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Unnamed Cinder pit [40], Ash Fork, Coconino Co., Arizona, USAi
Regional Level Types
Unnamed Cinder pit [40]Pit
Ash ForkTown
Coconino Co.County
ArizonaState
USACountry

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Latitude & Longitude (WGS84):
35° 17' 8'' North , 112° 28' 28'' West
Latitude & Longitude (decimal):
Locality type:
Nearest Settlements:
PlacePopulationDistance
Ash Fork396 (2011)6.8km
Williams3,122 (2017)26.1km
Seligman445 (2011)36.8km
Paulden5,231 (2011)44.5km


A cinders/pumice occurrence located in the NW¼SW¼ sec. 14, T22N, R2W, G&SRM, 7.3 km (4.5 miles) N of Ash Fork, in the Hearst Mountain quadrangle, on private land. The USGS MRDS database stated accuracy for this locality is 100 meters.

Mineralization is a volcanic cinders/pumice deposit. Local rocks include Early Pleistocene to latest Pliocene surficial deposits.

Workings include surface openings comprised of a pit based on the title of the MRDS file.

Regions containing this locality

North America PlateTectonic Plate
Colorado Plateau, USAPlateau

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Standard Detailed Strunz Dana Chemical Elements

Commodity List

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


No minerals currently recorded for this locality.

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

Middle Pleistocene - Piacenzian
0.126 - 3.6 Ma



ID: 2779617
Early Pleistocene to latest Pliocene surficial deposits

Age: Cenozoic (0.126 - 3.6 Ma)

Description: Coarse relict alluvial fan deposits that form rounded ridges or flat, isolated surfaces that are moderately to deeply incised by streams. These deposits are generally topographically high and have undergone substantial erosion. Deposits are moderately to strongly consolidated, and commonly contain coarser grained sediment than younger deposits in the same area. (0.75-3 Ma)

Comments: Original map source: Arizona Geological Survey, DI-8 Geologic Map of Arizona, Digital Spatial data for the Geologic Map of Arizona, v. 3.0, edited by S.M. Richard and S.M. Kneale, 2002, 10 p., 2 DOS HD disks. Arc/INFO export file (.e00) format, scale 1:1,000,000.

Lithology: Major:{gravel,sand}

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]

Pliocene
2.588 - 5.333 Ma



ID: 3191095
Cenozoic volcanic rocks

Age: Pliocene (2.588 - 5.333 Ma)

Lithology: Volcanic rocks

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]

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

References

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Year (asc) Year (desc) Author (A-Z) Author (Z-A)
U.S. Bureau of Mines (1995), Minerals Availability System/Mineral Industry Location System (MAS/MILS), U.S. Bureau of Mines, file ID #0040050106.
USGS (2005), Mineral Resources Data System (MRDS): U.S. Geological Survey, Reston, Virginia, deposit ID #10112807.

USGS MRDS Record:10112807
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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