Thalassa; an essay on the depth, temperature, and currents of the ocean . •AY /iS•M /Oi of OS00 VO 00 1 1 1 1 •AY /Sz •S ;Sl o*! ^o 00 OM o 00 O 00 8 VO l^ o to N •AV /«^ •S /2^ 00 O %> lo o O1- °o O to N •AY ,Sz•S /St 00 O lo to VO 8 to °N o ON AY /^2 •s /e o8 O VO 1 o OS 1 to to J- •AY ,iS •S /ft „6 VO §? vH O VO to 1 vq toto •AY/t^S /9i of I „ZI VO a OVO O OS vS vg 1 q ^m •AY /2^ •S/ff of I o O xrt Ov OVO Oto 8 to vq 8 to OS •AV /^S•S /9Z of I o^I 1 OO »0 00 to VON to to to 00 •AY ,z •S /Si o^I„IZ 1 O oo N fO 1 00 o to •AY /9f •S /S^ of Io^Zof I o o VO o toN eg % N to •AY/fi •s /•tS -* V
Thalassa; an essay on the depth, temperature, and currents of the ocean . •AY /iS•M /Oi of OS00 VO 00 1 1 1 1 •AY /Sz •S ;Sl o*! ^o 00 OM o 00 O 00 8 VO l^ o to N •AV /«^ •S /2^ 00 O %> lo o O1- °o O to N •AY ,Sz•S /St 00 O lo to VO 8 to °N o ON AY /^2 •s /e o8 O VO 1 o OS 1 to to J- •AY ,iS •S /ft „6 VO §? vH O VO to 1 vq toto •AY/t^S /9i of I „ZI VO a OVO O OS vS vg 1 q ^m •AY /2^ •S/ff of I o O xrt Ov OVO Oto 8 to vq 8 to OS •AV /^S•S /9Z of I o^I 1 OO »0 00 to VON to to to 00 •AY ,z •S /Si o^I„IZ 1 O oo N fO 1 00 o to •AY /9f •S /S^ of Io^Zof I o o VO o toN eg % N to •AY/fi •s /•tS -* V« 1 \J1 8 O 8 Ov 00 •AY /S•S /^Z of Ioff q 1 O VO Orn o to to N2 ?AY /02 ZIo^f q 1 1 1 lO VO OSOro 1- 1 ^-< d z o H< •aanxiOMOi QNV aanxiivT H . <u Uo 3 00 VO °Os °o ^ to ?o to S D £ o O03 s a a-Q °o VD °o to JO w N a II I OSl CJi ^ z<_J I H OCO S * O u z III <X z o < z D H O Ill QC H <Z < o < QC Ui Q < S. Is00 CQ I I l~i I I I \ nn 1 I roooooooooooooooooooooooooooooo— cNcoTj-iott>r^ooo>o:zcMco«i-io From Madeira to Tristan dAcunha. yy speak more definitely, the warm surface-water at the equatoris replaced by water flowing in from the colder strata im-mediately adjoining, which must result in the formation andmaintenance of a stratum of cold water immediately below thesurface of the equatorial belt. This cold stratum, in the presentcase, is found to extend to a depth of about 400 fathoms. In this sense the cold water may be said to rise up towardsthe surface at the equator, but if we compare the thickness ofthe strata under consideration with their horizontal extension inlatitude and longitude, whatever movement may take place in avertical direction must be absolutely insignificant in comparisonwith the horizontal currents thus created. This inflow of coldwater will take place more or less along the whole boundarybetween the equatorial belt and the colder belt immediatelya
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Keywords: ., bookcentury1800, bookdecade1870, bookidthalassa, booksubjectocean
