Log InRegister
Quick Links : The Mindat ManualThe Rock H. Currier Digital LibraryMindat Newsletter [Free Download]
Home PageAbout MindatThe Mindat ManualHistory of MindatCopyright StatusWho We AreContact UsAdvertise on Mindat
Donate to MindatCorporate SponsorshipSponsor a PageSponsored PagesMindat AdvertisersAdvertise on Mindat
Learning CenterWhat is a mineral?The most common minerals on earthInformation for EducatorsMindat ArticlesThe ElementsThe Rock H. Currier Digital LibraryGeologic Time
Minerals by PropertiesMinerals by ChemistryAdvanced Locality SearchRandom MineralRandom LocalitySearch by minIDLocalities Near MeSearch ArticlesSearch GlossaryMore Search Options
Search For:
Mineral Name:
Locality Name:
Keyword(s):
 
The Mindat ManualAdd a New PhotoRate PhotosLocality Edit ReportCoordinate Completion ReportAdd Glossary Item
Mining CompaniesStatisticsUsersMineral MuseumsClubs & OrganizationsMineral Shows & EventsThe Mindat DirectoryDevice SettingsThe Mineral Quiz
Photo SearchPhoto GalleriesSearch by ColorNew Photos TodayNew Photos YesterdayMembers' Photo GalleriesPast Photo of the Day GalleryPhotography

Nighthawk Ridge mine, White Pine Mining District, White Pine County, Nevada, USAi
Regional Level Types
Nighthawk Ridge mineMine
White Pine Mining DistrictMining District
White Pine CountyCounty
NevadaState
USACountry

This page is currently not sponsored. Click here to sponsor this page.
PhotosMapsSearch
Latitude & Longitude (WGS84):
39° 10' 51'' North , 115° 40' 27'' West
Latitude & Longitude (decimal):
Type:
Nearest Settlements:
PlacePopulationDistance
Eureka610 (2011)44.3km
Mindat Locality ID:
62258
Long-form identifier:
mindat:1:2:62258:6
GUID (UUID V4):
a4e34d71-880a-4e83-9089-98bd24634eee
Other/historical names associated with this locality:
Easy Junior Mine


Structure: Low Amplitude, Open Folds With Axes That Strike Between N-S And N15e. Nighthawk Fault.

Alteration: Silicification, Jasperization, Argillization, Decarbonization. Silicification Is The Most Common Alteration Within The Orebody. Chainman Shale And Pilot Shale Are Argillized And Silicified Adjacent To Nighthawk Fault.

Commodity: Au:ag ratios generally > 50:1.

Deposit: 75% of ore is in chainman shale, 25% in joana limestone. ; info.src : 1 pub lit refer to record re00028 for data on the adjacent decker flats deposit.

Deposit type: Carbonate-hosted Au-Ag

Development: The original easy junior claims staked in 1979 by earth resources co. On the basis of prominent jasperoid outcrops. These claims were acquired by houston international minerals co. In 1980. Himco drilled eight holes totalling 1810 ft. In 1980, but only one hole contained anomalous gold mineralization. Himco subleased easy junior to consolidated mineral resources 1981-1983, during which eight holes totalling 2620 ft. Were drilled. Drill results were discouraging. In 1984, consolidated minerals conveyed interest in easy junior to aaminex for stock, and aaminex sub-leased the property to santa Fe pacific mining co. During 1984-1985, santa Fe completed geologic mapping, a vlf survey and 16 drill holes totaling 9295 ft. Several of these holes intersected narro W zones of gold mineralization, the best being 45 ft./0.059 opt gold. All mineralized intercepts were at the contact of the chainman shale and joana limestone. Santa Fe terminated the lease in 1985, then aaminex returned claims back to tenneco minerals co. Which had since acquired himco. All drilling up to this time had been completed in the vicinity of the outcropping jasperoids. In 1986, tenneco extended the claim block north to include what would become the nighthawk ridge deposit. A soil geochemistry grid identified two linear gold anomalies which led to the discovery of outcrop of folded and silicified chainman shale with abundant barite and minor scorodite along fractures. 36 samples from this outcrop assayed As high As 2.33 ppm gold, but averaged 0.5 ppm gold. Hg,tl, as, and sb were also anomalous. A 41 drill hole program was initiated in september, 1986. The discovery hole was the 39th hole, intersecting 320 ft./0.066 opt gold. ; econ.com: cash cost of production of $240/oz. Gold.

Rock formation(s): Chainman Shale;Joana Limestone


Ore(s): Nighthawk Fault Strikes Northeast, Dips 80 Degrees West And Serves As The Primary Conduit For Mineralizing Fluids. Ore Is Thickest Where Nighthawk Fault Is Offset By Wnw En Echelon Faulting, A Result Of Secondary Porosity In Chainman Shale At The Fault Intersections. Joana Limestone Acted As A Porous Host Since Gold Mineralization Appears Stratabound And Closely Emulates The Fold Pattern.


Structure: Nighthawk Fault Rocks in the mine area have been affected by low amplitude, open folds with axes that strike between N-S and N15E.

Alteration: Silicification is the most common alteration within the orebody. Jasperization, argillization, and decarbonization have also affected the rocks. Chainman Shale and Pilot Shale are argillized and silicified adjacent to the Nighthawk Fault.

Commodity: Commodity Info: AU:AG ratios are generally > 50:1. Ore Materials: micron-sized gold grains Gangue Materials: hematite, limonite, opal, barite, scorodite

Deposit: Sediment-hosted disseminated gold

Deposit type: Carbonate-hosted Au-Ag

Development: The original Easy Junior claims were staked in 1979 by Earth Resources Company on the basis of prominent jasperoid outcrops. These claims were acquired by Houston International Minerals Company (HIMCO) in 1980. HIMCO drilled eight holes totaling 1810 ft in 1980, but only one hole contained anomalous gold mineralization. Himco subleased Easy Junior to Consolidated Mineral Resources from 1981 to 1983, during which eight holes totaling 2620 ft. were drilled. Drill results were discouraging. In 1984, Consolidated Minerals conveyed interest in Easy Junior to AAMINEX for stock, and AAMINEX sub-leased the property to Santa Fe Pacific Mining Co. During 1984-1985, Santa Fe completed geologic mapping, a VLF survey and 16 drill holes totaling 9295 ft. Several of these holes intersected narrow zones of gold mineralization, the best being a 45 ft intercept grading 0.059 opt gold. All mineralized intercepts were at the contact of the Chainman Shale and Joana Limestone. Santa Fe terminated the lease in 1985, after which AAMINEX returned the claims back to Tenneco Minerals Co, which had since acquired HIMCO. All drilling up to this time had been completed in the vicinity of the outcropping jasperoids. In 1986, Tenneco extended the claim block north to include what would become the Nighthawk Ridge deposit. A soil geochemistry grid identified two linear gold anomalies which led to the discovery of outcrop of folded and silicified Chainman Shale with abundant barite and minor scorodite along fractures. 36 samples from this outcrop assayed as high as 2.33 ppm gold, but averaged 0.5 ppm gold, with anomalous Hg, Tl, As, and Sb. A 41 drill hole program was initiated in September, 1986. The discovery hole was the 39th hole, intersecting 320 feet grading 0.066 opt gold.

Geology: All mineralized intercepts were at the contact of the Chainman Shale and Joana Limestone.

Ore(s): The Nighthawk Fault strikes northeast, dips 80 degrees west and serves as the primary conduit for mineralizing fluids. The ore is thickest where the Nighthawk Fault is offset by WNW-trending en echelon faulting, as a result of secondary porosity tat developed in the Chainman Shale at the fault intersections. The Joana Limestone acted as a porous host since gold mineralization appears stratabound and closely emulates the fold pattern.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Commodity List

This is a list of exploitable or exploited mineral commodities recorded at this locality.


Mineral List


5 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

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
β“˜Gold1.AA.05Au
Group 4 - Oxides and Hydroxides
β“˜Hematite4.CB.05Fe2O3
β“˜Opal4.DA.10SiO2 Β· nH2O
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
β“˜Baryte7.AD.35BaSO4
Group 8 - Phosphates, Arsenates and Vanadates
β“˜Scorodite8.CD.10Fe3+AsO4 Β· 2H2O
Unclassified
β“˜'Limonite'-

List of minerals for each chemical element

HHydrogen
Hβ“˜ OpalSiO2 · nH2O
Hβ“˜ ScoroditeFe3+AsO4 · 2H2O
OOxygen
Oβ“˜ BaryteBaSO4
Oβ“˜ HematiteFe2O3
Oβ“˜ OpalSiO2 · nH2O
Oβ“˜ ScoroditeFe3+AsO4 · 2H2O
SiSilicon
Siβ“˜ OpalSiO2 · nH2O
SSulfur
Sβ“˜ BaryteBaSO4
FeIron
Feβ“˜ HematiteFe2O3
Feβ“˜ ScoroditeFe3+AsO4 · 2H2O
AsArsenic
Asβ“˜ ScoroditeFe3+AsO4 · 2H2O
BaBarium
Baβ“˜ BaryteBaSO4
AuGold
Auβ“˜ GoldAu

Other Databases

Link to USGS MRDS:10310554
Link to USGS MRDS:10047584

Other Regions, Features and Areas containing this locality


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.
 
Mineral and/or Locality  
Mindat Discussions Facebook Logo Instagram Logo Discord Logo
Mindat.org is an outreach project of the Hudson Institute of Mineralogy, a 501(c)(3) not-for-profit organization.
Copyright © mindat.org and the Hudson Institute of Mineralogy 1993-2024, except where stated. Most political location boundaries are Β© OpenStreetMap contributors. Mindat.org relies on the contributions of thousands of members and supporters. Founded in 2000 by Jolyon Ralph.
Privacy Policy - Terms & Conditions - Contact Us / DMCA issues - Report a bug/vulnerability Current server date and time: April 26, 2024 13:20:52 Page updated: March 28, 2024 23:35:22
Go to top of page