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Maryland Geological Survey, Volume 1, 1897
Volume 423, Page 452   View pdf image (33K)
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452 FIRST REPORT UPON MAGNETIC WORK

when making the intensity observations, and the small counter-weight
directly below the reflector serves as a counter-balance to the telescope.

The upper part of the magnetometer bearing the magnet box and
telescope is fastened to the base and horizontal circle by two screws
and may thus be quickly removed, and the theodolite for determining
the true astronomical direction may be substituted. The theodolite
or alt-azimuth attachment is shown in the right of the figure. Thus
the same base horizontal circle serves for both the magnetometer and
the theodolite attachments. The horizontal circle has a diameter of
11. 2 centimetres (4. 4 inches), and the vertical circle, of 9. 8 centimetres
(3. 85 inches). Both circles are graduated to half-degrees and read
by opposite verniers to minutes.

The horizontal circle is graduated clock-wise from O to 360°, while
the vertical circle is graduated anti-clockwise from 0 to 90° in each
quadrant. For vertical circle east, when sighting south, the readings
of the vertical circle give at once the altitude of the object, and in
the reversed position, the zenith distance.

For the intensity observations, when the magnet above described is
used as a deflector, two graduated wooden arms (not shown in the
illustration) are inserted beneath the magnet box. On the arms rests
a slider supporting the deflector at the same height as the auxiliary
magnet in the box and at any desired distance.

The next figure (Plate XV, No. 2) illustrates an instrument similar
to that used in determining the magnetic inclination or dip. It is of
the usual Kew pattern and known in the Coast and Geodetic Survey as
Casella Dip Circle No. 56/4440. In this instrument the needle is
flat, tapers to a point on each side, is 3 1/2 inches long and is mounted so
that it swings in a vertical plane instead of in a horizontal plane, as in
the case of the surveyor's compass. The pivots of the needle swing-
on agate planes and are ground as accurately as possible. The needle
is enclosed in a glass case to shut out all air currents and is provided
with a lifter for lifting the needle off the agates or letting it down
on them preparatory to observing. The angle of dip is read off on the
vertical circle outside the glass box. The pointings on the ends of
the needle are made with the aid of microscopes. The box with the


 

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Maryland Geological Survey, Volume 1, 1897
Volume 423, Page 452   View pdf image (33K)
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