When,
on the other hand, the planes of reflection are parallel, the ray is
wholly and at any intermediate angle partially reflected. A ray of
light polarized by reflection is also incapable of transmission through
a tourmaline slip in one position, which, however, is'at right angles
to that in which a ray polarized by passing through another slip is not
transmitted.
In
order to observe the polarization of light, a very simple instrument
will be found useful (fig. •96). At one end of a horizontal board Β a
black mirror a is fixed. In the middle is a pillar to which a tube c d is
fastened, with its axis directed to the mirror at an-angle of 35-1/2°.
On the lower end is a cover c, with a small hole in the centre, and at
the upper end another cover with a small black mirror m attached to it by two arms, as in the figure, and also at an angle of 35-1/2°. With this instrument the mirror rn can be so placed in relation to a that the planes of reflection shall have any desirable inclination to exhibit the simple polarization of light.
.
This instrument furnishes a simple test whether minerals that cleave
readily into, thin lamella} are optically mono-axial or binaxial. Place
the two mirrors with their, polarization-planes at right angles,· and
fix a plate of the mineral with a little wax over the hole c, and then
observe what takes place in the second mirror during the time that the
cover c is turned round. If the mineral belongs to the bi