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SG -A North L `A L! L A << A y r L> V 7 L A 1 L A L> b4 A L` L, L L ,< A 1 1 )1 L1V>'L`>LLL rL 7LA>L;Ya`TL7'7'L7� A` I. is 7Va 6, 1!>AAAL + < <! >l JA1 >1! >(aa nits <a`7y< Yl < + a > +< > < > ` V t A> L > < > ► L r A 7 A L r > 1 <v ' < y 1 < > > , >[, YLL 7lL YlA L >< tALr .n >A L7 <L7A r >" >�• <L >� L > L L> < V 7 l A V f♦ L J 7 A < 1 I, a L 1r, tJ +f LAY lL 7/L1 AVtrLlA J7La )A LL rNVVLJ P 1 r> 1 Y< 1 L> L 7 1 L! 1 < V A< l A L ) PV I j 7 r 7 ff < <!'/ Yty +Va L +aL A7A IL`L7 < +yaV < )LV '<+ 7A yJ <,1 <�.<�J a +A +7)AJ <F7V >wt a +>. �` +1L JLV >±AJ• w� L Y Al Yw AA a V < < are r> A ya to <L LA <a,LA a ;A AV J1a ;L J-L+ -1 lt')lY : <� <L L >A L A ya VPAl7 ) L LlL7L [' >L7AL >A fA'IA >A P't LPL IV, — _- CL > + 7v <AL 4 J7 , Ya <> Vr,> A V C +> < t< J L<> L> A+ L A A A A+ r ! V '4 A - -- Pf yA L1 rA JOAL7 A VL,>y> 1 > !L >A 7ALV - - -_— — ;L !`A < < >La L> V1L A <! <ALV >Aa L >CA _— _ —_ —_ —_ _- L Ala VA tV A V LAr. L> L7V 47 A LA l4 y V.rPLy7 rr1 Y <1Y > >Vr1PL t7L VLJ V 7 < Yr ar < > l < — — — — — — — — 7 „ 7 > L V < A A J L a A C -- - - - - -- -- - - -- - - - r V > Y Y L AA <V Y L t r ___ _ _ _ _ A — — — — — — — — ___ _ _ _ __ _ _ ) - - - - -- - -- — VA < L L >< v - - - - - -- - —_ 7 4 A V ) ________ _ _ , A V L -- - ------ -— < r __ _ _ _ _ _ __ _ A A J a 7 A - -- - -- -- _ -- V> _ _ ,t aV1LYC7a LACA <> - -- -- - -_ - -- _ — - A L > A V _ —_ _— _ —_ —_— _— — — L IL1V A<'A <r )JV <A <— _— _— _— __— _— _— _-- _ —_ —_ —_ [ ♦ w [ bN _// 4 ri0= p qv. - - - - - - - - - - - --- -- - ___ ___ _ _ __ �bb< — -- - - - - -- /l -- ---- - --- -- - -- - -- — - _ ___ _ ___ _ --- _ / — - - _ _ — _ _ _ / - --- - - -- - - -- -- /_rice ®•n ------------ _— ___ - - -- _ _ -- -_— — If Ili Gall. r _ _--------- -_ - -_— — - -- — cp -- — — — — — _ —_ —_— — _— _— _— _— _— _ —_ —_— —_ —_ —__ 0 ;/ 1111 — — _— _ —_ —_— — — — — — — — — - - - - -_ —_ - - -- — — — — _— _---- - - - - -- - -_- - 91' - -- - - - -- - - - - - - - -- - - -- NOTES: 1) Snberface data taken from boring logs: Boring Nos. SG- 1.93-A,6 SG-C from Wright Water Ergireers,(1977), Boring No. SG-2 from Wright Water Ergiresrs,(1978)., 2) No elevatiae vre:c given fcr borings. It is aselrmed that they are of similar elevation. 3) The layers storm are oadaeed from those rhown an the original boring logs, and are highly interpretive with respect to the data included in the report. SG -1 SG -C '7 `< A-4 ,1 L !+ 1 L) V .> > < 7 !A < L 1 > < r> V 1 7 A 7 .r < T. 7 <AI PL >V7 aA >LA AIL7 Ar L`a<L`) <A r7 f <AryL >V7 Lw7 AY3, all> AL 7a 70, A•ILA7 A,YA 1 LA <L >y >471, A� > >> a< L L 7 L 7 A L L! V r 7 L rat L 1 a> 7 L V >, a< L L l > A/ A A TAVA l rV >L A -9 L !> 7 r A> AIA >!YP A IJ >!)< >VAV caALa7r >aA7VaAL aJ >ALa<)A7v JL IN ^44t r VIVV. V < >V<ALi > <J L<> a> rL Af AAwl1♦ +A 7 r J" 7 Y >' L Y >� > A J` 7! A;! <) ya L 1 Y L♦ It L> V< w P L P< r< 7 L A L L l w L 1 >! <1 > L L V< V y! <!< LAY ! L> V L 1! V 7 A L l(! of !a A)A 7 t L Y P f + a A I, ! L 7< L 1 I' r T! <1�� A >P A ) <1 < Vr r< r >L v7LV O L >r Lj < >!+ Lr<1 L > <AVLy aVJ `aaYA w +l7A <aLayt�Vy< 7 < < <!1 r <♦ J2 +13 > P. P A f JL <A ,1 VAL <1V < <ry >Lwy +L1LV >AA < <LA +a +Aa7r[,L )J >Y A Y [,A 4 )!ra — a7, tAA L)fa <J <a VL14 LLA < < +A <r> — --- 1Ay! <A Vt V <A + > < <LA, VA<< ,t <!<7Ya1 -- - - - - -- !< w V&- l a A — — - - -- II, f) C 7) r) L A < < ( t f — _— __— _— _— _— _-- _— _ —__ —_— __ < <Lw v e ! << — _ —_ - -_ _— - - - -_— _— _— _ —_ —_— > a w L w 1a ----------------------- t la - - -- __ - -- __--- - -92'- _ 2 16 , [ SCALE: V -16' 10 HORIZONTAL AND VERTICAL 6' t) I- 4 >1 South A It ! 1 A+ ,A ! [ V A LEG€TSA Black Topsoil < V < CbllWlvn V Li- p I // Sand with black clay and gravel mWeathered Meaavertb teriock ® Intact Mesaverde bedrock NORTH -SOUTH CROSS SECTION OF STEVENS GULCH I IIIIII VIII VIII VIII VIII VIII IIII IIII 004456 GEO -HYDRO CONSULTING, Plats A -9 -M< . .. < ) ... . L <Y A7A7 7 t• < NOTES: 1) Snberface data taken from boring logs: Boring Nos. SG- 1.93-A,6 SG-C from Wright Water Ergireers,(1977), Boring No. SG-2 from Wright Water Ergiresrs,(1978)., 2) No elevatiae vre:c given fcr borings. It is aselrmed that they are of similar elevation. 3) The layers storm are oadaeed from those rhown an the original boring logs, and are highly interpretive with respect to the data included in the report. SG -1 SG -C '7 `< A-4 ,1 L !+ 1 L) V .> > < 7 !A < L 1 > < r> V 1 7 A 7 .r < T. 7 <AI PL >V7 aA >LA AIL7 Ar L`a<L`) <A r7 f <AryL >V7 Lw7 AY3, all> AL 7a 70, A•ILA7 A,YA 1 LA <L >y >471, A� > >> a< L L 7 L 7 A L L! V r 7 L rat L 1 a> 7 L V >, a< L L l > A/ A A TAVA l rV >L A -9 L !> 7 r A> AIA >!YP A IJ >!)< >VAV caALa7r >aA7VaAL aJ >ALa<)A7v JL IN ^44t r VIVV. V < >V<ALi > <J L<> a> rL Af AAwl1♦ +A 7 r J" 7 Y >' L Y >� > A J` 7! A;! <) ya L 1 Y L♦ It L> V< w P L P< r< 7 L A L L l w L 1 >! <1 > L L V< V y! <!< LAY ! L> V L 1! V 7 A L l(! of !a A)A 7 t L Y P f + a A I, ! L 7< L 1 I' r T! <1�� A >P A ) <1 < Vr r< r >L v7LV O L >r Lj < >!+ Lr<1 L > <AVLy aVJ `aaYA w +l7A <aLayt�Vy< 7 < < <!1 r <♦ J2 +13 > P. P A f JL <A ,1 VAL <1V < <ry >Lwy +L1LV >AA < <LA +a +Aa7r[,L )J >Y A Y [,A 4 )!ra — a7, tAA L)fa <J <a VL14 LLA < < +A <r> — --- 1Ay! <A Vt V <A + > < <LA, VA<< ,t <!<7Ya1 -- - - - - -- !< w V&- l a A — — - - -- II, f) C 7) r) L A < < ( t f — _— __— _— _— _— _-- _— _ —__ —_— __ < <Lw v e ! << — _ —_ - -_ _— - - - -_— _— _— _ —_ —_— > a w L w 1a ----------------------- t la - - -- __ - -- __--- - -92'- _ 2 16 , [ SCALE: V -16' 10 HORIZONTAL AND VERTICAL 6' t) I- 4 >1 South A It ! 1 A+ ,A ! [ V A LEG€TSA Black Topsoil < V < CbllWlvn V Li- p I // Sand with black clay and gravel mWeathered Meaavertb teriock ® Intact Mesaverde bedrock NORTH -SOUTH CROSS SECTION OF STEVENS GULCH I IIIIII VIII VIII VIII VIII VIII IIII IIII 004456 GEO -HYDRO CONSULTING, Plats A -9 2 16 , [ SCALE: V -16' 10 HORIZONTAL AND VERTICAL 6' t) I- 4 >1 South A It ! 1 A+ ,A ! [ V A LEG€TSA Black Topsoil < V < CbllWlvn V Li- p I // Sand with black clay and gravel mWeathered Meaavertb teriock ® Intact Mesaverde bedrock NORTH -SOUTH CROSS SECTION OF STEVENS GULCH I IIIIII VIII VIII VIII VIII VIII IIII IIII 004456 GEO -HYDRO CONSULTING, Plats A -9