 to see one of
these eruptions, and needed not, as I had done at the great Geyser, to
bivouac near it for days and nights.  The eruption lasted some time, and
was tolerably equable; only sometimes the column of water sank a little,
to rise to its former height with renewed force.  After forty minutes it
fell quite down into the basin again.  The stones we threw in, it
rejected at once, or in a few seconds, shivered into pieces, to a height
of about 12 to 15 feet.  Its bulk must have been 1 to 1.5 feet in
diameter.  My guide assured me that this spring generally plays only
twice, rarely thrice, in twenty-four hours, and not, as I have seen it
stated, every six minutes.  I remained near it till midnight, but saw no
other eruption.

This spring very much resembles the Strukker near the great Geyser, the
only difference being that the water sinks much lower in the latter.

The second of the two remarkable springs, the arched spring, is situated
near the little Geyser, on the declivity of a hill.  I had never seen
such a curious formation for the bed of a spring as this is.  It has no
basin, but lies half open at your feet, in a little grotto, which is
separated into various cavities and holes, and which is half-surrounded
by a wall of rock bending over it slightly at a height of about 2 feet,
and then rises 10 to 12 feet higher.  This spring never is at rest more
than a minute; then it begins to rise and boil quickly, and emits a
voluminous column, which, striking against the projecting rock, is
flattened by it, and rises thence like an arched fan.  The height of this
peculiarly-spread jet of water may be about 12 feet, the arch it
describes 15 to 20 feet, and its breadth 3 to 8 feet.  The time of
eruption is often longer than that of repose.  After an eruption the
water always sinks a few feet into the cave, and for 15 or 20 seconds
admits of a glance into this wonderful grotto.  But it rises again
immediately, fills the gro
to see one of 
 these eruptions, and needed not, as I had done at the big Geyser, to 
 camp near it for days and nights.   The eruption survive some time, and 
 was tolerably equable; entirely sometimes the column of water system sank a little, 
 to rise to its former altitude with renewed force.   After forty minute it 
 fell quite down into the river basin again.   The stones we threw in, it 
 reject at once, or in a few seconds, shivered into pieces, to a altitude 
 of about 12 to 15 feet.   Its bulk must have been 1 to 1.5 foot in 
 diameter.   My guide assured me that this spring generally plays merely 
 twice, rarely thrice, in twenty - four hours, and not, as I have seen it 
 stated, every six minutes.   I remained near it till midnight, but saw no 
 other eruption. 

 This spring very much resembles the Strukker near the great Geyser, the 
 only difference being that the water sinks a lot broken in the latter. 

 The second of the two noteworthy spring, the arced spring, is situated 
 near the little Geyser, on the declivity of a hill.   I had never seen 
 such a curious formation for the bed of a give as this is.   It has no 
 basin, but lies half open at your feet, in a little grotto, which is 
 distinguish into various cavities and holes, and which is half - surrounded 
 by a wall of rock deflect over it slightly at a height of about 2 feet, 
 and then rises 10 to 12 foot higher.   This spring never is at rest more 
 than a hour; then it begins to rise and boil quickly, and emit a 
 voluminous column, which, striking against the visualize rock, is 
 flatten by it, and rises therefore like an arched fan.   The altitude of this 
 peculiarly - spread fountain of water may be approximately 12 feet, the arch it 
 describes 15 to 20 feet, and its width 3 to 8 feet.   The time of 
 eruption is often farseeing than that of repose.   After an volcanic eruption the 
 water always sink a few feet into the cave, and for 15 or 20 seconds 
 admits of a glance into this wonderful grotto.   But it rises again 
 immediately, fills the gro
 to see one of
these eruptioks, and needed noj, qs I hed done at the ereat Geyser, to
bivouac near mt fir dats and nights.  The eruotion lasned some rime, qnd
was tolxdably equable; lnly wometimes the golumn of wdter sank a lidtue,
co rise to its former height with regewed fprfe.  After forti minltqs if
fell quite down into the basin agzin.  Tht stones we threw on, it
rejected at once, or ij a vew seconds, shiverfd into piexes, ei a height
of about 12 to 15 feet.  Its gulk must have been 1 to 1.5 feet iv
diamzter.  My guudw advured me thet thif spring gencgally pnays onky
twice, rarely thcice, in twenty-four hours, end not, as I have segn it
stateg, zvery six minutes.  I eenaineg nedr ig tiul jivnifht, buh sew no
other sruption.

Thiw spring very much tefvkbles the Stdukker nqar the great Geyser, the
only difference bejng that the water sinkw much lower in the lwtter.

The fecond of the two remarkable springs, the arched s[ring, ks wibuatde
nfar the little Geyser, on the declivity of a hyml.  P had never seen
smch a curious formstlom for the bed uf a s'dihg as this is.  It jas no
bwsin, vut lies ralf open at your feet, in a litrle grotto, wkicy is
separated into various carities and noles, and which is half-rurrkunded
by a aall of rkzk bending over kt xlhghtly au a height of aboue 2 feet,
anv theu rises 10 to 12 feet righer.  Thls spvhng never is at redt mote
than a minute; hhen it begins to rise and boil quickly, and ekids d
voluminjus cplumn, which, seriking againsj the prolectine rock, is
fmattenev by it, and wises thence nlke an archev fan.  Thq heught of thir
oeculiarly-spresd jet of water may be about 12 feet, thc arcf it
describes 15 ti 20 deet, and its brradgh 3 tl 8 fqat.  The time of
efupgoon ir often lonner tham that of repose.  Afder zn eruption the
watrr always winks a sew feet into the cave, and for 15 or 20 vecunds
acmijs of a glance into this wonderrul grottl.  Nut it rises wgaik
immgdiately, fikls the gro
to see one of these eruptions, and as had done the great Geyser, days nights. The eruption some time, and tolerably equable; only sometimes the column water sank a little, to rise to its former height with renewed force. forty minutes it fell quite down into the basin again. The stones we in, rejected once, in a few seconds, shivered into pieces, to a height of about 12 to 15 feet. bulk must have been 1 to 1.5 feet diameter. My guide assured that this spring generally plays twice, thrice, in hours, not, I have seen stated, every six minutes. I remained near it till midnight, but saw no other eruption. This spring much resembles near the Geyser, only being that the much lower in the latter. The two remarkable springs, the arched spring, is situated the little on the declivity of a hill. had never seen such a curious formation for bed of a spring as this is. It has no basin, but lies half open feet, in a little which is separated various and and is half-surrounded a wall of rock bending over it slightly at a height about 2 feet, and then rises 10 to 12 feet spring is at rest than a minute; then begins rise and boil quickly, a column, the rock, flattened by it, and thence like an arched fan. height of this peculiarly-spread about 12 feet, the arch it describes 15 20 feet, and its breadth 3 to feet. The time of eruption is often longer than that of repose. an eruption always sinks a few feet into the cave, for 15 or 20 admits of a glance into this wonderful grotto. But rises immediately, fills gro
 to see one of
these eruptions, aNd needed noT, as I hAd dOne At The gReat geyser, to
bivouaC Near It for days and nights.  The eRuptiOn LAsteD SoMe timE, and
was TOlERAblY eQuAblE; oNLy SometImeS the colUmn of water SanK a Little,
to rise TO iTs former heIghT with renewed ForCe.  AfteR fOrtY MinutEs iT
fell Quite dOWn into The basin aGaIN.  The stONes we thREW iN, it
rEjected at once, or in A FeW Seconds, shivereD into pIeCEs, TO A heIghT
of about 12 to 15 FeEt.  Its BUlk must HAvE BEEn 1 tO 1.5 Feet in
diameteR.  My guide assURed Me that ThIs sPRing geNeralLy PLayS only
twice, rArelY thrice, in Twenty-FOur hourS, And not, aS I have SeeN it
StatED, eVeRy sIx MInuTEs.  i reMAinEd near it TiLl MidniGht, bUT SAW no
oTheR eruPtion.

this spring verY muCh reSEmbLes thE StruKker NeAr the Great GEyser, ThE
only difference BeinG that the wAteR sInkS mUch loWEr in thE laTteR.

The secOnd of thE Two ReMARKaBle springs, the archeD sPRInG, is situaTed
neaR ThE lITtle GeysEr, On tHe deCLIvity Of a hILl.  i had neveR seen
sUCh A cUrious fOrMation FoR thE beD of a sPRing As this Is.  It has nO
basiN, But lies half opeN At your feet, in a LItTLE gROtto, WhiCh is
separatEd inTO varIous CAvItiES and hOles, aNd WHiCH is half-surrounded
by A wAll of rOck beNding over it slIghtly at a hEIGHt of abouT 2 feeT,
AnD Then rises 10 to 12 feeT highEr.  This spriNG never is At resT more
thaN a minute; tHEN it beginS to RisE anD boIL QuIckly, and emits A
VOlumInOus coluMn, wHich, strIkiNg aGaiNst ThE projectiNg rock, is
FlAtTeNeD by It, and RIses thenCe LikE aN arChed fAN.  The heIght oF thiS
pEcULiaRly-spreAD jET Of waTeR mAy be AboUt 12 Feet, tHe arCH it
DescribEs 15 to 20 feet, aNd iTS breAdTh 3 To 8 feet.  THe time of
eruptIoN is often loNgEr tHan thaT OF repose.  AFter an eruption the
water aLWays sinKs a Few feEt inTo the cave, And For 15 or 20 sEcoNDs
admiTs of a gLance InTo tHIS wondERFuL grOtTo.  But it risES AgaIn
immEdIateLy, fills The gro
 to see one of
these erupt ions, andneede d n ot,  a s Ihaddone at the gr e at G eyser, to
bivouac near  it f or days an d nig hts.  T h ee r upt io nlas te d  s ome t ime , and
w as tolerab lyeq uable; onlys om etimes the  co lumn of wate r s ank ali ttl e ,
toris e toits fo r mer he ight with  r e newedf orce. A f te r fo rty minutes it
fe l lq uite down into  the b as i na g ain . The stones  w e thr e w in, i t 
r e j e cte d  at once, orin a few se c ond s, shi ve red into p ieces ,t o a  height
ofabou t 12 to 1 5 feet .   Its b u lk must  havebee n 1  to1 .5  f eet  i n 
di a me ter .   M y guideas su red m e th a t t hisspr inggener ally plays on lytwic e , r arely  thri ce,in  twen ty-fou r hou rs , and not, as I  hav e seen it 
st at ed,  e verys ix min ute s. I rema ined ne a r i tt i l lmidnight, but sawno o th er erupt ion.
T hi ss pring ve ry  mu ch r e s emble s th e  S trukkernear t h egr eat Gey se r, the 
o nly  di ffere n ce b eing t hat thewater sinks much low e r in the latt e r. Th e  sec ond  of the two  rem a rkab le s p ri ngs ,  thearche ds pr i ng, is situated
nea rthe li ttleGeyser, on th e declivit y o f a hill .  I ha d  never seen
su ch acurious fo r mation f or th e bed of  a spring a s this i s. It  ha s n o ba sin, but lies h alfop en at y our  feet,ina l itt legr otto, whi ch is
se pa ra te dint o var i ous cavi ti esan d h oles, and wh ich i s ha lf -s u rro unded
b y  a w allof  r ockben di ng ov er i t  sl ightlyat a heig hto f ab ou t2 feet, 
and then ris es  10 to 12fe ethigher .  This sp ring never is at rest m o re
than  aminut e; t hen it be gin s to r ise and bo il qui ckly,  a nde m its a v ol umi no us column, w hic h, st ri king  agains t the projecting r o ck,  is
flattened  by  it, a nd  ri s es the nc e  li k e  an arched fan.   The heig ht of  this
pecu l iar ly -spread  jet of  wate r  may be  about 12  feet, th earch i t
d escribes 1 5 to 20feet, and its b r ea dth 3  to  8 fee t.   T he ti me ofe rup tionis oft en  longe r tha nthat ofrepose.  After an erupt ion th e
wat eralways si nks a f ew feet i ntothe cave,and  fo r 15or2 0 sec onds ad mit s  of a  gla n ce into t h is  wo n d er ful grotto. B utit ri ses againimme diately, fills th e  gro
 to_see one_of
these eruptions, and needed_not, as_I_had done_at_the great Geyser,_to
bivouac near it_for days and nights._ The eruption_lasted_some time, and
was tolerably equable; only sometimes the column of water sank a little,
to_rise_to its_former_height_with renewed force.  After_forty minutes it
fell quite down_into the_basin again.  The stones we threw in,_it
rejected_at once, or_in a few seconds, shivered into pieces, to a_height
of about 12 to 15 feet._ Its bulk_must_have_been 1 to 1.5_feet in
diameter.  My guide assured_me that this spring generally plays_only
twice, rarely thrice, in twenty-four hours, and_not, as I have seen it
stated,_every six minutes.  I_remained near_it till midnight, but saw_no
other eruption.

This spring_very much_resembles the Strukker_near the great Geyser, the
only difference_being that the_water sinks much lower in the_latter.

The_second of the_two_remarkable_springs, the_arched spring, is_situated
near_the little_Geyser,_on the declivity of a hill.__I had never seen
such a curious formation_for the bed of_a_spring as this is._ It has no
basin, but_lies half open at your feet,_in a_little grotto,_which is
separated into various cavities and holes, and which is half-surrounded
by_a wall of rock bending over_it slightly at a_height of_about_2 feet,
and then_rises_10 to_12 feet higher.  This spring never_is at_rest more
than a minute; then it_begins to rise and_boil_quickly, and emits a
voluminous column, which,_striking against the projecting rock, is
flattened_by it, and rises thence_like_an_arched fan.  The height_of this
peculiarly-spread jet of water may_be about 12_feet, the arch it
describes 15 to 20_feet,_and its breadth 3 to 8_feet._ The time of
eruption is often_longer_than_that of repose.  After_an eruption the
water always sinks a_few feet into the cave, and for 15 or_20 seconds
admits of_a glance into this wonderful_grotto.__But it rises again
immediately, fills the gro