May 29 2014
Walfordite was first discovered in the Tambo mine, Chile, in 1999. It is a mineral species of tellurite.
It was named after Phillip Walford, Vice-President and Chief Geologist of LAC Minerals, who first noticed the mineral.
Properties of Walfordite
The following are the key properties of Walfordite:
	- Cell Data
	
		- Space Group: Ia3
 
		- a = 11.011(5)
 
		- Z = 8
 
	
	 
 
	- Crystal Data
	
		- Cubic
 
		- Point Group: 2/m 3
 
		- Crystals are cubic {100}, may be modified by minor {111}, to 0.2mm
 
		- X-ray Powder Pattern: 3.175 (100), 1.658 (45), 1.944 (44), 2.749 (37), 4.486 (29), 2.943 (23), 2.592 (22)
 
	
	 
 
	- Chemical Composition
	
		
			
				| Elements | 
				Content 1 | 
			
			
				| TeO2 | 
				81.74 | 
			
			
				| TeO3 | 
				8.67 | 
			
			
				| Fe2O3 | 
				8.30 | 
			
			
				| TiO2 | 
				1.11 | 
			
			
				| MgO | 
				0.38 | 
			
			
				| Total | 
				100.20 | 
			
		
	
	 
 
	- Optical Properties
	
		- Optical Class: Isotropic
 
		- n = [2.23] (by the rule of Gladstone and Dale)
 
	
	 
 
	- Estimated Properties
	
		
			
				| Electron density | 
				Bulk density (electron density) = 2.53 g/cm3 
				note: Specific gravity of Walfordite = 2.94 g/cm3 | 
			
			
				| Photoelectric | 
				PEWalfordite = 259.14 barns/electron 
				U = PEWalfordite x ρElectron density = 656.88 barns/cm3 | 
			
			
				| Fermion index | 
				Fermion index = 0.05 
				Boson index = 0.95 | 
			
			
				Radioactivity
				
  | 
				Walfordite is not radioactive
				
  | 
			
		
	
	 
How to Identify Walfordite
Walfordite is an orange colored mineral, having translucent appearance, adamantine luster, and orange-yellow streak. Its fractures are brittle, usually exhibited by most of the non-metallic minerals and glasses. The crystals of walfordite are microscopic in nature.
Global Distribution
Walfordite is largely distributed in the Wendy open pit, El Indio-Tambo district, east of La Serena, Coquimbo, Chile.
Occurrence of Walfordite and Useful Mineral Association
Walfordite occurs very rarely in the brecciated oxidized zone of a tellurium-bearing hydrothermal gold deposit.
It is closely associated with pyrite, jarosite, emmonsite, gold, rodalquilarite, and alunite.
References