Albuquerque morning journal. [volume] (Albuquerque, N.M.) 1903-1926, 1910-03-16

ter supply for we have more snow
than AZ the same time last year Rcd
River, J.. r. P~cnn-tsnow is driftcd
and swept into canyons, the outlook
Is good for plenty or water. The
snow is heaviest In this locality for
years. Taos. A. Gusdorf-The snow
Is oyenly distributed ana well packed;
there Will be plenty Of water. Chi
mayo. r. Vigil-Thc snow is compact
and there win be enough TOR water
supply for The season. san Pedro, N.
j. strumquist-We lad zen inches
during the MOI u. an melted except
on northwest sides Of mountains
whore thorc remains 6 TO 10 inches
OF compact o SANTA Fe, f.. owen
There was no material decrease In
fhr mount OF snow over The noun
tains and upper canyons Of the Santa
Fe basin. now remains deep and
compact and the prospects Tor water
supply for ensuing season are excel
lent. Bland, j NJ. Morris-rhe snow
IS still very compact ON the north
slopes. although melting rather fast.
Prospect for water Is good. Pines, T..
g.. kinnisOn-We have more nov and
water here than for many years. !
BIuewatcr. J. Havana-The snow is
heavy In the mountains of Bluewater
watershed. P~ucrtecito, u. Lopez-The I
on the mountains is evenly dis
tributcd and propects for water are
better than last year. Bosedale. w
~. Martin-There are drifts on the
north slopes possibly 3 feet deep. Ag-
ricultnfal Collego-No snow remains !
Ia the organ mountains.
Poems kAnfppghaI mud |
Cowles, II. -. Winsor-On the north
the snow is evenly distributed
aud very compact, on tho west slope
arc only 2 few drifts. East Las
=. O. Blood-On the mesa
very little 10 has fallen ana II IS
fery dry. Estancia. NJ. A. Romero
Che snow in the mountains is com
)act ana there wiz be a good supply
II water during the coming season.
Arabeia. c. Warren-There is con-
idcrable SNOW in the CAPTAIN noun
aims and the outlook for water sup
'ly is good. Bonito. q Braune-
for water supply is not very
God SO far. Cloudcroft, J. J.. Bailey
nd T.. G.. Parker-Thcrc is very If
he snow in the Sacramento noun
aims; II has been q very dry spring ]
II snow melted except occasional I
riffs on north sides of mountains. !
ARftA ' 1ltVhffh1i VI AAiis
In general, the snowfall during 3
'ebruary was less than the average, I
much less than for the cores I
onding month last year. There was \
number Of sharp changes in tenn c
erature. the alternate warm ana cold
oells being very favorable for sci {
ing and solldifyine tho old snow. I
As compared with the usual depth G
the close of February, there is q n
rHnfDFVa4s la oil ~ 4sfp- AT flA platte ! 4
rainage area. Conditions are more j.
Worable on tho upper reaches OF the /
rkansas ana Rio Grande, the aver- a
&c, or somewhat more than the o
depth being reported. At i
gh attitudes the snow is well h
lcked, at moderate elevations, where e
e DEPTHS are not great, the condi- Is
IN OF the snow is favorable for early
on the Grand watershed N
deficiency is noted for tho tribu-
rics rising on the slopes of the on p
rental divide, and about the average IL
+ the more westerly part of the +.
ainage arcQ. nor uniformity is ~
lted on the watershed of tlle Gunni- 81
the majority of the reports show ~
g the averawe or somewhat more ~
an the average. For the Nampa q
d White a deficiency has been the ~
le. For the san Miguel, Dolores, q
a san Juan the depths are less than "a
ual. but in the main they are Tor m
e wen settled snow that fell early eV
tfHs sn0ron. ~
Rio Crande watershed: Creede- m
IA depth compares faVorahly with ~
= average for this time of year, IL pa
WtN packed ana tdriftcd. Hot w
good flow is indicated. ~
spgr-The fan during February was &c
Osier-The dcuth from 5000 ~
1 I. mn fs.st as L.ftsslt.,A IN NH a. 4 w