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I<br />
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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.