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<br />"e.nhertng ca"stng the" ta erode readily "<ld form thick tal,," ,~"d eolllJvi~l <br /> <br />GEOLOGIC HAZARD <br />AREA <br />AERiAL. Vl~W <br /> <br /> <br />Coalescing <br />Debris Fans <br /> <br />deposits a1008 the canyan ""Ltg. l)uring tntense thundcrstor::!>) or pr~lang"d <br /> <br />r"bstorm", this loo"" fMterL11 becomes satur"ted ca\lsing it to mobi1h~ ,~nd <br /> <br />fIo'" like freshly mLxed tOClcret~ do"" th~ Heel' "">untllirl canYOll'. <br /> <br />ThCFMjorityofthLs1!\()blU?edrMterl,,-ltscompo"edofsand-, silt-, and <br /> <br />elay-sh~d p~rtitles, but cobble- "nd b<luLdct-.hed p"rtLc1",Q ..,s "ell ,qg <br /> <br />significant amoo.mts of diaplaced soiL "nd vegctatLan are also pres"nt. . <br /> <br />WhiLe the larg'H constitu~nta of these fl""s are properly elaa.iEted a. <br /> <br />"debris", the aburldarlce of fine-grained panLcLes causeS th~"e flows to <br /> <br />hehave l1l<e ""'ud," Theretore, both "debris flow" and "mud no,," A'" v"Hd <br /> <br />term" d~scribing the flow_. along the Chntk Cutfs. <br /> <br />Coalescing <br />Debris Fans <br /> <br />This visco,," ,,"'l~$ of mud nnd dd>rL5 OrigiMtin,o; In e.~d1 ""'311 ,nountain b....sin <br /> <br />(~ag" ~), the 'Mlrl ,1d>ris flow el\,lnn~t ''''11 lY38 to 1961 cr".""~d t~.. c~"tr,~1 <br /> <br /> <br />GROUND <br /> <br />VIEW <br />---- <br /> <br />is del'oslt~J at the ""'''rltOltn frorlt, for",t~g ~ hroad, triangular-shaped <br /> <br />feOl""re c.,lied "- ,-(ebrts hn. Through time. successi\1<'. debris flows h,-,ve <br /> <br />Undulating Surface <br />Characteristic of <br />Debris Fans <br /> <br />h"tlt"pL,rgeckhrls faI\swhicilhavemer;:edorcoalesced"Uhfa1\s"tt:he <br /> <br />"'''''ths ot adJ"""rlt """yo"s. T".lav, th"~,, fans form n contln"",," blanket of <br /> <br />debris .1lo~g the norcll "tde of Chalk Cr(!~k. <br /> <br />D"posLtloI\ uf ",,,d and debris on these {(If'. Is ao oogoi"!! proc~"". flows <br /> <br />r~,,~hio~ th" h,.n~ of rh" f~n~ nFt~n Fnll'", th.. ch~on..1 form"~ hv natural <br /> <br />lc'''~cs depoRltd by the pr~cedlng flow or flows. F.v~ntually, ho",ev.or, tl",~~ <br /> <br />"or~ recent ehanrlels "ilt heco"", clogged ",ith debris, forcing the no~' over <br /> <br />th~ levees ..."d int<l adjacent "re,,-S. As Seerl In the ""rlel> of ?hcto"r,,-phs <br /> <br />ponion '" the t"n. Ibw~v"r. bet"een 19,,2 and l'Jti9, an ~'."nt oce"teed in <br /> <br />"htch the ~ebrls bitl~lly tollowed the "",In eh""",,l, b"t lAter, due to the <br /> <br />, <br /> <br />, <br />