monoclinic

It is a dark reddish brown to black monoclinic mineral.

All members of the series belong to the monoclinic crystal system with point group 2/m.

Its hardness is 3.5 and it has a monoclinic crystal system.

It belongs to the monoclinic system and is part of the P21/c group.

Above 29 C the stable form is monoclinic 2/m.

It too is pale green but has monoclinic crystals.

The transition from the monoclinic to hexagonal form occurs at 1740 C.

Most sources simply give it as monoclinic 2/m, space group C2/c.

Two other phases, monoclinic and hexagonal, are known for this oxide.

It occurs as grey, black, to silvery white monoclinic crystals.

Switzerite is a part of the monoclinic space group P 2/a.

Its flat molecules are arranged in a monoclinic lattice (see figure 3.29).

In crystallography, the monoclinic crystal system is one of the 7 lattice point groups.

Marrite is part of the monoclinic crystal class, and point group.

It belongs to the monoclinic system with space group C-Cm.

GaTe produced from the elements has a monoclinic crystal structure.

The mineral is monoclinic with the space group P2/c.

It occurs as aggregates of small monoclinic white crystals.

It crystallizes in the monoclinic system and forms prismatic crystals.

The mineral possess monoclinic symmetry and forms clear, often rounded crystals.

It is a soft yellowish white mineral which crystallizes in the monoclinic system.

The crystals of Mohr's salt are monoclinic in shape.

Its crystal system is monoclinic, and it is white, yellow, or transparent in appearance.

Crystals of roscoelite take on the monoclinic form, and are from the 2/m point group.

It occurs in monoclinic crystals, also fibrous, massive, and earthy.