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l I�f \�; -�^ \\ �\�\\\\ \ \\ \�\ \ \ \ \\ \ \ \� \ �1 \\1 \\ \ \\\ <br />/// lyI \I( / \ \ \ \\ \l _ \�\ \ \\ LEGEND: <br />-_ QIS \ 11 \ \I \ l \\ <br />_ _ Y 1 PROJECT BOUNDARY <br />-- J: / /i/ // / ll - \ \ I( IIII1 \I \ 1 I \ J 1 EXISTING TOPOGRAPHY (1999)(5 FEET CONTOUR INTERVAL) <br />C \� \\ \�JIIIIIIIIIIIIIII(Illl,lll // I // -ln'i� <br />\\\\\ / j/ / FF vy \\ l l 1 \ \ I \ I \ <br />s 1 111x1 \\ :�; <br />\ \\ \ \\\ <br />\\ \p \ \ \ \ \ \ \ \ \ \ \ \Ci j'/ i/ \\l \\\ IIIII(IIIIIIIIIIU� \\\ \\1 \\\\\ \\ 60X/ <br />N,\\\ \ \ J I III /// \ / ( / // / / 42y_ = 1 \ \ \ \\ \ \\ �� �\ 1 d' 1i INDICATES WHERE EXISTING FAULT IS VISIBLE. <br />�1 (D /U INDICATES RELATIVE MOVEMENT) <br />\\ \ \\ \ \ \\ \ \\� \\\ hIIJIII/ <br />INDICATES WHERE FAULT IS OBSCURED. <br />\ \ � \`N \\\� � \ \ \� \ \ \ \� \ \ \ /Ilf(IIIIIIUIIIII'lll✓II f �� / /� / //� //- -_ -_ _ - / II 1 \1 K <br />\� \ \\,\\\ \`OO \ \\ \ \\ \ \ \ 1 \ \ \ \ \/ I - -__- -__mil/ \ \ \\ \\ P (D /U INDICATES RELATIVE MOVEMENT) <br />\ \ \ \\ 1 \ \II I1)I(i \\ \�\ II IIIII�= �\ \1 \Y _ �i'/ J 1 \ \ I \ \ <br />/ ... THRUST FAULT <br />\\ \l \ \ \\ 11111 /IIII \\� T I 1/ (Illy- 111111 \, _ /_ - -_- 1/l J I I I\ <br />\\ \ \ \\ \>> \\ \1 f /JI = '� -�: / _ I �\ it SCARP <br />\ �'�1 / / / /I IIII(! �� ti- .�_� /i /%/ III IIIIIIII\ -� :// ,'�� -� _/' OBSCURED SCARP <br />111111/ \\\*`r / 'ate' -- - - - - <br />Illh //I /ll lllllllll )� \ \�\ � <br />BEDDING (DIRECTION AND DIP ANGLE) <br />/!I \ \NO \l' // d- <br />\\ // / \ ( OVERTURNED BEDDING <br />,, I \1 \II I �\ / � \L /- FRACTURES /JOINTS <br />/I /� „ I / /i /IIY.� \ \ \� \ \ \� \� �\\\ / <br />���- ��\�� \ \� \111111 J / / Il \ \r\; �) \ \�\\`� \ \L" RELATIVE MOVEMENT ON FAULT <br />�0 IIII ^1 \ \1 — / / /� / / / y /' // _ \`j �\ y \J (1 \ \ \ \l�\ / /ii' /i /iii /ii /i/ _ / // / / / �/ I )<\ \ / \ \ \` \ \ NOTE: <br />/r�iiti'i /_�'I <br />y1� . \; SYMBOLS IN BLACK WERE REFERENCED FROM THE COLORADO GEOLOGIC <br />\ \ \_ / / / / / / / /-- �\ \ 11 �// r- 7 \,.� \ SURVEY (CGS) AND SYMBOLS IN MAGENTA OR RED WERE MAPPED BY CTLI <br />\\ j\ \\. \\ \ \ \ \ \ \ \ \\ \ \\ \ \I / I/ /Ill/ // ;\ \\ 11 \I \\I i'pr \ ":` / j l lam' \ \ \ - \ \�\ _ / I I / I \ 1 \ \\ \�� C i• \\ \\ \\ I I f % f ll / /� \ (- I'' _ l I 1 \ THOMPSON, INC. (CTLIT) FOR THIS INVESTIGATION. <br />\ \�`'�! GEOLOGIC UNITS AND (MODIFIERS) <br />�')?$�\�� \� \\ \ \ \I \IIII \\ Qm \� \_J / /// / l \, /l�I1y11,I � /:<�I \ \ \ \ \1J \) J 1/ I III ! / / - % /�---- - / I 1 ISI RECENT LANDSLIDE: L - LAN <br />�8��� \ \\ \\ \ \ Ili IIII \I1 \ \ \ Rr�C \ \\ r Iv (rfI / ( \ \! \ \\ // ( \\ \11('17 /LI_� \IIII IIIij / /lIl /�l // / / - -- / I / J 1 Q OF RECENT OR ONGOING MOVEMENT, WITH EVIDENCE <br />r�r�Hf /zE /=_ \ \ \ \\ 1__t_ <br />_ \ \�E T \TfNt7� tit <br />l IIT \! \�1 \ \ \ \� / �/ i= ��f - /// / l� II QC FROMINI PLACE WEATHERING OF BEDROCK DEPOSITED PRIMARILY <br />\ \ \ \ \ \ \ \� \�� /• // , %,t %J A__= 1 \ \ \ \ \ \ 11 IIII / / / % / /// BY GRAVITY AND SHEET WASH. <br />=_i -_ -_�_�' /i / /i�)J \1 \ \ \\ 1\ \ \ \ \11\ \IIIIIIII 11 /(/ / ' �'� / // �' / 1 <br />\ \ \ \ \ \�\��\ �O �\ —"PROCESSING\ / \ _ — — <br />\ \\ \ \ \ \ \ \ \ \\ \ \ \ \\ • .\ // i II / \ QIS LANDSLIDES: LANDSLIDES WITH EVIDENCE EM <br />\ \ \\ \ \ \ \�� \ \ \ \ \ \ \ \ \ \ \I \�\, \ \ \ \� \ \\ \ \ \ \Iqq NC� PLANT 1• // \ \ \` j/j /// - i ii /��_�i111 /IJ II IIIIVIII IIII I/ // /�/ / /� /-i' // /// // )JII LIKELY OA ONG BEDDING PLANES EN THE PIERRE SHALE. I. <br />BELONG i /IIII IIIIIIIIII(IIII/ /' - /1`J / / / / / / /2Y -/ \ <br />/� 11 Qp PINEY CREEKALLUVIUM- ORGANIC -RICH CLAYEY SILT <br />\ \ J / 1 111 / / /�i_ "� //l I / / / / /// '�'•' -' -- - i / I III // ' AND SAND IN TERRACES ALONG MANY PRESENT <br />ii /j /llll) /1%11111111 /lIl /l' // III // i� j / / / / / / / / //t ice% ) /l/ / /III I /l // ��� ' ^1/ // / / - ^\ -\ <br />/�\- \ STREAMS, TOP OF TERRACES ABOUT 20 FEET ABOVE <br />STREAM LEVEL. <br />, QV VERDOS ALLUVIUM- POORLY SORTED STRATIFIED <br />/ / , % / / _/ / / / / / / / / /'° / Om (��\ /=iy/� /��p. \ Illy / / I \\ /J // //\ / \ GRAVEL CONTAINING LENSESOFSAND, SILTAND CLAY. <br />/ �J / / / / / / / / / / / / / / / / /// 1 0 `s° l /l j %)) /'L / / / / / / / / / / /�j /r.�j - i �� %j Ste% % % / / % / / / / //� I 1 I Ill(\/ / \-- 6�_ = /�/ 2�- THE TOP OF TERRACES ARE 160 TO 200 FEET ABOVE <br />/ / / 1 // 111/— _ —i/ // v — _ l _ I / ^ - -_ _ <br />4/�/ j j //l t{ f r o BLASTING • /� �j�j � / i ri % / % % / / /�/ _I I I I (`_/ //\ <br />/ / - /i- /�--i% // /////�.\ ( / MAJOR STREAMS. <br />QHI BENCH a 51,�,d1 g_ ��� // 1 <br />',/K•' / � � / / / /\ \� \� <br />\ I 1 1 1 I 1 I \ \ \ \ \ \ \ \�C (C //i / / /i% /// _ �/i \ 1 `� I / / �, -+•p1 / / (C- ��� _�'1 1 ) t - / / ) Kp PIERRE SHALE (UPPER CRETACEOUS): GRAY TO <br />l / IIII \VIII \ \11J \1111(1 e d ' / i / �,% ��� / J �)� � (r / /�/ I I) r= \\ L \ � \ I l \ \ �J, \ `. /j // / I DARK-GRAY MARINE <br />NETHAT CONTAINS INTERBEDDED <br />OCCASIONAL (I I \!' Vii- /y / I I \` \ /%/ / AND ,AND WEATHERS CONTAINS AND OLIVE-GREEN CLAY. <br />Qp <br />BEDS, AND WEATHERS TO BROWN AND OLIVE -GREEN CLAY. <br />l l I l / / /O / / / /LU /( /(rt i ✓ ;�!\ 1 \ Il I' <� ' 1 �-•�\C / / «) �./ / —J f — <br />I /( I / / ;._r / / / /` i„r� - /) L \y I--. I 11 ( -Fj -�� l\ 1 ) ✓ ' % y / Om MANITOU FORMATION (ORDOVICIAN): GRAY TO PINK <br />/ I I I I \ _ O \ \`�\ \ \ \C\ / // - r" / 1 I \ \ / / / /_ -� - \ ! LIMESTONE AND DOLOSTONE WITH OCCASIONAL THIN <br />/ f I I \ �� � � � \ �\ V \ \ \ \ \ \� /1 l l(I F� /'- �� ^�S \� � /%`�'� ^ L ~\ \\ I l l ll I I \ \� 1d � \ \�/ \ \ \\ \ \ ( / /i'' / / / I \ /'! ' SHALE (CLAY). UNIT INCLUDES MATERIALS PREVIOUSLY <br />_ / <br />\ \ \\ \( (a Kp 111 ( i I I i \ \ I �- / /) \ \ \� LIEADVILLE LIMESTONE S DEVONIAN), WILLIAMS CANYON HE <br />QP l \II / I \ \ - ` / )� \ J / FORMATION (MISSISSIPPIAN), AND PEERLESS DOLOMITE <br />\ ` / / (CAMBRIAN). <br />I / <br />IDD6 AAAA1 1 1 I v �.o �� Om I <br />�)) \\ -CS SAWATCH SANDSTONE (UPPER CAMBRIAN) VARIES FROM <br />/ /// / a �VA, A \'�� Atev v VA� \�AAAVAAA VA\ DEEP PURPLE AND GREEN GLACONITE SANDSTONE AT TOP <br />TO WHITE TO LIGHT -GRAY -GREEN ARKOSIC SANDSTONE. <br />vvv A1A IIII <br />__ ���Vi(/1 / �� V/�iA_ A� i'_Av �.1 /I 1 j vI��/ ,I- v IA!A / IlA�? ��A vlj)1A 1J �jAVA lA? %I J VI lA1 l I�/AI /I 1- V_ � 1� \ 1A/ v1v/V - AI\1 v\ I 11 - l 1IA/A /— VA�I l )IlA AIA/,A llIIl- l \I\VA nA1 llI J vl Vl 1 I AA VAI 111110111 <br />llllll1I v1 / / / 'vI / I <br />V\/ — / v A -7� � v � ; viz _ v - <br />C �V lv w v A v�XcV w - A - <br />V ' <br />. <br />YP P <br />PIKES P <br />EA <br />K GRANITE (PRECAMBRIAN): <br />O <br />R <br />ANGISH- BROWN, <br />REDDISH BROWN TO PINK COARSE GRAINED PRECAMBRIAN <br />\ V <br />C AC \ V �� GRANITE. Of lit, (8f) ARTIFICIAL FILL / DISTURBED AREA <br />LPAIAI I//IlIl IIIlI11 / STO It,E <br />H _ PIT FILL BEAVI(IIl A1V( \ (P) <br />\�AA�AAw °M RECLAMATION FILL A \R (Irf) <br />/� SURFICIAL GEOLOGIC CONTACTS (CGS) <br />1 SURFICIAL GEOLOGIC CONTACTS CTL In V P / <br />l A I / v)y /�,� NOTE: <br />SYMBOLS IN BLUE WERE REFERENCED FROM THE COLORADO GEOLOGIC <br />S V"_ SURVEY CGS AND SYMBOLS IN MAGENTA WERE MAPPED BY CTL <br />/FtEAK I 1 ( I f� / �vA�A v 1 /� VIII Al - \� AtV— S?r� �'�a —�"��— _ —�_t= �c�7��G-- >]}�I��� ( ) ( I) <br />v A / - v - - - _ � y ) G ; � ^ THOMPSON, INC. CTL T FOR THIS INVESTIGATION. <br />-- - -� / / / / // ,�VVAi 1) V IIII�L�A�V 1/ 1A \-� vVCS V �V_ �- - / <br />Iliil l 1 I._ -- .82 / / / / I 1 a m \ \V AA AA V l ( l //f vAVA /-.v V�' //) QV w �� -v A v A \� A /� / /i' -V / <br />J�?V���AA�1 v �/ AAI 11 A/ vv I A v = L / / /c�vvv_ —vvv <br />I <br />\ \ <br />� \lP � \ \ \\ IL / \�II IL -\ \ \/ �l <br />I / / <br />\ <br />/ ° \%t\ \11 \ \ \ \ \I\ 1 <br />/(CL; U,`a \\ \ <br />\\ \� \ \ \ \\ \ \ \\ \ �\ C, �1 � \ \ �s\ \ \\ \\ /J �\\ \ 1 \)1 \\ \ 1 /j /` /�i 's NOTES: <br />\ \ \'\ \\ \ \ \\ \ \ \ \ \ \ \ \ \� \ =_� \ \ \\ \` (� I / 1 1111 I1j111 I 1 )\ 1 \ �I I \ \ l I / / / / / // /�� \\ �\� 650 ? l - 1. BASE TOPOGRAPHY DRAWINGS FROM BANKS AND GESSO <br />/ / / / /// 1\ \/ !\ (JOB NO. 20006, DATED JANUARY 17,2001) AND NOLTE, RECEIVED <br />\\\\ \ \ \ \..\ \ \ �\ \\\ \ �\ \\ \�� \ \\ �\\\ \\ // / /%i /i �/( \1 \L \ \(� I / \Ill\ 1 // �-\ \ \ \ \\ /\ I lI��DT$��\ \ \\ �. \ \ \ \\ \\ \\\ MARCH 20.2009. <br />\\ \\\ \ V \\\ \\ \\ \IIII /(( // 2. ALL BOUNDARIES SHOWN SHOULD BE CONSIDERED <br />V \ \ \\ \ \\ \ \ \ \\ II (IIII 11\) I \ ( \I\ \\ \ \ \ I I ) I I/ / ✓ / -\ APPROXIMATE. THEY ARE BASED UPON \SUBJECTIVE <br />\ \ \h \ \ \\ \ \ \ \\ \ \ \ \\ j lllllllllll 1 \1 \� \1 \ \\ \I \I\ l \ I / 1 / f' <br />I\ \ I \ \ \ I 1 \ I I / / ✓� i� y 1 INTERPRETATION OF PUBLISHED MAPS, AERIAL PHOTOGRAPHS <br />\ \� \ \ \ \ \ \\ 1 \\ \) / I II II \ \\ \ \ I 1 \ \ \1 1 \ ( -� •il / I \ \ \I� (�-�' \ AND AN INITIAL FIELD RECONNAISSANCE CHANGES IN THE <br />\ \\ ON\�_/ \ \e \ \ \/ I)Illlll(I \ \ \ \ \ \\\ C \\ \ \ \ \ \1 \ \I\ \llllll 1 11111 II tI \� �\ I.,.tl \�\\\ \ \ MAPPED BOUNDARIES SHOWN ARE POSSIBLE AND SHOULD BE <br />\�7Ip'L \\ \ 1 I I 1 \ 1 999pj EXPECTED WITH MORE DETAILED WORK AND FURTHER <br />III \I \I /) 3. MAP SMMODIFIED FROM GEOLOGIC MAP OF THE PIKEVIEW <br />\ 11111 I III I f/ I I IIII Y \ \l\ \ \\ \ IIII 1 1 II \ I I I \ \ \I \ \ \ / QUADRANGLE, EL PASO COUNTY, COLORADO, COLORADO <br />/ / / //I I /1jIIIIIIIIII)I /)IIIIIII�/ II\ \ \\ \ \III IIII / / /' GEOLOGIC SURVEY OPEN FILE REPORT01 -3. <br />\ \ \ \ \ \ \I11iIllill hlllr / 1 /ll /�llllllllllllr lllll4�1 <br />_- Y I ��`= =\_111 \ \\ \� \ \�\\� p101 I 1111 // iri //l llgl Il �lll lI IIII II <br />\ ti _ - / -y 11\ \\ �\ UU I II\ / / /r /r /l/1 ll� Ill/ //l I II <br />/ jllll /l � 1ll Iji II II It <br />\ \_/ / / / / a' A - -•t � - -.� _- __.1111 IIII I I I I �II \ / ,�/ <br />\_ <br />og / / \ <br />\ SurFicial Geologic Conditions %/i l <br />�nlll /lr� _; alllllllllll/ i /j //V //i /iiii // II / / j l <br />\� \\ D / /iC, _ -7650- 9-I \�-- �� — //� /' /Nl /lac_\\` Jl %� /I�Illl����o-_ /i / % / / / / / % / //i i�i� J /Ill JII �1) II IIII�I11 \ / \��\ \ \ \\ \\ \ \ \I II \ 0 100 zao• PIKEVIEWQUARRYSLOPE <br />/ 9� =_ _ COLORADO SPRINGS, COLORADO <br />— a I111l11'1�yy i` / / \llllll! ( / \ \ 1 1 1 1 \I I I I I SCALE \ \\ `� \s / / / / % 1 \p � / /i //i - — \ I III II L \ \ <br />\ \ \ \ \ \ � \ � \' \ \ � v � eo.� •� -� —. - � � \ \\ � \ � \ \ \ \ \\\\ \ � 11 \ \ \ \\ 1 \ I1I1II I 111 1�1I � 1 \P \ �$ � _�'��- _ �--•_� � ' / / / / / / / / / / / / / / /� %%// // �\ \ \ \ \\\\\\r ` �� �/ /�� // � I % /i/ice / , /� // � // / i/ / / / ce /// / � / / / / / / / / // i'ce � — _ — � _ - _ _- __ > -__ -_ _ ==J : �i J I1I 11 \I I 1 I / I II l ll 1/1I \/\ � � )/�/ \ \I /�/� / 540E ARK G <br />BLVD.COLORADO SPRINGS PHONE (]19) 528-8900 FAX 719)52 582 \ �dmom.o9wm r <br />ce '_�_ \ \�\ DATE: DRAWN BY <br />Ypp —� -. \\ 1 I IIII l / �, (� \ \ \� \� \ \ \ \\\� \\ •ii / %%%/ \� f /fl�� \'\� \\ \ �_� \\•C_ MAY 4.2009 TEM FIGURE <br />CTLT PROJECT NO. REVIEWED BY 4 <br />CS17341 -125 TAT /WCH <br />