|
Click on a
letter above to view the list of gems. |
|
|
|
| Arrojadite
was named to
honor Miguel Arrojado Ribeiro Lisbôa (1872–1932),
a Brazilian engineer, geologist and geographer. He gained international renown for his studies of manganese and monazitic sands.
| Discovered
in 1925; IMA
status:
Valid (pre-IMA; Grandfathered) |
|
Chemistry
|
|
|
Chemical
Formula: |
KNa4Ca(Fe2+,Mn2+)14Al(PO4)12(OH)2
|
|
Potassium
Sodium Calcium Iron Manganese Aluminum Phosphate Hydroxide
|
Molecular
Weight: |
2,033.08 gm
|
Composition: |
Potassium |
1.92 % |
K |
2.32 % |
K2O |
|
Sodium |
4.52 % |
Na |
6.10 % |
Na2O |
|
Calcium |
1.97 % |
Ca |
2.76 % |
CaO |
|
Magnesium |
2.39 % |
Mg |
3.96 % |
MgO |
|
Manganese |
10.81 % |
Mn |
13.96 % |
MnO |
|
Aluminum |
1.33 % |
Al |
2.51 % |
Al2O3 |
|
Iron |
19.23 % |
Fe |
24.74 % |
FeO |
|
Phosphorus |
18.28 % |
P |
41.89 % |
P2O5 |
|
Hydrogen |
0.12 % |
H |
1.11 % |
H2O |
|
Oxygen |
38.95 % |
O |
|
|
|
Fluorine |
0.47 % |
F |
0.47 % |
F |
|
— |
—
% |
F |
-0.20 % |
-O=F2 |
|
|
100.00 % |
|
99.61 % |
= TOTAL OXIDE |
|
|
Classification
|
|
|
Mineral
Classification: |
Phosphates
|
Strunz 8th
Ed. ID:
|
7/B.20-10
|
Nickel-Strunz 10th
Ed. ID:
|
8.BF.05
|
|
8 : PHOSPHATES, ARSENATES, VANADATES
B : Phosphates, etc., with additional anions, without H2O
F : With medium-sized and large cations, (OH, etc.):RO4< 0.5:1
|
Related
to: |
Arrojadite Group. Arrojadite-(KFe)-Dickinsonite-(KMnNa) Series
|
Members
of Group: |
Arrojadite Group:
Arrojadite-(BaFe), Arrojadite-(BaNa), Arrojadite-(KFe),
Arrojadite-(KFeNa), Arrojadite-(KNa), Arrojadite-(NaFe),
Arrojadite-(PbFe), Arrojadite-(SrFe), Dickinsonite-(KMnNa),
Ferri-arrojadite-(BaNa), Fluorarrojadite-(BaFe), Fluorarrojadite-(KNa),
Fluorarrojadite-(NaFe)
|
Varieties: |
None
|
Synonyms: |
Arrojadite,
Headdenite
|
|
|
Crystal
Data
|
|
|
Crystallography:
|
Monoclinic - Domatic
|
Crystal
Habit:
|
As
cleavable masses, to 15 cm
|
Twinning:
|
None
|
|
|
Physical
Properties
|
|
|
Cleavage: |
Good
on {100}, poor on {102}
|
Fracture: |
Uneven/Irregular
to Subconchoidal
|
Tenacity:
|
Brittle
|
Moh's
Hardness: |
5.0
|
Density:
|
3.50
- 3.60 (g/cm3)
|
Luminescence:
|
None
|
Radioactivity:
|
Barely
Detectable;
GRapi = 26.90 (Gamma Ray American Petroleum Institute Units)
|
|
|
Optical
Properties
|
|
|
Color: |
Dark
green, bottle-green, yellowish green, brownish yellow,
|
Transparency: |
Translucent
|
Luster: |
Vitreous
to greasy |
Refractive
Index: |
1.664
- 1.675 Biaxial ( + )
|
Birefringence: |
0.011
|
Dispersion: |
Strong, r
< v |
Pleochroism: |
Visible; X
= colorless; Y
= colorless to pale green; Z
= pale yellow-green |
|
|
Occurances
|
|
|
Geological
Setting: |
A
high-temperature (~ 800°C) primary mineral in granite
pegmatites. |
Common
Associations: |
Graftonite,
Cassiterite, Spodumene, Beryl, Muscovite (Nickel Plate
mine, South Dakota, USA)
|
Common
Impurities: |
n/a
|
Co-Type
Localities: |
•
Serra Branca pegmatite, Pedra Lavrada, Borborema mineral province, Paraíba, Brazil
• Nickel Plate Mine, Keystone, Keystone District, Pennington Co., South Dakota, USA
|
Year
Discovered: |
1925
|
View
mineral photos: |
Arrojadite
Mineral Photos and Locations |
|
|
More
Information
|
|
|
|
Mindat.org
Webmineral.com
|
|
|
Arrojadite-(KFe)
is a rare phosphate mineral. It was named to
honor Miguel Arrojado Ribeiro Lisbôa (1872–1932),
a Brazilian engineer, geologist and geographer. He gained international renown for his studies of manganese and monazitic sands.
In 2005 Arrojadite's name was changed to Arrojadite-(KFe)
by the International Mineralogical Association (IMA)
as
part of the revision of the nomenclature of the Arrojadite Group to
distinguish it chemically from the other members of
the group. Many of the other members of the group have
the same root name with various suffixes added to denote
their unique chemical structures. The following are
some of the members of the Arrojadite Group: Arrojadite-(BaFe),
Arrojadite-(BaNa), Arrojadite-(KFe), Arrojadite-(KFeNa),
Arrojadite-(KNa), Arrojadite-(NaFe), Arrojadite-(PbFe),
Arrojadite-(SrFe).
Arrojadite
is rarely, if ever, found as transparent crystals large
enough for faceting. It is typically found as translucent
to opaque, cleavable masses. Gems have been faceted
from this material purely as a rare collector's gem.
The best specimens for mineral collectors come from a find in
2001 at the Big Fish River–Rapid Creek area, Dawson Mining District, Yukon Territory, Canada.
This source has produced some of the richest examples of Arrojadite
ever found.
Distribution:
In Brazil, from the Serra Branca pegmatite, 13 km south
of Pedra Lavrada, Picuí, Paraíba; in the
Énio pegmatite mine, northeast of Galiléia,
and the Sapucaia pegmatite mine, about 50 km east-southeast
of Governador Valadares, Minas Gerais. In the USA, in
New Hampshire, from the G.E. Smith mine, Newport, Sullivan
County, and at the Rice, Nancy #2, and Palermo #1 mines,
near North Groton, Grafton County; in South Dakota,
from the Nickel Plate and White Cap mines, near Keystone,
Pennington County, and in the Victory mine, four km
northeast of Custer, Custer County. From the Big Fish
River–Rapid Creek area, Yukon Territory, Canada. In
the Mangualde pegmatite, near Mesquitela, Portugal.
From Glenbuchat, Aberdeenshire, Scotland. In the Norrö
pegmatite, on Rånö Island, Sweden. At Sidi-Bou-Kritcha,
Morocco. In Zimbabwe, from Ruwanzi Ranch, Karoi East,
Miami, and on the Star Twin, Pearl and Chiwya claims,
Urungwe district. In the Buranga pegmatite, near Gatumba,
Rwanda.
|
Arrojadite
gems for sale:
We
have not photographed our Arrojadite
gems yet. Please
check back soon.
|
|