Fort Worth daily gazette. (Fort Worth, Tex.) 1882-1891, 1886-09-05
MOYHHR HkRYH'S SHAKE.
contlnnoA rom FIral Paae.


rived that che character Of the scene WAS
changed, They ran about In crowds
wi cries. "DOwh on your facel'
iiDown a. your kneeaii miserable sin
ners, pmy 10 0od2'i my Sister, my
brother, prayi pray pray "Don't ]
toll you. The night III comop
Prayer meetings we're organized ana
hinglnR and screaming was kept uprntll
daylight AZ that time thc watchW0rd
WAS passed ar0und ''1he battle Is over,
but soldiers must not rest, and this or
der Was carried out on Wednesday and
Thuradey nights On Thursday night,
however, on Marion square, tbs
sights and scenes baliiGd det Grip.
tion. The col0red people, unre.
strained, committed all manner 81 frenkled
crcensea, a report Of thelr actione ~
they took place would perhaps DO cOnsld-
cred blahphomOua, Tho first object, and
ono that Interested eyerybOdy'a atlen-
tl0n, Was an Aasemblage OF colofod boys,
about half dozen In number, who had
fallen 70 the ground In n paroAiem OF re-.
ilgious frenzy, They were gfoyeling With
their faces down In the grass and were
singing a hymn In n loud voice. The
hymn was "Ihe Angels RappinR at the
Door, and refrain sung rapidly was,
"Oh, tell old Noah ~ M oh dc ark, W OH
oh do ark, 70 III OBJ do ark.n
This fonR was repeated over and over
again until they were quite tired, and
ceased from exhaustion. In few min
uieg they we're taet asleep
The following additional casualtes are
reported
Miss Lucy ELLIOTT, ankle fractured.
WM, fIpDa, knee tliHloeaiod.
JAMIE CALLAHAN, avrlouAly Injured In |
the face and Jaw.
uKoRnn WFnD, skull fractured.
FRED hIMrgos, coiored, OF New York, |
double fracture OF left log,
MAudIe SANDmna, white, amputated
foot,
A, - BuLwngLn, head bruised aud hip
injured,
IlAmy AARoss and LIzyiE AAnoEB
white children, cut and bruised
MoHhs nnowN, colored, ianltor of ost
building, Lex amputaied,
0ADBpKN,
Lucy JAAlKH, oOlofed, skull fractured
SAN WAITING, o0l0rod, arm aud Lex
fractured,
olAhtrs EIyrRa, colored, leg ampu.
tated
ELIZA FtowEHs, colorod, compound
fracture Of leg,
MARY DELANEY, oolored, leg ampu.
tatcd
MANY wnIaAMa,colored face aud head
badly bruised.
JoserinNN cAmrnrrI, colorcd, scalr
wound
ADDITIONAL DKArna,
ILoRHRon llE0roR,
SARAu uLoVRn,
MANY LIRE.
The total loss at bummeryllo IN est.
meled at 100000,
TIM suENoE on m.
AllAnINHruR, n, O., Sept, 1.-THE ,
News and Courier Haysi There can be- !
40 doubt that the various earthquake !
hhOpks had their origin In tho ihlAnda OF \
The Medl I0fanean aud Greece and Italy =
Dn Anapsl 50 there WAS reported tho oc- I
4rfcnQy "a destructive earthquakes 1
hs.sRnVI.t Greece and Italy. There ,
90 bpen two eruptona Of Voauyius aud /
40 volcano was still very active. These
rhptluna gave vent TO an internal com
loton which has produced tho quallng
~ the earth Ia this vicinity, but the
shocks, being communicated 20 tho earth,
have travelled In various directions, In
acme With moro violence than In others !
~ they were felt tho same day through
OUT Egypt, nut there doing little damage
The shocks seemed 10 extend westward ,
with more rapidlty and moro volume than I,
IN any other direction, and vibration of +,
PARTICLES OF the oafth'B aurfaoe beinu ,
under tho sea at the rate Of ,
about ono hundred miles an hour, occupy. ,
lnR about Aeyenty-two hours
IN travelling distance Of $500 /.
miles before reaching the western
shores Of tho Atlantic, Travelling as II
did, almost due west, one OF the nrst /
pninlA ON the shore which Il could reach
was tho coast OF South Carolina. Hut We !
SOC y was felt along tho entire coast M
lat hortn ~ hptton and spread across 4
The continent with diminishing force, an /,
various more solid aud rocky porllona of /,
The surface crust retarded lta vibrations :
until " seems 10 have been almost entire. ,
g stopped by friction IN tho extreme !
northwestern states, The reason why
mo shocks were more violent IN the vi.
llniy OF charleston IN that thoro IL more :,
lt a0tt, yielding nature In tho superficial
appnr strata which conducted this yihra. !
Hon and forward movements OF the earth .
Ihe waves meeting with less feslatanoo :
Ihen from the hard substance farther In 2
NE interior, were moru rapid and Iefky, y
aud shook the surface withmora violence. !
Ihq presence OF innnmerahle assures, OBJ. :
iervahle In the city ana country M far as !
auhmeryillc aud beyond, IL accounted !,
W. ~ hho hhHhN hOlN hAhttflul ytVluluu =
rapidly 70 the pressure OF the Garth waves y
which pushed up thin orusts aud =
,quee1ad out tho water and sand sub, \
Iect 70 ~ pressure, Tue blue sand '
and yellow sand thus emitted are found :
N thc upper strata, and that II came nom ,
near mo surface IL proved by the fact that !
no mari u found Ia u, aud Il hOglna from !
.lAV'fve 20 ninety feet hollow tho sur.
lace and extends nearly 1900 feet deep y
10 show avn moro eOnonsiyely that the y
wave motions we're confined tOa very
limited depth beneath the surface, II "A Y
lnly necessary 20 state that none OF the u
lhalloW or four hundred foot artenian u
tpha ara 81 all affected, OF IL there any .
'hRuge noticeable IN The iiow OF quality
y inc water from the two deep artauian
wells az would have been tho case II the a
'Ausen 81 me earthquake had been local 4
u deprecated, iss 0.ll O5 !,
IhAt the statement of tho communlca 4
lVn pi,sho lone wAve 10 Aha en0nmous dis. 4
ence lafnlly verified by the observations 1
y previous earthquakes Hinou and even /
lrioFe Me Christian era, The nhaeueo Of \
uaa wave proves conolMsiyoly that the h
Auso q the disturbance was eoaanau Ia
spu, and The lHrky motion concentrated a
2 w eNftn - reported w@a caused hy
pfhpEl yloFallona intermediate between 4,
% rapid forward motlon and nlo,ser a
awkward jerks /,
ninOnDRR Al AuouarA X