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U.S. control ourvoy nata-’l’he two corrtml<br />

survey nafe bdng extended over the United<br />

stabs by fhe National f3eodefk survey fer the<br />

tird of rrautkaf cAarfe and fcfmgrapfric mapa,<br />

z=d(k~=z”sv<br />

=-d’”””+”” fJ=Wma, afawofwhioflhava<br />

bean Llxullfd by the Unflad stems Geological<br />

Survay. The Corps& Englnaara, arxl other<br />

-~ m date Cfarivd h lfrls survey<br />

are being c&@Lefad and CcrTafatad on the<br />

North A~ datum d 1927. lb Natfcrral<br />

Gacdafk Survey la currently rawrrrpufirrg the<br />

hortsonfaf corrfmf network to the North American<br />

dalwn of 19ss. (2) The Variical amfml cAlrvey<br />

net consisting of tires & firsf-crdar and aacmld.<br />

order spirit bavahg wtrkdr datarrnirre the<br />

ebvatbns of tfrouaarrdsd bansh rmwka nbove<br />

a aernmorr datum, mean aee level. Thb nd<br />

includas times of levels run by the United States<br />

Geobgkal Survey, ha Cape of Enginaem, and<br />

other organizafii.<br />

U.S. Engineer praolso taveling rod- A<br />

~king rat of T-ahepad cmes aasfiotr, 12 bet<br />

*, 9tid In .arrtirnfrters.<br />

U.S. Gaologkal Survey lavet-A level of<br />

~ d- ~, -wed at atah+as ateet. ft<br />

has en infernal fccusing la!aasopw the level<br />

b-e is omfemd by the end-ccrirrckienca<br />

method, affeofad -h t~ aid of s ptfwll dSVi04<br />

and Sfellife mirmr wirkh can be ad@tad by the<br />

observer.<br />

U.S.<br />

rod-1.<br />

Gaologkal<br />

A -tdrm .C––.<br />

SurvoY prods.<br />

d rkduetad<br />

Iermllfrg<br />

in mrde md<br />

hactima deyard. %”rn-&forea&~th&<br />

oruaatvima tothenaaraat thcuaarxifh of ayard.<br />

llw eum of tha three readings is than the mean<br />

raetimg in feet to fha naamst thouacndfh. 2. A<br />

target md of ptus-algn (+) cross aaclkn, a Me<br />

over 12 feat in Iwrgfh. Rrare are two krrrns cd<br />

this rod fhe aingla-fargat rod and the doubkrtergat<br />

rod.<br />

U.S. National Map Accuracy<br />

Sfsndarda-1. Horizontal accuracy: (I) for<br />

~P8 al Publkat”mn scales Iargar than I :20,000,<br />

90 percent of al wall-dafhed faaIurss, with the<br />

exsaptbn of those unavoidably displaced by<br />

exaggerated aynrbcfizatbn, will h foctded Within<br />

1/20 inch (0.8S mm) of their geographic<br />

MIL-HDBK-8S0<br />

u<br />

paffbna as rderrad<br />

fwrraqr at p&fbUon<br />

te the map pmiadkw<br />

scales d l:~,000or<br />

(2)<br />

smaller, I/W) irwh (0.54 mm). 2. Vertmsl<br />

OOparced daffsonfwasnd<br />

elavafti infaplafad from ocmtcum till ba<br />

ascwafe within ena-fmf cffhafmakcorrtour<br />

Ir$ervef. Dkcmpamw “ in ffwcccumcytrf<br />

ccmfcnus and S&vafiona bayond fflk tcl’sransa<br />

-Y ~ -~ by assuming a horizordal<br />

d~m wfthin 1/50 imfr (0.S0 rrun). Alac<br />

called map accuracy standards; national<br />

map ●ccuracy standards.<br />

ultrawlde-angk kna-%a suparwldo-<br />

●ngfo kna.<br />

uncheoked ●pot ekvatlon-Ekvalion<br />

detemrhad by undmakad Wd ew’vay maffrata,<br />

such as eida tis on rladia lima. undmkad<br />

verticai angles, and bammafria iavdkrg. Also an<br />

elevation datarminad by rapealad<br />

photogrammatric raadtrrg.<br />

uncontrolled meaak-(JCS) A masaic<br />

-- ~ uxerraded prints, the derails of<br />

whii have baarr r-na$chad from print to print<br />

withcut grmrnd control or other orientation.<br />

Accurate maasummenf and dimcfkrn cm?rrd ba<br />

asomn@ibhad. see ako controlled moaalc.<br />

undwgmund marfr-A survayinu mark eat<br />

●-d plurrbad below tha Oantar d a eurfase<br />

mark and eapamtad Iharefrorn so as to praserva<br />

t:~~ticm in 0ss0 of acsidari to the aurfaca<br />

undershoot-A data omisabn which coours<br />

during the dats CSpfUm p~m, prdc.shrfy<br />

during rnarrtsrd d@tiirng. In an undershoot<br />

situatbn, baar rkta falls ahwr d rrnsting an<br />

interaaafbn. An undarahool may be oormotad<br />

by a snap dtwam function.<br />

undevsrlopable-A surface, such as a<br />

6phera, that cannef be flattened to forma plane<br />

without compressing er stretchkrg aema part of<br />

it.<br />

u ndo-(dqifal) The ability to cwcel a previous<br />

command to the mmputar.<br />

undulation of the gaold—See geold<br />

halght.<br />

L71

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