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vcrlical ●xaggoratlon-1. The change in a<br />

rrrcdel aurfeca Crelted by pqerthafly raising<br />

lhe~rarrr heighrof alfpoitissbeve the b9sa<br />

~.<br />

level tie mkdning<br />

Urcmea90ftha<br />

the same base scale.<br />

vartksl scafernferthe<br />

2.<br />

herizontd<br />

retiaf map.<br />

scale ef ● Iermrn model or plssfii<br />

vortlcal ●xtenslo~ ●xtenslon,<br />

defsitii 2.<br />

vortlcal geodotlc drrtu~ee vwtkd<br />

control datum.<br />

VWUCSI lntonslty-The magnatk intens”~ of<br />

the vertical ~rrent of the Earth’s msgnetic<br />

field. rtrckened positive if dewnwsrd, negative it<br />

upward,<br />

vertical parallax—see y-parallax.<br />

vertical pass point-ses supplemental<br />

olevatlon.<br />

vertical photogmph—An eerisl photograph<br />

takerr with the axis of the earners being<br />

tintsined as okxdy as possible 10 a truly<br />

vertical posbion with the rssuftsnt photograph<br />

laying a~roxirrralefy in a horizerrtal plane.<br />

vertical ptana-1. Any plane psssing<br />

Ihmugh a point on the Earth end containing the<br />

zerdth and mdir of thst pdnt; else a plsne<br />

containing a plumb line. 2 (surveying) A plsne<br />

at right angles to a horizontal pfsne and within<br />

whkh angtes and dMmcee are observed.<br />

vertical sketchmeatar-A type of<br />

sketchrnaater in tilch verfiosl phoregmphs are<br />

Ufifiied.<br />

vortlcal etoreotriangulatlO*That perlien<br />

I OfStWSOtriSr@Morl &ncemed with lb<br />

eatabfiimanf of vedikot data. Varkal<br />

stersotriangulation is etten Iirnfted er prscluded<br />

aa an cparatkrn due to the more rigid scarmcy<br />

starxtards established for vertical pesitiens thsn<br />

for fwfzorrtal pcMorrs.<br />

vertical-anglo bench mark (VABM)—A<br />

bench mark with ef.evalion estsbliihed by<br />

vertksl angle me!hak. See alse bench mark.<br />

varllcel-anglfr station—See<br />

aupplamantal etation.<br />

MIL-HDBK-850<br />

Z77<br />

vOrtlc~f-The fine perparxliidsr to the gsoid at<br />

~Y~*.tktid~rn~ UWfCSCeaf<br />

grawry sch. sea UJsobed Vartkal; mass<br />

●ttmctfon vortkal: normal, rlefinltion 3.<br />

vfbmtiOrr-4 eingfa rnovemanf of a pendulum<br />

irrahher dbctbn,toorfro.sea Stso<br />

osclllstlon.<br />

Wdeo Point Posltionlng Data Baa.<br />

(VPPDB)-A DMA analofj VkfeO dac prodrrd<br />

rhii pmvkiaa ● mmmrxpk precise positiiing<br />

ca@@yniriihi amoreversattia rrdeaeLarfe<br />

uaa fhn the Anstyiiil Photogramotrk<br />

Peaitiing System (APPS). VPPOB was a<br />

WmOMl COIWJfw to Mow reel time aordinate<br />

rasdouK designed for ease of use arxl m“nirnsl<br />

Imining time.<br />

video disc [MCGTJ-A 30.5 cm (12”)<br />

Cmstont Angrisr VaJcdy (CAV) ansbg video<br />

discca#rle ofstorir# video imeges ones~<br />

aide (equkwlerd 10 spproxirdely 200 everag-<br />

Si2ed map chests at m dflemrrr kids of view).<br />

See also CD-ROM.<br />

vldao rrrop-hy one of a - of<br />

cartogrsphk preduds thst are *umd, stored,<br />

m-d d~yed using anslog video signals.<br />

vlewfltrder-(aerial camera) An atmiliiry devica<br />

which show the fiikt d view of a camera. tt is<br />

used in the takingd VOrticsl.9arkIpfrotqephy<br />

to con-act cmb angle and rrmintnin fonvmd Isp<br />

(end Iep).<br />

vlgnatthrg-t. (photogmphy) A gradual<br />

reductiorr hdenaity ofpafla ofephetegmphii<br />

image due to the stopping of some of the mys<br />

errtering the lens. Thus, a kms nmurrting rrmy<br />

Inlerfam with the sxtrems oblii mys. An<br />

ant”~netting fitter is one thst gmdrmlty<br />

decmsses in density frerrr the cs’ttw teward the<br />

adge$ it la used with msny wide-angle lenses to<br />

procfuce a photograph of uniform den.shy by<br />

cuiting down the overexposure d the center of<br />

the photograph. 2. (fiihography) A photographic<br />

IXOCeSS wfriih portrays a soiii cmlor in a soreen<br />

vdkh shsdes oft gredudiy inlo Ihe unprinted<br />

paper. @xr water is often ahown by this<br />

methed.<br />

vlrtuel gravity-The forca of gravity on an<br />

etmmspheric parcel, reduced by cerrtrrfugat hrce<br />

due to rhe rrmtk.n of the parcel ralalive to the<br />

Earth.

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