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<br />Presented on Table 3 is a summary of the known flood event, and selectedcharacterist ics <br />of each stonn recorded. The information recorded on Table 3 has been compiled from <br />newspaper accounts along with other articles. <br /> <br />ImperviOllsArea <br />In general. total runoff from a ";ater,bed is a function of the type of soils an dthe el<tent <br />of impervioU!; area within the basin. RUn\lff curve numbers, which are based on soil types and <br />impervious area. were determined for each sub-basin in the Monument Creek watershed for both <br />existing and future development conditions. Curve numbers were calculated based on the <br />prQ(;cuures idel1lifled in the City/C'oul1ly Drainage Criteria Manual. Tables 5-4 and 5-5 of the <br />criteria manual wasrcferred to when sclecting representative curve numbers. <br />The extent of imperviou, area within each sub-basin was estimated for existing <br />development conditions based on aerial photography of the watershed dated November, 1989. <br />Various land uses shown in the aerial photography were categorized according 10 the <br />infommtion shown in Table 4. A work map was prepared indicating the location of each land <br />use zone relative to drainage basin boundaries. Areas of the calegorized land uses within each <br />sub-basin were measuredus1l1g aplal1lmeter. <br />Sub-ba,in imperviousness for future developmel1l conditions was based on information <br />prepared by the City of Colorado Springs. EI Paso County. and Pikes Peak Area Council of <br />Governments for a recent planning study entitled "Socioeconomic Foreca,ts for Transportation <br />Planning Beyond the Year 20JO". In order to develop the plan. the ultimate ho\dmg capacity (in <br />term, of population and residential and busines~ density) wa~ estimated for a number of <br />transportationplanningwncs. These estimates. developed to ensure that growth would not bo: <br /> <br /> , - <br /> , , = , <br /> "ji I, .. !l~ m ....!:.!j <br /> g-:,~ i "' , <br /> !- ..,,'ij-l: <br /> m >, ~~ "'. ," " ~,] <br /> 0 c, jci.! " -] , <br /> . ,~~; 1!1>l . - ~~" <br /> 0' .~ U <ll .10 ,~ <br /> . <br /> ^ <br /> . " <br /> 8i ~ <br /> , <br /> .!'l - . <br />~ - <br /> ~, <br />~ >' > , ' > j <br /> . ." H <br /> I ~~ , ]~ ~N <br />~ <br /> >-, 0 e;-:lolj.... n <br />~i:l , z ." 0 <br /> 0 <br /> . <br />~~8 . -.' " i <br />301 _ , H . . j "-r !jg" <br /> , 'N' hi '''J · ~p <br /> g~= .!E '1!U <lil ., ."] .~~~ <br />~~ ~ - 0' 118 c.<] ] 'r <br /> '~ > , <br /> < . ~ ~ ~l~~ " ., <br />~" " > - . ~::E9 0 u . > <br /> u . >> 0 <br />00 " ..9.51- ::E:" c ~ <br />~~ ^ , <br />" <br />G ji8~ . 8 <br />~ - - <br />~ 0 '" <br />~ '0 <br />01- <br /> ;;~ .. <br /> m~ g g g g <br /> . = = >( <br /> ~ c: 3 ~ . <br /> 8~u <br /> . . ~~ . = , . <br /> ~ ~.~ = . <br /> , " <br /> "< " . <br /> - N . g <br /> 0 - 0 . - . ... - <br /> ~o ,. "< N. N' ;~ .,- -!i: ~, -- <br /> NI;; ^' >' N _ " .. <br /> " -' -- ;- ~ :!: ,.,~ ."c_ <br /> ,- >.- .- o- r ,- 0- <br /> , . N <br /> N , N - - <br /> . - <br /> '-- <br /> <br />Soils and Geolol!y <br />Soils within the Monument Creek basin vary between soils types A through D. as <br />identifictl by the U.S. Depanment of Agriculture. Soil Conservation Service. Type D soils are <br />predominate in the forested areas west of Monument Creek. These soils are generally associated <br />with the Pikes Peak Granite found in the region. Figure 3 depicts the hydrologic soil types <br />distributed throughoUl the Monument Creek basin. <br />Soils are classified in hydrologic groups A, B. C. and D according to their infiltration <br />capacity. Group A soils consist chiefly of weU-drained sands and gravels and have a low runoff <br />potential. A work map was prepared showing the distribUlion of the four soils groups throu ghout <br />the Monument Creek watershed. The percentage of each soil group within individual sub-basins <br />was estimated by using a planimeter to measure soil group areas. <br /> <br />1II-6 <br />