ࡱ>    >+ !"$%&'()*=-./0123456789:;?@ABCDEFGINJKLMOPQRSTUVWXYZ[\Root Entry uڕ ITEM000  F0xDwsڕ1Table#CompObjj՜.+,0 hp|   }A  Title  FMicrosoft Word Document MSWordDocWord.Document.89q%F\Object F4dMicrosoft Word DocumentD:\Youngs Bay final data\Stream reports\Lewis and Clark Tribs\Barrett Creek Report.docWordDocument"SummaryInformation( DocumentSummaryInformation8Oh+'0x   ( 4 @ LX`hpssAdrianne SchackartdriNormale Todd Boswellcka2ddMicrosoft Word 10.0@G@_D}@FA?ڕ@džڕD=5@ bjbj22 "XX         $p Rf) ) > = = =  =  = =   9Yڕ  T 0 (:( $( $L 6= B,n_) ) 3  Upper Nehalem Habitat Assessment Stream Report STREAM: Adams Creek Tributary A SUBBASIN: Upper Nehalem River DATES: February 8, 2006 SURVEY CREW: Todd Boswell, Mark McLaughlin REPORT PREPARED BY: Ben Walczak GENE CONSERVATION GROUP: 1-NC UTM COORDINATES: Start 0477550 E & 5095150 N End 0478005 E & 5095475 N USGS MAPS: Birkenfeld GENERAL DESCRIPTION: The Adams Creek Tributary A winter habitat survey begins at its confluence with Adams Creek and extends 335 meters. One reach was designated based on: Valley form. Riffles (90%) dominated the habitat, while Sand (28%), Gravel (43%), and Bedrock (25%) were the dominant substrate types. This short survey has some nice spawning habitat near the confluence with Adams Creek. The gravel diminishes as beavers dominate the upper half with old beaver dams observed near the end of the survey. REACH DESCRIPTIONS: REACH 1: Length 314 meters. The channel is constrained by terraces in a broad valley. The average valley width index is 6.0. Land use for the reach is second growth timber. The average unit gradient is 0.3%. The channel characteristics include: primary 314m and secondary 21m. One pool was greater than 1 meter deep, which averages to 3.2 pools per kilometer of primary channel length. There was little LWD with two logs greater or equal to 12m x .6m, which averages to 0.6 key pieces per 100m of primary channel. 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 15 30 cm dbh, with some deciduous 30 50 cm dbh. This survey begins at the confluence with Adams Creek. There is good gravel at the start of this small stream. No LWD or pools were observed. Beaver activity is present throughout the second half of the survey. The survey ends at a beaver dam with green water and a large amount of rough skinned newts. The stream has good LWD project potential near the start if it is coordinated with a large project on Adams Creek. The riparian has a good mix of conifer with good future LWD recruitment. So, a planting project is not necessary. 9 s hxHhsh5CJ\h%89[\{|  5 V W n o s t !!!!!!!!!!!!!!!!!!!!!!!!!!!!! de!! !!!!!!! 1h/ =!"#$%@@@ NormalCJ_HaJmH sH tH DA@D Default Paragraph FontVi@V  Table Normal :V 44 la (k@(No List H@H xH Balloon TextCJOJQJ^JaJ!z ze2%89[\{|5VWnostde000p000000 0000 00000 0 00 000 0p0 00 0 00 00000p0p0p    p p ppp^#ggmultzz8*urn:schemas-microsoft-com:office:smarttagsdate=*urn:schemas-microsoft-com:office:smarttags PlaceType=*urn:schemas-microsoft-com:office:smarttags PlaceName9*urn:schemas-microsoft-com:office:smarttagsplace 220068DayMonthYearcm:*\|V~Todd Landon BoswellTodd Landon BoswellTodd Landon BoswellTodd Landon BoswellTodd Landon BoswellTodd Landon BoswellTodd Landon BoswellTodd Landon BoswellTodd Landon BoswellMark McLaughlinsxH@MMӒ!!MM`@UnknownGz Times New Roman5Symbol3& z Arial5& zaTahoma"qh-m/mD=D=!24d}}3H(?Adrianne Schackart Todd BoswellOle 5OlePres000,ITEM000ODS ITEM000FMT;lX D  ."Systemr0E -@Times New Roman-  2 Z N-- 2  N, 2 , N, 2 X N,@Times New Roman-;2  Upper Nehalem Habitat AssessmentTAA44T4A:!4`[;A!&;'T.-4-.`4A' 2  N? 2 e N, 2 e, N, 2 eX N, 2 e N, 2 e N,2 e Stream ReportA'44;`T4A;4' 2 e N> 2  N?-;2 _ STREAM: Adams Creek Tributary A8=C=HYH2,N'C!,-2=!22,#0I 2 _ N  2 _ N- 2  N-82 ESUBBASIN: Upper Nehalem River8HBBH9 HH22,!H,3,,NC2,! 2 E N. 2  N-12 +DATES: February 8, 2006RHH==87,2!3,#022322 2 +W N- 2  N-L2 +SURVEY CREW: Todd Boswell, Mark McLaughlin 8HCH=HCC=_=221B2'H,Y,!2Z-<,3222 2 ^ N- 2  N-;2  REPORT PREPARED BY: Ben WalczakC=8HC=8C<8HC=HBHB,2_,,-,2 2  N. 2 j N-/2 GENE CONSERVATION GROUP:H=H=CHH8=CHH> IHHCHH8 2  N' 2 1N2 2 -N!2 /NCHC 2  N- 2 P N-#2 UTM COORDINATES:H=YCHHCI HH==8 2  N2 Start 8,! 2 N2.2  0477550 E & 5095150 N 2222222=M2232222H 2   N- 2 6 N, 2 6, N, 2 6X N, 2 6 N,2 6End =22 2 6jN2.2 6 0478005 E & 5095475 N 2222222=M2232222H 2 6  N- 2  N-,2  USGS MAPS: BirkenfeldH8H8YH88B!2,2!,2 2  # N- 2  N-)2  GENERAL DESCRIPTION:H=H=CI<H=8CD8>!HH 2   N- 2 u  N- 2  N,2 ,PThe Adams Creek Tributary A winter habitat survey begins at its confluence with =2,H2,N'C!-,2=!22,#0HH2,!3,2,'2!3-03-12',',22!2,2-,H2J2 [ *Adams Creek and extends 335 meters. One rH2,N'C!,,2,22,3,22'222N,,!'H2,"M2 [ ,each was designated based on: Valley form. ,-,2H,'2,'12,,23,',222H,.0!2!N2 QRiffles (90%) dominated the habitat, while Sand (28%), Gravel (43%), and Bedrock rC!!,'!22S!22N2,,22,2,2,H2,8,22"22S!H",2,!22T!,23B,2!3,2G2 A ((25%) were the dominant substrate types.!22S!I,!,2,22N2,2'22'!,,03,' 2 A | N. 2  N-2 ' XThis short survey has some nice spawning habitat near the confluence with Adams Creek. =2''22!'2!2-03,''3N,2,,'2,H2312,2,2,,!2,,22!2,3,,H3H2,N'C!,,2 2 TN=2 =Vhe gravel diminishes as beavers dominate the upper half with old beaver dams observed 2,2!,3,2N2'2,','2,,2,!'22N2,,2,232,!2,!H2222-,2,!2,N'22',!2,252 near the end of the survey. 2,,!2,,222!2,'2!3-0 2 = N. 2  N-(2 REACH DESCRIPTIONS::C=HCHH=8CD8> HI8 2 J N, 2 f N-2 REACH 1:C=HCH2 2  N- 2 L N- 2  N,2 ,Length :<,312 2 _N2y2 I 314 meters. The channel is constrained by terraces in a broad valley. e222N,,!'=3,,2,23,',22'!,2,230,"!-,,'2,2!3,22,-042 2The average valley width in =2,,2-!-1,3,.0H232h2 2]>dex is 6.0. Land use for the reach is second growth timber. 2,3'22;,222(,"2!2,!-,,2'',,2222"2H2N2,!2 VThe average unit gradient is 0.3%. The channel characteristics include: primary 314m =2,,2-!-1,221",2,3'22S=2,,2,22,-2,!,,,!','2,22,2!N,"0222N2 Rand secondary 21m. One pool was greater than 1 meter deep, which averages to 3.2 ,22',,222-#022NH2-222H,'2!,,,!2,22N,,!2,,2H2,2,3,!-1,'22222 pools per kilometer of pri222'2,!22N,,!2!2!a2 9mary channel length. There was little LWD with two logs eN,"0,2,23,,312=3,!,I,',;_HH2H221'2 Tgreater or equal to 12m x .6m, which averages to 0.6 key pieces per 100m of primary 1",,-!2!,23,222N22NH2,2,2,"-1,'2222-02,,,'3,!222N2!2!N,#02 q\channel. The vegetation is based on 2 riparian transects. The trees found most frequently ,2,22,=2,3-1,,22'2,',2222!2,!,2"-2',,'=2,!-,'!2222N2'!!,22,20.2 in the riparian zone we22,!2,!,2-22,H-X2 3re mostly mixed sizes of deciduous ranging from 15 !,N2'/N3,2'-,'2!2,,2222'!,3131!!2N22 2  N22   30 cm dbh, 22,N222.2 Wwith some deciduous 30 H2'2N,2,,2222'22 2 WN22 W  50 cm dbh.22,N222 2 W N- 2  N--NANIith a large project on Adams Creek. Beaver activity is present       $       #% ! !      -NANI $ k{\rtf1\ansi\ansicpg1252\uc1\deff0\stshfdbch0\stshfloch0\stshfhich0\stshfbi0\deflang1033\deflangfe1033{\fonttbl{\f0\froman\fcharset0\fprq2{\*\panose 02020603050405020304}Times New Roman;}{\f35\fswiss\fcharset0\fprq2{\*\panose 020b0604030504040204}Tahoma;} {\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 ITEM000FMT#3 F9Yڕ9YڕITEM000FMTRich Text Format8<oOle  OlePres000H#3Rich Text Formatat;lXp!Roman (Hebrew);}{\f42\froman\fcharset178\fprq2 Times New Roman (Arabic);}{\f43\froman\fcharset186\fprq2 Times New Roman Baltic;}{\f44\froman\fcharset163\fprq2 Times New Roman (Vietnamese);} {\f386\fswiss\fcharset238\fprq2 Tahoma CE;}{\f387\fswiss\fcharset204\fprq2 Tahoma Cyr;}{\f389\fswiss\fcharset161\fprq2 Tahoma Greek;}{\f390\fswiss\fcharset162\fprq2 Tahoma Tur;}{\f391\fswiss\fcharset177\fprq2 Tahoma (Hebrew);} {\f392\fswiss\fcharset178\fprq2 Tahoma (Arabic);}{\f393\fswiss\fcharset186\fprq2 Tahoma Baltic;}{\f394\fswiss\fcharset163\fprq2 Tahoma (Vietnamese);}{\f395\fswiss\fcharset222\fprq2 Tahoma (Thai);}}{\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;}{\s15\ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 \f35\fs16\lang1033\langfe1033\cgrid\langnp1033\langfenp1033 \sbasedon0 \snext15 \ssemihidden \styrsid9980024 Balloon Text;}}{\*\rsidtbl \rsid7544343\rsid8344474\rsid9980024\rsid10911724} \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\rsidroot10911724 \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 {\insrsid10911724 \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid10911724 \tab \tab \tab }{\b\fs28\insrsid10911724 Upper Nehalem Habitat Assessment \par \tab \tab \tab \tab \tab Stream Report \par \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid10911724 STREAM: Adams Creek Tributary A\tab \par \par SUBBASIN: Upper Nehalem River \par \par DATES: February 8, 2006 \par \par SURVEY CREW: Todd Boswell, Mark McLaughlin \par \par REPORT PREPARED BY: Ben Walczak \par \par GENE CONSERVATION GROUP:\tab 1-NC \par \par UTM COORDINATES:\tab Start \endash 0477550 E & 5095150 N \par \tab \tab \tab \tab End \endash 0478005 E & 5095475 N \par \par USGS MAPS: Birkenfeld \par \par GENERAL DESCRIPTION: \par \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid10911724 \tab The Adams Creek Tributary A winter habitat survey begins at its confluence with Adams Creek and extends 335 meters. One r each was designated based on: Valley form. Riffles (90%) dominated the habitat, while Sand (28%), Gravel (43%), and Bedrock (25%) were the dominant substrate types. \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid7544343 \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid7544343 This short survey has some nice spawning habitat near the confluence with Adams Creek. T he gravel diminishes as beavers dominate the upper ha;lX D  ."Systemr0E -@Times New Roman-  2 Z c-- 2  c, 2 , c, 2 X c,@Times New Roman-;2  Upper Nehalem Habitat AssessmentTAA44T4A:!4`[;Alf with old beaver dams observed near the end of the survey. \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid10911724 \par REACH DESCRIPTIONS: \par \par REACH 1: \par \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid10911724 \tab Length \endash 314 meters. The channel is constrained by terraces in a broad valley. The average valley width in dex is 6.0. Land use for the reach is second growth timber. The average unit gradient is 0.3%. The channel characteristics include: primary 314m and secondary 21m. One pool was greater than 1 meter deep, which averages to 3.2 pools per kilometer of pr i mary channel length. There was little LWD with two logs greater or equal to 12m x .6m, which averages to 0.6 key pieces per 100m of primary channel. The vegetation is based on 2 riparian transects. The trees found most frequently in the riparian zone w ere mostly mixed sizes of deciduous ranging from 15 \endash 30 cm dbh, with some deciduous 30 \endash 50 cm dbh. \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid10911724 \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid10911724 This survey begins at the confluence with Adams Creek. There is good gravel at the start of this small stream. No LWD or pools were observed. Beaver acti vity is present throughout the second half of the survey. The survey ends at a beaver dam with green water and a large amount of rough skinned newts. \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid9980024 \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid10911724 The stream has good LWD project potential near the start if it is coordinated with a large project on Ada ms Creek. The riparian has a good mix of conifer with good future LWD recruitment. So, a planting project is not necessary. \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid10911724 \par }}r C 2 {r C#2 r UTM COORDINATES:$, !$$!$$# 2 r Cn2 Xr Start  2 r C2 r 0477550 2 r N & 500 $ & 2 >r 951502 r E 5  2 r C!&;'T.-4-.`4A' 2  c? 2 e c, 2 e, c, 2 eX c, 2 e c, 2 e c,2 e Stream ReportA'44;`T4A;4' 2 e c> 2  c?-;2 _ STREAM: Adams Creek Tributary A8=C=HYH2,N'C!,-2=!22,#0I 2 _ c  2 _ c- 2  c-82 ESUBBASIN: Upper Nehalem River8HBBH9 HH22,!H,3,,NC2,! 2 E c. 2  c-12 +DATES: February 8, 2006RHH==87,2!3,#022322 2 +W c- 2  c-L2 +SURVEY CREW: Todd Boswell, Mark McLaughlin 8HCH=HCC=_=221B2'H,Y,!2Z-<,3222 2 ^ c- 2  c-;2  REPORT PREPARED BY: Ben WalczakC=8HC=8C<8HC=HBHB,2_,,-,2 2  c. 2 j c-/2 GENE CONSERVATION GROUP:H=H=CHH8=CHH> IHHCHH8 2  c' 2 1c2 2 -c!2 /NCHC 2  c- 2 P c-#2 UTM COORDINATES:H=YCHHCI HH==8 2  c2 Start 8,! 2 c2.2  0477550 E & 5095150 N 2222222=M2232222H 2   c- 2 6 c, 2 6, c, 2 6X c, 2 6 c,2 6End =22 2 6jc2.2 6 0478005 E & 5095475 N 2222222=M2232222H 2 6  c- 2  c-,2  USGS MAPS: BirkenfeldH8H8YH88B!2,2!,2 2  # c- 2  c-)2  GENERAL DESCRIPTION:H=H=CI<H=8CD8>!HH 2   c- 2 u  c- 2  c,2 ,PThe Adams Creek Tributary A winter habitat survey begins at its confluence with =2,H2,N'C!-,2=!22,#0HH2,!3,2,'2!3-03-12',',22!2,2-,H2J2 [ *Adams Creek and extends 335 meters. One rH2,N'C!,,2,22,3,22'222N,,!'H2,"M2 [ ,each was designated based on: Valley form. ,-,2H,'2,'12,,23,',222H,.0!2!N2 QRiffles (90%) dominated the habitat, while Sand (28%), Gravel (43%), and Bedrock rC!!,'!22S!22N2,,22,2,2,H2,8,22"22S!H",2,!22T!,23B,2!3,2G2 A ((25%) were the dominant substrate types.!22S!I,!,2,22N2,2'22'!,,03,' 2 A | c. 2  c-2 ' XThis short survey has some nice spawning habitat near the confluence with Adams Creek. =2''22!'2!2-03,''3N,2,,'2,H2312,2,2,,!2,,22!2,3,,H3H2,N'C!,,2 2 Tc=2 =Vhe gravel diminishes as beavers dominate the upper half with old beaver dams observed 2,2!,3,2N2'2,','2,,2,!'22N2,,2,232,!2,!H2222-,2,!2,N'22',!2,252 near the end of the survey. 2,,!2,,222!2,'2!3-0 2 = c. 2  c-(2 REACH DESCRIPTIONS::C=HCHH=8CD8> HI8 2 J c, 2 f c-2 REACH 1:C=HCH2 2  c- 2 L c- 2  c,2 ,Length :<,312 2 _c2y2 I 314 meters. The channel is constrained by terraces in a broad valley. e222N,,!'=3,,2,23,',22'!,2,230,"!-,,'2,2!3,22,-042 2The average valley width in =2,,2-!-1,3,.0H232h2 2]>dex is 6.0. Land use for the reach is second growth timber. 2,3'22;,222(,"2!2,!-,,2'',,2222"2H2N2,!2 VThe average unit gradient is 0.3%. The channel characteristics include: primary 314m =2,,2-!-1,221",2,3'22S=2,,2,22,-2,!,,,!','2,22,2!N,"0222N2 Rand secondary 21m. One pool was greater than 1 meter deep, which averages to 3.2 ,22',,222-#022NH2-222H,'2!,,,!2,22N,,!2,,2H2,2,3,!-1,'22222 pools per kilometer of pri222'2,!22N,,!2!2!a2 9mary channel length. There was little LWD with two logs eN,"0,2,23,,312=3,!,I,',;_HH2H221'2 Tgreater or equal to 12m x .6m, which averages to 0.6 key pieces per 100m of primary 1",,-!2!,23,222N22NH2,2,2,"-1,'2222-02,,,'3,!222N2!2!N,#02 q\channel. The vegetation is based on 2 riparian transects. The trees found most frequently ,2,22,=2,3-1,,22'2,',2222!2,!,2"-2',,'=2,!-,'!2222N2'!!,22,20.2 in the riparian zone we22,!2,!,2-22,H-X2 3re mostly mixed sizes of deciduous ranging from 15 !,N2'/N3,2'-,'2!2,,2222'!,3131!!2N22 2  c22   30 cm dbh, 22,N222.2 Wwith some deciduous 30 H2'2N,2,,2222'22 2 Wc22 W  50 cm dbh.22,N222 2 W c- 2  c--NANI