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sepiolite
EntityQ414096· pop 30· linked from 189 articles

Also known as Meerschaum

Sepiolite, also known in English by the German name meerschaum ( , ; ; meaning "sea foam"), is a soft white clay mineral, often used to make tobacco pipes (known as meerschaum pipes). A complex magnesium silicate, a typical chemical formula for which is Mg4Si6O15(OH)2·6H2O, it can be present in fibrous, fine-particulate, and solid forms.

Key facts

Mineral.name
Sepiolite
Mineral.category
Phyllosilicate minerals
Mineral.image
Mineraly.sk - sepiolit.jpg
Mineral.imagesize
260px
Mineral.formula
Mg4Si6O15(OH)2·6H2O
Mineral.IMAsymbol
Sep
Mineral.strunz
9.EE.25
Mineral.dana
74.03.01b.01 Palygorskite-sepiolite group
Mineral.system
Orthorhombic
Mineral.class
Dipyramidal (mmm) H-M symbol: (2/m 2/m 2/m)
Mineral.symmetry
Pnna
Mineral.unit cell
a = 5.21 Å, b = 26.73 Å c = 13.5 Å; Z = 4
Mineral.color
Grayish white, white, white with a yellowish or reddish tinge; bluish green
Mineral.habit
Compact nodular, earthy, clayey, massive; rarely fine fibrous along [001]
Mineral.mohs
2
Mineral.luster
Dull, earthy
Mineral.streak
White
Mineral.diaphaneity
Opaque

via Wikipedia infobox

Wikidata facts

Subclass of
palygorskite
Named after
stone
Image
Sepiyolit.jpg
Said to be same as
meerschaum
Show 11 more facts
Nickel-Strunz 9th edition (updated 2009)
9.EE.25
Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
9.EE.25
Commons category
Sepiolite
type locality (geology)
Bettolino
streak color
white
Mohs' hardness
2.25
IMA Mineral Symbol
Sep
chemical formula
Mg₄Si₆O₁₅(OH)₂·6H₂O
Strunz 8th edition (series ID, updated)
VIII/E.13b
Sources (5)

via Wikidata · CC0

~9 min read

Encyclopedic overview

8 sections
Contents
  • Characteristics
  • Location
  • Applications
  • Carved pipes
  • Other uses and substitutes
  • See also
  • References
  • External links

Sepiolite, also known in English by the German name meerschaum ( , ; ; meaning "sea foam"), is a soft white clay mineral, often used to make tobacco pipes (known as meerschaum pipes). A complex magnesium silicate, a typical chemical formula for which is Mg4Si6O15(OH)2·6H2O, it can be present in fibrous, fine-particulate, and solid forms.

The fibrous clay minerals have recently been shown to exist as a continuous polysomatic series where the endmembers are sepiolite and palygorskite. There is a continuous variation in chemical composition from sepiolite, the most magnesic and trioctahedral endmember, to palygorskite, the least magnesic, most Al- and Fe-bearing, most dioctahedral endmember.

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