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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.

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