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latitude. See also atrtronomlc equator;<br />
celeetlal ●quator; flctltlous squator;<br />
galsctlc equator; geodetic aqusstor;<br />
geomagnetic aquator; grid aquator;<br />
lunar caleatlal ●quator; rnagnatic<br />
●quator; obllque ●quStOr; Iranaversa<br />
equator.<br />
eqularr@ar ●plral-see rhumb Ilne.<br />
equlangulator-An opticsl instrument,<br />
em@Yi~ a 60° prism, used to determine<br />
astrmnomc fetifude and bngifude by equal<br />
affiiudes 01 heavenly b@es when the tima of<br />
the prime meridian (Greenwich) is known at the<br />
p~ce oi observation.<br />
equlgeopota;tlal eurtece-See<br />
equlpotentlel eurtace.<br />
MIL-HDBK:850<br />
equlllbrlum ●ptrarold-The shape !hat the<br />
Earth woufd attain ii il were entirely covered by a<br />
Ikteless ocean of constant deplh. See also<br />
geold.<br />
aqulllbrlum theory-A hypothesis which<br />
assumes an ideal Earth which has no<br />
mntinental barriers and is unilormly wvered with<br />
waler of mnsiderabie depth. 11‘also ‘assumes<br />
that the waler responds instantly to the lideproducing<br />
tortes of the Moon and Sun to form a<br />
surface in equilibrium and moves around the<br />
Earth whhout viscosity or friction. See also<br />
geold.<br />
equlllbrlum—A state of balance between<br />
forces. A body is said 10 fM in equilibrium when<br />
the vector eum of all tortes acting upon 11is<br />
zero.<br />
aqUlnOCtlal colure-The hour circle through<br />
the equinoxes.<br />
equlnoctial day—See sidereal day.<br />
equlnoctlal polrrt-See equinox.<br />
equlnocflal ayatam of coordlnalae- See<br />
celestial equator eyatem of coordlrsatea.<br />
aqulnoctlal yeer—See tropical year.<br />
equlnoctlal—See calestlal equstor.<br />
equhrox-One of the two points of intersection<br />
ot the ecfipt”c and the celestial equator,<br />
occupied by the Sun when its declination is OO.<br />
86<br />
Also called equlnoctlal point. Sae also<br />
autumnal equlrsox; mean aquhtox;<br />
vernal aqulnox.<br />
equlpotenllal ●urtace-A surtaoe having lhe<br />
same ptenlisl of gravity et every point, Also<br />
called level surface. See also gaold; OSOP;<br />
geopoterrllal aurlace.<br />
aqulecalar—A surface along whbh a scalar<br />
quantify has a constant vafue.<br />
equivalent focal lenglh—(JCS) The<br />
distance measured along the optical axis of the<br />
lens trom the rear nodal point 10 the plane of<br />
best average definition over the entire tiefd used<br />
in a camera. See also focal length.<br />
equivalent map projection—See equalarea<br />
map projection.<br />
aquhralent scale-The relationship which a<br />
small distance on a grephic bears to the<br />
mrresporrding distance on the Earth, expressed<br />
as an equivalence, such as 1 inch (on the<br />
graphic) equals 1 mile (on the ground). Also<br />
called verbal scale.<br />
equlvelenl vertical photograph—A<br />
theoretically, truly vertical photograph taken al<br />
the same camera station with a camara whose<br />
local length is equal to lhal 01 a camara taking a<br />
mrresponding tilted photograph.<br />
erasable opllcal disc (EOD)—A class of<br />
mmpact discs which allow users to rerecomf data<br />
onlo the disk.<br />
erect Image-An Image that appears upri9hi,<br />
or in lhe same ralatlve position as the object.<br />
arecllng telescope-An observer sees<br />
objacts right side up when Iooklng through an<br />
erecting telescope and upside down whan<br />
twking through an inverting telescope. The<br />
eyepiece In lhe optical syslem of an erecting<br />
teleswpe usually has four lenses, and the<br />
eyepiece in the opticel system of an inverling<br />
telescope has two lenses. See also Inverflng<br />
tefeacope.<br />
erratic error—An error caused by an<br />
incomplete element in an inatrumenf, such as<br />
backlash in a gear train. Sea also Instrument<br />
arror.<br />
error budgel—A correlated set of the