UC-NRLF B 3 3bl 133 PRIVATE LIBRARY OF CHARLES A. KOFOID No.* A? Cost..T.* THE LIBRARY OF THE UNIVERSITY OF CALIFORNIA PRESENTED BY PROF. CHARLES A. KOFOID AND MRS. PRUDENCE W. KOFOID FLEET OF MEDUSAE. (See page 161.) THE OC BAN WORLD: KF.ING A DESCRIPTION OK The Sea and some of its Inhabitants. 1 ROM IMF. FKFNCll OF LOUIS F I G U I E R Xl'.ir RDITIOX. RRl'ISRD /,'!' E. PERCEVAL WRIGHT, M.D., F.L.S., Professor of Botany in the University of Dublin. WITH 435 ILLUSTRATIONS. CASSELL, FETTER, GALPIN & Co, LONDON, PARIS & NEW YORK. [ALL RIGHTS RESERVED.] U\by aw PREFACE. A NEW edition of this work having been called for, I was requested to revise it and see it through the press. The attempt to render scientific subjects popular and attractive to the general reader has always appeared to me a most laudable one. It has always received the support of our most original workers and deepest thinkers ; and yet, so far as the English language is concerned, the attempt to make zoological science familiar to the ordinary reader has, in my opinion, most generally been a failure. Such essays as the " Studies of Animal Life," by G. H. Lewes, were indeed full of promise ; but such served scarcely more than to introduce the reader to the very threshold of the science, though they at the same time showed what thoroughly good work could be done in this direction by our British scientific men. In the meanwhile, a series of most attractive works on biological science, and beautifully illustrated, was being pub- lished in France, some written or edited by names well known in the fields of scientific research, others — as those by M. Figuier— by men eloquent after the fashion of their countrymen, but much wanting in that exact knowledge of the sciences about which they wrote, and which would have enabled them to avoid falling into many and grievous errors. IV PREFACE. With the faint hope that I would have no difficulty in simply retaining the text that helps to explain the in general excellent woodcuts that illustrate the present volume, I undertook to revise it. Those familiar with the subject will perhaps appreciate the statement that, as it proved, it would have been an easier and certainly a more pleasant task to have re-written the work. Those who will compare the present edition with that of 1869, will see that the alterations in this one have been very numerous and important, several chapters being nearly re-written ; that all the dogmatic asser- tions, so striking in the edition of 1869, have been toned down in conformity with that modesty that should characterise the searchers after truth ; and that the more rampant twigs of French eloquence have been pruned in conformity with our quieter if not better taste. Would that I could add that they will also find all errors corrected, but of the contrary I am painfully aware. At the same time, I believe the candid critic will see that if in this matter I have not done all I should, I have at least, under all the circumstances, done all I could. I am indebted to my friend, G. J. Stoney, M.A., F.R.S., for the short account of the cause of the tides, to be found on pages 32 to 35. Perhaps never before has the subject been treated in a more popular and yet scientific a way. E. P. W. n . CONTENTS. CHAPTER I. THE OCEAN Depth of the Sea Colour of the Sea Phosphorescence . Saltness of the Sea CHAPTER II. CURRENTS OF THE OCEAN Trade Winds Gulf Stream Tides The Arctic Regions The Antarctic Regions CHAPTER III. LIFE IN THE OCEAN CHAPTER IV. PROTOZOA . . . Sponges Rhizopods . . Infusoria CHAPTER V. CCELENTERATA CHAPTER VI. HYDROZOA Hydridie Corynidae . . . Sertulariadae . . Calycophoridas . . Physophoridse Medusidae . CHAPTER VII. PAGE 1 ACTINOZOA; ZOANTHARIA PAGR 171 3 Antipathidae 172 10 ii Madreporidae Coral Islands 173 190 i^ 20^ *o CHAPTER VI 11. •WJ 25 ACTINOZOA ; ALCYONARJA 218 26 28 Tubiporidae . . . Gorgonidae .... 218 220 32 Isidinae .... 224 40 Corallinse .... 225 46 Coral Fishing 236 Pennatulidae 240 Alcyonidae .... 244 55 ACTINOZOA; CTENOPHORA 248 CHAPTER IX. 62 ECHINODERMATA . . 253 6s Crinoi'dese .... 263 **3 76 Asteriadae .... 269 /y 88 Ophiuridae . 269 Echinidae .... 275 Holothuroideae . 286 MOLLUSCA. GENERAL REMARKS 300 107 CHAPTER X. MOLLUSCOlDA .... 302 1 1 o Polyzoa .... 302 113 Tunicata .... 308 122 124 CHAPTER XI. 126 MOLLUSCA PROPER . 3i6 128 ACEPHALA .... 317 I56 Siphonida .... 32i VI CONTENTS. CHAPTER XII. ACEPHALA . . . Asiphonida . . . . Mussel Fisheries . . . Pearl Oyster Fisheries . Oyster Fisheries and Parks CHAPTER XIII. BRACHIOPODA . CHAPTER XIV. CEPHALA . Three classes of Cephala i. GASTEROPODA Order I. Nucleo-branchiata ,, 2. Opistho-branchiata 410 CHAPTER XV. Order 3. Pulmonifera . CHAPTER XVI. Order 4. Prosobranchiata CHAPTER XVII. ii. PTEROPODS CHAPTER XVIII. PAGE 354 in. CEPHALOPODA . PAGB • 470 354 Order I. Tetrabranchiata • 470 356 ,, 2. Dibranchiata • 473 366 Distribution of Mollusca . 498 385 CHAPTER XIX. CRUSTACEA . 50} . 407 Orders of Crustacea . 510 CHAPTER XX. . 409 FISHES .... . 527 . 409 . 409 i 410 Leptocardia . Cyclostomata . . Selachia • 533 • 533 . 535 a 4IQ Ganoidea . • 552 CHAPTER XXI. . 414 TELEOSTEA, OR BONY FISHES • 558 Plectognatha . . • 558 . 428 Lophobranchia . Pharyngognatha . . 562 • 565 Physostomata • 570 Anacanthina '• »dA . 604 . 466 Acanthopterygea . . 621 FULL-PAGE ILLUSTRATIONS. FLEET OF MEDUSA Frontispiece I. SPONGE FISHING ON THE COAST OF SYRIA . . To face 70 II. GALEOLARIA AURANTIACA ..... ,, 128 III. AGALMA RUBRA ,, 135 IV. CORAL ISLAND IN THE POMOTOUAN ARCHIPELAGO ,, 192 V. SEA ANEMONES (I.) ,,211 VI. SEA ANEMONES (II.) ,,212 VII. CORAL FISHING OFF THE COAST OF SICILY . . ,, 239 VIII. SEA-URCHINS ,,275 IX. FISHING FOR HOLOTHURIA ..... ,, 290 X. SYNAPTA DUVERNEA ,, 296 XI. TEMPLE OF SERAPIS. ...... ,, 331 XII. SOLENID^E (Razor-fish] , ,,334 XIII. VENUS AND CYTHEREA ,, 341 XIV. TRIDACNA GIGANTEA ,, 344 XV. ANODONTA ,, 348 XVI. DREDGING FOR OYSTERS ,, 38$ XVII. OYSTER PARKS ON LAKE FUSARO .... ,,388 XVIII. PECTID^E ,401 XIX. SPONDYLUS ,,405 XX. VOLUTA ,,449 XXI. CONUS .,450 XXII. CAPTURE OF A GIGANTIC CUTTLE-FISH ... ,, 489 XXIII. SHARK FISHING .- ,, 546 XXIV. STURGEON FISHING ON THE VOLGA ... ,, 554 XXV. FISHING FOR ELECTRICAL EELS .... ,, 572 XXVI. THE HERRING FISHERY ,, 592 XXVII. GREENLANDERS FISHING FOR HOLIBUT . . . ,, 613 XXVIII. A ROMAN FEAST .... . ,,624 XXIX. FISHING FOR TUNNY IN PROVENCE ... „ 633 XXX. FISHING FOR MACKEREL OFF THE CORNWALL COAST „ 636 THE OCEAN WORLD. CHAPTER I. THE OCEAN. ''Apiorov nev uScop — "The best of all things is water." — PlNDAR. IT is estimated that the sea covers nearly two-thirds of the surface of the earth. The calculation, as given by astronomers, is as follows : The surface of the earth is^3 1,625, ^25iV square miles, that portion occupied by the waters being about 23,814,121 square miles, and that consisting of continents, peninsulas, and islands, being 7,811,504 miles ; whence it follows that the surface covered with water is to dry land as 3-8 is to i'2. The waters thus cover a little more than seven-tenths of the whole surface. " On the surface of the globe," Michelet remarks, " water is the rule, dry land the exception." Nevertheless, the immensity and depth of the seas are aids rather than obstacles to the intercourse and commerce of nations ; the maritime routes are now traversed by ships and steamers conveying cargoes and passengers equal in extent and in point of numbers to the land routes. One of the features most characteristic of the ocean is its continuity ; for, with the exception of inland seas, such as the Caspian, the Dead Sea, and some others, the ocean is one and indivisible — "it embraces the whole earth with an uninterrupted wave." Ilept ira&av 0' fl\iffffo/ut.fvovs AESCHYLUS in Prome'heus Vmcfus. The mean depth of the sea is not very exactly ascertained, but certain phenomena observed in the movement of tides are supposed to be incapable of explanation without admitting a mean depth of 2 THE OCEAN WORLD. 3,500 fathoms. It is true that a great number of deep-sea soundings fall short of that limit ; but, on the other hand, many others reach 7,000 or 8,000. Admitting that 3,000 fathoms represent the mean depth of the ocean, Sir John Herschel finds that the volume of its waters would exceed 3,279,000,000 cubic yards. This vaiit volume of water is divided by geographers into five great oceans : the Arctic, the Atlantic, Indian, Pacific, and Antarctic Oceans. The Arctic Ocean extends from the Pole to the Polar Circle ; it is situated between Asia, Europe, and America. The Atlantic Ocean commences at the Polar Circle, and reaches Cape Horn. It is situated between America, Europe, and Africa, in length of about 9,000 miles, with a mean breadth of 2,700, covering a surface of about 25,000,000 square miles, placed between the Old World and the New. Beyond the Cape of Storms, as Cape Horn may be truly called, it is only separated by an imaginary line from the vast seas of the south, in which the waves, which are the principal source of tides, have their birth. Here, according to Maury, the young tidal wave, rising in the circumpolar seas of the south, and obedient to the sun and moon, rolls on to the Atlantic, and in twelve hours after passing the parallel of Cape Horn is found pouring its flood into the Bay of Fundy, whence it is projected in great waves across the Atlantic and round the globe, sweeping along its shores and penetrating its gulfs and estuaries, rising and falling in the open sea two or three feet, but along the shore having a range of ten or twelve feet ; sometimes, as at Fundy on the American coast, at Brest on the French coast, and Milford Haven and the mouth of the Severn in the Bristol Channel, rising and falling thirty or forty feet, " impetuously rushing against the shores, but gently stopping at a given line, and flowing back to its place when the word goes forth, ' Thus far shalt thou go and no farther.' That which no human power could repel returns at its appointed time so regularly and surely, that the hour of its approach and the measure of its mass may be predicted with unerring certainty centuries beforehand." The Indian Ocean is bounded on the north by Asia, on the west by Africa, on the east by the peninsula of Molucca, the Sunda Isles, and Australia. The Pacific, or Great Ocean, stretches from north to south, trom the Arctic to the Antarctic Circle ; being bounded on one side by Asia, the island of Sunda, and Australia, on the other by the west coast of America. This ocean contrasts in a striking manner with the Atlantic : the one has its greatest length from north to south, the THE SEA. 3 other from east to west ; the currents of the Pacific are broad and slow, those of the other narrow and rapid ; the waves of this are low, those of the other very high. If we represent the volume of water which falls into the Pacific by one, that received by the Atlantic will be represented by the figure five. The Pacific is the calmest of seas, and the Atlantic Ocean is the most stormy. The Antarctic Ocean extends from the Antarctic Polar Circle to the South Pole. It is remarkable that one half of the globe should be entirely covered with water, whilst the other contains less of water than dry land ; moreover, the distribution of land and water— if, in considering the extent of the oceanic basins, we compare the hemispheres separated by the Equator and the northern and southern halves of the globe — is found to be very unequal. Oceans communicate with continents and islands by coasts, which are said to be scarped when a rocky coast makes a steep and sudden descent to the sea, as, for example, in Brittany, Norway, and the west coast of the British Islands. In this kind of coast certain rocky indentations encircle it, sometimes above, sometimes under water, forming a labyrinth of islands, as at the Land's End, Cornwall, where the Scilly Islands form a compact group of from 100 to 200 rocky islets, rising out of a deep sea. The coast is said to be flat when it consists of soft argillaceous soil descending to the shore with a gentle slope. Of this description of coast there are two — namely, sandy beaches, and hillocks or dunes. What is the average depth of the sea ? It is difficult to give an exact answer to this question, because of the great difficulty met with in taking soundings, caused chiefly by the deviations of submarine currents. No reliable soundings have yet been made in water over five miles in depth. Laplace found, on astronomical consideration, that the mean depth of the ocean could not be more than 10,000 feet. Alexander von Humboldt adopts the same figures. Dr. Young attributes to the Atlantic a mean depth of 1,000 yards, and to the Pacific, 4,000. Mr. Airy, the Astronomer Royal, has laid down a formula, that waves of a given breadth will travel with certain velocities at a given depth, from which it is estimated that the average depth of the North Pacific, between Japan and California, is 2,149 fathoms, or two miles and a half. But these estimates fall far short of the soundings reported by navigators, in which, however, as we shall see, there are important and only recently-discovered elements of error. Du 4 THE OCEAN WORLD. Thouars, during his scientific voyage in the frigate Venus, took some very remarkable soundings in the Southern Pacific Ocean : one, without finding bottom at 2,411 fathoms ; another, in the equinoctial region, indicated bottom at 3,790. In his last expedition in search of a north-west passage, Captain Ross found soundings at 5,000 fathoms. Lieutenant Walsh, of the American Navy, reports a cast of the deep-sea lead, not far from the American coast, at 34,000 feet without bottom. Lieutenant Berryman reported another unsuccessful attempt to fathom mid ocean with a line 39,000 feet in length. Captain Denman, of H. M.S. Herald, reported bottom in the South Atlantic at the depth of 46,000 feet ; and Lieutenant J. P. Parker, of the United States frigate Congress, on attempting soundings near the same region, let go his plummet, after it had run out a line 50,000 feet long, as if the bottom had not been reached. We have the authority of Lieutenant Maury for saying, however, that " there are no such depths as these." The under- currents of the deep sea have power to take the line out long after the plummet has ceased to sink, and it was before this fact was discovered that these great soundings were reported. It has also been discovered that the line, once dragged down into the depths of the ocean, runs out unceasingly. This difficulty was finally overcome by the ingenuity of Midshipman Brooke. Under the judicious patronage of the Secretary to the United States Navy, Mr. Brooke invented the simple and ingenious apparatus (Fig. i), by which sound ngs are now made, in a manner which not only establishes the depth, but brings up specimens of the bottom. The sounding line in this apparatus is attached to a weighty rod of iron, the lower extremity of which contains a hollow cup for the reception of tallow or some other soft substance. This rod is passed through a hole in a thirty-two pound spherical shot, being supported in its position by slings A, which are hooked on to the line by the swivels a. When the rod strikes the bottom, the tension on the line ceases, the swivels are reversed, the slings B are thrown out of the hooks, the ball falls to the ground, and the rod, released from its weight, is easily drawn up, bringing with it portions of the bottom attached to the greasy substance in the cup. By means of this apparatus, specimens of the bottom have been brought up from the depth of four miles. The greatest depth at which the bottom has been reached with this plummet is in the North Atlantic between the parallels of 35° and 40° north, and immediately south of the great bank of rocks off Newfoundland. This does not appear to be more than 20,000 feet deep. " The basin of the Atlantic," says Maury, DEPTH OF THE OCEAN. 5 '•according to the deep-sea soundings in the accompanying dia- gram, is a long trough separating the Old World from the New, and extending, probably, from pole to pole. In breadth it contrasts strongly with the Pacific Ocean. From the top of Chimborazo to Fig. i —Brooke's Sounding Apparatus the bottom of the Atlantic, at the deepest place yet reached by the plummet in that ocean, the distance in a vertical line is nine miles." " Could the waters of the Atlantic be drawn off, so as to expose to view this great sea gash which separates continents, and extends from the Arctic to the Antarctic Seas, it would present a scene the most rugged, grand, and imposing ; the very ribs of the solid earth 6 TUB OCEAN WORLD. with the foundations of the sea would be brought to light, and we should have presented to us in one view, in the empty cradle of the ocean, ' a thousand fearful wrecks/ with the array of * dead men's skulls, great anchors, heaps of pearls,, and inestimable stones,' which, in the poet's eye, lie scattered on the bottom of the sea, making it hideous with the sight of ugly death." The depth of the Mediterranean is comparatively inconsiderable. Between Gibraltar and Ceuta, Captain Smith estimates the depth at Fig 2 —Chart of the Atlantic Ocean. about 5,700 feet, and from 1,000 to 3,000 in the narrower parts of the straits. Near Nice Saussure found bottom at 3,250. It is said that the bottom is shallower in the Adriatic, and does not exceed 140 feet between the coast of Dalmatia and the mouths of the Po. The Baltic Sea is remarkable for its shallow waters, its maximum depth rarely exceeding 600 feet. It thus appears thaUthe sea has similar inequalities to those observed on land ; it has its mountains, valleys, hills, and plains. The deep-sea sounding apparatus of Lieutenant Brooke has already- furnished -some very remarkable results. Aided by it. DEPTH OF THE OCEAN. J Dr. Maury has constructed his fine orographic map of the basin of the Atlantic. Dr. Maury has also published many charts, giving the depths of the ocean, the substance of which is given in the accom- panying map, which represents the configuration of the Atlantic up to the tenth degree of south latitude, not in figures, as in Dr. Maury's charts, but in tints ; diagonal lines from right to left, representing the shores of both hemispheres, indicate a depth of less than 1,000 K. thorns ; from left to right indicate bottom at 1,000 to 2,000 ; hori- zontal lines, 2,000 to 3,000 fathoms ; cross lines show an average depth of 3,000 to 4,000 fathoms ; finally, the perpendicular lines in- dicate a depth of 4,000 fathoms and upwards. Solid black indicates continents and islands ; waving lines, surrounding both continents at a short distance from the shore, indicate the sands which surround the coast line at a little distance from the shore. The question may be asked, what useful purpose is served by taking soundings at great depths? To this we may quote the answer of Franklin to a question of similar tendency, addressed to aeronauts — "What purpose is served by the birth of a child?" Every fact in physics is interesting in itself; it forms a rallying point, round which, sooner or later, others will meet, in order to establish some useful truth ; and the importance of making and recording deep-sea soundings is established by the successful immersion of the transatlantic telegraph. At the bottom of the Atlantic there exists a remarkable plateau, extending from Cape Race in Newfoundland, to Cape Clear in Ireland, a distance of over 2,000 miles, with a breadth of 470 miles ; its mean depth along the whole route is estimated at two miles and a half. It is upon this telegraphic plateau, as it has been called, that the attempt was made to lay down the cable in 1858, and it is on it that the enterprise was so successfully completed during the year 1866. The surface of the plateau had been previously explored by means of Brooke's apparatus, and the bottom was found to be composed chiefly of microscopic calcareous shells {Foraminifera\ and a few siliceous shells (Diatomacecz). These delicate and fragile shells, which seemed to strew the bottom of the sea in beds of great thickness, were brought up by the sounding-rod in a state of perfect preservation, which proves that the water is remarkably quiet in these depths — an inference which is fully borne out by the condition in which the cable of 1858 was found, when picked up in 1866. The first exploration of this plateau was undertaken by the American brig Dolphin, which took 100 soundings 100 miles from 8 THE OCEAN WORLD. the coast of Scotland, afterwards taking the direction of the Azores, to the north of which bottom was found, consisting of chalk and yellow sand, at 9,600 feet. To the south of Newfoundland the depth was found to be 16,500 feet. In 1856, Lieutenant Berry man, of the American steamer Arctic, completed a line of soundings from St. John, Newfoundland, to Valentia, off the Irish coast; and in 1857, Lieutenant Dayman, of the English steamship Cyclops, repeated the same operation : this last line of soundings, the result of which is represented in the accompanying section, differed slightly from that followed by Lieutenant Berry man. In the Gulf of Mexico the depth does not seem to exceed 7,000 feet. The Arctic Ocean has, probably, no great depth. Hence, salt water, following the general law of con- tracting as it cools, until it freezes, no ice can be formed on its surface till the temperature has fallen through its entire depth nearly to freezing point, when the entire mass is consolidated into pack-ice. According to Baron Wrangel, the bottom of the glacial sea, on the north coast of Siberia, forms a gentle slope, and, at the distance of 200 miles from the shore, it is still only from ninety to 100 feet. Nevertheless, in Baffin's Bay, Dr. Kane made soundings at 11,600 feet. The inequalities of the basin of the Pacific Ocean are, comparatively, unknown to us. The greatest depth observed by Lieutenant Brooke in the great ocean is 2,700 fathoms, which he found in 59° north latitude and 1 66° east longitude. Applying the theory of waves to the billows propelled from the coast of Japan to Cali- fornia, during the earthquake of the 23rd of December, 1854, Professor Bache calculated that the mean depth of this part of the Pacific is 14,400 feet. In the Pacific Ocean, latitude 60° south and 160° east longitude, he found soundings at 14,600 feet — about two miles and a half. Another cast of the lead in the Indian Ocean was made in 7,040 fathoms, but without bringing up any soil from the bottom. Among the fragments brought up from the bottom of the Coral Sea, a remarkable absence of calcareous shells was noted, whilst the siliceous frag- ments of sponges were found in great quantities. Other soundings made in the Pacific, at a depth of tour or five DEPTH ~OF THE OCEAN. 9 miles, were, examined by Ehrenberg, who found 135 different forms of Infusoria represented, and among them twenty-two species new to him. These Protozoa draw from the sea the mineral matter with which it is charged— that is, the lime or the silica, which form their shell. These shells accumulate after the death of the animal, and form the bottom of the ocean. The animals construct their habitations near the surface ; when they die, they fall into the depths of the ocean, where they accumulate in myriads, forming mountains and plains in mid ocean. In this manner, we may remark en passant, many of the existing continents probably had their birth in geological times'. The horizontal beds of marine deposits, which are called sedimentary rocks, and especially the cretaceous rocks and calcareous beds of the Jurassic and Tertiary periods, all result from such remains.* The sea level is, in general, the same everywhere. It represents the spherical form of our planet, and is the basis for calculating all terrestrial heights ; but many gulfs and inland seas open on the east are supposed to be exceptions to this rule : the accumulation of waters, pressed into these receptacles by the general movement of the sea from east to west, it is alleged, may pile up the waters, in some cases to a greater height than the general level. It had long been admitted, on the faith of inexact observation, that the level of the Red Sea was higher than that of the Mediter- ranean. It has also been said that the level of the Pacific Ocean at Panama is higher by about forty inches than the mean level of the Atlantic at Chagres, and that, at the moment of high water, this difference is increased to about thirteen feet, while at low it is over six feet in the opposite direction. This has been proved, so far as direct evidence goes, to be an error in so far as regards the difference in level of the Red Sea and Mediterranean ; and the opening of the Suez Canal has now furnished convincing proofs of it. Recent soundings show that the mean level of the Pacific and Atlantic Oceans are identical. It has been calculated that all the waters of the several seas gathered together would form a sphere of fifty or sixty leagues m diameter, and, supposing the surface of the globe perfectly level, that these waters would submerge it to the depth of more than 600 feet Again, admitting the mean depth of the sea to be 13,000 feet, its estimated contents ought to be nearly 2,250,000,000 of cubic miles of water ; and, if the sea could be imagined to be dried up, all # * " World Before the Deluge," 2nd edition. B IO THE OCEAN WORLD. the rivers of the earth would require to pour their waters into it for 40,000 years, in order to fill the vast basins anew. If we could imagine the entire globe to be divided into 1,786 parts by weight, we should find approximately, according to Sir John Herschel, that the total weight of the oceanic waters is equivalent to one of these parts. The specific density of sea water is a little above that of fresh water, the proportion being as 1,000 to 1,027. The Dead Sea, which receives no fresh water so as to enable it to maintain itself at the same level as other seas, acquires a higher degree of saltness each year: its present density is equal to 1,028. The colour of the sea is continually varying, and is chiefly caused by filtration of the solar rays. According to the testimony of the majority of observers, the ocean, seen by reflection, presents a fine azure blue or ultramarine (cceruleum mare). When the air is pure and the surface calm, this tint softens insensibly, until it is lost and blended with the blue of the heavens. Near the shore it becomes more of a green or glaucous tint, and more or less brilliant, according to circumstances. There are some days when the ocean assumes a livid aspect, and others when it becomes a very pure green ; at other times, the green is sombre and sad. When the sea is agitated, the green takes a brownish hue. At sunset the surface of the sea is illumined with tints of every hue of purple and emerald. Placed in a vase, sea water appears perfectly transparent and colourless. According to Scoresby, the Polar seas are of brilliant ultramarine blue. Castaz says of the Mediterranean, that it is celestial blue, and Tuckey describes the equinoctial Atlantic as being of a vivid blue. Many local causes influence the colours of marine waters, and give them certain decided and constant shades. A bottom of white sand will communicate a greyish or apple-green colour to the water, if not very deep ; when the sand is yellow, the green appears more sombre; the presence of rocks is often announced by the deep colour which the sea takes in their vicinity. In the Bay of Loango the waters appear of a deep red, because the bottom is there naturally red. It appears white in the Gulf of Guinea, yellow on the coast of Japan, green to the west of the Canaries, and black round the Maldive group of islands. The Mediterranean, towards the Grecian Archipelago, sometimes becomes more or less red. The White and Black Seas appear to be named after the ice of the one and the tempests to which the other is subject PHOSPHORESCENCE. OF THE SEA. -tf At other times coloured animal or vegetable bodies give to the water a particular tint. The Red Sea owes its colour to a minute microscopic algae (Trichodesmium erythr