. Thalassa; an essay on the depth, temperature, and currents of the ocean. as to Halifax (Plate 7, Table II.).—This section extends in a direction nearly due north along o vo q CO 1 1 1 8 co 1 CO 0 CO 0 vo CO H-1VO AV^i °^9 q vo 1 0 OVO O CO ro 00 10 0 * 0 CO 0 CO CO 10 AV/^ °e9 •N ^ o6£ 1 0 O vo OOVO 8 VO 10 0 * 8 COCO COvo M P* °f 9 N P$ o9^ *0 0 co CO 4 OCOro Ovo OVOvo Ovovo CO0 0 vo VO CO vo M />S 0^9 CO 0 CO OVOro 1 1 1 1 0 vo VOCO vovo M /£ o>9 N P2 o^^ 0CO 0 CO 5 ro O VO 00 VO 1 1 00 vo CO 10 iJO CO0 *COCO 0 Ororo vovo 8 vo 8 CO 1 vovo CO N /» <A CO co CO VO vo 00 CO OCO vo CO
. Thalassa; an essay on the depth, temperature, and currents of the ocean. as to Halifax (Plate 7, Table II.).—This section extends in a direction nearly due north along o vo q CO 1 1 1 8 co 1 CO 0 CO 0 vo CO H-1VO AV^i °^9 q vo 1 0 OVO O CO ro 00 10 0 * 0 CO 0 CO CO 10 AV/^ °e9 •N ^ o6£ 1 0 O vo OOVO 8 VO 10 0 * 8 COCO COvo M P* °f 9 N P$ o9^ *0 0 co CO 4 OCOro Ovo OVOvo Ovovo CO0 0 vo VO CO vo M />S 0^9 CO 0 CO OVOro 1 1 1 1 0 vo VOCO vovo M /£ o>9 N P2 o^^ 0CO 0 CO 5 ro O VO 00 VO 1 1 00 vo CO 10 iJO CO0 *COCO 0 Ororo vovo 8 vo 8 CO 1 vovo CO N /» <A CO co CO VO vo 00 CO OCO vo CO VO 0 vo vq OO CO 00CO M/^ o^9 0 ro CO 0 CO VO COCO vo CO <<* 0 VO VO O vo vo 0 *1—1 0 vo COCO CO MPi o^9 N P17 oZZ co# 0 * <* CO 1 0 VO CO 0 ro Oro VO O 2 VO 0 VO c\ CO vo CO M / 0S9N ,1* 061 <* 0 co 0 0 CO Ovo ro O 5 00 10 1 vo COro O ft 0 H «!HCO •aanxiONOT onvaanxixvT a * V - K .0 0 c In m 0^ CO ^ vo 0 ONvo 0Ovo 0 5- IO °vOro a H a0 O PQ a c Oh1 CO 0 vo 0O 0 VO 10 0 .CO jIO JMX3HX0SI CO £ 2 < D I cc < Ul 2. From St. Thomas to Halifax. 65 the meridian of long. 650 W., from St. Thomas, in the WestIndies, to Halifax in Nova Scotia, the group of the Bermudasdividing the section into two nearly equal halves (Plate 2). Anexamination of the isotherm of 20° C, as well as of the surface-temperatures, shows that, between Station 27 and Station 28,we cross the northern limit of that portion of the North AtlanticEquatorial Current which flows outside the West Indian in depth, the warm surface-stratum continues towardsthe Bermudas, beyond which group it suffers further reductionby coming in contact with the Labrador current. At thestation of the 24th May, we once more fall in with theequatorial current, namely, that portion of it which, afterentering the Caribbean Sea and after making the circuit ofthe Gulf of Mexico, issues out of the latter through the Straitof Florida and flows along the coast under the name ofthe Gulf Stream. A
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Keywords: ., bookauthorwild, bookcentury1800, bookdecade1870, booksubjectocean
