Page:Encyclopædia Britannica, Ninth Edition, v. 21.djvu/209

Rh . The at the  of StPaul in  was— landed, 45,800;  shipped, 13,300; passengers carried, 34,625. Two lines of ply between StPaul and  and intermediate points. The average of  lasts six and a half. The has within its  limits, but removed some  from the  proper, two —Macalester  and Hamline —both only partially  or supplied with. There are twenty-two , built at an aggregate cost of 663,000. There are also several and  under private or al management. The  system of StPaul is as yet undeveloped, but an  of 250  has been secured near  Como to be laid out as pleasure-grounds. Rice and Smith  are public squares in the central portion of the, tastefully adorned with  and. The of StPaul, according to the , was 840 in , 10,600 in , 20,300 in , and 41,473 in  ( 22,483,  18,990). According to the, it was 111,334 in.

1em 1em  ST PAUL, a remarkable which, along with the  of, is situated in the  about midway between  and, a little to the north of the ordinary route of the  from  (via ) to. Its exact position as determined by the in  is 38°42′ 50″S. and 77°32′ 29″E. Though the distance between the two StPaul and  is only 50, they belong to two separate  areas characterized by quite different products; and the comparative bareness of StPaul is in striking contrast to the dense  of. StPaul is 1 long from north-west to south-east and its -line is estimated at 5. In shape it is almost an with a  inscribed ially to the north-east side,—the  (3940  in diameter) being the   which previous to  formed an inland, but which, since the  broke down its eastern barrier, has become practically a land-locked  entered by a narrow but gradually widening passage not quite 6  deep. The highest of the  is not more than 820  above the. On the south-west side the s are inaccessible. According to M.Vélain, the originally rose above the  as a mass of rhyolithic trachyte similar to that which still forms the Nine Pin  to the north of the entrance to the. Next followed a period of activity in which basic s were produced by —s and  of anorthitic character, palagonitic, and ic ; and finally from the , which must have been a vast  of  like those in the , poured forth quiet streams of ic s. The  has been rapidly cooling down in historic times. DrGillian (’s visit, ) mentions spots still too warm to walk on where no trace of is now perceptible; and the remarkable zone of   extending westwards from the  has lost most of the more striking characteristics recorded by Hochstetter in, though it is still easily distinguished by its warmth-loving ,— and.

1em 1em

1em  STPAUL DE LOANDA. See.  ST PAUL’S ROCKS, not to be confounded with the of  in the, are a number of small  in the , nearly 1°north of the  and 