for great distances, and the great Sargasso Sea of the North Atlantic Ocean is probably only renewed by the constant addition of plants detached from the shores of the Caribbean Sea and Gulf of Mexico.
The German Plankton Expedition of 1889 added greatly to our knowledge of the floating vegetable life of the North Atlantic Ocean, while many laboratories established on the shores of inland seas and lakes have rendered a similar service in the case of our freshwater phyto-plankton.
From these hills which catch the first downpour of the rains from the ocean, the ground falls eastward.
Moerenhout, Voyages aux Iles du Grand Ocean, &c. (Paris, 1837); Abraham Fornander, An Account of the Polynesian Race (1878).
In the event, toward the end of the 9th century all Frisia between Walcheren and the German Ocean seems to have become the permanent possession of the invaders.
From the Indian Ocean the Gulf of Oman is entered approximately where Persian territory begins at the tiny port of Gwattar.
It has been conjectured that the "estuary" here mentioned refers to the Baltic, the existence of which as a separate sea was unknown to all ancient geographers; but the obscure manner in which it is indicated, as well as the inaccuracy of the statements concerning the place from whence the amber was actually derived, both point to the sort of hearsay accounts which Pytheas might readily have picked up on the shores of the German Ocean, without proceeding farther than the mouth of the Ems, Weser or Elbe, which last is supposed by Ukert to have been the limit of his voyage in this direction.
No pantheistic theory of an eternal substance continuously expressing itself in different individuals who fall back into its being like drops into the ocean will here be sufficient.
The ocean is the drops.
While market fluctuations might be tided over, the future of Nyasaland remained very much dependent upon the completion of through railway communication from the ocean to Lake Nyasa.
In the northeast it shelves to a shore, but otherwise the coast is rugged and much indented, numerous caves having been carved out by rain, stream and ocean.
More precisely, they may be considered as two groups, one of which, including Teneriffe, Grand Canary, Palma, Hierro and Gomera, consists of mountain peaks, isolated and rising directly from an ocean of great depth; while the other, comprising Lanzarote, Fuerteventura and six uninhabited islets, is based, on a single submarine plateau, of far less depth.
Ocean steamers are able to enter it at all states of wind and tide.
The harbour is a fine one, and the above-named company possesses three wharves capable of berthing the largest Easterngoing ocean steamers.
The fact that the southern extremity of South America is the only land extending into this belt gives it special physical importance in relation to tides and currents, and its position with reference to the Antarctic Ocean and continent makes it convenient to regard it as a separate ocean from which the Atlantic, Pacific and Indian Oceans may be said to radiate.
In this way, then, Africa would have an irregular coast-line, prolonged greatly south of the equator into the Indian Ocean, and running up with an advance upon the present line until it reached its northwest limit outside and south of Sokotra.
On the north side is a sandy beach; on the south cliffs rise abruptly from the ocean.
Then the ocean gradually retired into the great Central Asian depressions.
Its form is that of a great triangle, with its base resting upon the Himalayan range and its apex running far into the ocean.
In many parts they rise in magnificent precipices and headlands out of the ocean, and truly look like colossal " passes or landing-stairs " (ghats) from the sea.
On the south the ocean gives it an oceanic climate, the chief features of which are great uniformity of temperature, small diurnal range of temperature, great dampness of the air, and more or less frequent rain.
Its products are exported from Puntarenas, on the Pacific Ocean, 32 m.
Amsterdam and St Paul, uninhabited islands in the South Indian Ocean, included in an official list of the dependencies of Mauritius drawn up in 1880, were in 1893 annexed by France.
The greater divisions of "the sea," in this sense, are called oceans, and are dealt with under the heading Ocean And Oceanography, the latter being the term now generally applied to the scientific study of the sea.
Such are the Mediterranean Sea and the Caribbean Sea, connected with the Atlantic Ocean; the Arabian Sea, a division of the Indian Ocean, and the China and Japan Seas of the western Pacific Ocean.
The Hadas, in time of flood, reaches the ocean near Adulis in Annesley Bay.
Submarine mountain ranges connect not only the islands within the archipelago, but also the archipelago itself with Borneo and Celebes, so that only shallow channels connect the interior waters with the Pacific Ocean and the China Sea.
Russia, apart from her desire to protect the Orthodox nationalities subject to the Ottoman power, aimed at owning or controlling the straits by which alone she could find an outlet to the Mediterranean and the ocean beyond.
Benton of Missouri, and it was in no small measure through Benton's influence with the government that Fremont was enabled to accomplish within the next few years the exploration of much of the territory between the Mississippi Valley and the Pacific Ocean.
The rivers that drain the Atlantic slope of the Appalachians are comparatively short; those that drain the Pacific slope include only two, the Columbia and the Colorado, which rise far inland, near the easternmost members of the Cordilleran system, and flow through plateaus and intermont basins to the ocean.
The geological processes that placed a much narrower ocean between North America and western Europe than between North America and eastern Asia secured to the New World the good fortune of being colonized by the leading peoples of the occidental Old World, instead of by the less developed races of the Orient.
The transoceanic invasion progressed slowly through the 17th and 18th centuries, delayed by the head winds of a rough ocean which was crossed only in slow sailing vessels, and by the rough " backwoods " of the Appalachians, which retarded the penetration of wagon roads and canals into the interior.
Distance from the ocean, situation with reference to the mountain ranges, and altitude are all important determinants of these climatic differences; but of these the last seems to be most important.
Sunda Strait is the channel separating Sumatra from Java and uniting the Indian Ocean with the Java Sea.
See articles under these headings, and Pacific Ocean (section on Islands).
Along the shores of Chesapeake Bay and the Atlantic Ocean are low, sandy beaches, often enclosing lagoons or salt marshes.
I have studied the subject most extensively, and have had opportunities of judging which no European can have, and I have no hesitation in saying that, ' the mystic songs' of Jayadeva and the ' ocean of love ' notwithstanding, there is nothing in the rituals of Jagannatha which can be called licentious."
A recently described species, Dolichorhynchus indicus, characterized by the great length of the praeoral lobe or snout, has been dredged in the Indian Ocean.
Some of the species can live in the ocean at a depth of two or three miles.
They burrow in the sands of every shore; they throng the weeds between tide-marks; they ascend all streams; they are found in deep wells, in caverns, in lakes; in Arctic waters they swarm in numbers beyond computation; they find lodgings on crabs, on turtles, on weed-grown buoys; they descend into depths of the ocean down to hundreds or thousands of fathoms; they are found in mountain streams as far above sea-level as some of their congeners live below it.
Over the ocean surface, as well as at various depths, float and swim innumerable Hyperiidea - the wonderful Phronima, glass-like in its glassy barrel hollowed out of some Tunicate; the Cystisoma, 4 or 5 in.
These are, briefly speaking, the decay of those great fabrics, church and empire, which ruled the middle ages both as ideas and as realities; the development of nationalities and languages; the enfeeblement of the feudal system throughout Europe; the invention and application of paper, the mariner's compass, gunpowder, and printing; the exploration of continents beyond the ocean; and the substitution of the Copernican for the Ptolemaic system of astronomy.
In the history of the Renaissance, Spain and Portugal represent the exploration of the ocean and the colonization of the other Explora- hemisphere.
To say that it displaced the centre of gravity in politics and commerce, substituting the ocean for the Mediterranean, dethroning Italy from her seat of central importance in traffic, depressing the eastern and elevating the western powers of Europe, opening a path for Anglo-Saxon expansiveness, forcing philosophers and statesmen to regard the Occidental nations as a single group in counterpoise to other groups of nations, the European community as one unit correlated to other units of humanity upon this planet, is truth enough to vindicate the vast significance of these discoveries.
Nor should Raleigh, Drake, Hawkins, the semi-buccaneer explorers of the ocean, be omitted.
To the north-west of the volcanic island of Zebayir the depth is less than 500 fathoms; the bottom of the channel rises to the ioofathom line at Hanish Island (also volcanic), then shoals to 45 fathoms, and sinks again in about the latitude of Mokha in a narrow channel which curves westward round the island of Perim (depth 170 fathoms), to lose itself in the Indian Ocean.
Kriimmel's more recent calculations (see Ocean) give values somewhat higher than those of Karstens.
From the observations of salinity it is inferred that a surface current flows inwards to the Red Sea in the eastern channel of the Strait of Bab el-Mandeb, while a current of very salt water flows outward to the Indian Ocean, through the western channel, at a depth of 50 to loo fathoms from the surface.
The great evaporation going on from the surface probably causes a slow vertical circulation in the depth, the salter colder waters sinking, and ultimately escaping to the Indian Ocean.
Cambrian, Silurian, Devonian and Carboniferous deposits are found on the coasts of the Gulf of Finland and Lake Ladoga, and also along the coasts of the Arctic Ocean (probably Devonian), and in the Kjolen.
Some Finnish geologists - Sederholm for one - consider it probable that during the Glacial period an Arctic sea (Yoldia sea) covered all southern Finland and also Scania (Sickle) in Sweden, thus connecting the Atlantic Ocean with the Baltic and the White Sea by a broad channel; but no fossils from that sea have been found anywhere in Finland.
In the valleys there are many small streams whose waters never reach the ocean, but disappear by seepage or evaporation.
The Yoruba-speaking peoples generalized the spirits of mountain and hill into Oke, god of heights; and the multitude of local sea-gods on the western half of the slave coast was fused into one god of the Ocean, Olokun.
It discharges its waters northward by Slave river and the Mackenzie system to the Arctic Ocean.
A similar idea also occurs in legends of world-wide currency, the best known of these being the Greek, and the medieval Norse, Celtic and Arab legends which describe an earthly Paradise in the Western or Atlantic Ocean (see Atlantis).
With this exception these regions are the most arid on the face of the globe, highly heated by a tropical sun during the day and chilled at night by the proximity of snow-covered heights and a cold ocean current.
Long before the Christian era the satrapies of Darius com.prehended roughly an immense range of territory, from the Mediterranean to the Indus and, from the Caucasian chain and Jaxartes to the Persian Gulf and Arabian Ocean.
The steppe vegetation extends in the south to the outer range of the hills which separate inner Persia from the Persian Gulf and the Indian Ocean.
The coast, fully exposed to the open ocean, abounds in fine cliff scenery, including numerous caves and natural arches, but is notoriously dangerous to shipping.
In its lower course the Bum passes through the Mendi country and enters the network of lagoons and creeks separated from the ocean by the long low tract of Turner's Peninsula.
In the south the drainage is to the Atlantic, chiefly through the Orange River, in the north to the Indian Ocean through the Zambezi, Limpopo and other streams. A large number of smaller rivers rise on the outer slopes of the mountain ramparts and flow direct to the sea.
The eastern escarpments (the Drakensberg, &c.) of the plateau intercept the rain-bearing winds from the Indian Ocean, so that over the greater part of the interior the rainfall is slight (5 to 24 in.).
It was in that century that Portugal rose to prominence as a maritime power; and being anxious to enjoy at first hand some of the commerce which had brought such prosperity to Venice, Portugal determined to seek out an ocean pathway to the Indies.
From early Palaeozoic times the peninsula of India has been dry land, a part, indeed, of a great continent which in Mesozoic times extended across the Indian Ocean towards South Africa.
He gives no precise indication of their geographical position, but states that, together with six other tribes, including the Varini (the Warni of later times), they worshipped a goddess named Nerthus, whose sanctuary was situated on "an island in the Ocean."
They began where the Arabs left off, by penetrating far into the Atlantic. The long littoral of their country, with its fine harbours and rivers flowing westward to the ocean, had been the training-ground of a race of adventurous seamen.
The conception of an ocean route to India appears to have originated after his death.
In Malacca they possessed the connecting link between the traderoutes of the Far and Middle East, and thus they controlled the three sea-gates of the Indian Ocean and Arabian Sea - the Straits of Hormuz, Bab el-Mandeb and Malacca - and diverted the maritime trade with Europe to the Cape route.
The principal form taken by prose writing in the 16th century was historical, and a pleiad of distinguished writers arose to narrate the discoveries and conquests in Asia, Africa and the ocean.
A beautiful drive follows the shore, giving views of the Golden Gate and the ocean.
Every afternoon, especially from October to May, a stiff breeze sweeps the city; every afternoon in the summer the fogs roll over it from the ocean.
But as the most dreaded of these Celtic tribes came down from the shores of the Baltic and Northern Ocean, the ancients applied the name Celt to those peoples who are spoken of as Teutonic in modern parlance.
Ancient writers spoke of all these Gauls as Cimbri, and identified them with the Cimmerians of earlier date, who in Homeric times dwelt on the ocean next to the Laestrygones, in a region of wintry gloom, but where the sun set not in summer.
Those who, as it has been happily put, identify Rabelais with Pantagruel, strive in vain, on any view intellectually consistent or morally respectable, to account for the vast ocean of pure or impure laughter and foolery which surrounds the few solid islets of sense and reason and devotion.
The exhumation and burning of his body in 1428, when the ashes were cast into the Swift, gave rise to the saying that their distribution by the river to the ocean resembled that of Wycliffe's doctrines over the world.
In Scotland and Ireland the pearl mussel fishery was also of importance, but has altogether dwindled into insignificance since the opening up of commercial intercourse with the East and with the islands of the Pacific Ocean, whence finer and more abundant pearls than those of Unio margaritiferus are derived.
These records of temperature afford a striking illustration of the moderating influence of the ocean upon the extremes of summer and winter.
As the heat is thus made less oppressive along the coast, the beaches of New Jersey have rapidly built up with towns and cities that have become popular summer resorts - among the best known of these are Long Branch, Asbury Park, Ocean Grove, Atlantic City (also a winter resort) and Cape May.
In 1899 New Jersey produced nearly a fourth of the cranberry crop of the United States, the chief centre of production being the bogs of Burlington and Ocean counties.
The shell fisheries (oysters particularly) are centred in Delaware Bay and at Maurice River Cove, in Cumberland county, but are important also in Cape May, Atlantic, Ocean and Monmouth 1 The following statistics of the products for 1900 and for 1905 are for factory products, those for 1900 differing, therefore, from the statistics which appear in the reports of the census of 1900.
In 1909 the State Bureau of Shell Fisheries estimated the annual value of shell fisheries in the state at nearly $6,000,000, of which $500,000 was the value of clams. Monmouth, Ocean and Cape May counties furnish large quantities of menhaden, which are utilized for oil and fertilizer.
When the British had gained possession of Philadelphia, in September 1777, their communication between that city and the ocean through the Lower Delaware was obstructed on the New Jersey side by Fort Mercer, commanded by Colonel Christopher Greene, at Red Bank; three battalions of Hessians under Colonel Karl Emil Kurt von Donop attacked the fort on the 22nd of October, but they were repulsed with heavy loss.
The great plains are traversed by a few rivers, whose long and uncertain courses carry their waters to the river Murray, which empties itself into the Southern Ocean through the state of South Australia, and during 1250 m.
He then continued his voyage along the east coast of Australia, and returned to England by way of Torres Strait and the Indian Ocean.
The ocean of water buoys or floats the ship, and the ocean of air, or part of it in motion, swells the sails which propel the ship. The moving air, which strikes the sails directly, strikes.
A balloon differs from a sailing ship in being immersed in only one ocean, viz.
It resembles the flying creature only in this, that it is immersed in the ocean of air in which it sustains itself.
It must launch itself in the ocean of air, and must extract from that air, by means of its travelling surfaces - however fashioned and however applied - the recoil or resistance necessary to elevate and carry it forward.
The coasts are nowhere washed directly by the ocean, except in the extreme south-west; the south coast faces the English Channel, which is bounded on the southern side by the coast of France, the two shores converging from loo m.