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I<br />

I<br />

I<br />

I<br />

I<br />

Ihe p0b6. AfsC ded ●pOX.<br />

Vorfox of curve-sea point of<br />

Int.rsoctlon.<br />

Vettkal Obetructlon Data (VOfl)-Oata<br />

fib containing dmte poaitim and hei@t<br />

irderrrmt”bn d menrneda smf nstursl objads<br />

exfartdii ebove the esrth’s a.urfeca et haiihte<br />

thst Coufd mnstmin eipkanean dcnliwmisaife<br />

ffiiht6 at levels Sslsbliihed by tin planners.<br />

Vetlkd obcfr@kta Include msmnsde<br />

ObStfUCf”~S such es radm towers, emekastaoka,<br />

b~es, powwfinas, and other ebjada above<br />

apeciried minimum efsvatbna. vOD is<br />

~ by the Prcb6fMiiic Varfksd<br />

obstruction Dsfe (Pvoo). see akm<br />

Probabillstb Vottlcd ObstructIon Data.<br />

vartkd sngk-t. An angfe In a vatticsl<br />

plsne. 2. (surveying) One of the direstbns<br />

whii form a vemid engle & uauaffy either the<br />

dirsctbn of the verticsl (zenith), snd the angle in<br />

termed the zorrfth dlatanccu or the fine of<br />

intersection of the vertkal pfane in wtkh the<br />

errgfm free with the pfsne of the trorizen, and Ihe<br />

angle is termed the angfa of clevctlon or<br />

●rgb of dopresslon, or simply the altltudo<br />

(plus or minus, as the csse msy be). Ths vartiil<br />

~W~ ~~ We di=ims, rrsilhsr of ti~h<br />

has in the ptma of the horizon er caincicbs with<br />

the vertii, is uauelfy dtsined from the<br />

canbinatim of tvm verticsl sngfas se defined<br />

above.<br />

vartical ●gulatiOn-The pmcesa of<br />

OMaining difhe.nces of efevation by means of<br />

obearvaf vertical engfae, cotinad with Iangfha<br />

ef fines. In geodatb wdc, trigermrnatric fevefing<br />

is used wilh the same rneening.<br />

v.rtlcd ●xla+lheodefiie: trsnsif) Tha fine<br />

through the center d the msfrumsnf abouf<br />

#ii the akdede rotates. FW an instrument in<br />

cxm@sfe adjustment, this axia occupies a<br />

verfioel pesifkm, passes through the oemer of<br />

the fmrizorrtal tilde, and is perpendicufer to its<br />

plane.<br />

vortlcd bridging-see brldglng.<br />

v.rtlcal ckcla-1. A great circle af the<br />

celestial sphere, through tfrs zenflh and nadir.<br />

Veti’ksl clmfss are perpendhhr to the hodzc.n.<br />

2. A gradueted disk mounted on en instrument<br />

in such a manner thst the plane of its gredusted<br />

surfsce can be pfsced in e vetticsl plane. It is<br />

primarily used for rn9ewring vertical angles in<br />

MIL-HDBK-850<br />

-.<br />

z’76<br />

warenomic and gacdetic wark.<br />

vanicsl colllmafor-A tekcoopa so mounted<br />

fJ’WtiCdtiti@-k~ tocmirckle<br />

wifftffre vettisa d(wdktitidti~k).<br />

The Vanicef COllinmaor Satv- as en @u<br />

Plun-hhxl tmaybadaaimadf or-hpf=+tw<br />

amsrkctt thOgrOUrKf dwOCfiY~r an<br />

h’@Nti en n h~h tower w * cantering an<br />

iluSN_ Oil 0 h@l klWSr di=t& OVOr a I_tUt’k<br />

on ths gmurrd. Abe r4ed optfcd plummet.<br />

verflcd cornparator+pendulum) A stand<br />

das@tedforfhasqurtcfapnduJm, aixr<br />

of known length, and fvm mismrnefar<br />

~, so placed with rdaretv=a to one<br />

another that the fengfh d the pandulun can be<br />

measured.<br />

vertkal control datum-Any feval surface<br />

(as, far exan’pfa, mesn see Isvef) teken aa a<br />

wrtssa d refere- fmm which to reckon<br />

elevations. Alee called vwtlcaf datum;<br />

vertical gnodetlc datum. Sea also d ●t urn<br />

Ieval; refarence level; reference plane.<br />

vorflcal control net-+ee eurvey net.<br />

doflnltlon 2. ,<br />

verflcal control pOlnt—See controf point;<br />

control mtmtlon.<br />

vertical eontrof-The rnessurements taken<br />

by aurveymg methods for the detemrimsfbn of<br />

ebvetbn onty with respect to an imsgfnery favef<br />

wrfac9, uauaffy rnsm aee leveL Sea afse<br />

survey nat dafinitiin 2.<br />

vertical coordlnetea-llm vartical dwtanca<br />

of a point above or babw a rsfarenoe datum.<br />

Points mey bs piua or minus ~mg to<br />

whether the point is ebeve or bebw the datum.<br />

vertkal cutva-A psrabofii curve d to<br />

connect gradea d dtierurd afepe, and used at<br />

the vertex d e grade to avdd the sudden<br />

chsngs M directim in peaa4ng from ma grsde to<br />

the other. Tfis rnathed of grsda change fa<br />

ususliy used when there is an afgebmis<br />

dflerence of more thsn 0.2 percent in the two<br />

opposing gredes.<br />

verflcal datum—See vertical control<br />

datum.<br />

vertical deformation—in refetive orientetien,<br />

the cumulst”we medel warpage affecting Ihe<br />

vettksl detum from x-fill error and ~tift error.

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