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Ilthograpfrlc copy—A graphic reproduced<br />

by the lithographic precess. Also called<br />

Iltho COpy.<br />

Ilthographlc drafting—See Iuschlng.<br />

lithography—A planographlc method of<br />

printing based on the chemical repulsion<br />

between grease and waler to separate the<br />

printing from rronprinting areas. See also<br />

offset Illhogrephy;<br />

photolithography.<br />

lithosphere-The solid part of lhe Earth or<br />

other spSflal body. Distinguished from the<br />

efmosphera and the hydrosphere.<br />

local adjustment—See station<br />

ad]uatmen!.<br />

local apparent tlma—The apparant solar<br />

time for fhe meridian of the observer.<br />

local sefronomlc tlma—Mean time<br />

reckoned from the upper branch of the<br />

bcal maridian.<br />

Iocel attraction—See local magnetic<br />

anomaly.<br />

Iocsl chart-A large-scale aeronautical charf’<br />

designed tor contact fiighl in a congested<br />

area.<br />

local clvll time—See local mean time.<br />

local coordinate system—A right-handed<br />

rectangular coordinate system of which the<br />

z-esis coincides with the plumb fine through<br />

the origin<br />

local datum—The point of reference of lhe<br />

oeodetic control used exclusively in a small<br />

iirea. Usually iden(ifiad by a pro-per name.<br />

local horlzcm—See epparenl horizon.<br />

local trour angle-Anguler distance wesl 01<br />

the bcal celestial meridian; the arc of Ihe<br />

celestial equator, or the angla at the<br />

celestial POle, belween the upper branch 01<br />

the local celestial meridian and Ihe hour<br />

circle of a point on the celeslial sphere,<br />

measured westward from Ihe local celestial<br />

meridian through 360”.<br />

MIL-HDBK-850<br />

145<br />

local lunar time-The arc oj the celeslla)<br />

squalor, or the angla at Ihe celasiial pie,<br />

between the bwer branch of the kx.al<br />

calestial meridian and lhe hour clrcfe of the<br />

Moon, measured westward from the lower<br />

branch of the bcal csfestlal mertcfian<br />

through 24 hours; focal hour arrgla 0! the<br />

Moon, exprasaad in lime unffs, PIUS 12<br />

hours. See also Greenwich lunar time.<br />

IOIX31 magnatlc anomaly-Abnormal or<br />

irregular variation of the Earth’a rnegnafii<br />

field extemfing over a ralalivaly small araa,<br />

due to local magnetk inlluencas. Also<br />

called anomaloua megnetlc varlatlon;<br />

local attraction; local magnatlc<br />

disturbance; magnetic anomaly.<br />

local mean time-l. (JCS) The time<br />

interval elapsed since tha mean WI%<br />

transit of the observets amemaridian. 2.<br />

The arc of the celestial equator, or the<br />

angle at the celestial pole, between the<br />

lower branch of the local celestial meridian<br />

and fhe hour circle of the mean sun,<br />

maasured westward from the lower branch<br />

of the bcal celestial meridian through 24<br />

hours: local hour angle of fhe mean sun,<br />

expressed in time units, plus 12 hours.<br />

Called local cIvII tlmo in United stales<br />

terminology irom 1925 through 1952. See<br />

also local aawonomlc time:<br />

Universal Time.<br />

local merldlan-The meridian through any<br />

particular place or observer, serving as the<br />

reference for local time. Also called<br />

reference meridian.<br />

Iocel eldereal time-The local hour arwle<br />

of the vernal equinox, expressed in time<br />

units. Locel stiareaf lime at the Greerrwich<br />

maridlan is called Greenwich aldereal<br />

time.<br />

local tlma-1. Time based upon the local<br />

meridian as reference, as contrasted with<br />

that based upon a time zona mesidlan, or<br />

the meridian of Greenwich. 2. Any time<br />

kept locally.<br />

local vertbal—The direction of the<br />

acceleration of gravity, aa opposed to tha<br />

normal 10 a reference eurlace.<br />

Iocatlon survey-The establishment on the<br />

ground of points and fines in positions

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