Ontario Mineral - Serpentine

Rocks minerals Ontario Serpentine
Chemistry:
 (Mg,Fe)3Si2O5(OH)4, Magnesium Iron Silicate Hydroxide
Class:
 Silicates
Subclass:
 phyllosilicates
Group:
 Kalolinite-Serpentine
Uses:
 many industrial applications, including brake linings and fireproof fabrics and as an ornamental stone.
Color:
 olive green, yellow or golden, brown, or black.
Luster:
 greasy, waxy or silky
Transparency:
 crystals are translucent and masses are opaque.
Crystal System:
 variable, see Description
Crystal Habits:
 never in large individual crystals, usually compact masses or fibrous. Veins of viberous serpentine can be found inside of massive serpentine or other rocks.
Cleavage:
varieties of crysotile have none, in lizardite and antigorite it is good in one direction.
Fracture:
 conchoidal in antigorite and lizardite and splintery in the crysotile
Hardness:
 3 - 4.5
Specific Gravity:
 2.2 - 2.6
Streak
 white
Other Characteristics:
 serpentine in the rough has a silky feel to the touch and fibers are very flexible.
Associated Minerals:
 include chromite, olivine, garnets, calcite, biotite and talc.
Local Occurance:
 Desmont Mine, Saranac Mine, Warwickite Occurrence
Best Field Indicators:
 softness, color, silky feel and luster, asbestos if present and its flexibility.

Description:

Serpentine is a major rock forming mineral and is found as a constituent in many metamorphic and weather igneous rocks. It often colors many of these rocks to a green color and most rocks that have a green color probably have serpentine in some amount.Serpentine is actually a general name applied to several members of a polymorphic group. These minerals have essentially the same chemistry but different structures. The following is a list of these minerals, their formulas and symmetry class:

Antigorite; (Mg,Fe)3Si2O5(OH)4; monoclinic.
Clinochrysotile; Mg3Si2O5(OH)4; monoclinic.
Lizardite; Mg3Si2O5(OH)4; trigonal and hexagonal.
Orthochrysotile; Mg3Si2O5(OH)4; orthorhombic.
Parachrysotile; (Mg,Fe)3Si2O5(OH)4; orthorhombic.

Their differences are minor and almost indistinguishable in hand samples. However, the chrysotile minerals are more likely to form serpentine asbestos, while antigorite and lizardite form cryptocrystalline masses sometimes with a lamellar or micaceous character. Asbestos had been used for years as a fire retarding cloth and in brake linings. Its links to cancer however has led to the development of alternative materials for these purposes. Serpentine's structure is composed of layers of silicate tetrahedrons linked into sheets. Between the silicate layers are layers of Mg(OH)2. These Mg(OH)2 layers are found in the mineral brucite and are called brucite layers. How the brucite layers stack with the silicate layers is the main reason for the multiple polymorphs. The stacking is not perfect and has the effect of bending the layers. In most serpentines, the silicate layers and brucite layers are more mixed and produced convoluted sheets. In the asbestos varieties the brucite layers and silicate layers bend into tubes that produce the fibers. Serpentine can be an attractive green stone that takes a nice polish and is suitable for carving. It has been used as a substitute for jade and is sometimes difficult to distinguish from jade, a testament to the beauty of finer serpentine material.Non-fiberous serpentine is not a cancer concern. Asbestos serpentines should be kept in closed clear containers, but makes an attractive specimen. Sometimes with a golden color as the name chrysotile in greek means golden fibers.