Ellsworthite

From Wikipedia, the free encyclopedia
Jump to: navigation, search
This article is about the mineral. For other uses, see Ellsworthite (disambiguation).
Ellsworthite
General
Category Pyrochlore group
Formula
(repeating unit)
(Ca,U)2(Ti,Nb,Ta)2O6(OH)
Crystal symmetry Cubic 4/m 3* 2/m
Identification
Color Amber yellow to dark brown
Crystal system isometric
Cleavage None
Fracture conchoidal fracture
Luster Vitreous
Streak yellow to brownish
Other characteristics Translucent to opaque
References [1][2]

Ellsworthite (Ca,U)2(Ti,Nb,Ta)2O6(OH) is a rare earth mineral mostly found in the northern parts of North America. It is named after H. V. Ellsworth of the Canadian Geological Survey by Walker and Parsons[who?]. Ellsworthite is also known under the name {Betafite}. It is a very U and Th rich mineral, which in fact makes it slightly radioactive. U makes up about 17.1% of the mineral.[3]

Introduction[edit]

Ellsworthite is part of pyrochlore super group and the sub group betafite and was named after the Canadian Mineralogist and surveyor H. V. Ellsworth. Ellsworthite is also known as the mineral Betafite. Ellsworthite is a Th- bearing mineral that is found mostly in Canada and Alaska. It was first discovered in Hybla, Ontario, which is now a ghost town.[2] Minerals of the pyrochlore group present one of the most important modes of occurrence of trace elements (Nb,Ta) and were found in various geological (geochemical) environments. It is very important geochemically that the pyrochlore structure is very suitable for diverse isomorphic substitutions.[4]

Composition[edit]

Ellsworthite has complex hydrous oxides of Nb, Ta, Na, Ca, with hydroxyl and fluorine; it may contain as much as 17% U.[5] It is composed of calcium, uranium, titanium, niobium, tantalum, and oxygen. Ellsworthite is heavily abundant in uranium, niobium and titanium oxides.[1] It is very uranium, thorium, and water rich. One can consider Betafite as a hydrous uranium pyrochlore.[6]

Structure[edit]

The structure of Ellsworthite is cubic and has a point group of 4/m 3* 2/m. It is part of the isometric system and has the space group Fd3m. It forms into a Hexoctahedral with {110}, {100}, {113}, {233}, and {230}.[1] It has conchoidal fracture with no cleavage. Betafite is a synonym to Ellsworthite.

Physical Properties[edit]

Ellsworthite is mostly found in Canada and is amber yellow to dark brown in color. In most cases it has an amber rusty color and has a hardness of about 5.5. The luster is waxy or greasy to vitreous.[1] The outer, more altered parts are relatively high in water and low in uranium. Its streak is yellow to brownish.[1] The inner parts are brown, greenish brown, yellowish brown, or yellow. It is translucent to opaque [1]

Sources[edit]

  1. ^ a b c d e f "Betafite". The Handbook of Mineralogy. Retrieved 21 October 2013. 
  2. ^ a b Frodel, Clifford. (1958). Systematic Mineralogy of Uranium And Thorium, Geological survey bulletin 1064 pg.326-330
  3. ^ Frondel, J.W., Fleischer, M. (1950) A Glossary of Uranium-and Thorium-Bearing minerals. Geological Survey Circular 74, pg.11, http://babel.hathitrust.org/cgi/pt?id=uc1.32106020887797;view=1up;seq=1
  4. ^ Yaroshevski, A.A., Bagdasarev, Yu.A. (2007). Geothermal Diversity Of Minerals of the Pyrochlore Group.
  5. ^ Bates, R.G., Wedow Jr, H. (1953). Preliminary summary review of Thorium- Bearing mineral occurrence in Alaska. Geological Survey bulletin 202
  6. ^ Hogarth D.D. (1961) A study of Pyrochlore and Betafite, volume 6, issue 5. Canadian Mineralogist pg.610