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One reach was designated based on: Valley width and Channel morphology. Riffles (35%), rapids (32%), and scour pools (22%) dominated the habitat, while sand (15%), gravel (60%), and bedrock (13%) were the dominant substrate types. The survey begins at the confluence with Rock Creek and ends at a large step due to a lack of flow. A salmon spawning survey (26098.00 seg.1) is also located at the start. The stream runs through timberland. REACH DESCRIPTIONS: REACH 1: Length – 875 meters. The channel is constrained by moderate hillslopes in a narrow valley. The average valley width index is 1.7. Land use for the reach is timber harvest. The average unit gradient is 3.4%. The channel characteristics include: primary 875m and secondary 70m. Zero pools were greater than 1 meter deep. There was an average amount of LWD with twenty-seven logs greater or equal to 12m x 0.6m, which averages to 3.1 key pieces per 100m. The vegetation is based on 4 riparian transects. The trees found most frequently in the riparian zone were mostly mixed sizes of deciduous ranging from 15 – 30 cm dbh, with some mixed deciduous and conifers 30 – 50 cm dbh. This survey begins in a timbered area. The habitat throughout the survey is average. The reach is characterized by gravel, sand, and bedrock dominating the substrate. There are little pools with heavy fines and bedrock scattered throughout the survey. The riparian shade through this section of the stream is excellent. There is poor LWD project potential with little access for industrial equipment. The riparian area has excellent riparian shade throughout the entire reach but has recently been harvested creating fair riparian enhancement project potential. CЅќѓќhЬ{Œ5CJ\hЬ{Œ/BCWXwx‘КЛмнћќ, L M d e z { Ъ Ы  Ÿ Г Д §Р!Ќ§Р!Ѕ§Р!Ѕ§Р!Ѕ§Р!Ќ§Р!Ќ§Р!Ќ§Р!Ќ§Р!Ќ§Р!Ќ§Р!Ќ§Р!Ќ§Р!Ќ§Р!Ќ§Р!Ќ§Р!Ќ§Р!Ќ§Р!Ќ§Р!Ќ§Р!Ќ§Р!Ќ§Р!Ќ§Р!Ќ§Р!Ќ§Р!Ќ§Р!Ќ§Р!Ќ§Р!Ќ§Р!ЌЅ§Д Н О kl­ЎЃЅ§Р!Ќ§Р!Ќ§ Р!Ќ§Р!Ќ§Р!Ќ§Р!Ќ§Р!Ќ§Р!Ќ 1hАа/ Ар=!А"А# $ %Аœ@@ёџ@ NormalCJ_HaJmH sH tH DAђџЁD Default Paragraph FontVi@ѓџГV  Table Normal :V і4ж4ж laі (k@єџС(No List Ѕџџџџ џџ z™ џџ z™lЅA/BCWXwx‘КЛмнћќ,LMdez{ЪЫŸГДНОkl­ЎЃЇ˜0€€˜0€€˜0€€˜0€€˜0€€˜0€€˜0€€˜0€€˜0€€˜0€€ˆ˜0€€˜0€€ˆ˜0€€ €˜0€€˜0€€˜0€€˜0€€˜0€€˜0€€ €˜0€€˜0€€ €˜0€€˜0€€˜0€€ €˜0€€˜0€€ €˜0€€˜0€€ ˜0€€ €˜0€€˜0€€ €˜0€€˜0€€(˜0€€ €M90€M90€M90€Ѕ Д Ѕ Ѕ џџ $jзьS#%jзlќ&jзЌќ'jзьќ(jз,ќ)jзlќ*jз„ќ+jзДќ,jзфњ-jзМњ.jзЄњLLPcciq€€„Ї  OUUhpvvƒ‰‰Ї  8*€urn:schemas-microsoft-com:office:smarttags€date€=*€urn:schemas-microsoft-com:office:smarttags €PlaceType€= *€urn:schemas-microsoft-com:office:smarttags €PlaceName€9 *€urn:schemas-microsoft-com:office:smarttags€place€ €15€2006€3€Day€Month€Year  ІЌВЙдл@AYcќ/2fiЇ,KuzHXЇ::ќ0KЇ@AЇџџTodd Landon BoswellTodd Landon BoswellTodd Landon BoswellTodd Landon BoswellTodd Landon BoswellTodd Landon BoswellTodd Landon BoswellTodd Landon BoswellTodd Landon BoswellMark McLaughlinхЬ{Œџ@€@@ˆб’33@@Ѕ@@џџUnknownџџџџџџџџџџџџG‡z €џTimes New Roman5€Symbol3& ‡z €џArial"qˆ№аh‚[ЕІ‚[ЕІJ[J[!№ ДД>4ЁЁˆ 3ƒ№мH(№џ?фџџџџџџџџџџџџџџџџџџџџџЬ{ŒџџAdrianne Schackart Todd BoswellOle џџџџџџџџџџџџ5OlePres000џџџџ,<ITEM000ODS џџџџITEM000FMTџџџџџџџџџџџџџџџџџџџџˆ;lXњ }”  №.ћœџ@Times New Roman-  2 Zу -ћ‹џМ@Times New Roman-- 2 пу , 2 п,у , 2 пXу ,-J2 п„*уUpper Nehalem Watershed Habitat AssessmentTAA44T4A:!4`u;'44.A3A[;@!&;'T--4..`4A' 2 пЩ у > 2 eу , 2 e,у , 2 eXу , 2 e„у , 2 eАу ,2 eм уStream ReportA'44;`T4A;4' 2 eУу > 2 ыу ?-&2 _уSTREAM: Ivy Creek8=C=HY40C!-,3 2 _qу  2 _„у - 2 ву -82 EуSUBBASIN: Upper Nehalem River8HBBH9 HH22,!H,3,,NC2,! 2 EЏу . 2 Иу -.2 +уDATES: March 15, 2006HH==8Y,!,2222232 2 +%у - 2 žу -G2 (уSURVEY CREW: Trevor Diemer, Ben Walczak8HCH=HCC=_=!,22!H,N,!B,2_,,-,3 2 Зу - 2 „у -;2 ї уREPORT PREPARED BY: Ben WalczakC=8HC=8C<8HC=HBHB,2_,,-,2 2 ї у . 2 jу -/2 нуGENE CONSERVATION GROUP:H=H=CHH8=CHH> IHHCHH8 2 нЕу ' 2 нму12 2 ну-!2 н/уNCHC 2 нКу - 2 Pу -2 УуUTM H=Y2 Уї уCOORDINATES:CHHCI HH==8 2 Уеу л2 УАуStart 8,! 2 У†у–2.2 УИу 0476697 E & 5080648 N 2222222=M2232222H 2 Ун у - 2 6у , 2 6,у , 2 6Xу , 2 6„у ,2 6АуEnd =22 2 6jу–2,2 6œу 0475950 E & 5081222 N2222222=M2232222H 2 6Ј у - 2 Љу -,2  уUSGS MAPS: BirkenfeldH8H8YH88B!2,2!,2 2  #у - 2  у -)2  уGENERAL DESCRIPTION:H=H=CI<H=8CD8>!HH 2  ‘у - 2 u у - 2 ш у ,…2 ш ,QуThe Ivy Creek winter habitat survey begins at its confluence with Rock Creek and =2, 40C!-,2H2,!2-2,'2!2-03-12',',22!2,2-,H2C2,2C",,2,22X2 [ 3уextends 875 meters. 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The channel is constrained by moderate hill222N,,!'=3,,2,23,',22'!,2,230N22,",,22 П… уslopes in a '22,'2,‘2 2Yуnarrow valley. The average valley width index is 1.7. Land use for the reach is timber e2,!!2H3,.0=2,,3,",2,2,.0H2222,3'22;,322',!2!3,!-,,2'N2,!”2 Ѕ[уharvest. The average unit gradient is 3.4%. The channel characteristics include: primary 2,!2,'=2,,2,"-1,221!,2,2'22S=2,-2,22,,2-!,,,!','2-22,2!N,#0k2 @у875m and secondary 70m. Zero pools were greater than 1 meter de222N,22',,222-#023N<-!2222'H,",1!--,!2,22N,,!3,&2 Ž уep. There was an ,2>2,!,I,',2=2 ‹!уaverage amount of LWD with twenty,2,!-2,,N2222!<_HH2H,20 2 ‹иу-!U2 ‹љ1уseven logs greater or equal to 12m x 0.6m, which e(,2,231'2!,,-!2!,23,222N322NH2,22 ўXуaverages to 3.1 key pieces per 100m. The vegetation is based on 4 riparian transects. ,2,!-2,'2222.02-,-'2,!222N=2,2-2,,22'2,',2222!2,!,2!,2',,'p2 qCуThe trees found most frequently in the riparian zone were mostly mi=2,!,,'!2222N2'!!-22,2022,!2-!,2-22,H,",N2'0N2 qЉ уxed sizes of 3,2',,'2!22 фуdeciduous ranging from 15 2,,2222'!,3131"!2N22 2 фQу–2\2 фƒ6у 30 cm dbh, with some mixed deciduous and conifers 30 22,N222H2'2N,N3,22,,2222',22,22!,!'22 2 фm у–2 2 фŸ у 2 W у50 cm dbh.22,N222 2 WПу - 2 Ъу -ћМ"System|$ф-NANI,N222 2 §Пу C- 2 pу C--NANI  -NANI  % 8{\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 (ArabITEM000FMT#3џџџџ РFрЌС”Чр С”ЧITEM000FMTRich Text Format8џџџџџџџџџџџџ<<Ole џџџџџџџџ OlePres000џџџџџџџџџџџџJА#3Rich Text Formatatˆ;lXp!„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{\ql \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 \rsid9206732\rsid16650192} \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\rsidroot9206732 \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 {\insrsid16650192 \par \tab \tab \tab }{\b\fs28\insrsid16650192 Upper Nehalem Watershed Habitat Assessment \par \tab \tab \tab \tab \tab Stream Report \par \par }{\insrsid16650192 STREAM: Ivy Creek\tab \par \par SUBBASIN: Upper Nehalem River \par \par DATES: March 15, 2006 \par \par SURVEY CREW: Trevor Diemer, Ben Walczak \par \par REPORT PREPARED BY: Ben Walczak \par \par GENE CONSERVATION GROUP:\tab 1-NC \par \par UTM }{\insrsid9206732 COORDINATES:\tab Start \endash 0476697 E & 5080648 N}{\insrsid16650192 \par }{\insrsid9206732 \tab \tab \tab \tab End \endash 0475950 E & 5081222 N}{\insrsid16650192 \par \par USGS MAPS: Birkenfeld \par \par GENERAL DESCRIPTION: \par \par \tab The Ivy Creek winter habitat survey begins at its confluence with Rock Creek and extends 875 meters. One reach was designated based on: Valley width and Channel morphology. Riffles (35%), rapids (32%), and scour pools (22%) dominated the habitat, while sand (15%), gravel (60%), and bedrock (13%) were the dominant substrate types. \par \par The survey begins at the confluence with Rock Creek and ends at a large step due to a lack of flow. A salmon spawning survey (26098.00 seg.1) is also located at the start. The stream runs through timberland. \par \tab \par REACH DESCRIPTIONS: \par \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid16650192 REACH 1: \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid16650192 \par \tab Length \endash 875 meters. The channel is constrained by moderate hill slopes in a narrow valley. The average valley width index is 1.7. Land use for the reach is timber harvest. The average unit gradient is 3.4%. The channel characteristics include: primary 875m and secondary 70m. Zero pools were greater than 1 meter d e ep. There was an average amount of LWD with twenty-seven logs greater or equal to 12m x 0.6m, which averages to 3.1 key pieces per 100m. The vegetation is based on 4 riparian transects. The trees found most frequently in the riparian zone were mostly m ixed sizes of deciduous ranging from 15 \endash 30 cm dbh, with some mixed deciduous and conifers 30 \endash 50 cm dbh. \par \par This survey begins in a timbered area. The habitat throughout the survey is average. The reach is characterized by gravel, sand, and bedrock domina ting the substrate. There are little pools with heavy fines and bedrock scattered throughout the survey. The riparian shade through this section of the stream is excellent. \par \par There is poor LWD project potential with little access for industrial equipment. The riparian area has excellent riparian shade throughout the entire reach but has recently been harvested creating fair riparian enhancement project potential. \par }}';'T..4..`4A' 2 tЯ у C? 2 њу C, 2 њ,у C, 2 њXу C, 2 њ„у C, 2 њАу C,2 њм уStream ReportA'44;`T4A;4' 2 њУу C? 2 €у C?-&2 уSTREAM: Ivy Creek8=C=HY2/C!,,2 2 kу C 2 „џџџџџџџџˆ;lXn З”&џџџџWordMicrosoft Word  ућМ"System &Šџџџџ”ЧЄ-ћœџ@Times New RomanFO р0-  2 у c-- 2 …у c, 2 …,у c, 2 …Xу c,ћ‹џМ@Times New RomanFO р0-J2 t„*уUpper Nehalem Watershed Habitat AssessmentTAA44T4A;!4`u;'44.A4A[;A!';'T..4..`4A' 2 tЯ у ? 2 њу , 2 њ,у , 2 њXу , 2 њ„у , 2 њАу ,2 њм уStream ReportA'44;`T4A;4' 2 њУу ? 2 €у ?-&2 уSTREAM: Ivy Creek8=C=HY2/C!,,2 2 kу  2 „у - 2 xу -82 ыуSUBBASIN: Upper Nehalem River8HBBH8HH22,!H,2,,NC2,! 2 ыЊу - 2 ^у -.2 буDATES: March 15, 2006HH==8Y,!,2222222 2 б$у - 2 Dу -G2 З(уSURVEY CREW: Trevor Diemer, Ben Walczak8HCH=HCC=_=!,22!H,N,!B,2_,,-,2 2 ЗЕу - 2 *у -;2  уREPORT PREPARED BY: Ben WalczakC=8HC=8C=8HC=HBHB,2_,,-,2 2 Ёу - 2 у -/2 ƒуGENE CONSERVATION GROUP:H=H=CHH8=CHH=HHHCHH8 2 ƒВу * 2 ƒму12 2 ƒу-!2 ƒ/уNCHC 2 ƒКу C- 2 іу C-2 iуUTM H=Y2 iї уCOORDINATES:CHHCHHH==8 2 iву Cо2 iАуStart 8,! 2 i†у–C2.2 iИу 0476697 N & 5080648 E :2222222HM2222222= 2 iм у C- 2 му C, 2 м,у C, 2 мXу C, 2 м„у C,2 мАуEnd =22 2 мjу–C2,2 мœу 0475950N & 5081222 E 2222222HM2222222= 2 мЇ у C- 2 Oу C-,2 ТуUSGS MAPS: BirkenfeldH8H8YH88B!2,2!,2 2 Т"у C- 2 5 у C-)2 Ј уGENERAL DESCRIPTION:H=H=CH;H=8CC8=HH 2 Ј ‹у C- 2  у C- 2 Ž у C,…2 Ž ,QуThe Ivy Creek winter habitat survey begins at its confluence with Rock Creek and m=2,2/C!,,2H2,!2,2,'2!2,/2,12',',22!2,2,,H2C2,2C!,,2,22X2  3уextends 875 meters. One reach was designated based,3,22'222N,,!'H2,!,,,2H,'2,'12,,22,',282  Xу on: Valley width and Channel 22H,,/H22,22C2,22,Ž2 t Wуmorphology. Riffles (35%), rapids (32%), and scour pools (22%) dominated the habitat, rN2!22221/C!!,'!22S!!,22'!22S!,22',22!222'!22S!22N2,,22,2,2,‰2 ч Tуwhile sand (15%), gravel (60%), and bedrock (13%) were the dominant substrate types.H2,',22!22S!1!,2,!22S!,222,2!2,2!22S!H,!,2,22N2,2'22'!,,/2,' 2 ч Ј у C- 2 Z у C-[2 Э 5уThe survey begins at the confluence with Rock Creek a=2,'2!2,/2,12',2,,22!2,2,,H2C2,2C!,,2,=2 Э !уnd ends at a large step due to a 22,22',,,!1,',222,2,”2 @ [уlack of flow. A salmon spawning survey (26098.00 seg.1) is also located at the start. The ,,22!!2HH',N22'2,H221'2!2,/!2222222',12!','22,,,2,2,',!=2,;2 Г уstream runs through timberland. '!,,N!22'2!2212N2,!,22 2 Г у C- 2 &у C, 2 &,у C-(2 ™уREACH DESCRIPTIONS::C=HCHH=8CC8=HH8 2 ™Fу C- 2 у C-2 уREACH 1:C=HCH2 2 Ку C- 2 ђу C- 2 eу C,2 e,уLength :;,212 2 e]у–C2a2 e9у 875 meters. The channel is constrained by moderate hill222N,,!'=2,,2,22,',22'!,2,22/N22,!,,22 e| уslopes in a '22,'2,‘2 иYуnarrow valley. The average valley width index is 1.7. Land use for the reach is timber R2,!!2H2,,/=2,,2,!,1,2,,/H2222,3'22;,222',!2!2,!,,,2'N2,!”2 K[уharvest. The average unit gradient is 3.4%. The channel characteristics include: primary 2,!2,'=2,,2,!,1,221!,2,2'22S=2,,2,22,,2,!,,,!','2,22,2!N,!/k2 О@у875m and secondary 70m. Zero pools were greater than 1 meter de222N,22',,222,!/22N<,!2222'H,!,1!,,,!2,22N,,!2,&2 Оƒ уep. There was an ,2=2,!,H,',2=2 1!уaverage amount of LWD with twenty,2,!,1,,N2222!;_HH2H,2/ 2 1бу-C!U2 1ђ1уseven logs greater or equal to 12m x 0.6m, which Q',2,221'1!,,,!2!,22,222N322NH2,22 ЄXуaverages to 3.1 key pieces per 100m. The vegetation is based on 4 riparian transects. ,2,!,1,'2222,/2,,,'2,!222N=2,2,1,,22'2,',2222!2,!,2!,2',,'p2 CуThe trees found most frequently in the riparian zone were mostly mi=2,!,,'!2222N2'!!,22,2/22,!2,!,2-22,H,!,N2'/N2 Ё уxed sizes of 3,2'-,'2!22 Šуdeciduous ranging from 15 2,,2222'!,2121!!2N22 2 ŠNу–C2\2 Š€6у 30 cm dbh, with some mixed deciduous and conifers 30 22,N222H2'2N,N3,22,,2222',22,22!,!'22 2 Šj у–C2 2 Šœ у C2 § у50 cm dbh.22,N222 2 §Пу C- 2 pу C--NANI