
 
		C H A P .  is  about  twenty-three  miles  to  the  northward  of the  island in Arrow-  
 Mar. 
 1827. 
 smith s  chart,  and  in  all probability  it is  the same  place. 
 With fine weather and  a fair wind we pursued our course, without  
 experiencing  any  inconvenience  except  that  occasioned  by a long swell  
 from  the  northward  which  made  the  ship  roll  heavily almost  all  the  
 passage.  On  the  :25th we  saw  the  island of Assumpti on,  and  the next  
 day passed  close  to it  in  order  to  determine its position.  The  island is  
 about a league  in  eircumference,  aud  rises  from  the  sea  in  the  perfect  
 form  of a cone  to  the  height  of 2096  feet.  Time  must have made an  
 agreeable  alteration  in  the  appearance  of this  island  since  it was  visited  
 by  La Perouse.  Instead  of a cone  covered with  lava and volcanic glass,  
 and presenting  the  forbidding  aspect he describes, we traced vegetation  
 nearly  to  the  summit,  and  observed woods  of palm-trees  skirting  its  
 base;  particularly  in  the  south-west  side.  We were  more  fortunate  
 than Perouse  in  obtaining a  view of the crater formed  at  the apex of the  
 cone ;  it  appeared  to be  very small and  perfect, and to  emit no smoke.  
 Perouse  in  sailing  to  leeward  of this  island  experienced  a  strong  sulphurous  
 odour.  There was none, however, when we visited the spot; but  
 it  is very probable  that  the  volcano  may have  been  in  action  when  he  
 passed, which might  also account  for  the desolation  of which he speaks. 
 There  appeared  to  be  no danger near  this  island,  but on  the con-  
 trary,  judging  from  the  deep  blue  colour  of the  sea,  there was  deep  
 water close  to the  rocks.  The  south-west  side  of the  island  is  the  least  
 abrupt, but even  in that direction Perouse informs us ships are obliged  to  
 come  very  close  to  the  shore before  they  can  find  anchorage,  and  then  
 only with a very  long  scope  of cable.  This bank  is formed  of lava  and  
 scorim,  and being on  the  leeward  side  of the  island  has  probably  been  
 raised by frequent eruptions of the  volcano.  There were no  projections  
 in  any  part  of  the  island  that  we  could  perceive,  sufficient  to  afford  
 protection  to  a boat  attempting  to  land,  and  the  sea  in  consequence  
 broke heavily  against  it in  every direction. 
 The day being clear we looked  to  the  southward  for  the island  of  
 Agrigan, which on  Arrowsmith’s  chart is placed within  twelve miles  of  
 the Mangs,  but  no  land  could be discerned in  that direction,  and  from  
 the  state  of the weather,  I  should  tliink  there could not have been any  
 within  twelve  leagues  distance  of us  at  the  least.  This would  make 
 llfi  if : 
 llltî I  ^  ’ 
 the channel between Assumption and Agrigan  about  forty miles wide :  C H A P .  
 the jesuits  extend  it  to  sixty ;  but  this  cannot be  the  case,  as  it would  ,  
 place Agrigan  near  the  latitude  of 18”  45' N . in which  parallel A bar-  
 April, 
 1827. 
 gottia, according  to Espinosa, has placed  the  island of Pagon.  It seems  
 necessary  therefore  to  contract  the  channel  between Assumption  and  
 Agrigan  as marked  in the jesuitS’ plan, and  to reduce the size of Agrigan  
 in  order  to  reconcile  the position  of the  islands,  Arrowsmith  has  incorrectly  
 placed  the Mangs  on  the  south  side  of Assumption ;  by  our  
 astronomical bearings  they are  situated N .  27“ 7'  30" W. (true) from the  
 south-east  end of that island,  and  are in  latitude  19"  57'  02" N .  They  
 consist of three high rocks,  lying  in  a south-easterly direction*. 
 From  what  I  saw  of the  island  of Assumption  it  appears  to  be  a  
 very  proper headland  for  ships  coming from  the  eastward  and bound to  
 Canton  to  steer  for.  It  is  high,  and  may  be  safely  approached  in  the  
 night if the weather  is  clear ;  and  there  is  a wide  channel to the  southward  
 ofit.  It  is  far preferable  to  adopt  this channel than to pass to the  
 northward of the Mariana group, which  is  sometimes done;  as  I am  credibly  
 informed  that  there  is  much  broken  ground  in  that  direction. 
 We have  as  yet  no  good  chart  of this  group  of islands.  The geographical  
 position  of Assumption  and  of  the Mangs will be  found  in  the  
 table  at  the  end  of this work. 
 Under  the  lee  of the  island we  observed a great many  birds,  principally  
 of the  pelican  tribe,  of which  there  was  a  species  supposed  by  
 our  naturalists  to  be  new.  It  is described  as being  smaller  than  the  
 frigate-bird,  and  of a  dark brown  colour, with  the exception  of the belly  
 aud breast, which were white, and  the  bill, which was  either white  or of  
 a light lead  colour. 
 •   I t  is somcwliat  remarkable tliat  in passing to  th e southward of the island  of Assumption,  
 a t th e  distance  of four miles  and  a  half, we  did  not discover the rocks which Captain F rey c in e t  
 has  supposed  to  be  the Mangs,  situated  in  latitude  19" 32' N.  O u r  latitude  when  in  the  
 meridian of Assumption was  19“ 36' N.  by  wliich  it is  evident th a t we must  have passed w ithin  
 four miles  of these  rocks, provided both  latitudes  be  correct.  H a d   I knmvn  ot tlieir existence  
 a t  the  time,  I   should  certainly  have  stood  to  the  southward,  in  order  to  connect  them  by  
 triangulation with  the Assumption  and  the  M an g s ;  b u t  Captain  F rey c in e t’s  discoveries were  
 not  then published.