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Millet Brook U-Ag deposit, Windsor, Hants Co., Nova Scotia, Canadai
Regional Level Types
Millet Brook U-Ag depositDeposit
Windsor- not defined -
Hants Co.County
Nova ScotiaProvince
CanadaCountry

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Latitude & Longitude (WGS84):
44° 51' 25'' North , 64° 17' 20'' West
Latitude & Longitude (decimal):
44.85694,-64.28889
GeoHash:
G#: dxfr1jfq8
GRN:
N30W34
Type:
Deposit
Köppen climate type:
Dfb : Warm-summer humid continental climate
Nearest Settlements:
PlacePopulationDistance
Windsor3,864 (2010)18.7km
Hantsport1,253 (2008)25.3km
Wolfville3,523 (2008)25.9km
Kentville12,636 (2014)29.4km
Hayes Subdivision1,121 (2019)32.2km
Mindat Locality ID:
68829
Long-form identifier:
mindat:1:2:68829:0
GUID (UUID V4):
0


A U-Ag deposit in sheared granodiorites, located south of Windsor.

The GPS coordinates are the approximate (not ground truthed) location of the A9 zone. It is heavily covered in till but based on drilling, it is the most mineral rich zone. The other areas of interest are the C1 and C2 zones, located about 1.5 km ENE from the A9 zone.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


14 valid minerals.

Rock Types Recorded

Note: data is currently VERY limited. Please bear with us while we work towards adding this information!

Select Rock List Type

Alphabetical List Tree Diagram

Detailed Mineral List:

ⓘ Autunite
Formula: Ca(UO2)2(PO4)2 · 10-12H2O
ⓘ 'Biotite'
Formula: K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
ⓘ Bornite
Formula: Cu5FeS4
ⓘ Chalcocite
Formula: Cu2S
ⓘ Chalcopyrite
Formula: CuFeS2
ⓘ Covellite
Formula: CuS
ⓘ Galena
Formula: PbS
ⓘ Muscovite
Formula: KAl2(AlSi3O10)(OH)2
ⓘ Orthoclase
Formula: K(AlSi3O8)
ⓘ Proustite
Formula: Ag3AsS3
ⓘ Quartz
Formula: SiO2
ⓘ Saléeite
Formula: Mg(UO2)2(PO4)2 · 10H2O
ⓘ Sphalerite
Formula: ZnS
ⓘ Torbernite
Formula: Cu(UO2)2(PO4)2 · 12H2O
ⓘ Uraninite
Formula: UO2
ⓘ Uraninite var. Pitchblende
Formula: UO2
ⓘ 'Wolframite Group'

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
ⓘChalcocite2.BA.05Cu2S
ⓘBornite2.BA.15Cu5FeS4
ⓘCovellite2.CA.05aCuS
ⓘSphalerite2.CB.05aZnS
ⓘChalcopyrite2.CB.10aCuFeS2
ⓘGalena2.CD.10PbS
ⓘProustite2.GA.05Ag3AsS3
Group 4 - Oxides and Hydroxides
ⓘQuartz4.DA.05SiO2
ⓘ'Wolframite Group'4.DB.30 va
ⓘUraninite
var. Pitchblende		4.DL.05UO2
ⓘ4.DL.05UO2
Group 8 - Phosphates, Arsenates and Vanadates
ⓘAutunite8.EB.05Ca(UO2)2(PO4)2 · 10-12H2O
ⓘSaléeite8.EB.05Mg(UO2)2(PO4)2 · 10H2O
ⓘTorbernite8.EB.05Cu(UO2)2(PO4)2 · 12H2O
Group 9 - Silicates
ⓘMuscovite9.EC.15KAl2(AlSi3O10)(OH)2
ⓘOrthoclase9.FA.30K(AlSi3O8)
Unclassified
ⓘ'Biotite'-K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2

List of minerals for each chemical element

HHydrogen
Hⓘ AutuniteCa(UO2)2(PO4)2 · 10-12H2O
Hⓘ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Hⓘ MuscoviteKAl2(AlSi3O10)(OH)2
Hⓘ SaléeiteMg(UO2)2(PO4)2 · 10H2O
Hⓘ TorberniteCu(UO2)2(PO4)2 · 12H2O
OOxygen
Oⓘ AutuniteCa(UO2)2(PO4)2 · 10-12H2O
Oⓘ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Oⓘ MuscoviteKAl2(AlSi3O10)(OH)2
Oⓘ OrthoclaseK(AlSi3O8)
Oⓘ Uraninite var. PitchblendeUO2
Oⓘ QuartzSiO2
Oⓘ SaléeiteMg(UO2)2(PO4)2 · 10H2O
Oⓘ TorberniteCu(UO2)2(PO4)2 · 12H2O
Oⓘ UraniniteUO2
FFluorine
Fⓘ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
MgMagnesium
Mgⓘ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Mgⓘ SaléeiteMg(UO2)2(PO4)2 · 10H2O
AlAluminium
Alⓘ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Alⓘ MuscoviteKAl2(AlSi3O10)(OH)2
Alⓘ OrthoclaseK(AlSi3O8)
SiSilicon
Siⓘ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Siⓘ MuscoviteKAl2(AlSi3O10)(OH)2
Siⓘ OrthoclaseK(AlSi3O8)
Siⓘ QuartzSiO2
PPhosphorus
Pⓘ AutuniteCa(UO2)2(PO4)2 · 10-12H2O
Pⓘ SaléeiteMg(UO2)2(PO4)2 · 10H2O
Pⓘ TorberniteCu(UO2)2(PO4)2 · 12H2O
SSulfur
Sⓘ BorniteCu5FeS4
Sⓘ ChalcopyriteCuFeS2
Sⓘ ChalcociteCu2S
Sⓘ CovelliteCuS
Sⓘ GalenaPbS
Sⓘ ProustiteAg3AsS3
Sⓘ SphaleriteZnS
KPotassium
Kⓘ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Kⓘ MuscoviteKAl2(AlSi3O10)(OH)2
Kⓘ OrthoclaseK(AlSi3O8)
CaCalcium
Caⓘ AutuniteCa(UO2)2(PO4)2 · 10-12H2O
TiTitanium
Tiⓘ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
FeIron
Feⓘ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Feⓘ BorniteCu5FeS4
Feⓘ ChalcopyriteCuFeS2
CuCopper
Cuⓘ BorniteCu5FeS4
Cuⓘ ChalcopyriteCuFeS2
Cuⓘ ChalcociteCu2S
Cuⓘ CovelliteCuS
Cuⓘ TorberniteCu(UO2)2(PO4)2 · 12H2O
ZnZinc
Znⓘ SphaleriteZnS
AsArsenic
Asⓘ ProustiteAg3AsS3
AgSilver
Agⓘ ProustiteAg3AsS3
PbLead
Pbⓘ GalenaPbS
UUranium
Uⓘ AutuniteCa(UO2)2(PO4)2 · 10-12H2O
Uⓘ Uraninite var. PitchblendeUO2
Uⓘ SaléeiteMg(UO2)2(PO4)2 · 10H2O
Uⓘ TorberniteCu(UO2)2(PO4)2 · 12H2O
Uⓘ UraniniteUO2

Other Regions, Features and Areas containing this locality

Canada
North AmericaContinent
North America PlateTectonic Plate

This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders for access and that you are aware of all safety precautions necessary.

References

www.novascotia.ca (n.d.) http://www.novascotia.ca/natr/meb/data/pubs/ofr/ofr_me_2009-001.pdf
Chatterjee, A.K., Strong, D.F., Clarke, D.B., Robertson, J., Pollock, D., and Mueke, G.K. (1985) Geochemistry of the grandiorite hosting uranium mineralization at Millet Brook. Guide to the Granites and Mineral Deposits of Southwestern Nova Scotia, Nova Scotia Department of Mines and Energy, Paper 85-3: 63-114.
Carruzzo, S. (2003) Granite-hosted mineral deposits of the New Ross area, South Mountain Batholith, Nova Scotia, Canada. Ph.D. Thesis, Dalhousie University, Halifax, Nova Scotia, Canada: 571 pgs.
O'Reilly, G.A. and Mills, R.F. (2009) 2009 Fall Field Trip, Selected Mineral Deposits and Other Sites of Geological Interest in Kings and Western Hants County Area, Nova Scotia. OFR ME 2009-1.
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