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EntityQ421527· pop 14· linked from 177 articles

Howlite, a calcium borosilicate hydroxide (Ca2B5SiO9(OH)5), is a borate mineral found in evaporite deposits.

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Vinony's link graph records 177 inbound references to howlite, and connects out to borate class of minerals, Mohs scale of mineral hardness and gold.

Vinony files it under Inoborates, Minerals in space group 14 and Monoclinic minerals.

Vinony links it to 13 Wikipedia language editions.

Key facts

Mineral.name
Howlite
Mineral.category
Inoborates
Mineral.image
Howlite.jpg
Mineral.imagesize
260px
Mineral.formula
Ca2B5SiO9(OH)5
Mineral.IMAsymbol
How
Mineral.strunz
6.CB.20
Mineral.dana
25.3.5.1
Mineral.system
Monoclinic
Mineral.class
Prismatic (2/m) (same H-M symbol)
Mineral.symmetry
P21/c
Mineral.unit cell
a = 12.82 Å, b = 9.351(1) Å c = 8.608(2) Å; β = 104.84(2)°; Z = 4
Mineral.color
White, colorless
Mineral.habit
Massive to nodular, occurs as tabular prisms flattened parallel to [100]
Mineral.cleavage
None
Mineral.fracture
Conchoidal, uneven
Mineral.mohs
3.5
Mineral.luster
Subvitreous, glimmering

via Wikipedia infobox

Wikidata facts

Image
Howlite - tumble polished stone.jpg
Show 8 more facts
Strunz 8th edition (series ID, updated)
VIII/A’.13
Commons category
Howlite
Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
6.CB.20
Nickel-Strunz 9th edition (updated 2009)
6.CB.20
streak color
white
IMA Mineral Symbol
How
chemical formula
Ca₂B₅SiO₉(OH)₅
Sources (1)

via Wikidata · CC0

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Encyclopedic overview

7 sections
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Howlite, a calcium borosilicate hydroxide (Ca2B5SiO9(OH)5), is a borate mineral found in evaporite deposits.

== History == Howlite was discovered near Windsor, Nova Scotia, in 1868 by Henry How (1828–1879), a Canadian chemist, geologist, and mineralogist. How was alerted to the unknown mineral by miners in a gypsum quarry, who found it to be a nuisance. He called the new mineral silico-boro-calcite; it was given the name howlite by the American geologist James Dwight Dana shortly thereafter.

Excerpted from Wikipedia’s “howlite” article, available under the CC BY-SA 4.0 licence.

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