174 J.D. Dana on Changes of Level in the Pacific Ocean. 
Paumotu Archipelago,........ Honden,......... 1} or2 
“ “ Clermont Tonnere, 
“ “ Nairsa or Deans’s, 6 
he ie Elizabeth, bo a 4 on 
ze i Metis Ot AUrorn, . ouse coc ks cen oem 250 
Ba ” Ducie’s, - lor? 
Tahitian Group, ............. Tahiti, veil 
- « Bolabola, 4 
Setvey and Hurnty Groune,. ...  Ativ, 50+ + aveesvayeoes o> ot oh) ieee 
7 * “ uP MAURO, SOS eears foeeeas ee eet ste nv deat 
ze ” ¥ “ Mitiaro, - 
© ba = . Mangnia, s\¢ cas veges owes én me dies ope eae 
ad i =e - Rurutu, 150 
~ - x - Remaining Islands, geeeeeee ot 
North of the Tabitian,........ Wanting Island, 1 eS 
' “asia in ( hris' tmas, ee ee ee ee ee Oe doh tne J Sie 
“ “« « « alden, ead ‘7 Pr 
“ ee “ P ti = > Reese Goo Nee CSR TE or 
Tongan Groupy.'is i) oss <5 — vevev es 8008 
“« ry, wid 
i" “ Samu a the Bape: acnn eee 
Savage Island, . rt Aenea . 100 
Samoan Islands, Ear reser ee: 
North of Samoa,............ it ROI Ms es sn n't pdcn tena 3 to 6 
si " yas. OF Bowditch, ......eseceonseser® 8 
aagpa ee - Duke of York’s,.....+-++ weed oe 
Ate Ms renee aaa Hall 8 idney, Newmarket-.-+-5 0! 
Weejed’ Talatida.......5... 0". Viti Leva and fbn neck Ovalau, ...-5 Ae 
Bastern Islands; 22 ofa eet Gees ine 
North of Feejees,............ HB Torne, Wallis “Eilk D OM 
Sandwich Islands, viens roe fe Ce ee «cried 
aba, ....svscc asec tee teense 25 or 30 
a * Molokai, seeete 
wags! Maui, eecwl 
Tarawan DT eee ae : ADULOONES, . + i+s sake mene eae eseee 1 or 2 
. i Nanouki, Katia, Maiana and ‘Tarawa,.. 2 ot fae 
fi * Apamama). 5.4 Pi LAS ; 
* Maral or Chara, ee ‘erase ws te ee* 6 or 
“ “ arald eee 8 or 3 
« cilia laasted sachets TP A see ie A Me ge I al 0. 
Carolines, .... . n0} 
Ladrones, : Guam, doves 600 
Rota. Pe en ce itil 
on ete PO Gete es lies ccowmaCr ee ge ee 
ieic Le ee 
New Hebrides New Caledonia, Salomon iaianity. tenet st none ei 
Several deductions are at once obvious: ey 
1, That the el elevations have taken place in atl parts of ihe oc 
= he they have in some instances affected single islands, 
and no 
ae dj t islands 
nt is often very tingatiat in a Neale 
A. That in ete! instances the change has been experie? ced 
by a whole group or chain of islands, The Tarawan Group 
ee instance, and the rise appears to increase from a Fe abe 
most island to Apia, and then to diminish Wer “al 
tremity. 
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