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• ' F_�1�559G1721� GME �=ONS!_ILTHNT'� IP�l�_ F-;�1 T-�rr'? F-;=':�= `�=11=P� �Uf�J = "__ '4:l_'� <br /> ' PRD.IECT SITE <br /> Reta;ning Wall Design Orono, ivlinnesata <br /> CLIENI' ARCHI'�ECT-ENGINEER <br /> �iobert �wens E3oonestrao Fiosene Andertik & Associates <br /> � , fn �UNCONFINEO COMPRE33iVE STAENGTH TCNS/FS'`. <br /> wJ ^ ' _ 'O' _ ' <br /> y�, � � u�.. 1 2 3 4 6 <br /> uy ? in <br /> � c�7 DESCRIPT[ON OF MATERIAL � L 3 WATER <br /> m � Z f"" ,� � CONTENT % <br /> � � d u�i m m <br /> � -- -�--- <br /> � � _ � " <br /> t� w � � Q � � � STANDARD PENETAAT70N (BLOWSIFOOl'1 <br /> � } � F- <br /> C� n Q _ �_ . <br /> � � 2 Q f,°C„ SURFACE ELEVATI4N • n"�. �� �' <br /> c� v� 4 }s vi 120.d vs � z ,o zo ao ao so <br /> Daric brawn SANDY SILTY CL�Y, trace <br /> 0.7 gravel, trace roots, grave! - (CL) iToRsoil) <br /> �SS Brown SiLTY CLAY WITH SAND, trace jo � <br /> roots, gravel - firm - (CL) (FILL} r <br /> � <br /> r <br /> e <br /> t <br /> 28 t <br /> �SS Darfc brown SILT WiTH CLAY, trace raots 5 • <br /> - loose - damp - (ML) fPossible buried , <br /> t�ps0il} ' <br /> t <br /> 1 <br /> l <br /> � <br /> 3ST 5.0 • <br /> �rown and gray fine SANDY CLAY, trace ', <br /> gravel - very stiff to stiff - (CL) `t <br /> � <br /> , <br /> 5 <br /> 4SS 16 � <br /> i <br /> , <br /> ` <br /> � <br /> i <br /> 5SS �fi � <br /> 10.0 <br /> �nd of boring at 10 fe�t <br /> Hand auger used futl d�pth <br /> Borehole backfit(ed with cuttings <br /> Biow �c�urits obtained from an $9 pound <br /> hammer falling 11 inches co�rQlaied to a <br /> 14Q pound hammer faliing 34 irtches- <br /> WATER LEVE!OBSERVATIONS BORI1dG STARTED 6I�fi/93 <br /> W.L. Groundwatet not encount�red aME CONSIJLTAMS.!NC_ gORlNG COMPLETED � 6116/93 <br /> G�etaahniool�M�uri�•Environmental R�� �anc! Au �f �R��-�-E� K}`�K <br /> W.�. while drillin or after +�oao z�.�a„�^�.r+o. <br /> Mi�ne.poiu,MN 6b647 pRAWN CK APP'HOVED ��R <br /> W.L. dfllll(t {e,s�s6a-�esa <br /> JOB# 3766-A SNEET � D# � <br /> Borin caved at 1.$ feet afi8r au er 'rhe stratification lines represent approximate boundaries <br /> removal beiween soil types; insitu tfie iransition may be gradual. <br />