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| Montmorillonite
is named
after the type locality at the
town of Montmorillon, Vienne, Poitou-Charentes
region, in western France where it was discovered in
1847.
| Discovered
in 1847; IMA
status:
Valid (pre-IMA; Grandfathered) |
|
Chemistry
|
|
|
Chemical
Formula: |
(Na,Ca)0.33(Al,Mg)(Si4O10)(OH)2
•
n(H2O) |
|
Hydrated
Sodium Calcium Aluminum Magnesium Silicate Hydroxide
|
Molecular
Weight: |
549.07 gm
|
Composition: |
Sodium |
0.84 % |
Na |
1.13 % |
Na2O |
|
Calcium |
0.73 % |
Ca |
1.02 % |
CaO |
|
Aluminum |
9.83 % |
Al |
18.57 % |
Al2O3 |
|
Silicon |
20.46 % |
Si |
43.77 % |
SiO2 |
|
Hydrogen |
4.04 % |
H |
36.09 % |
H2O |
|
Oxygen |
64.11 % |
O |
|
|
|
|
100.00 % |
|
100.58 % |
= TOTAL OXIDE |
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Classification
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Mineral
Classification: |
Silicates
(Germanates)
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Strunz 8th
Ed. ID:
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8/H.18-20
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Nickel-Strunz 10th
Ed. ID:
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9.EC.40
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9 : SILICATES (Germanates)
E : Phyllosilicates C : Phyllosilicates with mica sheets, composed of tetrahedral and octahedral nets
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Related
to: |
Smectite
Group.
Isostructural with
Montmorillonite-Vermiculite Group. Beidellite-Montmorillonite Series.
Interstratifies with Chlorite, Muscovite, Illite, Cookeite,
Kaolinite.
|
Members
of Group: |
Smectite
Group:
Aliettite,
Beidellite, Ferrosaponite, Hectorite, Montmorillonite,
Nontronite, Pimelite, Saliotite, Saponite, Sauconite,
Stevensite, Swinefordite, Volkonskoite, Yakhontovite,
Zincsilite
|
Varieties: |
Alumodeweylite,
Askanite, Batrachite, Calcium-Montmorillonite, Delanovite
|
Synonyms: |
Amagorsite,
Daunialite, Fuller's Earth, Goumbrine, Gumbrine, Stolpenite,
Walkerite (of Dana), Walkthon
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Crystal
Data
|
|
|
Crystallography:
|
Monoclinic - Prismatic
|
Crystal
Habit:
|
Tiny
scaly crystals, tabular on {001}; as lamellar or globular
microcrystalline aggregates; clayey, compact, massive.
|
Twinning:
|
None
|
|
|
Physical
Properties
|
|
|
Cleavage: |
Perfect
on {001}
|
Fracture: |
Irregular/Uneven
|
Tenacity:
|
Brittle
|
Moh's
Hardness: |
1.0
- 2.0
|
Density:
|
2.0
- 3.0 (g/cm3)
|
Luminescence:
|
Usually not fluorescent, except by mixtures with Autunite, etc.
|
Radioactivity:
|
Not
Radioactive
|
|
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Optical
Properties
|
|
|
Color: |
White,
pale pink, bu®, yellow, red, green; pink to red coloration is due to high valance Manganese
(Mn).
|
Transparency: |
Translucent
|
Luster: |
Dull,
earthy; low luster due
to fine-grained nature of the mineral |
Refractive
Index: |
1.485
- 1.550 Biaxial ( - )
|
Birefringence: |
0.020
|
Dispersion: |
None |
Pleochroism: |
Visible.
X
= colorless to pale brown, yellow-green; Y
= dark brown to yellow-green, olive-green, pale yellow;
Z
= brown to olive-green, pale yellow.
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Occurances
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Geological
Setting: |
An
alteration product of volcanic tuff and ash, forming
bentonite beds, and of pegmatite dikes and wall rocks
bordering hydrothermal mineral deposits. Forms under
alkaline conditions of poor drainage, with Mg, Ca, Na,
and K remaining in the soil. |
Common
Associations: |
Cristobalite,
Zeolites, Biotite, Quartz, Orthoclase, Dolomite, Amphiboles,
Pyroxenes, Olivine, Calcite, Gypsum, Pyrite, Limonite.
|
Common
Impurities: |
Fe,
K
|
Type
Locality: |
Montmorillon, Vienne, Poitou-Charentes, France
|
Year
Discovered: |
1847
|
View
mineral photos: |
Montmorillonite
Mineral Photos and Locations |
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More
Information
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|
Mindat.org
Webmineral.com
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Montmorillonite
is a member of the Smectite Group of minerals that also
includes Volkonskoite.
Montmorillonite
and Volkonskoite are also considered members of
the general mineral group simply called "the clays".
The clays typically form microscopic or very small, soft,
platy,
micaceous crystals. As
a mineral specimen, Montmorillonite is
usually massive and dull and not very attractive or
interesting. However, Montmorillonite
as inclusions in Quartz can
be very attrractive and interesting. These Montmorillonite
inclusions along with Chlorite and other mineral inclusions
are often referred to as Garden Quartz, Landscape Quartz
or Scenic Quartz because of the interesting forms that
resemble growths of moss or underwater garden or forest scenes. Lodolite is another term,
or trade name, used for this varity of Quartz
with various mineral inclusions. The name Lodolite
translates to mud stone from the Spanish word lodo meaning mud
or sludge. Teófilo Otoni in the northern
part of the Brazilian state of Minas Gerais is one of
the most prolific producers of Lodolite Quartz. Depending
on the type of minerals, Lodolite inclusions can be
found in various shades of green, brown, pink, red,
orange, white and even purple. Montmorillonite
inclusions tend to be pinks, reds and browns while Chlorite
inclusions are mostly shades of green.
Montmorillonite
is named
after the type locality at the
town of Montmorillon, Vienne, Poitou-Charentes
region, in western France where it was discovered in
1847. The
town of Montmorillon is located on the Gartemp River in the east of La Vienne
and dates back to around the end of the eleventh century.
Distribution:
A common clay mineral, with numerous localities worldwide.
From Montmorillon, Vienne, France. As inclusions in
Quartz from Teófilo Otoni, Minas Gerais,
Brazil. In the USA, material considered as standards
from Bayard and Santa Rita, Grant County, New Mexico;
near Chambers, Apache County, Arizona; at Belle Fourche,
Butte County, South Dakota; in Wyoming, on the John
C. Lane tract, Upton, Weston County, at Clay Spur, near
Newcastle, Crook County, and elsewhere. In the Itawamba
mine, Itawamba County, and in mines around Polkville,
Simpson County, Mississippi; at Strasburg, Shenandoah
County, Virginia.
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