. Thalassa; an essay on the depth, temperature, and currents of the ocean. V ,iS 06 vo 9- o vO UN OvO 1 vq°CM UN 3- CO AV /?* S /9i o^I 0Z1 °vO o CO O VO o ON OvO OvOCO 1 q oCO UN OCO AV /«* o^I O O UN ON vg o UN CO oo UN vq oCM oo UN ON CO co AV /Z?S /9Z .Si CM 1 UNUN 8 UN oo UN VOCM UN 2 UN 5 oo COCO AV ,2•S /?i o*I oIZ CM 1 O UN CM oo CM OCO CO 8<* 00o O OnOn COCO •AV /9^•S /8^ 0£i O °voCM o o vO o UN UNUN CM O00CO CM UN oCM O<*? CM VO COCO •AV /Si•S ,« CM 1 UN CO oo o CM o oo CO 8 CM ON o ON00 NCOCO AV /S o^I o*£ q °cOCM 1 UN co UN o un vOCM o CO O UN co UN CM2 UN CO AV /OZ S ,oz 51
. Thalassa; an essay on the depth, temperature, and currents of the ocean. V ,iS 06 vo 9- o vO UN OvO 1 vq°CM UN 3- CO AV /?* S /9i o^I 0Z1 °vO o CO O VO o ON OvO OvOCO 1 q oCO UN OCO AV /«* o^I O O UN ON vg o UN CO oo UN vq oCM oo UN ON CO co AV /Z?S /9Z .Si CM 1 UNUN 8 UN oo UN VOCM UN 2 UN 5 oo COCO AV ,2•S /?i o*I oIZ CM 1 O UN CM oo CM OCO CO 8<* 00o O OnOn COCO •AV /9^•S /8^ 0£i O °voCM o o vO o UN UNUN CM O00CO CM UN oCM O<*? CM VO COCO •AV /Si•S ,« CM 1 UN CO oo o CM o oo CO 8 CM ON o ON00 NCOCO AV /S o^I o*£ q °cOCM 1 UN co UN o un vOCM o CO O UN co UN CM2 UN CO AV /OZ S ,oz 51 o cm 1 1 1 UN vO o vO CO oo vO 1 O 8 6o < H m •aannoNoiaanxixvi d .g fa <u H .u u o ID o 0 CM So vO °o CM °ONUN UN UN °o oo* °UN UN oVO co UN oM Sa HS O o in a Q JO KH3HXOS1 < I Z D O < n Q h Z 7. < < H -I CO h QC < K X Q h Z D < n . h CO - DO Z 3< 7) 5 UJ S 8 3 <i < to tu CD T O) h J LU C O orr D < h o 2 - GC <Z< o <oc UJQ <2. t i r- ~~i i r T i i rooooooooooooooooooooooooooo OICO«friOtOh-COO>OZ:CNCO O! < ^t IO! jJ CO DO fr 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 immediatelyadjo
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Keywords: ., bookauthorwild, bookcentury1800, bookdecade1870, booksubjectocean
