To install click the Add extension button. That's it.

The source code for the WIKI 2 extension is being checked by specialists of the Mozilla Foundation, Google, and Apple. You could also do it yourself at any point in time.

4,5
Kelly Slayton
Congratulations on this excellent venture… what a great idea!
Alexander Grigorievskiy
I use WIKI 2 every day and almost forgot how the original Wikipedia looks like.
Live Statistics
English Articles
Improved in 24 Hours
Added in 24 Hours
Languages
Recent
Show all languages
What we do. Every page goes through several hundred of perfecting techniques; in live mode. Quite the same Wikipedia. Just better.
.
Leo
Newton
Brights
Milds

From Wikipedia, the free encyclopedia

Samuelsonite
General
CategoryPhosphate minerals
Formula
(repeating unit)
(Ca,Ba)Ca8Fe22+Mn22+Al2[(OH)2(PO4)10]
IMA symbolSms[1]
Strunz classification8.BF.10
Crystal systemMonoclinic
Crystal classPrismatic (2/m)
(same H-M symbol)
Space groupC2/m
Unit cella= 18.495 Å, b= 6.805 Å
c= 14.000 Å, β= 112.75°; Z = 2
Identification
ColorPale yellow
Crystal habitPrismatic crystals, elongated and striated
CleavageFair on {001}
Mohs scale hardness5
LusterAdamantine, Sub-Adamantine
StreakWhite
DiaphaneityTransparent
Specific gravity3.353
Optical propertiesBiaxial (+)
Refractive indexnα = 1.645 - 1.648 nβ = 1.650 - 1.655 nγ = 1.655 - 1.667
Birefringence0.0100-0.0190
References[2][3][4]

Samuelsonite is a complex mineral that is found near North Groton, Grafton County, New Hampshire, US. Additionally, it is most commonly found as a secondary mineral in granite pegmatite. Samuelsonite is named after Peter B. Samuelson,[2] a prospector from Rumney, New Hampshire.

The mineral has a pale yellow color and has a hardness of 5 on Mohs scale.[3] The crystal is generally yellow, flat, and with straited crystals and blue trolleites.[5] Samuelsonite is monoclinic. There are three vectors of unequal length in this crystal system. The three vectors form a rectangular prism with a parallelogram at the base. Therefore, two of the vectors are perpendicular, while the third makes an angle that is not equal to 90°.[6] Samuelsonite has biaxial birefringence (trirefringence), meaning when light passes through the optic axis it is split into two rays due to the difference in refractive index of the ray with parallel polarized light compared to the ray with perpendicular polarized light.

References

  1. ^ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.
  2. ^ a b "General Samuelsonite Information". Retrieved 2 October 2010.
  3. ^ a b Jolyon Ralph and Ida Chau. "Samuelsonite". mindat.org. Retrieved 2 October 2010.
  4. ^ Handbook of Mineralogy
  5. ^ "Samuelsonite R080081". Retrieved 2 October 2010.
  6. ^ Rapp Jr. G.R., Campbell, T.J., and Roberts, W.L. (1990) Enclycopedia of Minerals (2nd Edition) 797 p. Library of Congress Cataloging, Washington, D.C.


This page was last edited on 10 August 2023, at 01:15
Basis of this page is in Wikipedia. Text is available under the CC BY-SA 3.0 Unported License. Non-text media are available under their specified licenses. Wikipedia® is a registered trademark of the Wikimedia Foundation, Inc. WIKI 2 is an independent company and has no affiliation with Wikimedia Foundation.