342 STANDARD ELECTRICAL DICTIONARY.

Magnetic Declination.

The angular deviation of the magnetic needle, causing it to rest at an

angle with the true meridian; the variation of the compass. (See

Magnetic Elements.)

Magnetic Density.

The intensity of magnetization expressed in lines of force per stated

area of cross-section in a plane at right angles to the lines of force.

Magnetic Dip.

The inclination from the horizontal assumed by a magnetic needle free to

move in the vertical plane. (See Magnetic Elements.) The angle of dip or

inclination is entirely a function of the earth, not of the needle.

Magnetic Discontinuity.

A break or gap in a magnetic circuit. To make a complete circuit the

iron or other core must be continuous. If the armature of a horseshoe

magnet is in contact with both poles the continuity is complete. If the

armature is not in contact magnetic continuity gives place to

discontinuity. It is an attribute of a paramagnetic substance only, and

is identical for permanent magnets, or for electro-magnets.

Magnetic Elements.

The qualities of the terrestrial magnetism at any place as expressed in

its action upon the magnetic needle. Three data are involved.

I. The Declination or Variation.

II. The Inclination or Dip.

III. The Force or Intensity.

I. The Declination is the variation expressed in angular degrees of the

magnetic needle from the true north and south, or is the angle which the

plane of the magnetic meridian makes with that of the geographical

meridian. It is expressed as east or west variation according to the

position of the north pole; east when the north pole of the needle is to

the east of the true meridian, and vice versa. Declination is different

for different places; it is at present west in Europe and Africa, and

east in Asia and the greater part of North and South America. The

declination is subject to (a) secular, (b) annual and (c) diurnal

variations. These are classed as regular; others due to magnetic storms

are transitory and are classed as irregular, (a) Secular variations. The

following table shows the secular variations during some three hundred

years at Paris. These changes are termed secular, because they require

centuries for their completion.

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