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,/<br />

I<br />

d-y C’$Ndialdata.<br />

Gsogmphk Nsrw*s Procosslng Syskm<br />

(GNPS)-Ths DMA system which includes the<br />

hardware, cmffwsre srsj eras to nminfain<br />

the geographic nsmee data requirsd for digital<br />

maps ad gsztmeam.<br />

MIL-HDBK-850<br />

gsogm hlc (~oogrephbel)-Signify ing<br />

bade MRfbnehpto the Eartfrcxmddamd asa<br />

gbbe-ahapad body. The term geographic is<br />

applied dike to dsta bad on ths geeid and on<br />

othw spheroids.<br />

geographic coordlnat@a-(JCS) The<br />

qusnfitbe c4 fatituda and Iengituda wlriih ds&ne<br />

the~indapnfonffnswf~ efm.s<br />

Edh with respect to thtr rsferenca spheroid.<br />

Also called astronomic coordlnetes:<br />

gravimetrlc coordlnatea; tormotrial<br />

coordinates. See also coordlnatas;<br />

geodetic coordinates.<br />

geographic lstltude-A general term,<br />

aPPbinjl afike to asfrancsnic 181iidBs ~~<br />

geodetc latitudes.<br />

geographic llmlta-The lines heving Istirude<br />

and Iongkde values bounding the area of a<br />

mm or chart: that eras exclusive of overlao<br />

areas. See siseneatlh-rsis.<br />

geographic location-see geographic<br />

pooltlon.<br />

geographic longltude-A general term,<br />

a@Yin9 afike to astronomk and to geodetic<br />

longitudes<br />

geographic merldlan—A general temf<br />

;~~~~,atike to an as!ronomio or gsodetrc<br />

geogmphlc nama-Aleo called place<br />

name and toponym. sea also Board of<br />

Geographic Names.<br />

geographic nonllnoarlty—The error<br />

introduced by digitization and subsequent<br />

processing 10 Ihe total error of both abdute<br />

ard reletfie positioning of any Ieature on the<br />

gmphk.<br />

geographic perallef-A general term,<br />

applying atike to an eafronomic parallel or e<br />

geodetic parallel .<br />

gaographlc posltlo~Tha position of a point<br />

Ontheaurfea c4the Earfhuupmeed krmrrtw<br />

of latiiuda end bngitude, either geodetic or<br />

astronomic.<br />

gaographlc ●urv*y-A general term. mt<br />

~pfibk & defined Iirritsfion, covering a wide<br />

mWe & Wweye fying between and merging<br />

into axpbmfory wrvaye on the one hand and<br />

bsdc topogmphii eurvays on the cdher.<br />

Gaographk etevays WJ.4y cover kwga areas,<br />

are based on coordinated control, end am uaad<br />

to record ptryskal and statistical ctssmcferfsrks<br />

of the area surveyed.<br />

geographic vertical-See vertical.<br />

googrephlcaf ●ma claaWtcatlon<br />

eyatern-A fogicsl snd orderfy gaographksl<br />

division of the world using nufirs, Iattem! and<br />

ccmbinaticms of the same for the deeignakxr of<br />

areas and subsraas.<br />

goographlcef ●xploretlon trmrome-A<br />

route followed scross some parts of the Earth,<br />

approximate positions ebng whmh are<br />

determined by surveying or nevigslional<br />

methods.<br />

gaographlcel mile-The length of 1 minute<br />

of erc at the Equator, or 6,067.08 feel (on the<br />

Clarke cpheroid of 1666).<br />

gaographbrd pofe-Eiiher of the two points<br />

cd intersection of the sudece of the Earth tih its<br />

axis, where all meridtans meet.<br />

geoidaf contour-A line on the suriace of the<br />

geoid of mnstant elwation with reference to the<br />

surface of the spheroid of reference. Geoidd<br />

contours depend on the surta of reference as<br />

wellaeon lheahapedthegeoid. Theeama<br />

gecid referred to different surfeoes of refemnos<br />

will give different sets of gaoirhl contours.<br />

geoldel holght profile-See<br />

●strogoodetlc Ieveflng.<br />

gooidal height—The distence of the gaoid<br />

above fpodive) er bebw (nagative) the<br />

methemalicsl reference spheroid. Also celled<br />

geold separstlon; undulation of the<br />

geold. See alw sstrogeodetic<br />

undulations.<br />

geoldd horlzors-llat circle of the celestial<br />

)5

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