_ узаган 22. 1862.] THE GARDENERS CHRONICLE AND AGRICULTURAL GAZETTE, 167 
the op n wall is given, and n s [bz of vg they would һауе had to pay the Water Company | аз if, in ancient days, the spot where Kensington 
e Tone bid thoroughly ventilated ^y sen otio bé US e: voi Pour Should | Gore now stands, had been one of the deep parts 
ur, and hangs long on the й ^ be found necessary to е. те what was required for them | Of the basin in which the London clay was being 
' being forced gently > а & pit in à 1 н › à 
к а Ў i b on, Amos & бош 
i : оаа. for instance, indo two are the only instances in which 
d in such abundance, that, i : d j ү С 
early 3 feet apart, and the 100, 000 15 110,000 gallons" posteg AULA ee iom it has occurred. Whilst boring through the chalk, in 
y eee liberal га the row a А m. it can readily supply a million  gallohs in that | both cases, ША instrument came upon a fissure and 
f room for qum : ture, an rger pumps and m i f d 
гета n roo SEP ош mploy ed. Tht r total pate i М" SEL n ap org val күз down a space of : several eet, To un nues 
in; 2 М 
ere in a pit Ms an осна ай ar zied down 7 SON E n PP ad 3 barp then % | the e way in which th rin the chalk finds its way 
d mpanyi: Te бойо shows the nature and | to the surface, or into ^ sea, is though such fissures. 
r roots, which a e Sinte red in | depth of "the geological чан Аж: through which the | An example of its finding its way to the surface from 
the sake of contr; them 
well passed, For ast, „а similar * cub of | day e seen in the river Wandle, which takes its 
are forced in brick | the Artesian well whieh баев the at Carshalton, near Croydon, pouring out 5 its 
; for | fountains, the Palaces and Public Omes 
‚ їз placed 
Although no pred z it. ҮР p r sketch, so yw " the Simia | instance Lj T bmp 
be 
/ into the sea out of such foni 
ek with p^ {бауын pr вооп generate suffi- | their dept ncerned, very well represent may & low water n ear Brighton, where a 
th. French Beans and o ther A crops of| ihe usual relations ot these as found i in numerous other 
stription are also grown in the same and in n | Artesian wells which have e been sunk in the I 6 incl id 
s and all other houses where there is Ме Ач of | basin b m +} 
ui an immense ану of fresh enin 
Such {А act as the main channels һу: which the 
iety differ somewhat from the p ruler 
Г by the Soc 
1 a ridge and. furrow-roofed conservatory attached Тойдон ау, especially, being found of much ih oe 
water i in the chalk finds. its way to the When а 
mansion is а collection of large Orange той, depth than is usually the case. It would a h f these, 
xt of which though very old have recen tly bee 
th ng the e terrace 
g effect. In Pies ROYAL rr El ы Exo ане rs WATER- 
i RUE E SOCIETY: WORKS' WELL. 
Pk е ан of Engine-house Floor. гарии ouse Floor. 
Among other sorts are Winter H æ [ж Earth. E Made Earth. 
T Monarch, Easter Beurré, Beurré i n 33$ н aii inc D 
us Meuris, Prince ce Albert, Josephine de : 125 Oui dE d oz { " И 
deren Passe Colmar, les also ll [2 little water. і Н 
5 Whose walls are built hollow, and it also | 2-85 Po [s 
hine ter the walls are covered with | : ; ЕЧ 
frost. In spring the latter Н g 
ing plants, ч i 
mS an of the kitchen garden "e H 
with healthy treos. The Peaches ї | 
are in excellent , Condition, and promi: E H 
L dint стор "Their P o © | London, 
аре d Hemp covering manufac- - Е 1 eT 
ч Knnisford eshire, аё about 544. a yard ; i : 
"py HOFA ah. "being in Water level in well. Blue Clay. 
it forms a close and s = H 
durable. Th s == Топаоп, H 
1 ixture of soot, © == Н 
; but instead of E pe i 
ters brush it is put on = Blue Clay. f 
е, which does the work sufi- & { 
be it could be done i3 
Г 
| nr т а Eier or darker tint 3: P Mottled Clay. 
®! 
3 я + Band and Gravel. 
3 gz $i s 
5 СЕ Green Sand. 
t & Н о 
akaa | 
E i 
e B 
У Mottled Clay. p 
У Pebbles and Sand. { 
B E Chalk. 2 
^ Green Sand. » 
E Running Grey Sand T 
Flint. 1 
H 
Chalk. i 
it $ d. d nt for ^ Wet Nass Y ДЕА ө, 1. у £4n: £ +} £v, нае пой ад 
+ Tounding cl hits upon | кач, Trudgar Square 
t | a fissure, it draws its с=з Зы а stream itself, and | which was sunk in mi ihe passing Ө of 100 gallons а А 
it will, or course, depend upon its size how far it may | minute for 48 hours lowered its surface 4 feet, and it 
be exhaustible. The quantity of water кыы ing has ever since maintained the same standing-level, 
MUN through the chalk, however, is so grea и that for all | varying only with the season. The — well has 
Шо aapply o СЕ d walat ordinary purposes, any well sunk for so G depi. їй » only been lowered 16 inches by the same amount of 
tolis sufficient. Ifa very large supply umping. The y of the Societ s wel may, 
only drawback on such a well is that it may be rede therefore, be fairly тыш: to be many times larger 
dso | by unusual or continuous pumping, so as to require | than that from the Square well, which pre- 
ed | some time to be given to allow i to refill; and that in | viously was the largest in London. 16 will also be 
со ti i the standing point of the water gradually | observed that the «іо evel of the Society's well is 
sinks. a well which has dropped upon a fissure, on | in point of fact actually considerably higher than that 
the other hand, may ap арра ied be Mage ep for ever|of the Trafal - This may perhaps be 
od | without lowering its g poin ws its | accounted for by the greater number of other Artesian 
su vin а Tunning s xm d "Y - мы! eastward of the latter, and possibly 
applies pu as it wi иу as аа бай wells irs 0 а ] 
as it is pumped out it flows in. This remark, however, | also by its being nearer to the outlet of the water 
only applies to the ding point when it bas once been | The lovem may, therefore, congratulate кг оп 
found; for after the well is opened and first tried, there | possessing the finest well in the Metropolis. То form 
