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Kid Island Clay deposit, Kootenai Co., Idaho, USAi
Regional Level Types
Kid Island Clay depositDeposit
Kootenai Co.County
IdahoState
USACountry

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Latitude & Longitude (WGS84):
47° 38' 42'' North , 116° 48' 18'' West
Latitude & Longitude (decimal):
Locality type:
Nearest Settlements:
PlacePopulationDistance
Coeur d'Alene49,122 (2017)4.1km
Fernan Lake Village173 (2017)5.5km
Huetter102 (2017)7.3km
Dalton Gardens2,386 (2017)9.8km
Hayden Lake599 (2017)13.1km


COMMODITY FILES, USGS, SPOKANE, WA
Commodities (Major) - Clay
Development Status: Occurrence


Commodities (Major) - Aluminum
Development Status: Prospect

Regions containing this locality

North America PlateTectonic Plate
Rocky Mountains, North AmericaMountain Range

Select Mineral List Type

Standard Detailed Strunz Dana Chemical Elements

Commodity List

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


Mineral List

 No mineral species recorded.

Detailed Mineral List:


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List of minerals arranged by Strunz 10th Edition classification

Unclassified Minerals, Rocks, etc.
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List of minerals arranged by Dana 8th Edition classification

Unclassified Minerals, Mixtures, etc.
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List of minerals for each chemical element

Regional Geology

This geological map and associated information on rock units at or nearby to the coordinates given for this locality is based on relatively small scale geological maps provided by various national Geological Surveys. This does not necessarily represent the complete geology at this locality but it gives a background for the region in which it is found.

Click on geological units on the map for more information. Click here to view full-screen map on Macrostrat.org

Precambrian
541 - 4000 Ma



ID: 2086581
Priest River metamorphic complex, quartzofeldspathic gneiss and schist

Age: Precambrian (541 - 4000 Ma)

Lithology: Major:: {quartz-feldspar-mica gneiss}; Minor:: {sillimanitic schist, quartzite}

Reference: Zientek, M.L., P.D. Derkey, R.J. Miller, J.D. Causet et al. Spatial Databases for the Geology of the Northern Rocky Mountains - Idaho, Montana, and Washington. U.S. Geological Survey Open-File Report 2005-1235 Version 1.0. [25]

Mesoproterozoic
1000 - 1600 Ma



ID: 3186914
Mesoproterozoic sedimentary and volcanic rocks

Age: Mesoproterozoic (1000 - 1600 Ma)

Stratigraphic Name: Purcell Group

Comments: Omineca Belt

Lithology: Mafic-intermediate volcanic rocks; limestone,shale,argillite,quartzite,dolomite,siltstone; turbidite

Reference: Chorlton, L.B. Generalized geology of the world: bedrock domains and major faults in GIS format: a small-scale world geology map with an extended geological attribute database. doi: 10.4095/223767. Geological Survey of Canada, Open File 5529. [154]

Orosirian
1800 - 2050 Ma



ID: 2780007
Orthogneiss

Age: Orosirian (1800 - 2050 Ma)

Description: Biotite tonalite gneiss and hornblende-biotite tonalite gneiss (~1870 Ma) north of North Fork of Clearwater River, and south of Coeur d'Alene. (Mesoproterozoic to Archean Basement Rocks).

Comments: Original map source: Lewis, Reed S., Link, Paul K., Stanford, Loudon R., and Long, Sean P., Geologic Map of Idaho, 2012, Idaho Geological Survey, Geologic Map 9 (M-9); Scale 1:750,000.

Lithology: Major:{orthogneiss}

Reference: Horton, J.D., C.A. San Juan, and D.B. Stoeser. The State Geologic Map Compilation (SGMC) geodatabase of the conterminous United States. doi: 10.3133/ds1052. U.S. Geological Survey Data Series 1052. [133]

Data and map coding provided by Macrostrat.org, used under Creative Commons Attribution 4.0 License

USGS MRDS Record:10011565
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.
 
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