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~ ~ ~ ~ ~ ~^ ~ ~ ~ ~ ^~ ~ ~ ~ ~ ~ ~ s <br />0 <br />SCS-5'pILS•7C fRev.) On-A: Glenberg - Haverson fine sandy loamT 0 to 1~ slopes (Gl@nb2rfyJ, $, DEPARTA!ENT OF AGRICULTURE <br />B'r' SOIL SURVEY INTERPRETATIONS portion) $DIL CONSERVATION SERVICE <br />FILE CODE SOILS-17 Glenberg soils are deep well drained soils on the river terraces. Typical }zylES~ pn-A <br />they have a fine sandy ~oam surfaces and a sandy loam subsoil. 'ihe sub- Colorado <br />soil is stratified and contains thin layers of silt or sand in places. STATE: <br />Gravel underlies in places. These soils have a moderately rapid intake "Lq^ 49 <br />and moderately rapid permeability. Glenberg soils occur in the landscape CLASSI F: <br />in association with Iiaverson soils which have silty subsoils. RJL A 72 <br />ESTIMATED SOIL PROPERTIES SIGNIFICANT TO ENGINEERING ~ <br />MAJOR COAgSE PERCENTAGE LESS THAN )INCHES <br />SOIL <br />NOggONS CLASSIFICATION FgACT. <br />> 1 IM. PASSING SIE VE NO.--- <br />AVAILABLE <br />pNCHES) t PE q"EA- HATER S(JIL SAL INIT~' S1+MiN K- POTENTIAL <br /> USDA <br /> <br />TE%TURE <br /> <br />UNIFIED <br /> <br />MSNO <br /> <br />. <br /> <br />10 <br /> <br />b <br /> <br />]00 <br /> <br />LL <br /> <br />PI BILITY <br /> <br />UN./~O CAVgITY <br /> <br />IIn:I^I REACTION <br /> <br />(RNI <br />IEC.10 <br />P15'CI <br />SWRL <br />FOTEN TIAL <br />FROST <br />ACTIOH <br />0-5 Fine <br />S <br />L 1•II. or <br />SPi A-!~ 100 9r <br />I00 70-8 40-6 Non- <br />P 22~°3 <br />i .13-°15 .9-B.LI - 2 Lox high <br /> oa <br />ancjy las s <br />5-58 Sandy Loa St9 A-4 100 95- 60-8 30-4 2-b°3 °11-°13 °9-8.1 - 2 Lolr nigh <br /> 100 <br />OEPTN TO BEDROCK OR 4ARDPAN: Very deep FLOOD NAZAgD. Moderate (l/1G yr°) <br />DEPTH TO SEASONAL HIGH W'A'i ERTABLE $aTJgeS 5 tp 8 ft° HYDROLOGIC GROUP <br />SI IITAflII IN OF SOIL AS SOURCE OF SFI FCTFD 6L4 TFRIAL AND FEATURES AFF FCTWG USF <br />TocsmL: Good GRAVEL: nsulted - Gyu in a/ac~_f~,`pL~<' i {-T~ <br />SAND: Poor -hig h percent Sines ROADFILL: Fair -fair to poor st.ability_ and corpactien <br /> DEGREE OF SO IL LIAtITATION <br />LOCnI ROPpS AND ST HEFTS: SEPTIC TANK ABSORPTION WELDS. <br />Id 3$~ -flood hazard Severe -flood hazard <br />SHALLOW ExCAVAnONS: <br />Moderate - Gavin <br />hazard EWAGE LAGOONS: <br />Severe -rapid permeability of substratirT!; flood contr <br />O'hELLINGS: CORROS IVITY: <br />•'~'bi••~•^'• Severe -flood hazard """`°"'°"'°' Lox <br />bl -~R e.+eTem+ el e°nv°rc <br />SAryI TngY LAND FILL' <br />(TRENCH TYPEI <br />MAJOR SOIL FEATURES AFFECTING SELECTED USE <br />POND RESERVOIR AgEAS <br />S v re - ranid ermeabilit of substratum IRRIGATION <br />E"BANKMEHTS.OIKES, Antl LEVEES TERRACES Rn0 DIVERSIONS <br />ORAIHAGE n/ CROPLAND Ntl PASTUgE GRASSED WATERWAYS <br />1 <br />• <br /> <br />bJ <br />H <br />H <br />H <br />E-1 <br />n <br />c'F <br />a <br /> <br />