
 
        
         
		as  the great basin was composed of,  but of so  
 delicate a nature that it was scarcely possible,  
 even  with  the  utmost  care,  to  bring  any  of  
 them away perfect.  I remarked, in particular,  
 a Jungermannia (asplenioides)  so beautifully  
 coated  with  this  incrustation,  that  it looked  
 as  if it were  a  model  of the  plant  in  plaster  
 of  Paris.  One  specimen  was  so  protected  
 under  the  shelter of  larger  plants  incrusted  
 together, that I was able to convey it in safety  
 to Reikevig.  The  plants  I met with  by  the  
 side  of  the  river,  which  I  had not  remarked  
 before, were Car ex Reliardi and a new species  
 of the same  genus,  with  Koenigia  islándica  
 in  great  profusion,  and  Funaria  hygrome-  
 trica.  Leaving  the  river, I  walked over several  
 vast mounds of red earth, at the north end  
 of the  Geyser, in  my way  to  the  top  of the  
 mountain.  Here and  there a  boiling-spring  
 was  forcing  its  turbid  and  discolored waters  
 through  holes  in  the  surface.  Some  were  
 completely  in  the  thiek  muddy  state  of  a  
 puddle,  and were  bubbling,  as any glutinous  
 substance  would  do  over  a  fire.  In  many  
 places  was  heard a rumbling  noise  like  the  
 subterraneous  boiling  of  water,  although  
 there  was  no  orifice  near,  by  which  the 
 fluid  could  make  its  escape.  On  these  
 spots,  which  were  so  much  heated  by  the  
 boiling  streams beneath  that I could scarcely  
 bear  my hands  upon  the  ground,  I  found  
 a  great  profusion  of Riccia glauca *,  growing  
 in  patches,  and  extending almost  uninterruptedly  
 over  a  space  of  ten  or  twelve  
 feet  in  diameter.  The  soil  for  more  than  
 half  way  up  the  mountain was  composed of  
 a  coarse  reddish  kind  of  earth,  intermixed  
 with  some  other  of  a  dirty  yellow  color,  
 with small  intervals  of  hard  rock,  and with  
 this  terminated  the  highest  of  the  hot-  
 springs,  which,  however,  was  but  a  feeble  
 one.  Thence  to  the  summit  the  mountain  
 was  entirely  formed  of  a  loosely-laminated  
 rock,  whose  strata  seemed  to  lie  in  
 almost every direction,  but chiefly vertically.  
 There was no appearance whatever of any part  
 of  the hill  having  been  in  a  state of  fusion.  
 Many  of  the  strata  were  still  in  their  ori- 
 *  I  think,  but  dare  not  trust  too  implicitly  to  my  
 memory,  that  I  saw abundance  of  it  in  fructification.  
 I made  no memorandum  on  this  subject,  and the specimens  
 which were  intended to  enable me to  answer  this,  
 as well  as  other  questions  relative  to  natural  history,  
 were all, unhappily,  lost.