Thalassa; an essay on the depth, temperature, and currents of the ocean . 8^1 ^ 1 0 0 0 0 t^ 1 ° vo VO M •S .SS ,62 C) u-l u-j On ?3 .2^ 06^1 vq u^ ^ CM 0 O V 1 00 0 0 ;s >^ 0^^ M VO ^ t^ oo •3 .^^ o^^I S .83 oO^ qV 1 •1 1 IT) 0 VO 8 0 0 0CM 8 VO ?3 P^ 0691 r^ 0 >- VD V 1 t^ I 1 1 r^ S .oS ,8^ M CM U •3 .6e ,991 •S .9^ o8f vq V 1 1 1 0 VO 0 0 00 q °CM 8 W ?3 .81 0^91 CO 0 0 0 ON >-n 0 1 2. rn VO 0 VO •s .f s ,ze LO 1 1 ^ M >-n ON 0 On •3 .6^ 08Si 0 0 1 1 0 0 0 R VO 8 O •S A^ o9^ t^ 1 1 VO 04 u-i ON 0 VO CM P3 •3/S .-t^Si 00 0 0 0 0 -^ ° 1 1 0 vo CO u-i 1 VO •s A 0^^ t^ 1 1 VO ^ 00
Thalassa; an essay on the depth, temperature, and currents of the ocean . 8^1 ^ 1 0 0 0 0 t^ 1 ° vo VO M •S .SS ,62 C) u-l u-j On ?3 .2^ 06^1 vq u^ ^ CM 0 O V 1 00 0 0 ;s >^ 0^^ M VO ^ t^ oo •3 .^^ o^^I S .83 oO^ qV 1 •1 1 IT) 0 VO 8 0 0 0CM 8 VO ?3 P^ 0691 r^ 0 >- VD V 1 t^ I 1 1 r^ S .oS ,8^ M CM U •3 .6e ,991 •S .9^ o8f vq V 1 1 1 0 VO 0 0 00 q °CM 8 W ?3 .81 0^91 CO 0 0 0 ON >-n 0 1 2. rn VO 0 VO •s .f s ,ze LO 1 1 ^ M >-n ON 0 On •3 .6^ 08Si 0 0 1 1 0 0 0 R VO 8 O •S A^ o9^ t^ 1 1 VO 04 u-i ON 0 VO CM P3 •3/S .-t^Si 00 0 0 0 0 -^ ° 1 1 0 vo CO u-i 1 VO •s A 0^^ t^ 1 1 VO ^ 00 1 CM 0 0 •S .95 o9f N 1 ^ I- ^ 0 CMCM d 12^ so On0 ^ 0 ^ VO s aanxiONOT !U 0 fc ^ H 0 0 i-r> °o 0 ~1 H c O QNV 0 cj c. • M M CM a jz H tS 0 -t-i O <a. XH Om COUJQC <HI a. tu I- o u. o <a. IH OCO COUJ QC < HICL tu OUJ o < QCUl < UJN UJ z OO o. to <M £i V _ n I I I r oooooooooooooooooooooooooo tlOCOI^OOOiOlICNCO-^t 00 O—!2 o cQoa ^ From Cook Strait to Tonga Tabu. 99 Ocean by a submarine plateau which rises to within 1000 fathomsof the sea surface, and unites Australia, New Zealand, NewCaledonia, and Papua into a single area of elevation, it may beconsidered as forming a bight of the Southern Ocean (Plate 2).The cross section of this area presents the not unfrequent con-trast of deep soundings and a comparatively rapid fall of the sea-bottom along its western boundary, and of shallow soundingsand a slowly rising bottom towards the east. The western halfof the basin is occupied by an area of depression of more than2500 fathoms, or about three miles in depth, extending from thesouth point of Tasmania along the east coast of Australia as faras Great Sandy Island, where the coast turns towards the north-east. The eastern half forms a broad plateau, which ultimatelyrises above the level of the sea under the n
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Keywords: ., bookcentury1800, bookdecade1870, bookidthalassa, booksubjectocean
