42 
THE AGRICULTURAL UIDES. 
EL эш 
Altegethe 
tale of Irish agr 
culture has —]pyet e ha 
Wiha rapidity of that nare es 
m gatisfaétorlly gathered from them 
Havtsc conimenced a series of v last сар 
ART UNK 
is 
pe very. easily. attai , ће | 
discussion hans excited. and gaining end je 
this matter, urges us once тоте to our task ; 
that эт уулы м Кае drifted snow, all of whieh | 
will have may be setting some minds upon | 
the Toren ida will this downfall find its exit ? | 
and are the channels alon 
he great proporti 
who Eus во comfortably sited, a whos 
faible pipe-layings and bee eye penu 
form during several months in the 
i егор 
Mini only alf 1 
ural or 
e purs v all inicie: of | 
imes, — all difficulties, with more 
ailu 
| dra ше D 
princip ев.; 
| r than 
| once in existence, may evidently be m 
| improved by applying one > of rul 
igi of their Teepe 
not conten 
e quite irre- 
| 
m domini 
former margin nclosed 
eltas and marshes are all held under this най 
bili gain, if man will draw off the volume o 
ES water vuturally d ught in some inland lake or basin, 
x. hifo sak 
r the sake of filling its hollow bed, he must 
pu. the charge of permanently baling out e the ја 
s inflowing rivulets and Halae T m pumps, as 
.|in the case of “ Whi 
809 dar effects they ought—this que becomes 
of great consideration, and awaken coricern. 
It is a prevalent error pa: the gracie 0 
reat scale only in 
e ut d to baty 
in regard to strea eams. that Nature 
w channels 
ou please, 
ir imitate imperfectly upon your fenus and m 
the rivers which form убит models on the verd 8 
epe pto surface; but beware 
Roig or. attempt te 
заре; > Неге а 
b 
or div m 
4 
8 to. 
финн an upon.th 
ism oí 
only 
orks. of d а ОЕА аге T са 
d. Mee ө, а lies. to 
av T 
бнри  DENTON «pz (nd 
sent system ы reversing the de 
r. DENTON con- 
tendo. to` failu pis! pt at 
опеё А ecd and main mee i tbat 
the best plan now wili ^" to work by co 
ihe or CC erse order UE: joe tasa Р * Yt is with 
ihe т mon "ade dusk ак "now жн ose water- 
^on which no which peculiar 
water interests are жае i аА ча nevertheless the | 
arterial receivers and Кок of the drainage and surface 
waters the higher land The following. then, is Mr. 
ggestion =“ y" the larger proportion of the corn 
lands of this kingdom are the higher are so sítuate ! 
bh the minor arteries n outfall ditehes receivin surfa 
Мату in waters 5 to the mill-streams what the ordinary 
кый wen ‚у 
{no edet mi ils | 
veo of any landowner, prejudiced | 
reupon report the same to С" 
direct, after no have 
given s ons heard, such works of cleansing, scouring, 
Meer Praten and в! 
vis vas ex mean to be executed as they | 
е ркорег, with funds сымы Ri et Seir ihe | W 
OWnerS, n. shares proporti VI Vict ор. t 
works. As се EERS now Pianis T6 М, Е 5-4 pra A = 
et sen.) the necessity o 
y and delay. tro jun 
a8 an 
thé personal anno es spe 
opponent toa ca 2. neigia who, peradverture, ce o армада а м 
sem E A "ns a € for eosts 
Domen ‘other invidious discomforts trou 
proe the Aci—render it practically nugatory.. An 
all, the Act contemplates merely the cleansing and scouring 
of rec ne ditches; no 9 made for widening, deepen- 
wi 
ich it is w wasto of money to interfe with them. By the 
piment of а Е pe € officer ivi] р fact, Fs od ie 
с prosecutor as we ш ie neer for the dis friet 4А ait s Med 
нн will Беатоідей. s к. 
ult to find 
jneers who MI perform the local duties i 
ftably to the eóuhtry and to them 
t m iem of general 
е su e cg were 
DE Am to be «ды A ia, кт 
"drain ны 
remarka, 
пот» estuary, bnt. immem sal sa 
ne 
an 
ently say. that if such/p 
TM їп tbe d [es s А7 em Con b 
— 
mbering it 
urnish it with extra facilities ла drynes 
warmth suited : эч now vá omini. 
me thing o be either. upon. old 
eclaimed Mew fe that ; d — requires the 
тег amount of outla ay iis exer 
ultivable surface T rud rd may Mr 
w fo ny e ply in o elasses, one 
(Prisma the Martine and m subsoiled tracts, Lr 
like well-sloped roofs, shoot off descending rains; 
the other embraci cing r 
e of which, 
| more resemble pump-dr ank 
| which the Vae s discharge d themselves ame 
rs as to 
servo well may | 
agh, mà in like 
а 
| yet to scour out the main st 
and water-weeds innumerable 
ly yet Ces the dreade 
те?) which we still allow to — ai 
EM ш our brooks and dit ches. 
Our 
| and those of er мэл еу һауе рг ed in their 
orks of general drainage, opem with some 
| information upon the subject of steam e. 
t 
rainagi 
re communications will therefore run in 
this direction. 7. А. C. 
Iris very common to refer the мїїрхевѕ 
WINTERS io lin effects of the Gulf Stream, which i 
wel known to issue from the Gulf o ndn 
е the езүне агі en ida: oe This ea 
of Nw 
the 
Gulf Stream has a certain amount of influence on the 
character of the climate of Britain w € do not doubt, 
i ally very 
"ran 
repon 
on the 
alidi of western Europe, while he- overlooked 
ы тт" syphon or hi 
nas a 
The cai ns ut the x 
mild and rainy, in а we had the tempe perature | 
of A ril with great floods. But what 
ordinary contrast have we in 1853-4. 
temperature of the week ending 15th ult. was gen 
A гае не of the season, the boh 
year since 1 Less rain has fallen in Lond 
last month than has fallen in the same month ^: 
ped а m of à century, 
Wha ; is the cause of this great variatii" 
he four of this season and. that of last year? 
Can we for а moment suppose that it is owing to 
difference in the temperáture of the narrow Чаш | 
which issues from the Gulf of Mexico, and whid 
o great a sur 
the curious curves to the monthly. 
vt lines of winter 
e mere Drei. ofa warm сштеп of water 
i country should have much influence on its 
PARE cem узу North America 
very 
in raising the m 
the changes in the direction wind 
| causes а difference of more than 60° within 24ho 
па the piny r months, The absence of r 
iracts о in. winter, allows the 
Niel m of ice and snow to take place on. 
Labrador camet and in Baffin's д 
In antic, 8 W win 
n 
8 à reserv. 
me inflaenes ; 
elem — en eir 
о they 
hours. w 
Mine. point. 
other 
ve us hard winters by:bringing air cooled down 
and snow, and the Tu of the 
severe 
monly are, an 
heard much аны. те eig the influence ot te 
wes 
Gulf Stre 
ози ae 
The SE, E, and NE. winds which presi 
during the last pand were of a very 
character, They have been quite te different in t 
у 
