The Ocean: A Treatise on Ocean Currents and Tides and Their Causes, Demonstrating the System of the WorldLongmans, Green, 1885 - 281 pagina's |
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Pagina xv
... ARCTIC CURRENTS XI . ANTARCTIC CURRENTS XIa . " " 99 XII . NEWTON'S ILLUSTRATION OF ORBITAL MOTION XIII . THE TIDES XIV . THE TIDES 42 " " " 9 44 " " 99 43 " " " " 70 " " " " 1 103 " " 99 36 111 • " " XV . SKETCH OF THE CURRENT ...
... ARCTIC CURRENTS XI . ANTARCTIC CURRENTS XIa . " " 99 XII . NEWTON'S ILLUSTRATION OF ORBITAL MOTION XIII . THE TIDES XIV . THE TIDES 42 " " " 9 44 " " 99 43 " " " " 70 " " " " 1 103 " " 99 36 111 • " " XV . SKETCH OF THE CURRENT ...
Pagina 41
... polar district of currents analogous to those whose formation has been described in Part III . of this chapter , and illustrated in Plate VI . The basin of the Arctic Ocean thus forms a part CHAP . II . ] 41 INERTION .
... polar district of currents analogous to those whose formation has been described in Part III . of this chapter , and illustrated in Plate VI . The basin of the Arctic Ocean thus forms a part CHAP . II . ] 41 INERTION .
Pagina 42
... Arctic Ocean thus forms a part of the Arctic district of the Atlantic Ocean : and , therefore , the stream which on the eastern side of the Atlantic flows northwards from the temperate zone enters the Arctic Ocean on the eastern side of ...
... Arctic Ocean thus forms a part of the Arctic district of the Atlantic Ocean : and , therefore , the stream which on the eastern side of the Atlantic flows northwards from the temperate zone enters the Arctic Ocean on the eastern side of ...
Pagina 42
... obser The normal su : Ocean , for it ter is not the preponderating force in the Arctic S ... BRITISH ISLES W.L.Jordan . Edw4Weller . London Longmans & Co. however , the Antarctic voyages of discovery under Sir James. Plate X.
... obser The normal su : Ocean , for it ter is not the preponderating force in the Arctic S ... BRITISH ISLES W.L.Jordan . Edw4Weller . London Longmans & Co. however , the Antarctic voyages of discovery under Sir James. Plate X.
Pagina 42
... ocean a stream flowing southwards and eastwards from the equatorial regions meets a stream flowing westwards and northwards from the polar regions , as shown in the plate : and , from the meeting - point in each ocean ... arctic coast , and ...
... ocean a stream flowing southwards and eastwards from the equatorial regions meets a stream flowing westwards and northwards from the polar regions , as shown in the plate : and , from the meeting - point in each ocean ... arctic coast , and ...
Overige edities - Alles bekijken
The Ocean: A Treatise on Ocean Currents and Tides and Their Causes ... William Leighton Jordan Volledige weergave - 1885 |
The Ocean: A Treatise on Ocean Currents and Tides and Their Causes ... William Leighton Jordan Geen voorbeeld beschikbaar - 2018 |
The Ocean: A Treatise on Ocean Currents and Tides and Their Causes ... William Leighton Jordan Geen voorbeeld beschikbaar - 2015 |
Veelvoorkomende woorden en zinsdelen
according action of vis-inertiæ Antarctic Arctic Ocean astral gravitation axial rotation axis body Caribbean Sea centre centrifugal force CHAPTER circulation coast combined action counter-current course Crown 8vo cube current-creating action deep and central direct force distance district earth's gravitation east Edition effects equator equatorial regions equilibrium flowing force of astral force of gravitation gravitation drawing gravitation tends greater force Gulf Stream Illustrations increase inertiæ inversely latter lesser forces lower strata meridian move Natural Philosophy North Atlantic northwards ocean currents onward motion opposite direction orbital force orbital motion orbital revolution Pacific particles planets Plate poles position power of gravitation Proposition regards resistance resulting revolving force round the sun shown side solar system solar tide Southern Ocean southwards square stream A B C sun and moon sun's gravitation temperate zones tendency tends to carry tends to cause tends to draw theoretical tion vols wards westward pressure Woodcuts
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