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Sc <br />. CHARACTERISTICS <br />RECD VE® <br />SEP 11983 <br />�IINE.9 LAND RECLAMATION DIVISION <br />Cola• Dept. of Natural Resources <br />LOAMY ALLUVIAL LAND, GRAVELLY SUBSTRATUM., OCCURS AS SMALL AREAS IN MAJOR <br />DRAINAGEWAYS. "IT IS A PRINCIPAL SOURCE OF GRAVEL. NEARLY ALL AREAS ARE <br />'SUBJECT TO'FLOODIKG FROM STREAMS AND THE FLOODS ARE OFTEN DAMAGING. THE <br />SOILS ARE SHALLOW AND'STRATIFIED. THE STRATA. ARE OF MODERATELY FINE TEX- <br />TURED MATERIAL THAT I'S UNDERLAIN BY RIVER'SAND AND GRAVEL. IY. SOME PLACES <br />THE SOILS ARE'SLIGHTLY INFLUENCED BY SOLUBLE SALTS. THE SOILS OF THIS LAND <br />TYPE ABSORB WATER AT A RAPID TO SLOW RATE. THE AVAILABLE WATER CAPACITY IS <br />LOW, BUT MANY AREAS HAVE A HIGH WATER TABLE THAT IS BENEFICIAL TO PLANT <br />GROWTH. MUCH OF THIS LAND TYPE IS CULTIVATED AKD'IRRIGATED. THE PRINCIPAL <br />CROPS ARE TRUCK CROPS ADAPTED TO THE AREA. THE BEST GROWING CONDITIONS CAN <br />BE MAIKTAINED'IF THE NORMAL WATER TABLE IS CONTROLLED SO THAT IT REMAINS AT <br />A DEPTH OF 10 TO 20 IKCHES BELOW THE SURFACE DURING THE GROWING SEASON. <br />OTHER IRRIGATED CROPS IKOLUDE PASTURE MIXTURES THAT REQUIRE SOME IRRIGATION <br />BUT ARE PARTLY SUSTAIKED BY THE WATER TABLE IN THE GRAVEL: LAYERS. SOME OF <br />THIS LAND TYPEA'S'It NATIVE GRASS. THE FETTER AREAS PRODUCE SEDGES, RUSHES, <br />AND CATTAILS.' LITTLE L IRRIGATION IS NEEDED. <br />WET ALLUVIAL LAND. THI'S TYPE OF LAND IS OK THE NEARLY LEVEL BOTTO"ol'LAKOS <br />OF LARGER 'STREAMS 'NEXT TO STREAM CHAKKELS.IK THE COUKTY. THISILAKD IS WET, <br />MOST OF THE TIME. MATERIALS ARE EXTREMELY,VARIASLE'IK TEXTURE; THEY'CONSIST <br />OF STRATIFIED LAYERS OF DARK COLORED 'SILT, (,LOAM AND CLAY,IUNDERLAIR BY SAND <br />AND'SOME GRAVEL. THEY ARE WET AT A DEPTH OF 2 FEET MOST OF THE TIME AND <br />ARE CWOOKLY WET TO THE'SURFACE THROUGHOUT THE GROWING SEASON_ NATURAL FER- <br />TILITY IS MODERATE TO GOOD.. AREAS OF TH1'S LAKD TYPE HAVE A VEGITATIVE COVER <br />OF WATER — TOLERANT PLANTS SUCH AS CATTAILS AND SEDGES, AND ARE NOT SUITABLE <br />FOR CULTIVATION BECAUSE OF THE HAZARD OF FLOODING FROM STREAMS AND A HIGH <br />__.IYATER TABLE _UNDER IMPROVED MANAGEMENT, THE PRODUCTION OF NATIVE GRASS FOR <br />GRAZING OR HAY IS GOOD. GENERALLY A. FEW COTTONWOODS ND WT0LL6WS"ARE F'REbLNI. <br />TERRACE ESCARPMENTS. TERRACE ESCARPMENTS OCCUR AS BREAKS OR STEEP SIDE <br />SLOPES ADJACENT TO THE CHARNELS OF PRESENT OR FORMER STREAMS. THEY ALSO <br />OCCUR AS THE STEEP FACES OF TERRACES THAT BORDER BOTTOM LANDS AND FLOOD <br />PLAINS. THIS LAND TYPE CONSISTS OF ALLUVIUM OF VARIABLE MATERIALS AND IS <br />VERY'SHALLOW OVER GRAVEL AND SAND. THESE MATERIALS HAVE A'LOAMY'SAKD OR <br />'SANDY LOAM'SURFACE LAYER. IN MANY AREAS THIS LAYER I'S 5 TO 20 PERCENT <br />GRAVEL. 'SHALE AND SANDSTONE OUTCROPS ARE IN SOME AREAS. 'SURFACE LAYERS <br />VARY IN REACTION FROM PLACE TO PLACE AND I E PLlZ;ES IS CALCAREOUS. "SLOPES <br />DIFFER WIDELY WITHIF 'SHORT DISTANCES AND RANGE FROM I TO BO PERCENT SOME <br />AREAS ARE USED FOR GRAZING, BUT THE SOILS ARE TOO STEEP, TOO SHALLOW, OR <br />TOO UNSTABLE FOR CULTIVATION OR GOOD GRASS MANAGEMENT. MUCH OF THI'S LAND <br />I'S RAPIDLY BEING MINED FOR SAND AND GRAVEL, AND THEREAFTER IS NOT USABLE <br />FOR FARMING. <br />Permit Nuryher ril <br />ss ®pe mit <br />Section/Exhi6it: <br />Class: 17 Revision ._._._._._._._._._._._._._._ <br />Class: p _ ____ - i <br />Port O Hytlro OGeneral <br />E)Applioaeon (Coal onl ' _ -- w <br />Y) O Bond O Enforcement O Inspection -- ' "-- ' --- - -- <br />�s <br />i <br />CT <br />D <br />e.r <br />51 <br />l� <br />r r�rrrr r��'� pp <br />IJJ > <br />am {1 <br />C0 tm <br />I <br />EXHIBIT C a I <br />