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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 />
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