I" '" 4 ~ - 'I. 4 Ja - '--.. .' b~#e Brettv maoch all the time in aracter of the soil and oae, in -r ubhaoil some parts of the country, i, than the conditions of the air. Isorme valuable statistics on thih imnoture, or a stiff and Thoroughly drained, is midst almost as i more importanaqp Dr. Bowditch has point. A soil retentive clayey subsoil impervious always prejudicial to it,.and the health of Abi4abitants. Parkes* says of soils " Some soils absorb and rrx a water more than others." passing through rapidly " Sand absorbs very little," " clay ten or twenty times more; Shbrmous or common surface more than forty or fifty as much as sand." soil, in this respect. In he able on account of its heat, " The sands are therefore the healthi- countries, unless it can sand *is be covered objec- with The effect of glare on the eyes 0u this becomes a very important point. tion and with a white surface, must is obvious, and If a spot, bare of be used for habits- some good result may be obtained by coloring the houses blue or green." "The amount of dust given off from soils a matter no soil of slight better moment." capable With of fulfilling regard to permeu- this requirement that of Florida, as sand the predominating and some- only ingredient in the localities where invalids con- though is not always to judge a nay more than the other constituents'of her climate by f.V& P r'nae. i$f almost fl theeoil In some localities the soil, pure which has the appear- sand, being quite productive. is permeable. But every- Palatka, unlike any other locility BtAte, is covered with a sod of green grass, for whioh s no one has been able to offer any conclusive explana- I obviates here ndy surfaces. a^ -* V. - many of the objections urged by Dr. comparative valid& nuf exemption -ft ag from l4 ^ *AJ -.*Q:.T 4 I C~ *f .i S1 i ; IfY -I ,' ,-! :fl~r* . -1