WHERE IS DRAINING NECESSARY?

Lake Wakatip Mail, Issue 2787, 4 October 1910, Page 3

WHERE IS DRAINING NECESSARY?

toai/Ofc-"Wncneviif affier ! rain water reti,i*iiaiast in the fMoVs;bV 'stump hoYes. ,„ Jog •)« WHetf Ifte soil Mstitfci to Ml shoes or hbreea' *eet aid farm tdold.^ 3 in tH' f .|ootj>4ntß of, ~a. horse or other anir ,j j hh&&. m *-* »! " y *-' rJ " fi *~ : ' ; ." 4. When anupals sink deeply intc the soil J IK I. L '¥ Wfip t&i'rayfl cStwi sunform a r hiw heavy:;rain;the■ little holes in the ground rshow more I '.) m il»ter in them than in other parts; .; .LioH 'rain'a stick is'trat'lnita.t 1 • tee ground ahd taikeh but, water. wiU :1 f p;;¥fee.lb v :,'.','..'_ ~,;.■.'.: • CTqps will. gray better when " 'land is gathered up into small ridges. -ECfjr,a6i;,:thftiflEst! plaoey • weoget rid: ©f the; - I'siagnant iwater, both on the;'surface. Qdi and held* it. Stagnant "Water his an' effect on vegetation,. it is a } 'its iit : nof j^erj,ftoiß li talf4ng:.: ite. place,oi Water Vs l held J in,.suspension' is detrimental to .L-jirjlaafr-Hf*, and «ust be • kept -moving, : -■solift spii atttf leti 1 air in. after it. .;v. r , v ;^'^i.7~' iKi .'. ~":' Ui •:•■ tt 3ffi j its stagnating and souring the -soil. -iai-JSP.b-WWWS .iunless. peAaps ri'ce and ed Moth* can-prosper' in b wate*4ogged Itihdr '; ' ( i .Jim: ■■■...-,. ,I'.'., 11,,'.'. 1 ■'■ 1JJ...1. .■■■■.■■J.-/'-'---