LXIX.
OLIVINE.
Silicate of magnesia, which receives the name from its colour.
It
is like the chrysolite, but less transparent and less hard. It is
coloured with iron. It is found in masses and also in round pebbles, as
frequently in France as in Italy, Scotland, Bohemia, Ireland, on
Vesuvius, and in many other places.
The cleavage of the olivine is imperfectly double, and its breakage is unequal and granulous.
Its specific gravity is equal to 3ยท240. Analysed it yields