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I<br />
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errore.<br />
mean sum--see flctltlous sun.<br />
mean tide level (MTL)-The reference<br />
plane midway between mean high wafer and<br />
mean bw water. Also called half tide level;<br />
ordlne~ tide level.<br />
mean time-see mean solar ilme.<br />
MIL-HDBK-850<br />
meender corner—A corner eslablishedat the<br />
infersecfionot standard, township, orsecfion<br />
Iineswifhtha maanclar line near banksol<br />
navigable straams or any meanderable body of<br />
water.<br />
meander llna—A traverse of the margin of a<br />
parmsnenf natural body of waler, along Ihe<br />
locus of the bank or shoreline at the elevation of<br />
maan or ordinary high watar, upon which bank<br />
or shoreline a riparian right may be predicated,<br />
measured ang le—An angle as read directly<br />
from an Instrumental observation and without<br />
any application of corrections for focal<br />
conditions. A measurad angle which has been<br />
wrrecfed for local conditions only at the point of<br />
observation is considered as an obsemed angle.<br />
mechanical arm templet—See spider<br />
templet.<br />
mechanical-tampfet plot—See<br />
mechan\cel.temp\et triangulation.<br />
mechanical-temfslet trlanoulatlon—A<br />
graphkal radtal triangulation u~ng slotted,<br />
spider, or any form of mechanical templel. Also<br />
called machanlcal-templet plot.<br />
mechanical-templet—Any templel which is<br />
manipulated and adjusted mechanically In<br />
laying out a radial triangulafiin,<br />
madlum.scale map-(JCS) A map having a<br />
scale larger than 1:600,000 and smaller than<br />
1:75,000. See stlao map.<br />
megabyte (MB)—A unit of memory. One<br />
megabyte equale 1,04S,576 bytes or<br />
approximately one million byfes.<br />
mamorlal—A durable article deposited in the<br />
ground at the position of a corner 10 perpetuate<br />
that position should the rnonumenl be removed<br />
or destroyed. The memorial is usually deposited<br />
160<br />
al Ihe base of the monumem and may cortsisf<br />
of anything durable such as glass or storwware,<br />
a marked stone, charred stake, or a quantify of<br />
charcoal.<br />
Mendenhall pendulum—An hrvariabla<br />
pendulum, one-quarter meter in length, with a<br />
vibration period of one-half second, composed<br />
of a Ienticular-shaped bob on a thin atam,<br />
swung in an airiight casa from whch the air haa<br />
been largely exhausted.<br />
menauratlon—1. The act, procaas, or arf of<br />
meaauring. 2. That branch of mathematics<br />
dealing with the determination of Iangfh, area,<br />
or volume,<br />
Mercator bearing—See rhumb baarlng.<br />
Mercator charr-A charr on the Mercator<br />
projection. This Is the charl commonly used for<br />
marine navigation, Also called equatorial<br />
cylindrical orfnomorphic chars.<br />
Mercator dlrecflon-Horizontal direction of a<br />
rhumb line, expressed as angular sfkstarwe from<br />
a relerence direction. Also ca}led rhumb<br />
dlrecllon.,<br />
Mercator equal-araa map pro)ectlon-<br />
See sinusoidal map projacflon.<br />
Marcalor map projection—A conformal<br />
map projection of the cylindrical type. Tha<br />
Equator is represented by a stra”ghf line true to<br />
scale; the geographic meridiana are represent ad<br />
by parallel straight Iinespwperdicmlar to the fine<br />
representing the Equaloc lhey are spaced<br />
according to their distance apart at the Equator.<br />
The geographic parallels are represented by a<br />
second system of straight fines perpendkxlar to<br />
the family of lines representing tha maridiana<br />
and therelora parallel with Iha Equator.<br />
Conformality is achievad by mathematical<br />
analysis, the spacing of the parallels being<br />
incraased with increasing distance fmm Ihe<br />
Equator to conform wlfh tha expanding scale<br />
along the parallels rasuffing from the meridians<br />
being represented by parallel fines. Also called<br />
equatorial cylindrical orfhomorphlc map<br />
projection.<br />
Mercator track-See rhumb Ilne.<br />
Mercury datum—A worldwide geodafic<br />
system derived from an analysis of data from<br />
astrogeodelic, gravimetric, and salellite sources.<br />
Results of this analysis provided a best-fitting