ࡱ>    >+ !"#$%'()*G=-./0123456789:;?@ABCDEFHKIJPLNOTQRSUVWXYZ[\]^_`Root Entry 䰼 ITEM000  F0xD䰼1Table&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+'0h   $ 0 <HPX`ssBenenNormal Todd Boswello2ddMicrosoft Word 10.0@@_D}@ C@ C 5@ bjbj22 " XX6666666JJJJ Vl vvvvvvvv  $" Rt H 6vv 66vv& )))6v6v ) )) 66 vj dJ < 0l " J$n6666 6 v0")vvv  JJ Upper Nehalem Watershed Habitat Assessment Stream Report STREAM: Unnamed Trib (Above Step Creek) SUBBASIN: Upper Nehalem River DATES: April 17, 2006 SURVEY CREW: Todd Boswell, Mark McLaughlin REPORT PREPARED BY: Ben Walczak GENE CONSERVATION GROUP: 1-NC UTM COORDINATES: Start 0473220 E & 5061290 N End 0472820 E & 5060875 N USGS MAPS: Timber GENERAL DESCRIPTION: The Unnamed Tributary (above Step Creek on the Left) winter habitat survey begins at its confluence with the Nehalem River and extends 646 meters. One reach was designated based on: Valley form. In the reach Riffles (35%) and Rapids (60%) dominated the habitat, while Sand (15%), Gravel (41%), and Cobble (41%) were the dominant substrate types. The survey begins at the confluence with the Nehalem River. An ODFW Spawning Survey sign was not noted. REACH DESCRIPTIONS: REACH 1: Length 646 meters. The channel is constrained by terraces in a broad valley. The average valley width index is 3.0. Land use for the reach is large timber. The average unit gradient is 5.4%. The channel characteristics include: primary 646m and secondary 88m. One pools was greater than 1 meter deep, which averages to 1.5 pools per kilometer of primary stream channel. There were six key pieces of LWD, which averages to 0.9 pieces per 100m. The vegetation is based on 2 riparian transects. The trees found most frequently in the riparian zone were mostly deciduous ranging from 3 15 cm dbh, with some deciduous 30 50 cm dbh. Conifers 30-50 cm dbh were also present. This survey begins at the confluence with the Nehalem River. There is a potential natural barrier above the start point with a 0.8m high step over log and no jump pool. The stream alternates between areas with not much spawning habitat to pockets of good spawning gravel. A couple of secondary channels were observed, but they lacked pools. In the first part of the reach, alders and vinemaple along the stream banks dominate the riparian, although there were some conifers on the hillslopes. Also, in the first half of the survey the stream passes under an ODF foot/horse bridge where there is a drinking trough for horses next to the creek, and a water diversion above the bridge for the trough. Above the bridge crossing, the stream appears to leave the Tillamook State forest and enter private industrial forestland, where the riparian becomes quite brushy with lots of salmonberry, vinemaple, and devils club along with smaller alders. There is a small seep on the right about halfway through the reach, which does have potential for alcove development. Above the seep, there is an old road crossing that is now used as an ATV crossing, which crosses the stream. The riparian improves above this crossing, with some larger conifers that are present closer to the stream, although vinemaple is still readily present. Not far from the end of the reach, there is another old road crossing, just below a small tributary junction on the left. There is an old decommissioned spur road, which follows the stream on the right. The survey ended at another tributary junction, this one on the right, due to an increase in gradient and a lack of spawning habitat or pools. There is good LWD project potential, but only fair access for industrial equipment. The access could be improved if a nearby horse trail could be used, which crosses the stream about 300m from the confluence with the Nehalem. The riparian has a nice mix of alders and conifers. Therefore, a planting project is not necessary. Cyh@hln5CJ\hln/BCmn  E f g z { Y [ o p !!!!!!!!!!!!!!!!!!!!!!!!!!!!!p y z '(!! !!!! !!! 1h/ =!"#$%>_`stRThi@@@ NormalCJ_HaJmH sH tH DAD Default Paragraph FontVi@V  Table Normal :V 44 la (k@(No List   z z(/BCmnEfgz{Y[opyz'( 00000000000 00000 0 00 000 00 00 0 00 00 0 00 0p00p0 p  Ai&Bi&Ci&LU#% % / . 4 4 =*urn:schemas-microsoft-com:office:smarttags PlaceType=*urn:schemas-microsoft-com:office:smarttags PlaceName9*urn:schemas-microsoft-com:office:smarttagsplace nn Todd Landon BoswellTodd Landon BoswellTodd Landon BoswellTodd Landon BoswellTodd Landon BoswellTodd Landon BoswellTodd Landon BoswellTodd Landon BoswellTodd Landon BoswellMark McLaughlinln@@ӒffOle 5OlePres000,ITEM000ODS ITEM000FMT;lX\ .  ."System8$r0E -@Times New Roman-  2 Z -- 2  , 2 , , 2 X ,@Times New Roman-J2 *Upper Nehalem Watershed Habitat AssessmentTAA44T4A:!4`u;'44.A3A[;@!&;'T--4..`4A' 2  > 2 e , 2 e, , 2 eX , 2 e , 2 e ,2 e Stream ReportA'44;`T4A;4' 2 e > 2  ?-G2 _(STREAM: Unnamed Trib (Above Step Creek)8=C=HYH22,N,2=!2!H222,8,2C!-,2" 2 _f 2 _4 - 2  -2 E SUBBASIN: 8HBBH9 H2 E<Upper H22,!2 EO Nehalem RiverH,3,,NC2,! 2 E . 2  -.2 +DATES: April 17, 2006HH==8H2!222222 2 + - 2  -L2 +SURVEY CREW: Todd Boswell, Mark McLaughlin8HCH=HCC=_=221B2'H,Y,!2Z-<,3222 2 ^ - 2  -;2  REPORT PREPARED BY: Ben WalczakC=8HC=8C<8HC=HBHB,2_,,-,2 2  . 2 j -2  GENE CONSEH=H=CHH8= 2 kRVATION GROUP:CHH> IHHCHH8 2  ' 2 12 2 -!2 /NCHC 2  - 2 P -#2 UTM COORDINATES:H=YCHHCI HH==8 2  2 Start 8,! 2 2.2  0473220 E & 5061290 N 2222222=M2232222H 2   - 2 6 , 2 6, , 2 6X , 2 6 ,2 6End =22 2 6j2.2 6 0472820 E & 5060875 N 2222222=M2232222H 2 6  - 2  -&2  USGS MAPS: TimberH8H8YH88=N2,! 2   , 2  -)2  GENERAL DESCRIPTION:H=H=CI<H=8CD8>!HH 2   - 2 u  - 2  ,|2 ,KThe Unnamed Tributary (above Step Creek on the Left) winter habitat survey =2,H22,N,2>!22,#0!,222,8,2C!-,2222-;-!!H2,!3,2,'2!3-0@2 [ #begins at its confluence with the N2,12',',22!3,2,,H22,HX2 [ l3ehalem River and extends 646 meters. One reach was ,2,,NC2,!,22,3,22'222N,,!'H2,!-,,2I,'2 Odesignated based on: Valley form. In the reach Riffles (35%) and Rapids (60%) 2,'12,,22,',222I,-0!3!N 22,",-,2C!!,'!22T!,22C,22'"22S!2 A Qdominated the habitat, while Sand (15%), Gravel (41%), and Cobble (41%) were the 22N2,,22,2,2,I2,8,22!22S!H",2,!22S!,22C222,!22T!H,",2,12 dominant substrate types.W22N2,2'22'!,,02,' 2  - 2 '  -&2 The survey begins =2,'2!2.02-12'e2 <at the confluence with the Nehalem River. An ODFW Spawning ,2,,22!2,2-,H22,H,3,,NC2,!H2HI7_82,H22152 Survey sign was not noted. 82!2-0'12I,'2222-2 2 k - 2  , 2 , -(2 REACH DESCRIPTIONS::C=HCHH=8CD8> HI8 2 J , 2 f -2 REACH 1:C=HCH2 2  - 2 L - 2  ,2 ,Length :<,312 2 _2y2 I 646 meters. The channel is constrained by terraces in a broad valley. (222N,,!'=3,,2,23,',22'!,2,230,"!-,,'2,2!3,22,-0Y2 24The average valley width index is 3.0. Land use for=2,,2-!-1,3,.0H2322,3'22;,222(,"2!=2 2#! the reach is large timber. The 2,!-,,2',"2,N2,!=2,2 Vaverage unit gradient is 5.4%. The channel characteristics include: primary 646m and ,2,!-2,222!,2,2'32S=2,,3,22,,3,!--,!','2,22,2!N,#1222N,222 Usecondary 88m. One pools was greater than 1 meter deep, which averages to 1.5 pools ',,222,#022NH3,232'H,'2!,,-!2,22N-,!2,,2H2,2,2-!-2,'222222'Y2 4per kilometer of primary stream channel. There were2,!22N,,!2!3!N,#0'!,,N,2,23,=2,",I,!,82 \ six key pieces of LWD, which '32-02-,,'2!<`HH2,22 Xaverages to 0.9 pieces per 100m. The vegetation is based on 2 riparian transects. The ,2,!-2,'2222,-,'2-!222N=2,2-1,,22'2,',2222!2,!,2!,3',,'=2,2 qVtrees found most frequently in the riparian zone were mostly deciduous ranging from 3 !,,'!2222N2'!",22,3022,!2,!,2-22,I,!,N2'03,,2222'",3131!!2N2 2 q 2 2 q  >2 "15 cm dbh, with some deciduous 30 22,N222H2'2N,2,,2222'22 2 2"2  50 cm dbh. Co22,N222C22 k nifers 30h2!,!'22 2  -!)2  50 cm dbh were also 22,N222H,!,,'22 Wpresent.2!,',2 2 W9 . 2  --NANI 0--NANI,! 2  C- 2 p C--NANI=2,2,1,,22'2,',2222!2,!,2!,2',,'=2,!,,'!2222-NANI'=2,!,,{\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#3 F>d>dITEM000FMTRich Text Format8<Ole  OlePres000M#3Rich Text Formatat;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 \rsid2163345\rsid7236816\rsid12140671} \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\rsidroot7236816 \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 {\insrsid7236816 \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid7236816 \tab \tab \tab }{\b\fs28\insrsid7236816 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 {\insrsid7236816 STREAM: Unnamed Trib (Above Step Creek)\tab \par \par SUBBASIN: }{\insrsid12140671 Upper }{\insrsid7236816 Nehalem River \par \par DATES: April 17, 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 0473220 E & 5061290 N \par \tab \tab \tab \tab End \endash 0472820 E & 5060875 N \par \par USGS MAPS: Timber \par \par GENERAL DESCRIPTION: \par \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid7236816 \tab The Unnamed Tributary (above Step Creek on the Left) winter habitat survey begins at its confluence with the Nehalem River and extends 646 meters. One reach was designated based on: Valley form. In the reach Riffles (35%) and Rapids (60%) dominated the habitat, while Sand (15%), Gravel (41%), and Cobble (41%) were the dominant substrate types. \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid7236816 \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid7236816 The survey begins at the confluence with the Nehalem River. An ODFW Spawning Survey sign was not noted. \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid7236816 \tab \par REACH DESCRIPTIONP@UnknownGz Times New Roman5Symbol3& z Arial"hGkGk  !S: \par \par REACH 1: \par \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid7236816 \tab Length \endash 646 meters. The channel is constrained by terraces in a broad valley. The average valley width index is 3.0. Land use for the r each is large timber. The average unit gradient is 5.4%. The channel characteristics include: primary 646m and secondary 88m. One pools was greater than 1 meter deep, which averages to 1.5 pools per kilometer of primary stream channel. There were six key pieces of LWD, which averages to 0.9 pieces per 100m. The vegetation is based on 2 riparian transects. The trees found most frequently in the riparian zone were mostly deciduous ranging from 3 \endash 15 cm dbh, with some deciduous 30 \endash 50 cm dbh. Conifers 30-50 cm dbh were also present. \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid7236816 \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid7236816 This survey begins at the confluence with the Nehalem River. There is a potential natural barrier above the start point with a 0.8m high step over log and no jump pool. The stream alternates between areas with not much s pawning habitat to pockets of good spawning gravel. A couple of secondary channels were observed, but they lacked pools. In the first part of the reach, alders and vinemaple along the stream banks dominate the riparian, although there were some cor4d 3H(?lnBen Todd Boswell;lX\ .  ."Systemr0E -@Times New Roman-  2 Z -- 2  , 2 , , 2 X ,@Times New Roman-J2 *Upper Nehalem Watershed Habitat AssessmentTAA44T4A:!4`u;'44.A3A[;@!&;'T--4..`4A' 2  > 2 e , 2 e, , 2 eX , 2 e , 2 e ,2 e Stream ReportA'44;`T4A;4' 2 e > 2  ?-G2 _(STREAM: Unnamed Trib (Above Step Creek)8=C=HYH22,N,2=!2!H222,8,2C!-,2" 2 _f 2 _4 - 2  -2 E SUBBASIN: 8HBBH9 H2 E<Upper H22,!2 EO Nehalem RiverH,3,,NC2,! 2 E . 2  -.2 +DATES: April 17, 2006 HH==8H2!222222 2 + - 2  -L2 +SURVEY CREW: Toddnifers on the hillslopes. Also, in the first half of the survey the stream passes under an ODF foot/horse bridge where there is a drinking trough for horses next to the creek, and a water diversion above the bridge for the trough. \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid7236816 \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid7236816 Above the bridge crossing, t he stream appears to leave the Tillamook State forest and enter private industrial forestland, where the riparian becomes quite brushy with lots of salmonberry, vinemaple, and devils club along with smaller alders. There is a small seep on the right abou t halfway through the reach, which does have potential for alcove development. Above the seep, there is an old road crossing that is now used as an ATV crossing, which crosses the stream. The riparian improves above this crossing, with some larger conife r s that are present closer to the stream, although vinemaple is still readily present. Not far from the end of the reach, there is another old road crossing, just below a small tributary junction on the left. There is an old decommissioned spur road, whi ch follows the stream on the right. The survey ended at another tributary junction, this one on the right, due to an increase in gradient and a lack of spawning habitat or pools. \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid7236816 \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid7236816 There is good LWD project potential, but only fair access for industrial equ ipment. The access could be improved if a nearby horse trail could be used, which crosses the stream about 300m from the confluence with the Nehalem. The riparian has a nice mix of alders and conifers. Therefore, a planting project is not necessary. } }=CHH=HHHCHH8 2  0* 2  Boswell, Mark McLaughlins8HCH=HCC=_=221B2'H,Y,!2Z-<,3222 2 ^ - 2  -;2  REPORT PREPARED BY: Ben WalczakC=8HC=8C<8HC=HBHB,2_,,-,2 2  . 2 j -#2 GENE CONSERVATIOH=H=CHH8=CHH> I2 N GROUP:HHCHH8 2  ' 2 12 2 -!2 /NCHC 2  - 2 P -#2 UTM COORDINATES:H=YCHHCI HH==8 2  2 Start 8,! 2 2.2  0473220 E & 5061290 N 2222222=M2232222H 2   - 2 6 , 2 6, , 2 6X , 2 6 ,2 6End =22 2 6j2.2 6 0472820 E & 5060875 N 2222222=M2232222H 2 6  - 2  -&2  USGS MAPS: TimberH8H8YH88=N2,! 2   , 2  -)2  GENERAL DESCRIPTION:H=H=CI<H=8CD8>!HH 2   - 2 u  - 2  ,|2 ,KThe Unnamed Tributary (above Step Creek on the Left) winter habitat survey 0=2,H22,N,2>!22,#0!,222,8,2C!-,2222-;-!!H2,!3,2,'2!3-0I2 [ )begins at its confluence with the Nehalemi2,12',',22!3,2,,H22,H,2,,NO2 [ - River and extends 646 meters. One reach was C2,!,22,3,22'222N,,!'H2,!-,,2I,'2 Odesignated based on: Valley form. In the reach Riffles (35%) and Rapids (60%) 2,'12,,22,',222I,-0!3!N 22,",-,2C!!,'!22T!,22C,22'"22S!2 A Qdominated the habitat, while Sand (15%), Gravel (41%), and Cobble (41%) were the o22N2,,22,2,2,I2,8,22!22S!H",2,!22S!,22C222,!22T!H,",2,12 dominant substrate types.W22N2,2'22'!,,02,' 2  - 2 '  -/2 The survey begins at the=2,'2!2.02-12',2,\2 6 confluence with the Nehalem River. An ODFW Spawning ,22!2,2-,H22,H,3,,NC2,!H2HI7_82,H22152 Survey sign was not noted. 82!2-0'12I,'2222-2 2 k - 2  , 2 , -(2 REACH DESCRIPTIONS:tC=HCHH=8CD8> HI8 2 J , 2 f -2 REACH 1:C=HCH2 2  - 2 L - 2  ,2 ,Length :<,312 2 _2y2 I 646 meters. The channel is constrained by terraces in a broad valley. (222N,,!'=3,,2,23,',22'!,2,230,"!-,,'2,2!3,22,-0b2 2:The average valley width index is 3.0. Land use for the r=2,,2-!-1,3,.0H2322,3'22;,222(,"2!2,!42 2each is large timber. The -,,2',"2,N2,!=2,2 Vaverage unit gradient is 5.4%. The channel characteristics include: primary 646m and ,2,!-2,222!,2,2'32S=2,,3,22,,3,!--,!','2,22,2!N,#1222N,222 Usecondary 88m. One pools was greater than 1 meter deep, which averages to 1.5 pools ',,222,#022NH3,232'H,'2!,,-!2,22N-,!2,,2H2,2,2-!-2,'222222'b2 :per kilometer of primary stream channel. There were six k2,!22N,,!2!3!N,#0'!,,N,2,23,=2,",I,!,'32/2 6 ey pieces of LWD, which -02-,,'2!<`HH2,22 Xaverages to 0.9 pieces per 100m. The vegetation is based on 2 riparian transects. The ,2,!-2,'2222,-,'2-!222N=2,2-1,,22'2,',2222!2,!,2!,3',,'=2,2 qVtrees found most frequently in the riparian zone were mostly deciduous ranging from 3 !,,'!2222N2'!",22,3022,!2,!,2-22,I,!,N2'03,,2222'",3131!!2N2 2 q 2 2 q  >2 "15 cm dbh, with some deciduous 30 22,N222H2'2N,2,,2222'22 2 2+2  50 cm dbh. Conifersc22,N222C22!,!'2 N  3022 2  -!)2  50 cm dbh were also 22,N222H,!,,'22 Wpresent.2!,',2 2 W9 . 2  --NANI2,!2,!,2%2 zone were mostly r-22,H,!,N2'/.2  deciduous ranging from 2,,2222'!,2121!!2N 2 T 3s2 2   s 2  s2 2   s2 1522;2 d