Amianthus Actinolite / Adularia

Object/Artifact

-

Crater Rock Museum

Name/Title

Amianthus Actinolite / Adularia

Entry/Object ID

2009.62.72

Description

Chemical Composition: see description Crystal System: Hexagonal System Description: Common Name: Amianthus(Asbostos) Actinolite / Adularia Chemistry: Ca2(Mg, Fe)5Si8O22(OH)2 , Calcium Magnesium Iron Silicate Hydroxide / KAlSi308 Group: Amphibole / Feldspar Location: Etzlital Canton, Graubunden, Switzerland Description: Large specimen with a layer of fine hairlike crystals with sporadic clumps of white crystals imbedded within, on a white to gray rocky matrix. PHYSICAL CHARACTERISTICS OF ACTINOLITE: Color is usually green.white or gray. Luster is vitreous. Transparency: examples are translucent to transparent. Crystal System is monoclinic; 2/m Crystal Habits include the flattened prismatic and elongated crystal with a dome-like termination that is actually a two of the four faces of a prism. Also as a fibrous mass (asbestos) and as a fibrous and very compact mass (nephrite jade). Cleavage: is perfect in two directions at close to 60- and 120-degree angles. Fracture is splintery to uneven. Hardness is 5.5 - 6. Specific Gravity is approximately 2.9 - 3.3 (very slightly above average for translucent minerals). Streak is white. Associated Minerals are quartz, lawsaonite, epidote and glaucophane. Other Characteristics: the compact nephrite variety is extremely tough and is actually stronger than steel. Best Field Indicators are toughness (nephrite jade), fibrosity (asbestos), typical green color, crystal habit and hardness. PHYSICAL CHARACTERISTICS OF ADULARIA: (orthoclase) Color is off-white, yellow, or shades of red, orange to brown. Luster is vitreous to dull if weathered. Transparency crystals are usually opaque, may be translucent or rarely transparent. Crystal System is monoclinic; 2/m Crystal Habits include blocky or tabular crystals. Crystals have a nearly rectangular or square cross-section with slightly slanted dome and pinacoid terminations. Twinning is common. (see above). A psuedo-orthorhombic or psuedo-trigonal variety, found in alpine veins is called adularia, and forms more flattened tabular crystals. Cleavage is good in 2 directions forming nearly right angled prisms. Fracture is conchoidal or uneven Hardness is 6 Specific Gravity is approximately 2.53 - 2.56 (average) Streak is white. Associated Minerals are quartz, plagioclase feldspars, micas, garnets, tourmalines and topaz. Other Characteristics: some crystals may show opalescence and are called moonstone. Best Field Indicators color, lack of striations, cleavage, twinning if present and occurrence. Fracture: conchoidal Hardness: 6 Orthoclase Luster: Vitreous Occurrence: Actinolite is commonly found in metamorphic rocks, such as contact aureoles surrounding cooled intrusive igneous rocks. It also occurs as a product of metamorphism of magnesium-rich limestones. Adularia forms in intrusive and extrusive igneous, and metamorphic rocks. Specific Gravity: 2.7 Streak: white Variety: Actinolite is a relatively common mineral in some metamorphic rocks. A variety of actinolite is composed of microscopically fibrous crystals (asbestos or amianthus) and is called byssolite. Other varieties are nephrite, which is one of the two minerals called jade. Adularia is orthoclase form under low temperature and commonly refer to as moonstone.

Collection

RAGM Mineral Collection

Acquisition

Accession

2009.62

Source or Donor

Museum Collection of Minerals

Acquisition Method

Donation

Dimensions

Weight

10.82 oz

Dimension Notes

Dimension taken at widest points

Location

Location

Drawer

far right

Shelf

middle shelf, middle shelf

Wall

South wall

Room

Delmar Smith Hall

Building

Crater Rock Museum

Category

Permanent

Moved By

Scott Longan

Date

September 19, 2009

Location

Container

Right

Drawer

3rd Shelf

Shelf

Right

Cabinet

Case #42

Wall

South wall

Room

Delmar Smith Hall

Building

Crater Rock Museum

Category

Permanent