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etween We points not et the earns fevel<br />
retstive to a spadfii datum.<br />
davo staflon-l%at *alien in a given system<br />
of stetiena that is cxmtrofbd trf the meater<br />
station. Also called remote station.<br />
divwa+digifaf) Pofyws formed when two<br />
diimftt ~fw.a do W *@ abng e single<br />
mrnrrmn ne and leave e smell SOSCa between<br />
the fargertwo.<br />
xdopa angle-The angle between a dope and<br />
the horizontal.<br />
slope chalnlng—See slop. taping.<br />
slope correction of tape-See grade<br />
correction.<br />
slope correction-l. (hydrography<br />
surveying) Tha correction applied to soundings<br />
ermneoudy fxieilionsd as a resuft of an echo<br />
smmdar rese”wing its initial return from a point<br />
upslopa frem its racerdad position. 2. (Isnd<br />
surveying) See grada correction.<br />
slope taping-Taping wherein ‘the ‘Iapa” (or 4<br />
chain) is hakd .s raquired by the sbpa of the<br />
ground, the slope of the tape measured, and<br />
the horizontal distance computed. Also cslled<br />
.Iope chalnlng.<br />
Elope—See gradient.<br />
slot cutter-See templet cutter.<br />
slotted templat—A Iempiet on wh}ch the<br />
radtals are represented as a slot cut in a sheet<br />
of cmdboard, metal, or othar material.<br />
slottod-templet plot—See @lotted.<br />
templet triangulation.<br />
slotfad-tamplet triangulation—A graphical<br />
radial triangulation made by the use of slotted<br />
templets. Also called slottad-tamplet plot.<br />
Small Wettad Area Twin Hull (SWATH)—<br />
A vessel designad for stability by having ils<br />
buoyant volume rrmstly underwater, presenlly<br />
being avaluatad for use in hydrographic<br />
surveying projests.<br />
small circle-A circle on the surfaca of the<br />
Earth, the plane of which does not peas through<br />
the Earth% center,<br />
234<br />
smell-ecale map-A map having a ecsle of<br />
1:Soo,olx or Smsfler.<br />
smooth ●haet-A final pbf o! fmfd corrlrd end<br />
hydrugraphc devebprnent such as courrdings,<br />
fathom curves, wire drag arass, etc., to b. used<br />
in chart mnetrucf ion.<br />
amoothlrrg-1. A sat ef pmceduraa for<br />
removing short-range, errzdic variat”mna from<br />
lines, aurfasm, or date series. 2. (itige<br />
prcca~ng) The avereging of dansitk in<br />
adjscanl ar~s to produce more gradual<br />
transitii.<br />
srrakosllp-see ●tch slip.<br />
snap markar—See point marker.<br />
Small’a law of refractloxThis law states<br />
that the sin. of the angle of incidence divided<br />
by the sine of the angle of refraction equefs a<br />
mnstant termed the index of rafrectiin when<br />
one ef tha media is air. The index C4 refraction<br />
can also be .xpIainad as the ratio of the vafocily<br />
of light in one medium to thst in anothar.<br />
. . . . .. .. .. . .<br />
aoftcopy —Products which are maintained in<br />
digital fomrst for use with automsted data<br />
processing equipment.<br />
solar rdtltude-Angular distanse of the Sun<br />
above the horizon.<br />
solar attachment-An auxiliary instrument<br />
which may h attachad to an engineer’s transii,<br />
parmitthg k u= as a solar oornpaes.<br />
solar day—1. The duration of one retation of<br />
the Earth on ifs axis, with respect to the Sun.<br />
This may be either a maan eefar dsy, or an<br />
apparent solar day, aa the referance is the<br />
mean or apparent sun, re6pectWety. See also<br />
.ePparent solar day; moan solar day. 2.<br />
The duration of one rotatkm 04 tha Sun.<br />
solar declination—Angular dktarwe of the<br />
Sun expreasad in degrees nerth or aoufh d the<br />
celestial aquatoc it is indicated as “+” wften<br />
north and .-. whan south of the Equator. Also<br />
called dcrclirretlon of the Sun.<br />
solar ●cflpse mathod—A means of<br />
determining the angular distanca betwean two<br />
observers along tha canter fine of fhe path of a<br />
aolsr .dipaa.