Base Geography About the CLackamas River Watershed Figure 2 The watershed drains more than 940 square miles, or 600, 700 acres. For more than halfits length, CLackamas River elevation and key places the Clackamas River flows through forested areas over rugged terrain. The lower reaches flow through agricultural areas and then densely developed areas. Collawash River (57.0) 6000 Oak Grove Fork (53.0) Roaring River (44.0) Fish Creek (41 .7) The Clackamas begins on the slopes of 0/a/lie Butte, a High Cascade volcano. The river flows 82.7 miles from its headwaters (elevation 6,000 feet) to its confluence with the Wil/amette River near Gladstone and Oregon City (elevation I 2 feet). The river elevation profile shown in Figure 2 was created South Fork of the Clackamas River (34.6) 4000 using a GIS and spreadsheet software. More than 3, 700 points along the Clackamas River (approxi- North Fork Dam (31.1) Faraday Dam (26.2) mately every I 00 feet) were assigned an elevation. The resulting sequence ofpoints was then loaded River Mill Dam (23.3) into spreadsheet software and plotted. 2000 Eagle Creek (16.7) Deep Creek (12.1) Base MapO Clear Creek (8.0) The road data for federal lands in the upper water- This base map shows an oulHne ofthe Clackamas shed are more detailed than in the privately owned River watershed along with rivers, streams, roads and portions ofthe lower watershed. This occurs be- subwatershed boundaries. cause federal agencies have done more extensive 0 80 60 40 20 0 River Mile (from mouth of river) mapping and field-checking of roads (including gravel Figure 3 Rivers and streams: Five sources supphed river and roads) on their lands than anyone has done on stream information for different parts ofthe waterprivate land. The U.S. Census Bureau's road file, Road density shed, as shown on this base map: the U.S. Forest which covers privately owned lands, contains some Service (USFS), U.S. Bureau of Land Management (but not all) private roads. (BLM), U.S. Geoogica Survey (USGS), Cackamas County assessor and a GIS flow accumulation modeL Figure 3 shows road density, or miles of roads per S u bwate rshed Upper Clackamas River 3.2 square mile of land, for each subwatershed. Both Hot Springs Fork Collawash River 3.0 An Arc/nfo program caHed the flow accumulation paved roads and gravel USFS roads are included. Collawash River 2.3 model was used to locate probable" streams in Note that the Lower Clackamas subwatershed Oak Grove Fork Clackamas River 3.3 areas where the existing stream network lacked ( mostly urban) has 5.6 road miles per square mile, Fish Creek 3.4 detail. Using a digital model ofthe terrain, the while the Roaring River subwatershed (mostly Roaring River 07 program calculates the direction ofwater flow from forested) has only 0.7 road miles per square mile. South Fork Clackamas River 3.4 each point in the watershed, based on the elevations Other subwatersheds in the Mt. Hood National surrounding that point. The streams and streambeds Forest (such as Fish Creek, with 3.4 miles ofroad per Middle Clackamas River 3.3 North Fork Clackamas River 3.1 resulting from this process were used to supplement square mile) show comparable road density with existing stream information. that in urban watersheds, likely because of the Note: On severa/ maps /n th/s at/as we have used extensive road data kept by the USFS. Eagle Creek 3.1 Goose Creek 4.2 Deep Creek 3.6 Richardson Creek stream and river informatian provided by the Oregon Note: Road density data were produced in I 988- 1 996 Department ofFish and Wildlife. This information shows 5.0 Clear Creek 3.9 and may not reflect current conditions. For example, only major streams and rivers and was used in situa- Rock Creek 4.7 because the LISPS road data were produced in / 994, Lower Clackamas River tions where showing all streams would have c/uttered 5.6 they do not reflect /ogging roads that have since been the map. 0.0 1.0 2.0 3.0 4.0 abandoned or removed. New roads built since I 996 in Roads: Four sources provided information about roads in the watershed: the USFS, BLM, USGS and U.S. Census Bureau. urban areas are a/so not inc/uded. Miles of road per square mile of land 5.0 6.0 Subwatersheds: Sixteen subwaiiersheds are shown on the map. The USFS provided boundaries for USFS. In contrast, most ofthe lower watershed is the upper eight subwatersheds; Metro provided privately owned. The area in between the national five; and both agencies delineated portions of three forest and the lower watershed includes parcels of subwatersheds. The watershed boundaries are non- land owned by private timber companies and the standardized breakdowns and were delineated at the TabLe 3 Hierarchical classification for the Clackamas subbasin Hierarchy name Code Region Subregion Accounting unit (basin) 17 09 00 Cataloging unit (subbasin) U.S. Bureau of Land Management. discretion ofthe originating agency. Because watersheds are hierarchical (nested within each other),the system for numbering them is also hierarchical.As shown inTable 3, each level ofthe hierarchy is Also shown on the map are private land holdings Note: /n the past, each agency has delineated bound- II I in the Mt. Hood National Forest and managed by the within the Mt. Hood National Forest, including the BP ar/es for river basins, subbasins, watersheds and John Industrial Forest (North Fork Clackamas), PGE subwaters/ieds to meet their purposes, meaning that property (North Fork Clackamas) and Austin Hot one agency might divide the C/ackamas River watershed Springs (Upper Clackamas). assigned a two-digit number beginning with the largest unit, region.The hydrologic unit code (HUC) for the Clackamas watershed is I 70900 I I . Note: Although some agencies call the land draining to the Clackamas River a "subbasin," we call it a "watershed" for this project. into seven subwatersheds, while another agency might separate it into I 2 subwatersheds. The county parks that appear on the map are Barton ( east of Carver), Eagle Fern (northeast of Estacada) The Natural Resources Conservation Service Table 4 Figure 4 Ownership in the Clackamas River watershed Ownership in the and Metzler (southwest of Estacada). The state also (NRCS, formerly the Soil Conservation Service) and owns several small parcels in the watershed, the the U.S. Geological Survey are currently developing a largest ofwhich is Mclver Park, west of Estacada. Owner USFS Ctackamas River watershed Acres Pc rce nt 413,850 68,89 I 2,786 2. I 3 I 708 0.28 16,827 2.80 I 20,986 20.14 standard set ofwatershed boundaries that can be applied throughout the United States. These new boundaries may be different than those shown on this map. Eventually each small watershed within the Clackamas will be assigned a standard "hydrologic unit code" (seeTable 3) so that data gathered by one agency can be referenced by another for the same area. At the time ofthis printing, these boundaries Ownership information shown on the map is based BLM on a combination ofthe Clackamas County tax assessor data base, State Service Center for GIS Other Federal statewide ownership data and private forest land data from the BLM. It represents ownership at the time the data were collected and will change as Tribal F Private G property is bought and sold. PrivateTimber 30,597 5.09 3,987 0.66 had not yet been delineated or standardized. Other Public ELevation 0 Property Ownership ) Land ownership information forthe Clackamas River watershed is included early in the atlas because ownership patterns greatly affected how we gathered and displayed information about the watershed. This map shows elevations in the watershed based on data from a digital elevation model with shaded Ecoregions relief A digital elevation model, or DEM, is a grid- on several levels, from broad expanses of land (Level geologic classifications shown on this map, contact ecoregions) to more specific, smaller ecoregions the Oregon Department of Geology and Mineral I Ecoregions are large areas that have a similar type, based computer model ofthe terrain. DEMs are quality and quantity ofenvironmental resources (Level 4). derived from contour lines, which are commonly such as soils, topography and native vegetation. For Note: The sca/e ofthis geology map, 1:500,000, is very seen on USGS topographic maps. For the Clackamas example, much ofthe upper watershed is classified as As shown inTable 4 and Figure 4, more than 72 watershed, each grid cell covers I /4 acre. 25 percent is privately owned. The Clackamas River watershed can roughly be "Cascade Crest, Montane Forest," while parts of the The Clackamas watershed DEM contains approxi- central watershed are classified as Western Cas- The general geologic units found in the watershed an overview for the entire watershed. The USFS has mately 2.5 million grid cells, each representing the cades, Lowlands andValleys." Ecoregions can assist are shown on this map, based on the I 99 I Walker! gathered more detailed data about geology on its lands. average elevation ofthat 114 acre. In this case, the resource managers in seeing broad regional patterns. McLeod geology map of Oregon from the USGS. This information is avai/able in watershed analyses Briefdescriptions ofthe geologic units - such as specific to each subwatershed. shaded reliefsimulation ofthe terrain shows shadows The Level 4 ecoregion boundaries shown on this divided in half with nearly all ofthe upper watershed coarse, meaning that it cannot be used to determine Geology precise geo/ogic units in small areas, but does provide percent ofthe land in the Clackamas River watershed is publicly owned, about 3 percent is tribal and Industries orthe USGS. cast by a light source from the northwest. map were provided by the U.S. Environmental sedimentary rocks, basalt, or glacial deposits - are given in the map legend. To learn more about the Protection Agency. Scientists designate ecoregions I uIiiriiu a I II II S .I II I S S I II S II II II IS S iv ft ,' :kf4! hn4fi; 't'I 4I ., I.I . " 'Elt ;) -\ o k II T:; Deep Creek ClackarnasRiver k _ 'ftL IIvTEL5O3797 ---V; k - I Gops 7 Creek &\ *!I Base Map .. vr4a 4... Q . - 4.tr'- ..! R . . -rw- ,L- ,4- ' ,-,, .___ C!;3 ( . Fwoc - 1 &._ ; )_ \ S V , AlI- (( / ,, I ' ,,. 1b CfCk) fiL S S , -Ii. 1/ -)- J 4 -, S :;;( 11 S ::: (r\) Salmon fr. e:iii;; R O' . 6 . tk&iL; I' J HWY2I/ E .dlI Molalla . , ) %4\\. 'q jc> I 1; :- . S RbaringRiver iØ' ; - ( 1 1 FER/W 41N j' $ti\'Ir& V ,I if s4,J%''-7(i lII4L ,c;wI4 I J 1;c: ac amas ' 4' 4Rive ;& \ Oarprk ' Rivers and Streams I' ' PJ , I N City Limits S ' \9r4, 5, # % , Lake s( ' , " Cec c;&r? 'l' ' ' \, '*F% 1;I(j, S S S \% j1 County Line S II II S . I S S S i4I Tmoth Clackamas River ::ter c:; iV .a c\ LEGEND IS S IS S I S 1909 Rz: S I II I II S I II II I FAX '-, [I C/ackans River 9l PORTLAND, OREGON 97232 2736 1742 S - C, 4_1 600 NORTHEAST GRAND AVENUE ! k' cLAcKAMAsco.:4. ( ' Co//awash :' I-. r W.LE UsGgH:1sil1 s& 124000 "I 'S ? NO7E IGISMAP !S!NIENDED TO BE USED TQBEB WITh IRE / '" Sc1e in Miles 0 1 2 3 4 5 . tJ1-- Y' k Lak! 7 1I;im wi u" .: 'I - ; t -'I' \' MtW F)ITI 1JiohnP' g $A_Ia I. ' - Mt , k Deep Creek ' ; .;. ( .: C/ar Creek ' ' 44p ' \S " S ,d /; eck .. I # +. is . t.:.. ;;:. - . M ETRO : : 'Sr s Salniom I - 7.. .-. - ' ' b Ra I R ,i.J' 1i flI iikiir :±1T f FENWOOO ' LEGEND 4%. Tmothy II ?1E:::th::ams I State fr ! \ ft I - County I V 441*4.4 Ej:L::t S.. (i.e. Water, Sewer, etc.) S _________________\ &ov,.* f:e$1 Private . CLACKAMASCd\ __1L NOJE E '1 ' 1HItt(P IS INIENDED TO BE USED TOt77IER WITh! 2EE RivEr IT I Scale in Miles 0 1 2 3 'I 4 5 1 4 !L -' '!:!s' ' I % % irC/ackamas River vi' ' \ I I. bk PJT ( "7 ,44&* f \ %% . jHPPIe4I 'J _/ _ "a o'Ir \4 jtLØr 4: : cTcHt:c1(, I . HE ICI \ \\ ' Watershed Project :i ' -: dL ClackamasRaver River '4IL cada ' j2, o -- . 4" ' .-- Elevation " 600 NORTHEAST GRAND AVENUE ---- , PORTLAND, OREGON 97232 2736 TEL 503 797 1742 FAX 503 797 1909 td@tsthr !r ._k .gt .. \\ ' 4 . ;k , LR0' : HWY2JJ Molalla I . tE $!Ic FERFW.ot. -;i,f e& . Salmon ; ':: ' . F ::, - . t ;1 jicre R', '4 4 ? - Td::TT I 4. Elevatwn 7000' 6000' '\ Ely Roads /A\/ 5000' Rivers and Streams CountyLine - P (' -' 4 ; Vg 1 ! CLACKAMAS CO. MARION CO. DIGITALELEVA77ONMODELUSGSThg1LGmph USFor DEMfik Sk I 24OOO : ; RIVERSAND SmEAMS Org D,fFih d WildI,fk 19%) Sr,kJ JW,060 ROADS CO,RESPONDING IE7TIJYCLUDED IN 771E no i ' "S W771 ThIE . fhpMt, npr hu1 C!ACKAMASRIVER WAIERSHEDAILAS. hi Th a. ,e * E N0Th2. IHISMAP ISLVIEWDED TOBE USED TOER A ,. N 1994)&11.4,8OO US8,r 79%) Sfr I 4800 f0rn4 USGS a98)Sk J-24060 vs CSrn 7IGER Lrn FiI 199O, pdd thsgh 19by \ & d o thpIid, dsdig th - S : smv f 0 ' k Scale in Miles 0 1 2 3 I 4 5 1 , iiir# w. ;(' , ::I iI\! Jmt : Tj p I- , ;_ , G1 --- , I ' :' wCIear Ceek 4z:) CiasRiver Ecoregions 1s I t 0 ' - METRO , y. R P , I oaP7q I ,1I w .. I .g. t td 't . Salmon /R D0 ? S. : P0 600NORTREASTGRANDAVENUE MoIaUa" Rive,. , I Roaring River *oc>L - V.. ) 'I - I FERNW I.k,nas ) LEGEND S f ;' , ' I r i \ S R,ver ' -,-- Zak '! 1 )i %. N %f, Prairie Terraces ,'\i' Valley Foothills /tVI Roads \\ , N RiversandStreanis ' ,: t , . LowiandsandValleys \ Subwatersheds ,- - ,.,- " \q3 y, ' . c I Western Cascades MontaneHighl:nds CountyLine ,t: L Springs Fork I tf? :4 I ,,r CLACKAMAS CO . MARION CO. . EcoREaloNsusEPAL:4gfogod:; 0 U , Scale in Miles l 2 3 R.Collawash River . - 4 1 T # 5 ,w S1 -' i : ,. ' , - ' ¶5 'ii, - f(4f4 , - .7 s t '' . * ' : I , -_ 124000 IHISMAP IS LVIENDED To BE USED TOG1BR W1771 IHE CORSPONDIVG7EXTINCLUDEDrnIUECLNCKAI4ASRJVER1NA7ERSHEDA7L4S 0 1ii I yo7 LU ' . , E a) : . N 0 Sf#(/ 'Co/!awas/ River 1 'V,i!$' per CIkir 4) 4 !d2A! : EIirdi ! s F ---i-s ,ikI: ClackatsRiver _ - dIlW Ts !IlL 1iIL T N Qs C/r Cree/ 44Li:-- , I'jQTS k kr- -'U ada lI,4:rl;I;;. Geology i 7& ;¼ \ \ '-:i) / Columbia River Basalt Group ".' I iioeene) PyroclasticRockofBasaltie and Andesitic Cinder Cones Øfzddle Mtocene) I A Qg "n 1::A::::andBasa1t JacialDeposits I owsandClasticRocks, /4 I BasaltandAndesitelntrusions (PlioceneMioeene,andOligocene) JQs cr2It Ts Tuffaceous Se4imentay Rocks and Tuff(Pliocene andMiocene) 7;nQg Undifferentiated Tuffaceous mseWxene) us a : /v R1YSANDS7EAMS usc \ / '-Is 1 aI 4 Q J'/A# ', QTp N Qb Tfc' Qg Qis Qis \ti. \\ j I 9 ., 4 QR'\ var ' j ' Qgf ) I QTmv Qg I QTba Qis I ' C .Tus )' : ' . 'Sp' 7 'e QTba ' ' \ 'rus LT " ,J4 t & Ti., Tus Qg Qis Tib TIs : QTv 'QTLa j ) OTba U/1I3'T Clackarnas Qc ,J: ( River ( 'i 0 - Q;_ ,Wrnv \ g i Tfc RiversandStreatns w Qis E I County Line ThG1RLj,,Fl, 9O),s.dthosgh15byMeo pSSnS, 'Si% %, Rocks N CiisLi,nits USThfLdMLS9sthl4,8OO j CLACKAMASCOS fl L0 GFOLOGY ' . Sedunentar Rocks, Tuffs, and Basalt _Ti b % # Collawash River Qgf Glacwfiuvaldeposzt, ILandslide and Debris-Flow Deposits t sus HQtprIflgS pOfl Trb GlacioJluvial,Lacustrine and PethmentSedirnentarv QI f Undifferentiated 9vfioeene) I Qal Lake 1 0 f4t ft abyssalIntruszveRock llolocene) (\ \.C/ackamas River II Ti ( _, Qg($J93 t'Trb Tç :1Tw cr9ba.a andkelatedFlows Miocene) WanapumBasalt Tib ://JY( _l /I I , fb \a:C TC9 if Ro9rinverg''\ Tib _cp T(;TcePrardL;Grave1s I .' Tc C\!QIS S R TTib C/ai7f<fVer7f1Nk! LEGEND GeoJnusp,) th,nentarvRocks P1eistoceneandPliocene) Salmon R Tcw c$*1f FERNW,Q j II METRO ,4p1 1 Basalt and Andesite Intrusions PieistocenePliocene,an4Miocene) ,terret drc@etrotr. \ I QTb !' G' I . : ' *, . r_ c:;:: Ie PORTLAND,ORE:0N972322736 600NORTHEAST:RANDAVENUE lv Subivatersheds l -. r ,' Scale in Miles 2 3 4 5 . çg , - t t q'I . Tbaa wolF nag Ms;1s ThTJTNIJED TORE USED TOGEThER miii iiip l Q. f S ' httIJI S 1' ', Qg j3rb QTba .' N Tbaa Tbaa 1 0 I 0 C) I QTp QTp