╨╧рб▒с>■   ■                                                                                                                                                                                                                                                                                                                                                                                                                                                   ¤     ■   ■   >+■    !"#■   %&'()H<=-./0123456789:;■   ?■   ■   @ABCDEFGJI■   KLM■   OPQRSTUVWXYZ[\]■                                                                                                                                           Root Entry         ░║m░Ф╟ АITEM000      └F0йxD╣─╞░║m░Ф╟1Table    $CompObj            j■ ╒═╒Ь.УЧ+,∙о0ш hp|ДМФ Ьдм┤ ╝ ╔ф ░ A  Title■   ■   ■   ■   ■                                                                                                                                                                                                                                                                                                                                                                                                                                                                                           ■       └FMicrosoft Word Document MSWordDocWord.Document.8Ї9▓q%└F\Object └F4dMicrosoft Word DocumentD:\Youngs Bay final data\Stream reports\Lewis and Clark Tribs\Barrett Creek Report.docWordDocument            "SummaryInformation(     DocumentSummaryInformation8            ITEM000FMT            ■ рЕЯЄ∙OhлС+'│┘0xРШд░╠╪ш   ( 4 @ LX`hpфssAdrianne SchackartdriNormale Todd Boswellcka2ddMicrosoft Word 10.0@F├#@╚_Dй}┼@NCzФ╟@ФЮФ╟Щ ье┴5@ Ё┐╡bjbj╧2╧2 "нXнX╡       И6666666ЖJJJJ VЖY ╢vvvvvvvv╪ ┌ ┌ ┌ ┌ ┌ ┌ $ Raf■ 6L vvL L ■ 66vv    L v6v6v╪  L ╪  в ╕ 66╕ vj ┴7ЯФ╟J┬ "╕ ╪ ) 0Y ╕ ╟ф ╟╕ J$n6666╟6╕ vh▐J (<dшvvv■ ■ ЖЖ─J ЖЖJ Upper Nehalem Watershed Habitat Assessment Stream Report STREAM: Fall Creek (Rock Creek Trib) SUBBASIN: Upper Nehalem River DATES: March 6, 2006 SURVEY CREW: Scott Young, Ben Walczak REPORT PREPARED BY: Ben Walczak GENE CONSERVATION GROUP: 1-NC UTM COORDINATES: Start Ц 0474949 E & 5079306 N End Ц 0474783 E & 5078643 N USGS MAPS: Clear Creek GENERAL DESCRIPTION: The Fall Creek winter habitat survey begins at its confluence with Rock Creek and extends 1,009 meters. One reach was designated based on: Valley width and Channel morphology. Riffles (60%) and scour pools (22%) dominated the habitat, while silt/organics (41%), sand (29%), and gravel (18%) were the dominant substrate types. The survey begins at the confluence with Rock Creek and ends at a large step that is a definite barrier to coho. A salmon spawning survey is also set up for this same section of stream. The stream runs through a rural residence and then into timberland. REACH DESCRIPTIONS: REACH 1: Length Ц 1,009 meters. The channel is constrained by alternating hillslopes and terraces in a broad valley. The average valley width index is 6.4. Land use for the reach is rural residential. The average unit gradient is 2.0%. The channel characteristics include: primary 1,009m and secondary 16m. Zero pools were greater than 1 meter deep. There was a low amount of LWD with three logs greater or equal to 12m x 0.6m, which averages to 0.3 key pieces per 100m. The vegetation is based on 2 riparian transects. The trees found most frequently in the riparian zone were mostly mixed sizes of deciduous ranging from 30 Ц 50 cm dbh, with some conifers 50 Ц 90 cm dbh. This survey begins in a rural residential area. The stream meanders through a terrace of Rock Creek and actually flows into Rock Creek below where the map shows it entering. The reach is characterized by silt/organics, sand, and gravel dominating the substrate. There are dam pools with light beaver activity in the survey below itТs crossing with Keasey Road. The culvert is a bit steep but does not appear to be a barrier and is in good shape. Above the road an old railroad trestle has collapsed into the stream. The survey ends at a 3.0m high bedrock step. The riparian shade through this section of the stream is average. Fall Creek has average habitat and is lacking in pools and large wood. There is excellent LWD project potential with great access for industrial equipment below the culvert crossing. The riparian area in this section has average riparian shade but has recently been thinned creating excellent riparian enhancement project potential. Further planning would be beneficial for a successful project in Fall Creek. C : < [ ╡№є№я№я№hlхh╧$5БCJ\Бh╧$/BCjkКЛвг╩╦ьэ < ] ^ v w М Н ╓ ╫ ╫ ┘ э ю ¤└!Нм¤└!е¤└!е¤└!е¤└!Нм¤└!Нм¤└!Нм¤└!Нм¤└!Нм¤└!Нм¤└!Нм¤└!Нм¤└!Нм¤└!Нм¤└!Нм¤└!Нм¤└!Нм¤└!Нм¤└!Нм¤└!Нм¤└!Нм¤└!Нм¤└!Нм¤└!Нм¤└!Нм¤└!Нм¤└!Нм¤└!Нм¤└!Нм╡¤ю ў ° ЫЬ▒│╡¤└!Нм¤└!Нм¤└!Нм¤└!Нм¤└!Нм¤└!Нм¤└!Нм¤└!Нм¤└!Нм 1Рh░╨/ ░р=!░"░#Ра$Ра%░0ААР0ААР0ААР0ААР0ААР0ААР0ААР0ААР0ААР0ААР0ААР0ААР0ААР0ААР0ААР0ААР0ААР0ААР0ААР0ААР0ААР0ААР0ААР0ААР0ААШ0ААШ0Ь@@ё @ NormalCJ_HaJmH sH tH DAЄ бD Default Paragraph FontViє │V  Table Normal :V Ў4╓4╓ laЎ (kЇ ┴(No List ╡        аzЩ   аzЩЬ╡ y/BCjkКЛвг╩╦ьэ  <]^vwМН╓╫╫┘эюў°ЫЬ  ▒ │ ╖ Ш0ААШ0ААШ0ААШ0ААШ0ААШ0ААpШ0ААШ0ААШ0ААШ0ААШ0ААШ0ААШ0ААШ0ААШ0ААШ0ААШ0АА АШ0АА АШ0АА АШ0ААШ0ААШ0АА АШ0ААШ0ААШ0ААШ0ААШ0АА АШ0ААШ0АА(Ш0АА АШ0ААШ0АА АШ0ААШ0АА M90АM90АM90АM90А╡ ю ╡ ╡   ▀}▓l^р}▓D_с}▓╧т}▓\╧у}▓Ь╧ф}▓╨х}▓\╨vv|ДФ√√╖ {ГЙЙб╖ 9*Аurn:schemas-microsoft-com:office:smarttagsАplaceА=*Аurn:schemas-microsoft-com:office:smarttags АPlaceNameА=*Аurn:schemas-microsoft-com:office:smarttags АPlaceTypeА8*Аurn:schemas-microsoft-com:office:smarttagsАdateА;*Аurn:schemas-microsoft-com:office:smarttagsАaddressА:*Аurn:schemas-microsoft-com:office:smarttagsАStreetА А2006А3А6АDayАMonthАYearcg┬╔фыZ[BF;EsvЦЩ√╖ <\БО╖ : @\╖ Z[╖   Todd Landon BoswellTodd Landon BoswellTodd Landon BoswellTodd Landon BoswellTodd Landon BoswellTodd Landon BoswellTodd Landon BoswellTodd Landon BoswellTodd Landon BoswellMark McLaughlinх╧$lх @А[[И╤ТЛЛ[[*{\rtf1\ansi\ansicpg1252\uc1\deff0\stshfdbch0\stshfloch0\stshfhich0\stshfbi0\deflang1033\deflangfe1033{\fonttbl{\f0\froman\fcharset0\fprq2{\*\panose 02020603050405020304}Times New Roman;}{\f36\froman\fcharset238\fprq2 Times New Roman CE;} {\f37\froman\fcharset204\fprq2 Times New Roman Cyr;}{\f39\froman\fcharset161\fprq2 Times New Roman Greek;}{\f40\froman\fcharset162\fprq2 Times New Roman Tur;}{\f41\froman\fcharset177\fprq2 Times New Roman (Hebrew);} {\f42\froman\fcharset178\fprq2 Times New Roman (ArabOle             5OlePres000    ,оITEM000ODS     ITEM000FMT#3     └FP5ЯФ╟P5ЯФ╟        И;ЕVl ╢Х  }.√Ь Р@Times New Roman-  2 Zp -√Л ╝@Times New Roman-- 2 ▀p , 2 ▀,p , 2 ▀Xp ,-J2 ▀Д*pUpper Nehalem Watershed Habitat AssessmentTAA44T4A:!4`u;'44.A3A[;@!&;'T--4..`4A' 2 ▀╔ p > 2 ep , 2 e,p , 2 eXp , 2 eДp , 2 e░p ,2 e▄ pStream ReportA'44;`T4A;4' 2 e├p > 2 ыp ?-C2 _%pSTREAM: Fall Creek (Rock Creek Trib)8=C=HY7,C!,,2"C2,2C!,,2=!2" 2 _Вp Ж 2 _p - 2 ╥p -82 EpSUBBASIN: Upper Nehalem River8HBBH9 HH22,!H,3,,NC2,! 2 Eпp . 2 ╕p -,2 +pDATES: March 6, 2006HH==8Y,!,222223 2 +єp - 2 Юp -D2 &pSURVEY CREW: Scott Young, Ben Walczak8HCH=HCC=_8,2H2221B,2_,,-,2 2 Wp . 2 Дp -;2 ў pREPORT PREPARED BY: Ben WalczakC=8HC=8C<8HC=HBHB,2_,,-,2 2 ўаp . 2 jp -(2 ▌pGENE CONSERVATION G0H=H=CHH8=CHH> IHH2 ▌ОpROUP:hCHH8 2 ▌╡p ' 2 ▌▄p12 2 ▌p-!2 ▌/pNCHC 2 ▌║p - 2 Pp -2 ├pUTH= 2 ├ЕpM COORDINATES:YCHHCI HH==8 2 ├╒p █2 ├░pStart 8,! 2 ├ЖpЦ2,2 ├╕p 0474949 E & 5079306 N2222222=M2232222H 2 ├─ p  2 ├▌ p - 2 6p , 2 6,p , 2 6Xp , 2 6Дp ,2 6░pEnd =22 2 6jpЦ2,2 6Ьp 0474783 E & 5078643 N2222222=M2232222H 2 6и p  2 6┴ p - 2 йp -.2  pUSGS MAPS: Clear CreekH8H8YH88B,,!C!-,2 2  Wp - 2 П p -)2  pGENERAL DESCRIPTION:H=H=CI<H=8CD8>!HH 2  Сp - 2 u p - 2 ш p ,А2 ш ,NpThe Fall Creek winter habitat survey begins at its confluence with Rock Creek =2,7,C!-,2H2,!3-2,'2!2-03-12',',22!2,2-,H2C2,2C",,2A2 [ $pand extends 1,009 meters. One reach,22,3,22'2222N,,!'H2,!-,,2L2 [ ┌+p was designated based on: Valley width and I,'2,'12,,22,',222I,-0H22,22М2 ╬ VpChannel morphology. Riffles (60%) and scour pools (22%) dominated the habitat, while C2,22,N2!222230C!!,'!22T!,22',23!232'!22S!22N2,,22,2,2,H2,Й2 A Tpsilt/organics (41%), sand (29%), and gravel (18%) were the dominant substrate types.'2!1,2,'!22T!',22!22S!,222!,2,!22S!H,!,2,22N2,2'22'",,03,' 2 A b p . 2 ┤ p -I2 ' )pThe survey begins at the confluence with d=2,'2!2.02-12',2,,22!2,2-,H2P2 ' Е.pRock Creek and ends at a large step that is a C2,2C",,2,22,22',,-"1,',22,',Ф2 Ъ [pdefinite barrier to coho. A salmon spawning survey is also set up for this same section of 2,!2,2,!!,!2,222H',N22'2,H221'3!3-0','2(,22!2!2'',N,',,222!2 Mpstream. The stream runs through a rural residence and then into timberland. '!,,N=2,'!-,N!22'2!2212-!2!,!,'2,2-,,222,222N2,!,22 2 ў p - 2 Аp , 2 А,p -(2 єpREACH DESCRIPTIONS::C=HCHH=8CD8> HI8 2 єJp , 2 fp -2 ┘pREACH 1:C=HCH2 2 ┘║p - 2 Lp - 2 ┐p ,2 ┐,pLength :<,312 2 ┐_pЦ2y2 ┐СIp 1,009 meters. The channel is constrained by alternating hillslopes and n2222N,,!'=2,,2,23,',22'!,2-230,-!2,312'22,',22Х2 2\pterraces in a broad valley. The average valley width index is 6.4. Land use for the reach ,!!-,,'2,2!3,22,.1=2,,2-!-1,3,.0H3222,3'22;,222'-!2!2,!-,,2О2 еWpis rural residential. The average unit gradient is 2.0%. The channel characteristics '!2!,!,'2,2,=3,-2,!-1,221",2,2'22S=2,,3,22,,3,!-,,!','2 pinc2,Л2 zUplude: primary 1,009m and secondary 16m. Zero pools were greater than 1 meter deep. s22,2!N,#02222N,22',,222-#022N<,"2222'H,!,1",,-!2,32N,,!2,,2Й2 ЛTpThere was a low amount of LWD with three logs greater or equal to 12m x 0.6m, which =2,!,I,',2H,N2222!;_HH22!-,21'1",,-!2!,23,222N222NH2,2О2 ■Wpaverages to 0.3 key pieces per 100m. The vegetation is based on 2 riparian transects. ,2,!-2,'2222.02-,-'2,!222N=2,2-2,,22'2,',2222!2,!,2!,2',,' 2 ■d p Г2 qPpThe trees found most frequently in the riparian zone were mostly mixed sizes of =2,!,,'!2222N2'!!-22,2022,!2-!,2-22,H,",N2'0N3,2',,'2!22 фpdeciduous ranging from 30 2,,2222'!,3131"!2N22 2 фQpЦ2>2 фГ"p 50 cm dbh, with some conifers 50 22,N222H2'2N,,22!,!'22 2 ф pЦ22 ф4 p 90 cm dbh.22,N222 2 ф p - 2 Wp -√╝"System|$ф-NANINI  -NANI  % ic);}{\f43\froman\fcharset186\fprq2 Times New Roman Baltic;}{\f44\froman\fcharset163\fprq2 Times New Roman (Vietnamese);}}{\colortbl;\red0\green0\blue0;\red0\green0\blue255;\red0\green255\blue255; \red0\green255\blue0;\red255\green0\blue255;\red255\green0\blue0;\red255\green255\blue0;\red255\green255\blue255;\red0\green0\blue128;\red0\green128\blue128;\red0\green128\blue0;\red128\green0\blue128;\red128\green0\blue0;\red128\green128\blue0; \red128\green128\blue128;\red192\green192\blue192;}{\stylesheet{\qlITEM000FMTRich Text Format8            *.Ole          OlePres000            NN            ■   О#3Rich Text FormatatИ;lXp!Д \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 \fs24\lang1033\langfe1033\cgrid\langnp1033\langfenp1033 \snext0 Normal;}{\*\cs10 \additive \ssemihidden Default Paragraph Font;}{\*\ts11\tsrowd\trftsWidthB3\trpaddl108\trpaddr108\trpaddfl3\trpaddft3\trpaddfb3\trpaddfr3\trcbpat1\trcfpat1\tscellwidthfts0\tsvertalt\tsbrdrt\tsbrdrl\tsbrdrb\tsbrdrr\tsbrdrdgl\tsbrdrdgr\tsbrdrh\tsbrdrv \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 \fs20\lang1024\langfe1024\cgrid\langnp1024\langfenp1024 \snext11 \ssemihidden Normal Table;}}{\*\rsidtbl \rsid2363343\rsid6768882\rsid15035416} \widowctrl\ftnbj\aenddoc\noxlattoyen\expshrtn\noultrlspc\dntblnsbdb\nospaceforul\formshade\horzdoc\dgmargin\dghspace180\dgvspace180\dghorigin1800\dgvorigin1440\dghshow1\dgvshow1 \jexpand\viewkind1\viewscale100\pgbrdrhead\pgbrdrfoot\splytwnine\ftnlytwnine\htmautsp\nolnhtadjtbl\useltbaln\alntblind\lytcalctblwd\lyttblrtgr\lnbrkrule\rsidroot2363343 \fet0\sectd \linex0\endnhere\sectlinegrid360\sectdefaultcl\sftnbj {\*\pnseclvl1 \pnucrm\pnstart1\pnindent720\pnhang {\pntxta .}}{\*\pnseclvl2\pnucltr\pnstart1\pnindent720\pnhang {\pntxta .}}{\*\pnseclvl3\pndec\pnstart1\pnindent720\pnhang {\pntxta .}}{\*\pnseclvl4\pnlcltr\pnstart1\pnindent720\pnhang {\pntxta )}}{\*\pnseclvl5 \pndec\pnstart1\pnindent720\pnhang {\pntxtb (}{\pntxta )}}{\*\pnseclvl6\pnlcltr\pnstart1\pnindent720\pnhang {\pntxtb (}{\pntxta )}}{\*\pnseclvl7\pnlcrm\pnstart1\pnindent720\pnhang {\pntxtb (}{\pntxta )}}{\*\pnseclvl8\pnlcltr\pnstart1\pnindent720\pnhang {\pntxtb (}{\pntxta )}}{\*\pnseclvl9\pnlcrm\pnstart1\pnindent720\pnhang {\pntxtb (}{\pntxta )}}\pard\plain \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 \fs24\lang1033\langfe1033\cgrid\langnp1033\langfenp1033 {\insrsid2363343 \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid2363343 \tab \tab \tab }{\b\fs28\insrsid2363343 Upper Nehalem Watershed Habitat Assessment \par \tab \tab \tab \tab \tab Stream Report \par \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid2363343 STREAM: Fall Creek (Rock Creek Trib)\tab \par \par SUBBASIN: Upper Nehalem River \par \par DATES: March 6, 2006 \par \par SURVEY CREW: Scott Young, Ben Walczak \par \par REPORT PREPARED BY: Ben Walczak \par \par GENE CONSERVATION GROUP:\tab 1-NC \par \par UT}{\insrsid15035416 M COORDINATES:\tab Start \endash 0474949 E & 5079306 N}{\insrsid2363343 \par }{\insrsid15035416 \tab \tab \tab \tab End \endash 0474783 E & 5078643 N}{\insrsid2363343 \par \par USGS MAPS: Clear Creek \par \par GENERAL DESCRIPTION: \par \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid2363343 \tab The Fall Creek winter habitat survey begins at its confluence with Rock Creek and extends 1,009 meters. One reach was designated based on: Valley width and Channel morphology. Riffles (60%) and scour pools (22%) dominated the habitat, while silt/organics (41%), sand (29%), and gravel (18%) were the dominant substrate types. \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid2363343 \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid2363343 The survey begins at the confluence with R ock Creek and ends at a large step that is a definite barrier to coho. A salmon spawning survey is also set up for this same section of stream. The stream runs through a rural residence and then into timberland. \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid2363343 \tab \par REACH DESCRIPTIONS: \par \par REACH 1: \par \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid2363343 \tab Length \endash 1,009 meters. The channel is constrained by alternating hillslopes and terraces in a broad valley. The average valley width index is 6.4. Land use for the reach is rural residential. The average unit gradient is 2.0%. The channel characteristics inc l ude: primary 1,009m and secondary 16m. Zero pools were greater than 1 meter deep. There was a low amount of LWD with three logs greater or equal to 12m x 0.6m, which averages to 0.3 key pieces per 100m. The vegetation is based on 2 riparian transects. The trees found most frequently in the riparian zone were mostly mixed sizes of deciduous ranging from 30 \endash 50 cm dbh, with some conifers 50 \endash 90 cm dbh. \par }\pard \q╡ @@  Unknown            GРЗz А Times New Roman5РАSymbol3&Р Зz А Arial"qИЁ╨hБ[╡жВ[╡жЩ Щ !Ёа┤┤ББ>4░ ░ И 3ГЁ▄H(Ё ?ф                     ╧$  Adrianne Schackart Todd Boswelll \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid2363343 \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid2363343 This survey begins in a rural residential area. The stream meanders through a terrace of Rock Creek and actually flows into Rock Creek below where the map shows it entering. The reach is characterized by silt/organics, sand, and gravel dominating the substrate. There are dam pools with light beaver activity in the survey below it\rquote s crossing with Keasey Road. The culvert is a bit steep but does not appear to be a barrier and is in good shape. Above the road an old railroad trestle has collapsed into the stream. The survey ends at a 3.0m high bedrock step. The riparian shade through this section of the stream is average. \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid2363343 \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid2363343 Fall Creek has average habitat and is lacking in pools and large wood. There is excellent LWD project potential with great access for industrial equipment below the culvert crossing. The riparian area in this section has average ripari an shade but has recently been thinned creating excellent riparian enhancement project potential. Further planning would be beneficial for a successful project in Fall Creek. \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid2363343 \par }}p , 2 e,p , 2 eXp , 2 eДp , 2 e░p ,2 e▄ pStream ReportA'44;`T4A;4' 2 e├p > 2 ыp ?-(2 _pSTREAM: Fall Creek08=C=HY7,C!,,2&2 _Жp (Rock Creek Trib)"C2,2C!,,2=!2" 2 _Вp Ж 2 _p         И;ЕV  ЖХ  }.√╝"System8$rэ╞0°E -√Ь Р@Times New Roman-  2 Zp -- 2 ▀p , 2 ▀,p , 2 ▀Xp ,√Л ╝@Times New Roman-J2 ▀Д*pUpper Nehalem Watershed Habitat AssessmentTAA44T4A:!4`u;'44.A3A[;@!&;'T--4..`4A' 2 ▀╔ p > 2 ep , 2 e,p , 2 eXp , 2 eДp , 2 e░p ,2 e▄ pStream ReportA'44;`T4A;4' 2 e├p > 2 ыp ?-C2 _%pSTREAM: Fall Creek (Rock Creek Trib)8=C=HY7,C!,,2"C2,2C!,,2=!2" 2 _Вp Ж 2 _p - 2 ╥p -82 EpSUBBASIN: Upper Nehalem River8HBBH9 HH22,!H,3,,NC2,! 2 Eпp . 2 ╕p -,2 +pDATES: March 6, 2006HH==8Y,!,222223 2 +єp - 2 Юp -D2 &pSURVEY CREW: Scott Young, Ben Walczak8HCH=HCC=_8,2H2221B,2_,,-,2 2 Wp . 2 Дp -;2 ў pREPORT PREPARED BY: Ben WalczakC=8HC=8C<8HC=HBHB,2_,,-,2 2 ўаp . 2 jp -(2 ▌pGENE CONSERVATION G0H=H=CHH8=CHH> IHH2 ▌ОpROUP:hCHH8 2 ▌╡p ' 2 ▌▄p12 2 ▌p-!2 ▌/pNCHC 2 ▌║p - 2 Pp -#2 ├pUTM COORDINATES:H=YCHHCI HH==8 2 ├╒p █2 ├░pStart 8,! 2 ├ЖpЦ2.2 ├╕p 0474949 N & 5079306 E 2222222HM2232222= 2 ├▌ p - 2 6p , 2 6,p , 2 6Xp , 2 6Дp ,2 6░pEnd =22 2 6jpЦ2,2 6Ьp 0474783N & 5078643 E 2222222HM2223222= 2 6и p - 2 йp -.2  pUSGS MAPS: Clear CreekH8H8YH88B,,!C!-,2 2  Wp - 2 П p -)2  pGENERAL DESCRIPTION:H=H=CI<H=8CD8>!HH 2  Сp - 2 u p - 2 ш p ,А2 ш ,NpThe Fall Creek winter habitat survey begins at its confluence with Rock Creek =2,7,C!-,2H2,!3-2,'2!2-03-12',',22!2,2-,H2C2,2C",,2C2 [ %pand extends 1,009 meters. One reach ,22,3,22'2222N,,!'H2,!-,,2J2 [ є*pwas designated based on: Valley width and I,'2,'12,,22,',222I,-0H22,22М2 ╬ VpChannel morphology. Riffles (60%) and scour pools (22%) dominated the habitat, while C2,22,N2!222230C!!,'!22T!,22',23!232'!22S!22N2,,22,2,2,H2,Й2 A Tpsilt/organics (41%), sand (29%), and gravel (18%) were the dominant substrate types.'2!1,2,'!22T!',22!22S!,222!,2,!22S!H,!,2,22N2,2'22'",,03,' 2 A b p . 2 ┤ p -J2 ' *pThe survey begins at the confluence with R=2,'2!2.02-12',2,,22!2,2-,H2CO2 ' ╚-pock Creek and ends at a large step that is a 2,2C",,2,22,22',,-"1,',22,',Ф2 Ъ [pdefinite barrier to coho. A salmon spawning survey is also set up for this same section of 2,!2,2,!!,!2,222H',N22'2,H221'3!3-0','2(,22!2!2'',N,',,222!2 Mpstream. The stream runs through a rural residence and then into timberland. '!,,N=2,'!-,N!22'2!2212-!2!,!,'2,2-,,222,222N2,!,22 2 ў p - 2 Аp , 2 А,p -(2 єpREACH DESCRIPTIONS::C=HCHH=8CD8> HI8 2 єJp , 2 fp -2 ┘pREACH 1:C=HCH2 2 ┘║p - 2 Lp - 2 ┐p ,2 ┐,pLength :<,312 2 ┐_pЦ2y2 ┐СIp 1,009 meters. The channel is constrained by alternating hillslopes and n2222N,,!'=2,,2,23,',22'!,2-230,-!2,312'22,',22Х2 2\pterraces in a broad valley. The average valley width index is 6.4. Land use for the reach ,!!-,,'2,2!3,22,.1=2,,2-!-1,3,.0H3222,3'22;,222'-!2!2,!-,,2О2 еWpis rural residential. The average unit gradient is 2.0%. The channel characteristics '!2!,!,'2,2,=3,-2,!-1,221",2,2'22S=2,,3,22,,3,!-,,!','2 pincl2,Й2 ЦTpude: primary 1,009m and secondary 16m. Zero pools were greater than 1 meter deep. 22,2!N,#02222N,22',,222-#022N<,"2222'H,!,1",,-!2,32N,,!2,,2Й2 ЛTpThere was a low amount of LWD with three logs greater or equal to 12m x 0.6m, which =2,!,I,',2H,N2222!;_HH22!-,21'1",,-!2!,23,222N222NH2,2П2 ■Xpaverages to 0.3 key pieces per 100m. The vegetation is based on 2 riparian transects. ,2,!-2,'2222.02-,-'2,!222N=2,2-2,,22'2,',2222!2,!,2!,2',,'Г2 qPpThe trees found most frequently in the riparian zone were mostly mixed sizes of =2,!,,'!2222N2'!!-22,2022,!2-!,2-22,H,",N2'0N3,2',,'2!22 фpdeciduous ranging from 30 2,,2222'!,3131"!2N22 2 фQpЦ2>2 фГ"p 50 cm dbh, with some conifers 50 22,N222H2'2N,,22!,!'22 2 ф pЦ22 ф4 p 90 cm dbh.22,N222 2 ф p - 2 Wp --NANI