Image provided by: University of Oregon Libraries; Eugene, OR
About The Bend bulletin. (Bend, Or.) 1903-1931 | View Entire Issue (Aug. 19, 1920)
BBNW HUMMCTIN, 1IKNI), OREGON THUflflDAV, AUGUHT JO, 1020. TAm 7 i ft CROSBY REPORT TELLS HISTORY OF EARLY AGES (Contlmioil from pngo 0.) rlvnr channel mitl (liu ronorvolr (iron. It In iluln, thoroforo, (lint, In vlow of tlio prolinbln loiikngii of Hut tiiiuuil roof, unil IIm jmnHlliln lorul collnpno, u lionvy ronpotiHlblllty roiilii upon tlilu cnrpot of nllt. A I ho In vlow of tlio fact Unit tho discovery of tlio tiinnol lit duo to u liuiro iiccldoiil, it cliitnco fall of tlio roof. It lit it natural thought Unit thorn may tin olhcirn, for hoyoud tlio llmltM of tlio collupiiod portion wo look In vain for any mirfaco Indica tion of tlm tunnel. AtinoHt our only nluo In nffordod by tlio thought that tlio tunnolH tnnd to follow tlio do lironnloiw or valloyH of tlio original or pro-lava nurfnco; and hero wo oiicoiinlur tlio dllllculty Unit tlio pro Ittvu depressions aro llltuly to bo Afncoil by tlio flow, In fact tlilu np ponrn to bo tlio ciiho with tlio tun nel uudor dlnciiNiiloii. It Ih not now connplGiioiinly inarkod by a mir faco dopronnhui. It docn appear ri'iMonahlo, howovor, that tlio lava timnnlN will not bo cloudy npnrcd, In other wnrdn, that tlio occurrence of a tunnel Iminuulzon a connldor nblo bnmdlli of lava on either Hldo. Bouillon tlio unnatnml tiinnol al ready doncrlbnd, I liavo kunwlmlgn, derived from tlio Donchuten National Forcnl map, of only two tiinnnlH on tlio eastern nlopo of tlio Donchuten vnlloy. Thoito aro ' tlio Arnold lco Cnvo, a iloxoii in I Ion notiltxinHt of Bend nod troiidlm: In that direc tion, and Mnrno Cuvn, about thrco mlloN onnt of Bond, but sharing, nluo tlio norlhwontnrly trend. Horso Cavo In Irregularly branching; and thitro aro liidlcatlnnit that tlio Arnold lco Cavo may also bo branched. Hut whether tlio branches aro trlbti tarloH or dlntrlbiitnrlon (converging or diverging) In not very clear. Tho Arnold lco Cavo also belongs, nil tho iinmo Implies, to tho claim in which tho drlftml nnow of wlntnr exceeds tho summer molting. Hucli examples might bo called natural lco hoimoH. Although wo con not nuppoHo that tho lco oxtmidn far from tho opening It mny account lato to nuch on oxtunt an to mako oxploratlou dimcult or Impossible. Tho Edison lco Cavo. nomo 17 miles In a direct lino nniithwosl of llond, and eight in IIm went of tho rciicr voir, In a ciiho In point. It In at nit olovotlon of about fl.000 foot. Tho wwtorn or cnscnr.o slope of tho DvhcIiuIoh valloy appears, by virtue of Hn rotatlvoly stoop nlopo, to bo especially favorablo to lava ! Central Oregon Garage REDMOND, OREGON Exclusive Agents for Northwest Auto Co. for Deschutes, Crook nnd Jefferson Counties Selling Marmon-Cole, Reo and Dort Cars Bethlehem, Indiana and Duplex Trucks Business and Professional Cards R. S. HAMILTON ATTORNBY-AT-LAW Rooms 13-10 First National Dank Uldg. Tol. Gil (Dr. Co Yotmn Offlc.) II. It. DeAfmon.1 Cha. W. EVln. DeArmond & Erskinc j, a w v k ii h O'Knno IlulldlnK, Dond, Orogon H. 0. M h L I 8 Attornoynt-Iiw Cnltcd Stutos Oommlnnlonor Flrnt Natlounl Ilnuk Uiilldlni MUNI). oiucnoN DR. A. LESSING PHYSICIAN AND SUnaiSON llond ProHa UldR. bhnd. onnaoN Plionon: OIllco Hort 41; Ron. 123 Read the Bulletin Classified Ads tiinnol duvolopmoiit; but tho old, woalhurod anil inoro or lonn rottoit condition of tlio tmiialt In unfnvor atilo to tunnel proiiorvatlou, Tliun tho IMIiion lco Cavo In otitorod by an artlllnlal nliaft nun tc In highly oxldlxod and docomponod tumult. And tlio glum iiprliiKii no clinntc torlHtla of thin well watered wost oru nlopo (nctipo, It In hollovod, from eollapniiil liiuuoln In woathered and rotten biiHiilt. Thin Ih, probably, the hunt explanation of tho out flown of water to which wo owo Kail rlvo'r, Hprlng river and Metolltin river, mid, pnHnlhly, noma of tho dozen or more other nprlugn named or Indicated on tho map, Of fairly frequent occurrence, iiIho, aro longl ttidlual depreHHlonn of the nurfnco niiKKontlvn of tho collapno of lava tunnolH, Assuming that Spring river and Fall river do repreiiout col lapMod tunnolH, tho quontlou nrlsos an to whether or not the ttmuoln aro choked beyond tho voutn of tho nprltiKH, Although doflnlto data on which to bano an aniiwor aro luck ing, more or Iohn comploto clogging of tho tiinnnln nppoiirn monl prob able Hut however thin may ho, wo can not doubt that tho tuuneln, either cloned or opou, do oxtond obliquely downward beneath tho rcnorvolr area to tho ax In of the valley, where, pusHlbly, thoy aro united, filuco they aro rofornblo to one and tho nnmo groat outflow of hanalt, and nro, thun, onnentlnlly coutemponiiiooiin, their union, orfg Itinlly If not now, nppoarn to bo n snfo coiiclunlon. Recognizing tho wentern an far older, many thou naiidn of yearn older, than tho east ern bnnnlt of tho Donchuten vnlloy, tlio aniumptlou In not warranted that tho wonteru tunneln nro or ever were confluent with tho nnnlorn and relatively modem tiinnol. Wo miiNt nuniimo, rather, that after tho wonteru basalt had nwopt well acronn tho valley crowding tho rlvor bo foro It and Isolating tho Ilcnliam Palln rhyollto rldr.o, which thun bo rnmo n ntoptoc, tho onntorn How of bnmilt overlapped tho wontorn and crowded tho rlvor back townrd It original location: but with both river channel and tunnel at n higher elevation. Another consideration unfavorable to the coincidence of tho eantern and woHtoru tunneln In that while tho normal trond In northwesterly for tho former It In northenntorly for tho latter. Tho two nyntemn thun tond to crosn nt largo niiglcn, an well an nt different level, and colucldonca In hopelonn. Hut thoy clenrly ngren In thin; They all underlie tho floor of tho pro poned llenhnm Kails rcnorvolr, Itecent Volcanic I'liennmenn Tlio term recent In hero lined In a geologic, and not In n human, neuno. Any geologic, and enpeclally MD Phono Black 1X91 LEH A. THOMAS, A. A. IA. Architect 8-4 O'Knno Bntldlnn; BEND OREGON 0, P. NIBWONQBR. Bond, Ore. UNDERTAKER Llceaied Kinbnlrucr, Vaaeral Director, Phono Rod iih Lady Aaat. DR. R. D. 8TOWELL Nnprnimllitc I'liynlcln Oror Logan Furnlturo Co, Wall Btreot lloura 9 to 6 Phono Red 4H3 DR. TURNER KYH 8PK0IALI8T Pormiiuontly Located In Bond with Now Uqulpniont Prlvnto Otllco In Thoraon'a Jowolry Storo Dr, Tumor will bo In Prlno vlllo ovory llrnt nnd third Fri day; In Mndrns oyory socoud and fourth Friday, nud In Rod mond ovory flrnt and third Thursday ot each month. cf Yours for Real Tobacco " says the Good Judge Men arc ftcttlng away RIGHT CUT Is a short W-B CUT Is nny volcanic, hnpponliiR within tho hint 0,000 yearn, may fairly ho do ncrllioil on rocont, and within tho lant 1,000 yearn an vory recent AI UioukIi tho contrary Imprcnnlon vory Konornlly provnlln, It In doulitful If any noteworthy rooIorIc occurronco of nu Igncoun or volcanic nntiiro ban como to pann In tho hint 1000 yearn In tho Cnncndo roKlon of Central OroKon; and wo can not bo nuro of nny mich linpponlnR within tho lant C,000 yoarn. Anyhow, wo will now oxtond tho term ecologically rocont to cover tho formation of all tho unorodod couch and flown of tho upper DcnchutcH valloy; and mako tho clannincntlou onny by regarding tho groat banalt platoau Including tho rolntlvoly old flow of tho went nlopo and tho relatively now flow of tho cant nlopo an geologically an cient (Mlocouo and Pllocono), and tho conen dotting tho nurfnco of tho nlatonu and tho flown making a patchwork of Itn nurfnco on geo logically modern (Quaternary and Recent). Mini)' Coup round. Within 40 mllcn nouth of Bond no fawer than 1C0 conen hnvo been mapped ranging" In elovntlon, ap proximately, from 300 to 3000 fcot nhovo tho nurfnco of tho plateau. It In, of course, probnbta that nomo of theno conen nro rhyollto ntoptoca and hencn older than tho surrounding hnnnlt plntoaii, but n largo majority, nuroly, aro of basaltic composition elthor cinder conen or nggnsgaten of cludorn, dunt nnd lapllll, and newer than tho plateau on which they ntund. Tho flown, representing tho moro pnnly nnd fluid part or tho ojucted tnntcrlul, appear to havo bcn much lonn completely mapped than tho conen, nnd nro nhown, In mnny or n majority ot Instances, without an noclutcd conen. Adding tho headless flown to tho lint of cones would In crease tho number of vontn nt leant to ICO. On tho western nlopo tho vontn aro distributed nomowhat uni formly, averaging ono to ovory ten nqunro miles, whllo on tho eantern nlopo thoro aro very fow vents north of tho Nowborry crntor, and thpy nro thickly grouped over a wldo xono nouth nnd Routhonst of tho crater, tho two slopes thus averaging nearly equal, area for area. It Hoemn Impossible on elthor nlopo, to dlncovor nny sort of regu larity or order In tho distribution of tho vontn. It might bo supposed that from tho groat flssuro ot tho Cuscndo crost springs a norlcH ot par allel obllquo fissures on which tho vontB nro located. That Is, no doubt, tho prlnclplo or koynoto of tho ills trlbutlon, but minus tho main part of tho regularity. Ono vory striking fonturo of tho distribution of tho vouts Is their fownens In tho vicinity ot tho river, cspoclnlly it wo keep to tho main lino ot tho rlvor.whlch Is tho r-ast Deschutes, or so-called Lit tle rlvor. Tho West Deschutes Is cnllcd.nlso , tho Big rlvor, simply bo cniiBO t drains tho hum III Cnscado slopo nnd, houco oxcols in volumo of water, though not In length, breadth or dopth ot vnlloy. Followlng.thon, this moro direct nnd nmplo drnlnago lino, wo find not ono basaltic vont within two tulles ot tho river nnd, within CO miles south ot Bond, only flvo vontn within four mtlos ot tho rlvor, theso flvo Including Pilot butto nnd Lnvn hutto, tho latter in tho latltiulo ot Bonhnm falls. Within 40 miles south ot Bonhnm falls, vouts, although within two to four miles on tho west, aro much moro distant on tho cast, ospoclully Bouth of Dittos butto, whoro tho nron prac tically froo from vouts oxpntulB rap Idly from a hrondth ot six miles to 25 miles. What part, If nny, tho rlvor may hnvo plnyod in tho deter mination ot this broad oxpauso treo from volcnnlo vouts wo enn only con jocturo. But It Is cortninly nn Inter esting and significant tact that tho proposod rosorvolr Hob wholly within this nron. Assuming, as wo must, that ovory volcnnlo vont is located on a profound fracturo travorBlng from the blft chew Idea. They find more satisfac tion in a little of the Real Tobacco Chew tiian they ever got from a blft chew of the ordinary kind. Costs you less, too the full, rich tobacco taste lasts so much longer. Any man who uses tlio Real Tobacco Chew will tell you that. Put up in two styles - cut tobacco a long fine-cut tobacco tho ontiro thickness of tho great Co lumbia basalt and many thousands of fcot In thlckncHH of tho subjacent formations, wo mny well feel grate ful that tho broad nyncllnal axial xono between tho canlward-dlpplng older buna It on tho west and tho woslward-dlpplng newer basalt on tho oast docn not appear to bo broken by olthcr tho eastern or tho western fissures. yinnurt-n Not LIim-m of Wntkncnn. Another way of regarding tho mat ter In to nupposo that tho fissures of tho western basalt do not extend nn far cast an tho river, nor thoso of tho eantern basalt nn far west nn tho rivor. Tho western slopo presents a continuous, wldo xono of vents and, wo must suppose, correlating fis sures, but all tho vents and related fissures of tho eastern slopo must, npnprontty.bo correlated with tho gi gantic Nowborry crater, tho "nphoro ot Influonco" of which extends out ward for 10 to 15 miles In all direc tions. Taking It for granted that tho vents havo their origin in profound fissures does not, however, mean that theso fissures must still bo regarded as lines of weakness, nor. necessar ily, as n menace to tho tightness of tho reservoir should they traverse Its floor, for wo aro warranted In sup posing that fissures sufficiently pro- ",,i t nmiri r i nni'nn nmenn an" ",ed w'tn tl, Clerk of the Coun found to develop volcanic vents iSW,?. SKa.0-?,'. ' i 0--. 0- would bo filled with tho molten lava and converted, Ity slow cooling, Into wnter-tlght dikes. Ot course tho caso would be radically different If dynamic cracking nnd rifting should follow tho formation of tho dikes and tho frcozlng of tho lavn In tho ground. Kivn Butto Cono and Flow. Tho relations of this most recent of nil tho volcanic eruptions of tho region to tho proposed Benham falls dam nnd reservoir nro so close and vital as to demnnd its separato de scription nnd discussion. From tho western base of n normal cono ot cin ders and lapllll nbout COO feet high, with a summit crater about 1C0 feet deep, there has flowed away n volumo of liquid nnd pasty lava sufficient to cover nn area of at least 10 square miles to n dopth ot SO to 100 or moro feet. Tho courso of tho lava flood was flrnt northwesterly about two miles, with a breadth of ono mile, to nud across tho Deschutes rlvor, and thou northerly, down tho valley for four miles, with a broadth of two to three miles. Tho surtaco and steep mnrglns of this flood of lava nro Indescribably rough nnd trnvollug ncross it Is necessarily slow and painful. Tho oruption nppenrs to havo bcon accompanied by but little wind, slnco tho surfaco of tho flow Is practically frco from dust nnd hence, also from vegetation, with tho exception of an occasional plno treo ono to sovoral to a squnro mllo. Tho dusty slopes ot tho cono aro, naturally, moro hos pltablo to vogctatlon than tho baro surfaco ot tho flow, and tho north enstorly aspect supporta a scattering growth ot pines. Tho lnvn Is throughout so black, hard nnd shining, so fresh nnd so freo from vlsiblo woatherlng or nltor ntlon of nny kind that tho first Ini- Brooks- Scanlon Lumber Company Lumber, Lath, Shingles, Building Material, Kiln Dried Flooring and all kinds of Finish SASrfAND DOORS COMPLETE STOCK oi Standard Size. BROOKS-SCANLON LUMBER CO. Local Salos Agout, MILLER LUMBER CO. TANLAC pression Is ono of groat roconcy of eruption, nnd fow nro disponed to es timate tho ago ot tho eruption at mora than n contury or two, nnd many would placo tho tlmo of tho ox trunlon of tho lavn at Icsn than a century In tho pant, but for tho fact that wo havo no human record nnd tho tontltnony of man Is wholly want ing. IllvT Tell Country's Ak'. Perhaps tho most cogent argument for tho ronnldcrablo antiquity of Lavn butto nnd Itn Inva Is afforded by tho fact that tho lavn, having crowded tho river out of Itn bed and over tho rhyollto rldgo, tho river has nlnco cut a gorgo approximately CO deep In tho mnsslvo rhyollto. An numlng 20 feet of weathered and moro or less decayed and eanlly erod ed rhyollto, we munt recognize that cutting a notch 30 feet deep In tho solid, unwenthorcd rhyollto was a largo task for n river of clear water entirely unnrmed by sand or graTol or other cutting material. Of this condition wo arc assured by tho fact that the river is deep nnd itn current sluggish for a considerable distance nbovo tho falls. Beyond a doubt, tho tlmo slnco tho lava turned tho river over tho rhyollto rldgo and brought Bonham falls Into oxlstcnco must bo reckoned In thousands ot years, and C00O years docs not appear an ex treme or unresonablo estimate. (To Bo Continued.) LEGAL NOTICES INDEPENDENT CANDIDATE FOR COUNTY JUDGE Tumalo, Ore Aug. 1G, 1920. At tho solicitation of a largo num ber of farmers of Deschutes county,' I announce myself as an Independent candidate for tho position of county Judge. Watch for my "platform." CHAS. HOFSTETTER. NOTK'II FOF; PUBLICATION (Not Con! Land.) Department of tho Interior, U. S. Land Offlco at Lakovlew, Oregon, August 11, 1320. Notlco Is hereby given tnni ic. stead Entry No. 010423 for lots 5-6,1;. .'(.T ,",7' " "' vpi cu'l' qpu vni'i! Section minisirauon oi saia estate, f Tonhln n, q T Ilnnce 10 E ! Will. tlmt lh J,,dR0 of the abov 6. Township 21 S.,Uange 10 t.., Win- ... r . . . c, ,,, nmette Meridian, has filed notlco ot Intention to make final three-year ;.-, . ..lll. -l-l . ,K lun.t T -- i...iiJV .fn, v r PinriT ' day nl ,h0 courl room ,n Bond, """f&iPcwhuie. County, Oregon, ns tho u. a. kuiiiuiiniuuvi, " uuh.uv, w.- mmiHiunur. " .,.. .. . - gon, ,on tno S6iii oay ot sepiemuer. account and of tho -,. of M,d i -i. nn.no n. tt-inoi.fl. estate, and all persons interested Claimant names as ' nefc-' aro cited to appear at said tlmo ?!rl "vVnoL'n.and place and show cause, if any. W. Case, all of Laplno. Oregon; Frank Foster of Powell Butte. Ore gon. JAS. H. BURGESS, 2C-29c Register. In tho County Court of the State of Oregon, for tho County ot Des chutes. In tho matter or the estate of F. M. Wright, deceased. To E. M. Wilson. Edgar Wright, Homer Wright. Etta Gustavls, Carrie Bottis. Nelllo Nugent, Mlnnlo Brad way, Lida Doud Young. Esther Doud, Leland Doud, Flora Stewart, Clara Wright, Arthur II. Moo, Rev. Verne Thompson, tho known heirs at law of F. M. Wright, deceased, and to all tho unknown heirs ot suid decedent, greeting. , You are hereby cited and required to appear In the County Court of tho tho Stnto of Orogon, for tho County of Deschutes, nt tho court room thereof. In the city of Bond. In said S"?i21vS? tt o'ill.h' OV)HVUIUUI 'v ,.w- ... ,,- nftornoon of said day, then and thoro to show cnuso why an ordor should not bo granted to tho administrator ot said estate to soil so much ot tho hereinafter descrlbod real estato of said decedent as shall be necessary to pay tho debts outstanding nnd tho expenses or administration, to-wti: Tho NWU of tho SWU of Section 35, in Township 17 South, Range 12 East of tho Willamette Meridian, In Doschutes Count). Orogon, to gothor with a 24-acro water right appurtenant thoroto. Witness, tho Hon. Robert W. Saw yer, Judgo of tho County Court ot tho Stnto of Oregon, for tho County of Doschutes, with the son! of said court affixed this 12th day of Au gust, 1920. Attest: J. H. HANER, 25-280 County Clork. FOR SALE DY The Owl Pharmacy "OLE A0ENT3 017JJ7.) 18008. NOTICIJ OK PUMLKMTION V. 8. Lnnd Offlco at Tho Dallos, Oregon, August 6, 1020. Notlco In horoby glvon that Wil liam A, Oolden of Bond, Orogon, who, on Juno 23, 1917, mndo homo stead entry No. 01(1737, nnd on Jan. 11, 1920, mado nddltlonnl homenlond ontry No. 018003, for NEVi SW, N,4 8B4, 8K4 8E4, Hoc. 20: 8 8WVJ, 8cc. 21; NWU, N SW4, Section 28, nnd NE14. Section 29. Township 19 South, Rango 14 Enst, Wlllamotto Meridian, has filed notlco of Intention to rnnko three-year proof, to establish claim to tho land nbovo described, noforo If. C. Ellin, United States Lnnd Commissioner, Bond, Orogon, on tho Cth day ot Oc tober, 1920. Claimant names as witnesses: Howard F. Dyer of Mlllican, Oregon; Denzll C. Dyer, of Bond, Oregon; R. A. Kllpatrlck, of Bond, Oregon; Archlo Pepin, of Mlllican, Oregon. 11. FRANK WOODOCCK. 24-28p Register. NOTICE OP HEARINO In tho County Court of the Stato pf Oregon for the Connty of Des chutes. In tho matter of tho estate ot Olo O. Dragsvold, deceased. Notlco Is hereby given that on Tuesday, tho 14th day of Sopt., 1920. at tho County Court Room, In tho city of Bend, Deschutes County, Ore gon, at tho hour of 2 p. m. of said day, tho following matter wilt bo heard and considered, to-wit: The petition of Julius Pcdersen for tho probata of those certain Instru ments In writing purporting to con stitute tho last will and testament of said Olo O. Dragsvold, deceased, for tho granting of letters testamentary therefor to said petitioner nnd for tho taking ot any testimony therein that may havo a bearing upon said alleged last wfll and testament and the disposal of tho estate of said de ceased in accordance with his wishes. Dated nt Bend, Oregon, August 7, 1920. ROBERT W. SAWYER. County Judge. 24-28o NOTICE OF lUvARING ON FINATj ACCOUNT In tho County Court of tho Stato of Oregon, for Deschutes County. In tho mater of tho estate of Olo Olson, deceased: Notlco Is hereby given that Theo dore Aune, administrator of tho es tate of Olo Olson, deceased, has mado account of his ad- and abovo cn- ,i,i.i r....- i -- i- a .. ".",- "?2.ri. " . '" "", , .., ',";;,"':" ", ' ,.X ' "tiUt. IUO Ul , d , . hGarIn ,,, fnnl wny said account should not bo nl- lowed, and said estate closed and settled. Dated this Cth day ot Augusn. 11920. THEODORE AUNE. Administrator ot tho cstato of Olo Olson, deceased. DE ARMOND & ERSKINE, Attorneys for Administrator. 24-28c-Ct NOTICK FOR PUBLICATION (Not Coal Lund.) Department of tho Interior, U. S. Land Offlco at Lakcviow, Oregon, July 12, 1920. Notlco Is hereby given that Corn Leland ot Laplno, Orcgou, who, on July 26, 1917, mado Homestead En try No. 010383, for SWU NWU. NWU SWU, E& SWU, Section 2, Township 23, South Range 9 East,. Willamette Meridian, nns filed notlco of lntentlon t0 inako'r,Dal tnrco-y0ar Proof, to establish claim to tho land abovo described, before E. L. Clark, U. 8. Commissioner, at La Pine, Oro gon, on tho 21st day of August, 1920. Claimant names as witnesses: Kato Zieralf, R. E. Eaton, B. C. Scott, Maude Eaton, all of Lapine, Oregon. JAS. F. BURGESS, 21-2Gc Rcgistor. NOTICE FOR PUBLICATION (Not Coal Lund.) Department of the Interior, U. 8. Land Offlco nt Lakcviow, Oregon, July 12, 1920. Notlco is hereby glvon that Her man A. Rose, ot Laplno, Oregon, who, on April 28, 1916, made Homo stend Entry No. 09227, for W NH 11, Soctlon 15; Wtf SBU. Section 10, Township 23 South, Rnngo 0 East, Wllliamctto Morldlan, hns tiled notlco of intoutlon to make tint! threo-year proof, to establish claim to tho laud abovo described, before H. L. Clark, U. S. Commissioner, ft Lapluo, Oregon, on tho 20th day ot August, 1920. Claimant names as witnesses: R. E. Eaton, Fred Mnhn, II. A. Rose, W. G. Fordham, all of Laplno, Ore goit. JAS. F. BURGESS, 21-2CC Register. Brand Directory HG Brand John Helfrich, 0-4 p - Brothers, Ore. Anign ped; Right side; right ear crop. wattle right hind leg. L. TONB, Sisters, Or. H8T.1VUC fc