Muscovite, Schorl and Albite

ID	515
Mineral	Muscovite Schorl Albite
Location	Ferruginha pegmatite - Ferruginha - Minas Gerais - Brazil
Fluorescence	LW-UV: close SW-UV: close
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Mindat data

ID	2815
Long ID	1:1:2815:4
Formula	`KAl₂(Si₃Al)O₁₀(OH)₂`
IMA Status	0 1
Other Occurrences	Muscovite is common in many different rock types as a primary mineral.
Diapheny	Transparent,Translucent
Cleavage	Perfect on {001}.
Tenacity	elastic
Colour	White to colorless, silvery-white, and tinged various colors by impurities.
Hardness (min)	2.5
Hardness (max)	2.5
About the name	The earliest names attributable to muscovite include Muscovy Glass, Cat Silver, and Lapis Specularis (stone mirror); these names appearing in texts in the seventeenth century and before. The stand-alone name 'Muscovite' was used as early as 1794 by Johann Gottfried Schmeisser in his System of Mineralogy and is derived from the term "Muscovy glass," which was in common use by that time. Muscovy Province in Russia yielded sheet mica for a variety of uses. Muscovite and sometimes similar species were earlier called mica (Phillips and Kersey, 1706), glimmer (Phillips and Kersey, 1706), and isinglass (1747 according to OED) but all of these terms are still in use to some degree. It should be noted that mica, glimmer, and isinglass were also used for a variety of materials before these given dates and in those earlier times did not always indicate what would be a mineral, much less muscovite proper. Isinglass, for example, was originally used for a gelatinous bladder found in sturgeon.
Streak	White
Crystal System	Monoclinic
Cleavage Type	Perfect
Fracture type	Micaceous
Morphology	Crystals uncommon, tabular {001} with rhombic to hexagonal outlines, often bound by {221}, {_111} and {010} (hkl refer to -2M^1 polytype). Less common as prismatic, parallel to [001], with a crude hexagonal cross section. Most typically found as "books" and as flaky grains in various rocks. Sometimes in plumose or fibrous aggregates.
Twinning	Mica law twins common [310] forming six pointed stars, less common with the composition plane perpendicular to {001} (hkl refer to -2M^1 polytype).
shortcode_ima	Ms
Group	Dioctahedral mica

ID	3578
Long ID	1:1:3578:7
Formula	`NaFe²⁺₃Al₆(Si₆O₁₈)(BO₃)₃(OH)₃(OH)`
IMA Status	0 1
Occurrence	In placers.
Other Occurrences	In granites and granitic pegmatites, high temperature hydrothermal veins, metamorphic rocks.
Discovery Year	1505
Diapheny	Translucent,Opaque
Cleavage	Very poor on {11_20}, {10_11}
Tenacity	brittle
Colour	Bluish-black to black, sometimes brownish-black, rarely greenish-black.
Hardness (min)	7.0
Hardness (max)	7.0
Luminescence	Nonfluorescent.
Lustre	Vitreous to oily, dull.
About the name	The early history of the mineral schorl shows that the name "Schorl" was in use prior to the year 1400 (AD) because a village known today as Zschorlau (in Saxony, Germany) was then named "Schorl" (or minor variants of this name). This village had a nearby tin mine where, in addition to cassiterite, a lot of black tourmaline was found. First mentioned by Ulrich Rülein von Calw 1505. The first relatively detailed description of schorl with the name "schürl" and its occurrence (various tin mines in the Saxony Ore Mountains) was written by Johannes Mathesius (1504-1565) in 1562 under the title "Sarepta oder Bergpostill". Up to about 1600, additional names used in the German language were "Schurel", "Schörle", and "Schurl". From the 18th century on, the name "Schörl" was mainly used in the German-speaking area. In English, the names "shorl" and "shirl" were used in the 18th century for schorl. In the 19th century the names "common schorl", "schörl", "schorl" and "iron tourmaline" were used in the Anglo-Saxon area (Ertl, 2006).
Streak	Greyish-white to bluish-white.
Crystal System	Trigonal
Cleavage Type	Poor/Indistinct
Fracture type	Irregular/Uneven,Sub-Conchoidal
Morphology	Prismatic to acicular.
Twinning	Rarely on {10_10} and {40_41}.
Publication Year	1524
key_elements	0
shortcode_ima	Srl
Group	Tourmaline

ID	96
Long ID	1:1:96:9
Formula	`Na(AlSi₃O₈)`
IMA Status	0 1
Other Occurrences	A major constituent of granites and granite pegmatites, alkalic diorites, basalts, and in hydrothermal and alpine veins. A product of potassium metasomatism and in low-temperature and low-pressure metamorphic facies and in some schists. Detrital and authigenic in sedimentary rocks.
Discovery Year	1815
Diapheny	Transparent,Translucent,Opaque
Cleavage	on [001], good on [010], imperfect on {110}
Tenacity	brittle
Colour	White to gray or colorless, uncommonly blue tinted or rarely green or red tinted, while much included albite may be strongly colored..
Hardness (min)	6.0
Hardness (max)	6.5
Lustre	Vitreous, pearly
About the name	Named in 1815 by Johan Gottlieb Gahn and Jöns Jacob Berzelius from Latin "albus", white, alluding to its usual color.
Streak	White
Crystal System	Triclinic
Cleavage Type	Perfect
Fracture type	Irregular/Uneven,Conchoidal
Morphology	Crystals commonly tabular parallel {010} (thin plates to blocky crystals), may be curved, to 3 cm; divergent aggregates, granular, cleavable massive.
Twinning	Common around [010] or perpendicular {010}, giving polysynthetic striae on 001 or {010}; many other laws, contact, simple and multiple.
Comment Luster	Pearly on cleavages
shortcode_ima	Ab
Group	Plagioclase

Price: € 20

Dimensions: Not registered

Weight: Not registered

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Notes:

Symbol	Element
Al	Aluminium
B	Boron
Fe	Iron
H	Hydrogen
K	Potassium
Na	Sodium
O	Oxygen
Si	Silicium

Muscovite, Schorl and Albite

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