Fluorite / Muscovite

Object/Artifact

-

Crater Rock Museum

Name/Title

Fluorite / Muscovite

Entry/Object ID

2009.62.68

Description

Chemical Composition: see description Crystal System: Cubic or Isometric S Description: Common Name: Fluorite / Muscovite Chemistry: CaF2, Calcium Fluoride / KAl2(AlSi3O10)(F, OH)2, Potassium aluminum silicate hydroxide fluoride Group: Halides / Mica Location: Sumayar, Nagor Noth, Pakistan Description: One large fluorite crystal, translucent white to green, embedded in a thick base of scalloped , layered muscovite on a grainy burnt yellow matrix. THE PHYSICAL CHARACTERISTICS OF FLUORITE: Color is extremely variable and many times can be an intense purple, blue, green or yellow; also colorless, reddish orange, pink, white and brown. A single crystal can be multi-colored. Luster is vitreous. Transparency: Crystals are transparent to translucent. Crystal System: Isometric; 4/m bar 3 2/m Crystal Habits include the typical cube and to a lesser extent, the octahedron as well as combinations of these two and other rarer isometric habits. Always with equant crystals; less common are crusts and botryoidal forms. Twinning also produces penetration twins that look like two cubes grown together. Cleavage is perfect in 4 directions forming octahedrons. Fracture is irregular and brittle. Hardness is 4 Specific Gravity is 3.1+ (average) Streak is white. Other Characteristics: Often fluorescent blue or more rarely green, white, red or violet and may be thermoluminescent, phosphorescent and triboluminescent. Associated Minerals are many and include calcite, quartz, willemite, barite, witherite, apatite, chalcopyrite, galena, sphalerite, pyrite and other sulfides. Best Field Indicators are crystal habit, color zoning, hardness (harder than calcite, but softer than quartz or apatite), fluorescence and especially the octahedral cleavage. PHYSICAL CHARACTERISTICS OF MUSCOVITE: Color is white, silver, yellow, green and brown. Luster is vitreous to pearly. Transparency crystals are transparent to translucent. Crystal System is monoclinic; 2/m Crystal Habits include tabular crystals with a prominant pinacoid termination. Muscovites four prism faces form diamond shaped "books" and if modified by another pinacoid they form pseudo-hexagonal crystal "books". The sides of the crystal often tend to tapper. Also as lamellar rock forming masses and small flakes in detrital matterial. Twinned crystals can form flat five pointed stars. Cleavage is perfect in one direction producing thin sheets or flakes. Fracture is not readily observed due to cleavage but is uneven. Hardness is 2 - 2.5. Specific Gravity is approximately 2.8 (average) Streak is white. Associated Minerals are quartz, feldspars, beryl and tourmalines. Other Characteristics: cleavage sheets are flexible and elastic, meaning they can be bent and will flex back to original shape. Best Field Indicators are crystal habit, cleavage, elastic sheets, color and associations. Fracture: uneven Hardness: 4 Flourite Luster: Vitreous Occurrence: Fluorite may occur as a vein deposit, especially with metallic minerals, where it often forms a part of the gangue (the worthless "host-rock" in which valuable minerals occur) and may be associated with galena, sphalerite, barite, quartz, and calcite. It is a common mineral in deposits of hydrothermal origin and has been noted as a primary mineral in granites and other igneous rocks and as a common minor constituent of dolostone and limestone. Muscovite is a common rock forming mineral and is found in igneous, metamorphic and detrital sedimentary rocks. Rock Type: Sedimentary Specific Gravity: 3.1 Streak: white Variety: Fluorite is a widely occurring mineral which is found in large deposits in many areas and comes in a wide variety of colors. Muscovite is not often valuable as a mineral specimen but sheets of muscovite have a high heat and electrical insulating properties and are used to make many electical components. Muscovite sheets were used for kitchen oven windows before synthetic materials replaced them.

Collection

RAGM Mineral Collection

Acquisition

Accession

2009.62

Source or Donor

Museum Collection of Minerals

Acquisition Method

Donation

Dimensions

Width

7-3/4 in

Depth

3 in

Length

6-1/4 in

Weight

6.84 oz

Location

Location

Display Case

DS-8

Room

Delmar Smith Hall

Building

Crater Rock Museum

Category

Permanent

Moved By

Curtis Gardner

Date

May 24, 2023

Notes

Added current location

Location

Container

Right

Drawer

3rd Shelf

Shelf

Center, Center

Wall

South wall

Room

Delmar Smith Hall

Building

Crater Rock Museum

Category

Permanent

Moved By

Steve Miller

Date

January 15, 2010

Location

Container

Right

Cabinet

Case #39

Wall

West

Room

Delmar Smith Hall

Building

Crater Rock Museum

Category

Permanent

Location

Drawer

far right

Shelf

middle 3rd shelf, middle 3rd shelf

Wall

South wall

Room

Delmar Smith Hall

Building

Crater Rock Museum

Category

Permanent