Stilbite on Apophyllite

Object/Artifact

-

Crater Rock Museum

Apophyllite

Apophyllite

Name/Title

Stilbite on Apophyllite

Entry/Object ID

2009.62.73

Description

Chemical Composition: see description Crystal System: Hexagonal System Description: Common Name: Apophyllite / Stilbite Chemistry: (K,Na)Ca4Si8O20(F,OH) - 8H2O, Hydrated Potassium Calcium Sodium Silicate / NaCa2Al5Si13O36 -14H2O, Hydrated sodium calcium aluminum silicate Fluoride Hydroxide Group: Zeolites Location: Jalgaon, India Description: Small specimen with translucent white crystals of various sizes clustered on a base, with a single Stilbite crystal, pink in color imbedded on it. The matrix is brown with worm-like striations across it, light brown in color. PHYSICAL CHARACTERISTICS OF APOPHYLLITE: Color is clear, white, green, yellow, pink, violet or rarely brown. Luster is vitreous to pearly on cleavage surfaces. Transparency: Crystals are transparent to translucent. Crystal System is tetragonal; 4/m 2/m 2/m; natroapophyllite is orthorhombic, 2/m 2/m 2/m. Crystal Habits include four sided prisms (with a square cross-section) truncated with either a steep four sided pyramid or a pinacoid termination or both. If the pyramids are missing, the crystals can look cubic. Rarely are the prisms missing, but if they are, crystals could appear octahedral because of the four sided pyramids. The faces of the pyramids do not lineup with the prism faces but with their edges, therefore the pyramid faces have four edges and appear diamond shaped instead of triangular like the pyramid faces of quartz. Rare tabular hydroxyapophyllite crystals are also known. Cleavage is perfect in one direction (basal). Fracture is uneven. Hardness is 4.5 - 5. Specific Gravity is approximately 2.3 - 2.4 (lighter than most translucent minerals). Streak is white. Other Characteristics: Prism faces are striated lengthwise, some specimens are fluorescent and crystals will flake when heated. Associated Minerals are prehnite, quartz, heulandite, stilbite, natrolite, analcime, datolite, babingtonite, cavansite, calcite, idocrase, wollastonite, kinoite, gyrolite and many other zeolites. Best Field Indicators are crystal habit, striations, associations, environment of formation, cleavage and luster on cleavage surfaces. PHYSICAL CHARACTERISTICS OF STIBITE: Color is pink or white; also tinted yellow and red. Luster is vitreous to pearly especially on the prominant pinacoid and cleavage surfaces. Transparency: crystals are transparent to mostly translucent. Crystal System is monoclinic; 2/m Crystal Habits include platy often thin crystals that can aggregate together into a wheat sheaflike structure. The prominant pinacoid is sometimes but rarely modified by other pinacoid and prism faces. Cruciform (cross-like) twins can also be found. Also forms radiating nodules. Cleavage is perfect in one direction parallel to the prominant pinacoid. Fracture is uneven. Hardness is 3.5 - 4. Specific Gravity is approximately 2.2 (very light) Streak is white. Associated Minerals are quartz, calcite, babingtonite, apophyllite, heulandite, natrolite and other zeolites. Best Field Indicators are crystal habit, luster, density and associations. Fracture: conchoidal Hardness: 3 Calcite Luster: Vitreous Occurrence: Apophyllite is found in the voids in the contact metamorphic zone limestones that surround intrusive rocks. Stilbite commonly forms nice crystals inside the petrified bubbles (called vesicles) of volcanic rocks that have undergone a small amount of metamorphism. Apophyllite specimens are found in ancient lava and basalt flows. The crystals grow in the now solid cavities, called amygdules or vesicles, formed by air bubbles when the rock was molten. Rock Type: Metamorphic Specific Gravity: 2.7 Streak: white Variety: The name apophyllite is derived from the Greek apophylliso, meaning "it flakes off," a reference to this class's tendency flake apart when heated, due to water loss. Stilbite crystals can aggregate together to form a structure resembling wheat sheafs. This hourglass structure looks like several crystals stacked parallel to each other with the tops and bottoms of this structure fanning out while the middle remains thin. Stilbite's hallmark crystal habit is unique to stilbite and a rarer but related zeolite called stellerite. Whether in the wheat sheafs or not, stilbite can be a hansome specimen with its pearly luster and often colorful pink tints.

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

Display Case

FS-11

Room

Frieda Smith Hall

Building

Crater Rock Museum

Category

Permanent

Moved By

Curtis Gardner

Date

May 25, 2023

Notes

Added current location