The Daytona daily news. [volume] (Daytona, Fla.) 1903-1926, 1912-02-21

m enc Can @ssrwRs Iss Bean9s-sran-
- sssekm Mssshsaa n TAoasana Tess
Tsssaa absut Lzks Pebsss&
a pond truunied ~ pebble glT@
cnmurehemmawe sdam q the ne<han1Szn
% aAe pmrpeenaf m0<sO1 81 tie oce1n-
now slow. regular AID majestic rzn-
nEne fr0m herzsoa 10 h0rz1Da- Bow
rzzakang IN ua@0verzAbSe f1ry zgzA1sE
de land Whea . pebble fails II
pu16 e peodnees = A1e circular hae
which wtaeas. mnlEspagfng anrSl stop
bed b. - boundaries last - i pro
dueed the surging e tie So
re judge from appearances. the
swezia transport the water toward the
eireureereace Of the psad IN p0anf Of
fact they Do a0shing Of the kiEi - :
easily pr0wed By match o. Splinter
% woOd beng cast upon the water
TIE match - hardly raised OF lowered
by the passage 81 the swesl- The action
IN exiG3eaee = sGEply the t<znsLniss40a
oe E0TzO1. nof the Transmission O.
Ezatxer
The ane waves Of the So are gen
SEATED by the wind s. 6ne waves are
ge0erzfed BY the wind when il rlpp2az
. aesd II grain ready fer the AGrvs$t-
gran are real waves, often wares Il
aeree sr&E0z- The spears 0f grain sre
tmnOvahay axed % the ground hy thar
ra-CeS. h1f every bsszse transmits is g.
I ckIlato-y movement 30 the B=xt 8lzsse-
/ jest 30 E3qaid molecules are formed
In the middle Of vast OCEAN. sleh
- the e9EATor1Ei Af2zarlc- for instance
great regular ua1aazraoas are sen uul-
tspsyfng IN parallels ike the furr8ws
IN vast psowed sesd On the bread
ocean the liquid mounds Of the sea rsse
With every swing With mere - -
e~ea regularity
/ TIE mariners Imagination has Ezven
/ the great waves q the high 50 the
! reputation q fabulous hesght- Resfa-
! be aRtbors hare talked q wsv@
/ Dognsn.n hfgh and 81 waves 10 faez
/ n height Exzcx measurement has glr-
I "a closer estimate.
L TIE wa~e< q the hsgn SEA q ne ms
+ sor oceans, zrtaIn the Aeaghs q afty
[ feet under the exceptional conditions
Of a TEMPEST IN the vseiniry = Cape
Ho-n AID the Cape 81 Good Here
1 The sIrges here estimated are fhose Il
free Circulation o. the high 49,
Whez 9 wave. whatever IS strength
% It's weakness, meets = sesid o1seacfe
whether that obstacle - 5 rocky cir
Ok 8 ship. the swell rebounds % *
trzocdiEsry heights Lighthouses aEs
often s<eEt y tie - fr0n bs$e q
summit
TIE leagsh q waves : besven
twenty and thirty Zines thel- height
and the slope o. the seas hills : vsry
gentle 4 wave sixty feet high :
somewhere between 1000 aid l-2s
feet long
At the axis Of the revolvIng senpeSt
called cTclo0e there are Esany Eavs
systems. moving IA al d1recEso1s
meeting snd combining Wen me s.
clone Is In acton the 50 ! sid 4
burst IFS bounds.
At such s tine Al regularity - Eavs
succession ceases, and tAe ~ ra1s
Wild, with force bey0Qd human p9Eei
% estimate Blocks .. granite weigh
luS from 100 . I1ss1 tons zre caUght
b. the So and relied Ike Pebbles &
distances % 80 FEET ard noCe, aaE
sea walls are splinteTe,5 as b. hatch
ess- The tive pover- o 3 fargG.
50 5 estimated b multiplying =.
mass q tie surge 81 the square - a.
1 speed
when The sur. fE1Qe5led by the drtvt
q the bzoaf 50. meets : sold obsta
] &c It's pressure ! thirty tors Re
square meter 81 Earer- This estimate
: which + close, explains h9E wa+e-
whea co1tin7z17y sapTt1g the tcoe o
elf. breaks doEu the aand- force
back TIE shore nEs ald Hrtie hy a-Tle
constantly s1d surely. iIegeases d
seas domain
4 wave ron g = s. feet high Sc
625 feet loag-slch wave Is the e
Trod2ces ever eighteen secoads-7el
reseats power 81 about 1-Sll ho-se
power. steam, =. square y4r5--aa:
] pey's Weekly.