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MIL-HDBK-850<br />

Croso.Country Mmmrnont MaP (cCM)- A<br />

DMA map de@cfirrg CfOSS-CUI.MfIymobility<br />

eafiiws tor the M-1 ts~ expressad in terms O{<br />

GO, RESTRICTED. SLOW, VERY SLOW, and<br />

NO GO with correaporrdirro everage speed<br />

range pradicfkme. Open water and urban areas<br />

are afao pmtrayed, as are ground movement<br />

obatackas and hydrobgk hkrdrarces. Ptoducsd<br />

at 1:50,000 and 1:250,000 ecale.<br />

croee-coum~ movement study-A graphic<br />

or sertes ot graphics and supporting text or<br />

tables ponraying off-road movement conditions<br />

for e@tic vehicles or a group of vehdea. tf ie<br />

usually overprinted on a medium- or large-scale<br />

topographic rrwp basa.<br />

cross.fllgfrt photography—ShWle photographic<br />

etr@ heving elaraoacopic overlap<br />

behveen exposures and having e flighl direction<br />

at right angles to that of coexistent area<br />

coverage photography. When applied to<br />

shoran, the Iarm hnplies that each of the crosslight<br />

expoeurea la accompanied by remrded<br />

ahoran distances. See also control atrlp.<br />

CrO~.-S0CtiOtiA horizontal grid system laid<br />

out on lhe 5r6i.-nd tor determining contours,<br />

quantifies of earthwork, etc.. by means of<br />

elevations of the grkl points.<br />

crossing sn@s-The angle at which hvo lines<br />

01 pesifiin, cxwae Iinas, etc., intersect.<br />

crossllne glass screrrrs-See halftone<br />

screen.<br />

crystal clock—A device tor keeping accurate<br />

lime. It consists essentially of a generator of<br />

constant frequency controlled by a resonator<br />

made of quartz crystal, with auifable methods for<br />

pm.ducing corsfinuoua rotatiin 10 oparele time<br />

indkxting and related mechanisms.<br />

culmination—The position of a heavenly body<br />

whan af h~heat apparent altitude (zenith).<br />

Kr!own as upper Culmination; also, tor a<br />

heavenlv bodv wftiih la comlnually above the<br />

hortzon,’the bshbn of bwest ep~rent altitude,<br />

known as lower culmination. CUhTtinaliOn<br />

rscwre whan lhe body transits the iocd<br />

meridian. See alao lower tranelt; trsmslt;<br />

upper transit.<br />

cultural dotalla—See culture.<br />

cultural taaturee—See culture.<br />

60<br />

cultura-(JCS) Featurea of lhe terrain thet<br />

have been cmalrucfed by man. Included are<br />

such tiems as roads, buildings, and canals:<br />

boundary Iiies, arsi in a bread sanae, all<br />

names and legends on a map. MO called<br />

cultural detalla; cultural teatures; manmede<br />

Ieaturee.<br />

currancy review—lhe comparison of an<br />

existing MC&G product against eoume materkil<br />

o} later date man that trom which fha producf<br />

was produced, for the pupae of determlrthsg<br />

the products camency.<br />

CUrrOnt chs1l-A map ot a watar area<br />

depicting current speads and directions by<br />

Cuf’renf roses, vectors, or other means.<br />

current CYCIS-A complete sel of Iidal currenl<br />

conditions, as fhose occurring during a tidal day,<br />

lunar month, or Metonic cycle.<br />

current diagram—A graphic presentation<br />

showing the speed of the tiood and abb<br />

currents and the times of slack and strenglh<br />

ovar a conekterable stretch of the channel of a<br />

tidal waterway. The fimes being referred 10 as<br />

tide or wrrem phases at some relarersca<br />

stations.<br />

current meter—A device for determining the<br />

vabcify of fbwing waler by ascertaining the<br />

speed at which a stream of water rotates a vane<br />

or wheel.<br />

current rose-A graphic presentation of<br />

w rrents for speciiied areas, rsliliilng armwa at<br />

the cardinal and inlercardlnal compass pOinlS to<br />

show the dhecfion toward whch the prevailing<br />

currenf flows and the percent frequency of set<br />

for a given period of time The arrows on some<br />

presentatbns may be further subdivided (by<br />

lhkkness or pattern) to designate categories ot<br />

current speeds.<br />

curvature correction—l. (as fronomy) A<br />

correction applied to the mean of a series of<br />

observat”nns on a star or planet to take account<br />

of Ihe d!vargence to the 6pp6reM pelh ot the<br />

star or planet Imm a straighl line. 2. (gaodesy)<br />

The correction appfied In some geodetk work fo<br />

fake account of the divergence 01 the surface ot<br />

the Earth (spheroid) horn a plane. In geodetic<br />

spirll Ieveting, the eflecte of curvalure and of<br />

efmospheric refraction are mnsldered together,<br />

and fables have been prepared trom which<br />

combined corrections can be taken.

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