| OCR Text |
Show 12 avera.ge. width of one and on$""halt mUeAf;.i; The i»tal. @.ea eowd is pptmatly walw and ems-hut squ_e e$t,f lear the margiN. r the ,flow the a,.vr·a.ge tbickne$s of lava is thirt:t fa t, the m depth ' of the' entire lio1(1 being fifty feet.l The .now apparently tQok place after the di.sappear@oe of ;'Lake l3tullls,1.11s . traces ot wav flo-tiQn oa· the Pa:tt'ant a'U:t,, as the a-re ae lake sediments ·la,w.,.' loeall,. eened $llIar Loaf r.[eunte.il'l4 is tQS mil. north of the Ice Spring group and is 'e, eOllspieuou.s lan&nark Uhion be seen as $DOll ·as the valley 1$ Gntsr€d from til' northeast. can $ Pavant But_ ie tb$' bigh$ri ('QUe ill the "auq ,and de. SaQ tet I.b&V0 th& Aoout b W' up th'$ side of 'be oon$ tb$ sbarEll oina pln tormed by lAke BeVine durin.1! the &Meville level of th lak$ is -vi$'lble (figwre 4) and at the bti,ae Qf the oane appea:-s in. Provo lEtvctl 6 'hbrelib, _ hdio.tian that thii C011$ ttQ .toftled· bet$1"'e th$ lava flow and al,o 'bet$'e or durt;g tn. $aGiien.e t $ .mev1llei, 1he fabe:rne.ole crater and thli dja,e_t ;$mall law field is directl,- south ot the tce 'r;ring ¢'ltatera eJld thoh it adjoinS the l$ S1>ing flow, it i$ sepate and difltinctl' from it. 'il16 tllQwii.ng destri,tl 0f thU ."$.te)l1, Gi1'b$t mSf$fJ ·ntt$ potil1i as $t;.tEtll t.J'On1 the rtex- eteit' $sembbzft th¢ }HJ.)rnltln fabem¢le at iSfU't LIke Cit11 llP;1fl. p_ ;U2 t .. 21y.. S2. ?i:t. .. 1'- 328. 30ilber-t" 2£- ,(,1. t. 1" .33. b '. to i eer, .2l!..' , p. 49. . SGilbt)·-t, l£' cit .•• ,p* , 32$. |
