Show the denial ot of relation between foists and tho the amount of rainfall in ili a clitu region by Sc Sebu hubut bit of will ruse little surprise among the american albough ready to admit th h it the rapidity of dra dragage lAge on slopes depends langely on the alic character of their co cov eilus ei lug the weather in this c on haie bac long been shep skeptical about the he influence of trees on precipitation it may be doubted whether Ii ether four years observations afford an ail adequate adt basis for conclusions and professor schubert s opinions decd corroboration before they are likely to be accepted evcic in nevertheless tits hl utterance of fit Is 13 not lot without Nt lout big g kance cance it if nothing more they or are abow how the wind alovis s |