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animal appears base beds bird body Brit British brown called characters circumstance coast colour common considerable considered contains continued covered described direction distinct Donovan dorsal fin Dublin Bay east effects examined extending extremity Falcon feet field fish formation four frequently granite half head inches Islands land length less Linn mark mass mentioned miles Montagu natural nearly noticed numerous observed occur ocean opening opinion organs original particular plumage Portmarnock present probably Professor JAMESON rare rays red sandstone remarks rocks rounded rows sand sandstone Secretary seems seen shell ship shores side similar Society sometimes species specimens spines stone strata supposed surface tail taken Test thickness tion uncommon usually variety veins viii whole wind
Page 568 - If I do prove her haggard, Though that her jesses were my dear heart-strings, I'd whistle her off, and let her down the wind, To prey at fortune.
Page 280 - ... producing a loud grinding, or lengthened acute tremulous noise, accordingly as the degree of pressure was diminished or increased, until it had risen as high as the deck. After about two hours, the velocity was diminished to a state of rest ; and soon afterwards, the two sheets of ice receded from each other, nearly as rapidly as they before advanced.
Page 277 - ... that of fields in general. " Fields may sometimes have their origin in heavy close packs, which, being cemented together by the intervention of new ice, may become one solid mass. In this way, are produced such fields, as exhibit a rugged, hummocky surface.
Page 321 - ... 3. On approaching a pack, field, or other compact aggregation of ice, the phenomenon of the ice-blink is seen whenever the horizon is tolerably free from clouds, and in some cases even under a thick sky. The ice-blink consists in a stratum of a lucid whiteness, which appears in that part of the atmosphere next the horizon. It is evidently occasioned thus : those rays of light which strike on the snowy surface of the ice, are reflected into the superincumbent air, where they become visible ; but...
Page 276 - July, whereby the covering of snow, annually deposited to the depth of two or three feet on the ice *, dissolves. Now, as this field is supposed to arise amidst the older and heavier ice, it may readily occupy the whole interval, and be cemented to the old ice on every side ; whence, the melted snow has no means of escape.
Page 271 - ... quantities that are dissolved and dissipated by the power of the waves, and the warmth of the climate into which it drifts. It has frequently been urged, that the vicinity of land is indispensable for its formation. Whether this may be the case or not, the following facts may possibly determine.
Page 281 - ... twenty-five feet from the level of the water ; they extended fifty or sixty yards in length, and fifteen in breadth'., forming a mass of about two thousand tons in weight. The majestic unvaried movement of the ice, — the singular noise with which it was accompanied, — the tremendous power exerted, — and the wonderful effects produced, were calculated to excite sensations of novelty and grandeur, in the mind of even the most careless spectator ! Sometimes these motions of the ice may be...
Page 299 - The place of their retreat, however, is regulated by various circumstances ; it may sometimes depend on the quality and quantity of food occurring, the disposition of the ice, or exemption from enemies. At one time, their favourite haunt is amidst the huge and extended masses of the field ice ; at another, in the open seas adjacent. Sometimes the majority of the whales inhabiting those seas, seem collected within a small and single circuit ; at others, they are scattered in various hordes, and numerous...
Page 279 - The weaker field is crushed with an awful noise; sometimes the destruction is mutual ; pieces of huge dimensions and weight are not unfrequently piled upon the top, to the height of twenty or thirty feet, while a proportionate quantity is depressed beneath.