New-York daily tribune. [volume] (New-York [N.Y.]) 1842-1866, 1864-02-15
true asthma nervous disorder OF The respiratory or
gans has been successfully treaties ~ electricity

Prof bGM In a memoir 10 the IHOSn htit' ~
states that tho inuSOra Bacerums. were found Ia inc
blood OF man who died Of this disease az tn; hospital
OF Sienna
| PARASITIC PEsTILENCE.
VAN RUDOLF LguCHARI states that one-SiNth OF tnc
annual deaths among the people OF Iceland Is sveY
owing to q little entozoon living in me dog rom Will
the arva ia generated which II kept IN m Icy
developed condition. grows 10 an immense SHe Aho'o
arga nfcsl both men and cattle.
NEW HYDRATE or LINE.
DR. JONI DAvY has published some experiments 81, on
lbo glacsiGr of quick limo which seem To warrant tle
less lime than is required 10 form bydrate Of one 70
one the weaker compound being probably two oil hne
SIRIUS AND us coMPASIoS.
The light Of Sirius according TO tho cnleaa'lohs OF
Sir JOHN Herscbel 10 ga times greater than that OF inc
ann n, parallax being 2OCths Of second us as
nnce from tho earth Is 81 900 go OF Leagues. and IT
light 1, about - years in reaching us.
Some rregularity in s motions have Induced me :nS
qe,tion that 1t was Influenced by star companion.
Such star was discovered by Alyah Clark the ceebrat
ed optican and observer Of Cambridge Mass January
81. ie62 Tho January number Of TIE EdiabprSh NeT
YIosoDlicol Journal for I-6 contains an interesting
communication from 4. ~. Stafford assistant at the OBJ
seryatory If Harvard College in relation % the motions
the companion Of SIRIUS IL which the observations Oh
Bond Of Cambridge Rutherford of New-fork and sew
ernl European astronomers cited IN relation 10 the
queries whether the new star IL unconnccted VITA
Sirius a snteilite or tie disturbing body; nc mus
conclude. II H. consequently. highly poDnDe ina.
the disturbing body has actually been found that Wnot
was predicted By theory has been confirmed by ss.t.
too highly felt The companion Of sirius must he meas
urcd for the coming year. and FOR several years. "ho
Sirius tscl. shcad be ro-obseryed wi'h menaiin III
- '''' sEw DEymorEs.
A. the February meeting Of the American Photo'
graphical society. held AZ the New-Iorh UNIVERSITY
Sir. DtcnOcuois described bis new developer, Wale5
consists Ia combining constituents previously ISed
In Photography In tie following manner: otphats
OF the pr0ioE.te OF lion. 40 grains Taer' - hnia
ounces. Af;.- complete solution drsclm OF aqua am
"a al fly
phac 10 formed oHyde Of llon s pecptltId ana aIle
wrrd converted into acetate ~ addition OF acec oclo
in excess Chlee hua ounces 10. 81. Tie coodlon must
be that which gives LITTLE inen,i and great sensitive
mes and the other materials used pc absolutely pure 20
avoid Jogging Under these conditions themosl pefee'
negatives obtained Ia time excessively shorebru
Air CRyN. n practical photographer presented nhe
pctg made with tn new developer ana s'aed 'n''
PAPER NEGATIVES. $500
At,he zane meeting Mr.. II. j. NEWTON exhibited
specimens OF paper negative. prepared by Nun WIN gun
bcnxor dissolved u alcohol By MI ions pfoves,
the graiu OF the paper j. 30 ongcFysihe fh"i'sIbPl
made from hese negatives we're also exhibited ana
TIDE WAVES AND wIYD wAyls.
The reg ular sIb"c, f0: dircu-sions a', n'u i"
Movemc lis and their Useful Applications Oy ID .chsu
In was then taken up. Tie following rNa.ss Ne'e
~, nrofonrd Kepicr was tie fret 90 eHil1in IN a
gcpera nav tho cause 81 tides by iriurion, appaI
entity unconneotcd with deductions ON Us tnTd gruhu
ccle.tin law he proclaimed "thrt all bodies attract
each other tho waters OF Tie ocean arr ~" D." 'D'',
bed b, Tie earth but elevated under The moon ana
on the opposite side OF Tie EARN because te ehItn
ga attracted hy the moon Than the nearer Nalrf p
more than tie vaters the opposite side Inc mhtne
moics dcmnnsrr,inp thn, t6s power u tie moon and
IN this respect is ~ accordance WIN t.s NV %
grnvitnton was the work u Newton: out n' eiIlI
br.m theory could not IL satisfactorily tppfd 10 sh
the phen1era Observed. II was left Tor LaIaee IN s
treatise Celestial Mechanics 10 cxp IN se aAtey to
many apparently dscoIlant move OF we - ~
what Is know ~ the dyDaucal theory Oh tiHeh. /.
which the laws % hydgody asmlcs tpYe Al iml~ten'
application. The cubic measure OF me ocean - essl
usied At - millions u eabc miles az aAl13 , es,'
atty as found two miles below tic surface hs ne mean
its et Is about l7s6th q that q tie whole giope
Although the is 3Jj co.. times heavier th9n me ean
upon n ocean ID far hes than ths' Of the body ony h
OF the weight OF The carth acting a, distance - 240
900 miles. The moss OF ihh sun Is more than - 10000
times greater than e OF the moon but being te6 times
her diance from the earth tho hight Of the tidal wave
produced by H. compared With that aissa by the noon
Il g 10 100 Wien those two attracting bodies are
In conjunction or are on opposite sides Of l1e eaftni
their joint action produces the highest water caled
the Spring tides. When the moon l. IN its lugdraures
that Il 90 from The ponis OF conjunction OF opposition
It's lowest effect is at the point OF !hS highest eject Of
the sun. and thels Joint ide-she dits sles II Ne sep
erale elas Us call &c Nsap tide The rise Ind isll
o. Spring and IL Neap ilfes are nearly as seven 70
three. The action Of either lumlnary consists in tie
difference Of the attractive force ,4ered ~ L on ,le
solid corc OF The earth and us covering the ocean and
the effect Is 10 form two waves on opposite sides u the
earth Were ihore continuous sea On the llne OF tie
Equator tie guoa tidal primary ave would move u
the Rate Of about go statute miles per hour but the
sea 4 broken ~ int three great basins, and tc.r only
Il, tidal movements axe S9mphe',sl ana
gFca,ly diminished in velocity. Ia eaeh
| basia the wave must start anew from
tie Eastern Shore bnt Ia the Southern Sea the circular
course unmpcdcl. IL also Spreads Rcluss the three
great basin. dingoually. 80 ~ 90 oyeriaAe anI con-
rnlAs with TIE tila wave proper These comnla gng
wafef tho regular currents Of tho ocean, ITS varying
dept, tie shape o, rs shores and tnare ~, causes
OF prrb,exty IN tidal calculations. Yet through al u
mas be perceived TINT Poe . g.e corresponding In
g. s-,nian ual riso and fall with nc lunar aY Of -
| hours and - minutes.
Fox detailed description OF the tides OF or Atlantic
coast IN the Gnif Of Mexico and u She iciRc Ocean,
refrovcc should he he 10 the reports q the Cn.!ed
state Coast sn-,cy. These annual quartos contain
vast iupl OF information. which seems 10 be progden
italy provided for the nee OF our navy. Nhent charged
With tie duty II guarding great extent OF coast. The
phenomenon " The meeting Of tdewayes occurs daily
m oar own vicinity Tie tide, which Is nearly smut9.
neon, along the sln heai.ands Ok our Atlantic coast
enters az Montauk 5.at and Sandy Hook IN about 2,
hours the waves meet al or rcnr Throgps Neck one
having travelled through Lons Island Sound 100 miles,
and the other through tho East River about 80 miles.
The dividing OF tho wave from sandy HOOK. NO the
junction OF the North and East Rve-s, the nsrrow
channel aud the natural DISTINCTIONS az HelHa1e VIII
| account for It's tardy movement
The range rise aud fall oi The spring tide at I'M
porant points is follow: Az HGyrc France. % feet
At London, 49, a, Liverpool -0i at Bristol sking
Road a; at st. John. n. T., -; az Saesyle. \. H..
90; ut Qgoboc 49, at Portland, %, at Boston, l.3, ri
Now Haven. 6.2i at New York 81 West Point a2i
Albany. 20, Philadelphia, o.6; baltimore, l.5i Wash.
ingion 81 Char ston 9. a little less tbin ono.haf
OF each Of these sums would respectively express the
range % the ncup tide
mo dcclnaton o. the has importer, relation
10 tie periodical decrease In the hight Vi te tdcNHyc
| IL viii be readily perceived the waters cannot in.
sauty respond 10 DE power OF the moOn and there is
consequently hSsis Of the great primary wave.
UsEPUL APPLICATION or TIDAL TOWER.
| L. The lido IL used 10 register lis own movements
| a. splt r II