n.
A white, red, or yellow zeolite mineral, CaO·Al2O3·6SiO2·5H2O.
[After Henry Heuland, 19th-century British mineralogist.]
Dictionary:
heu·land·ite (hyū'lən-dīt')
|
[After Henry Heuland, 19th-century British mineralogist.]
| 5min Related Video: heulandite |
| Sci-Tech Encyclopedia: Heulandite |
A mineral belonging to the zeolite family of silicates. It usually occurs in crystals with the prominent side being pinacoid, often having a diamond shape. There is perfect side pinacoid cleavage on which the luster is pearly; elsewhere the luster is vitreous. The hardness is 3½ to 4 on Mohs scale; specific gravity is 2.18–2.20. The mineral is usually white or colorless but may be yellow or red. See also
Heulandite is essentially a hydrous calcium aluminum silicate, Ca(Al2Si7Ol8) · 6H2O. Heulandite is a secondary mineral found in cavities in basalts associated with other zeolites and calcite. Notable localities are in the Faeroe Islands, India, Nova Scotia, and West Paterson, New Jersey.
| Rock & Mineral Guide: heulandite |
Environment
Typical zeolite associations.
Crystal descriptionAlways in elongated tabular crystals, to 1 in. (2.5 cm) in length but usually smaller. Shape characteristic, widest at center, like an old-fashioned coffin; hence, in older books, called "coffin-shaped."
Physical propertiesWhite, reddish, yellowish. Luster pearly on the often slightly concave cleavage face and glassy otherwise; hardness 3Ɖ-4; specific gravity 2.2, streak white; fracture subconchoidal to uneven; cleavage perfect side pinacoid. Brittle and flaky; transparent to translucent.
CompositionHydrous sodium, calcium, potassium aluminum silicate (9.2% CaO, 16.8% Al 2 O3, 59.2% SiO 2 , 14.8% H 2 O).
TestsOn fusion swells and writhes, finally melting at ends to white droplets; fused mass often has a stringy look.
Distinguishing characteristicsCrystal form very typical and usually suffices, when considered in its associations as a zeolite. Stilbite and apophyllite also have a pearly look in one direction but usually the crystal form is distinctive. Stilbite fuses in more splintery fragments; apophyllite fuses with bubbling but much less swelling.
OccurrencePerhaps the most common zeolite. Beautifully developed in the traprock quarries of the Paterson, New Jersey, region near New York City. Also in fine crystals in Nova Scotia in the Partridge I. area. Good crystals were found years ago in Berufjördhur, Iceland, and it was named for an early English mineral dealer, H. Heuland, who went there to collect specimens. Very common, but usually small, amygdular pocket linings. Common, but usually small in many Idaho, Oregon, and Washington traprock localities. Larger (2 in., 5 cm) red crystals are found at Gunnedah, New South Wales; and eastern Russia.
| WordNet: heulandite |
The noun has one meaning:
Meaning #1:
a group of minerals of the zeolite family consisting of a hydrous aluminum silicate of sodium and calcium
| Wikipedia: Heulandite |
Heulandite is the name of a series of tecto-silicate minerals of the zeolite group. Prior to 1997, heulandite was recognized as a mineral species, but a reclassification in 1997 by the International Mineralogical Association changed it to a series name, with the mineral species being named heulandite-Ca, heulandite-Na, heulandite-K, and heulandite-Sr. Heulandite-Ca, the most common of these, is a hydrous hydrous calcium and aluminium silicate, (Ca,Na)2-3Al3(Al,Si)2Si13O36·12H2O. Small amounts of sodium and potassium are usually present replacing part of the calcium. Strontium replaces calcium in the heulandite-Sr variety. The appropriate species name depends on the dominant element. The species are visually indistinguishable, and the series name heulandite is still used whenever testing has not been performed.
Crystals are monoclinic. They may have a characteristic coffin-shaped habit, but may also form simple rhombic prisms. Frequently, a crust of fine crystals will form with only the ends of the rhombs visible, making the crystals look like wedges. They have a perfect cleavage parallel to the plane of symmetry, on which the lustre is markedly pearly; on other faces the lustre is of the vitreous type. The mineral is usually colourless or white, but may be orange, brown, yellow, brick-red, or green due to inclusions of celadonite. It varies from transparent to translucent. Isomorphous with heulandite is the strontium and barium zeolite brewsterite.
The Mohs' hardness is 3-4, and the specific gravity 2.2. Heulandite is similar to stilbite. The two minerals may, however, be readily distinguished by the fact that in heulandite the acute positive bisectrix of the optic axes emerges perpendicular to the cleavage.
Heulandite was first separated from stilbite by August Breithaupt in 1818, and named by him "euzeolite" (meaning beautiful zeolite); independently, in 1822, H. J. Brooke arrived at the same result, giving the name heulandite, after the mineral collector, Henry Heuland (1778-1856).
Heulandite occurs with stilbite and other zeolites in the amygdaloidal cavities of basaltic volcanic rocks, and occasionally in gneiss and hydrothermal veins.
The best specimens are from the basalts of Berufjord, near Djupivogr, in Iceland and the Faroe Islands, and the Deccan traps of the Sahyadri Mountains near Bombay. Crystals of a brick-red colour are from Campsie Fells in Stirlingshire and the Fassathal in Tirol. A variety known as beaumontite occurs as small yellow crystals on syenitic schist near Baltimore in Maryland.
This entry is from Wikipedia, the leading user-contributed encyclopedia. It may not have been reviewed by professional editors (see full disclaimer)
| clinoptilolite (mineralogy) | |
| zeolite | |
| stilbite |
| Does Heulandite have any healing properties? Read answer... |
Copyrights:
![]() | Dictionary. The American Heritage® Dictionary of the English Language, Fourth Edition Copyright © 2007, 2000 by Houghton Mifflin Company. Updated in 2009. Published by Houghton Mifflin Company. All rights reserved. Read more | |
![]() | Sci-Tech Encyclopedia. McGraw-Hill Encyclopedia of Science and Technology. Copyright © 2005 by The McGraw-Hill Companies, Inc. All rights reserved. Read more | |
![]() | Rock & Mineral Guide. Peterson Field Guide to Rocks and Minerals, by Frederick H. Pough. Copyright © 1998 by Houghton Mifflin Company. Published by Houghton Mifflin Company. All rights reserved. Read more | |
![]() | WordNet. WordNet 1.7.1 Copyright © 2001 by Princeton University. All rights reserved. Read more | |
![]() | Wikipedia. This article is licensed under the Creative Commons Attribution/Share-Alike License. It uses material from the Wikipedia article "Heulandite". Read more |