Quartz var citrine

Object/Artifact

-

Crater Rock Museum

Name/Title

Quartz var citrine

Entry/Object ID

2009.62.127

Description

Chemical Composition: Silicon dioxide Crystal System: Tetragonal System Description: Common Name: Quartz Chemistry: SiO2 , Silicon dioxide Class: Silicates Location: Rio Grand do Sul, Brazil Description: Extremely large (1m), cylindrical, cavernous specimen, with a uniform yellow to brown crystalline structure throughout the inside on a white crystalline matrix. PHYSICAL CHARACTERISTICS: Color is as variable as the spectrum, but clear quartz is by far the most common color followed by white or cloudy (milky quartz). Purple (Amethyst), pink (Rose Quartz), gray or brown to black (Smoky Quartz) are also common. Cryptocrystalline varieties can be multicolored. Luster is glassy to vitreous as crystals, while cryptocrystalline forms are usually waxy to dull but can be vitreous. Transparency: Crystals are transparent to translucent, cryptocrystalline forms can be translucent or opaque. Crystal System is trigonal; 3 2. Crystal Habits are again widely variable but the most common habit is hexagonal prisms terminated with a six sided pyramid (actually two rhombohedrons). Three of the six sides of the pyramid may dominate causing the pyramid to be or look three sided. Left and right handed crystals are possible and identifiable only if minor trigonal pyramidal faces are present. Druse forms (crystal lined rock with just the pyramids showing) are also common. Massive forms can be just about any type but common forms include botryoidal, globular, stalactitic, crusts of agate such as lining the interior of a geode and many many more. Cleavage is very weak in three directions (rhombohedral). Fracture is conchoidal. Hardness is 7, less in cryptocrystalline forms. Specific Gravity is 2.65 or less if cryptocrystalline. (average) Streak is white. Other Characteristics: Striations on prism faces run perpendicular to C axis, piezoelectric (see tourmaline) and index of refraction is 1.55. Associated Minerals are numerous and varied but here are some of the more classic associations of quartz (although any list of associated minerals of quartz is only a partial list): amazonite a variety of microcline, tourmalines especially elbaite, wolframite, pyrite, rutile, zeolites, fluorite, calcite, gold, muscovite, topaz, beryl, hematite and spodumene. Best Field Indicators are first the fact that it is very common (always assume transparent clear crystals may be quartz), crystal habit, hardness, striations, good conchoidal fracture and lack of good cleavage. Fracture: Conchoidal Hardness: 7 Quartz Luster: Vitreous Occurrence: Pure quartz, sometimes called clear quartz, is colorless or white and transparent (clear) or translucent. Common colored varieties include citrine, rose quartz, amethyst, smoky quartz, milky quartz, and others. Quartz goes by an array of different names. The most important distinction between types of quartz is that of macrocrystalline (individual crystals visible to the unaided eye) and the microcrystalline or cryptocrystalline varieties (aggregates of crystals visible only under high magnification). The cryptocrystalline varieties are either translucent or mostly opaque, while the transparent varieties tend to be macrocrystalline. Chalcedony is a cryptocrystalline form of silica consisting of fine intergrowths of both quartz, and its monoclinic polymorph moganite.[2] Rock Type: Sedimentary Specific Gravity: 2.65 Streak: white

Collection

RAGM Mineral Collection

Acquisition

Accession

2009.62

Source or Donor

Museum Collection of Minerals

Acquisition Method

Donation

Dimensions

Width

38-1/4 in

Depth

9 in

Length

9-3/4 in

Location

Location

Display Case

DS-14

Room

Delmar Smith Hall

Building

Crater Rock Museum

Date

December 27, 2023

Location

Drawer

far left

Shelf

bottom front left, bottom front left

Wall

West wall

Room

Delmar Smith Hall

Building

Crater Rock Museum

Category

Permanent

Moved By

Scott Longan

Date

September 26, 2009

Location

Drawer

Middle

Shelf

Middle, Middle

Wall

West wall

Room

Delmar Smith Hall

Building

Crater Rock Museum

Category

Permanent

Moved By

Scott Longan

Date

September 26, 2009

Location

Container

center

Drawer

Bottom

Shelf

Center

Cabinet

Case #39

Wall

West wall

Room

Delmar Smith Hall

Building

Crater Rock Museum

Category

Permanent