Vote for your favorite mineral in #MinCup26! - Quartz vs. Asagiite
It's a classic vs a newbie as the most common named mineral in the crust Quartz is up against an exceedingly-rare sea foam-green mineral discovered just a few years ago Asagiite.
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Little Pine Garnet Mine, Marshall, Madison County, North Carolina, USAi
Regional Level Types
Little Pine Garnet MineMine
Marshall- not defined -
Madison CountyCounty
North CarolinaState
USACountry

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Latitude & Longitude (WGS84):
35° 45' 45'' North , 82° 43' 27'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Marshall876 (2017)5.3km
Weaverville3,936 (2017)16.5km
Mars Hill2,256 (2017)17.3km
Hot Springs562 (2017)17.4km
Woodfin6,349 (2017)19.3km
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
ClubLocationDistance
Mountain Area Gem and Mineral Association (MAGMA)Asheville, North Carolina24km
Southern Appalachian Mineral SocietyAsheville, North Carolina24km
Mindat Locality ID:
5516
Long-form identifier:
mindat:1:2:5516:4
GUID (UUID V4):
0


The Little Pine Garnet Mine was mined for abrasives in 1904 and 1905.

An adit extends into the hillside for approximately 150 feet (ca. 46 m).

Red almandine garnets up to 6 inches (ca. 15 cm) in diameter occur in a green chlorite schist (phyllite and chlorite schist with almandine porphyroblasts).

Willard & El-Shazly (2020) abstract:

"The Little Pine Garnet Mine (LPGM), located between the Mars Hill and Grenville basement terranes in the Western Blue Ridge province of the Appalachian Mountain Belt has outcrops of anthophyllitechloritebiotite ± garnet ± staurolite schists (group I), garnetbiotiteanthophyllite gneisses (group II), and talc - chloritegarnet ± anthophyllite ± gedrite schists (group III), interbedded with quartzofeldspathic mica gneisses. These mineral assemblages are characteristic of protoliths enriched in Mg, but with significant amounts of Al, making them rather unusual. Geochemical analysis of these rocks reveals that groups I & III were mostly E-MORBs affected by hydrothermal alteration, whereas group II rocks were likely shales. None of the rocks analyzed have any subduction zone signatures characteristic of boninites or High Mg andesites. Isocon diagrams show that the LPGM schists and gneisses were depleted in Si, Ca, Na, Sr, Ba, Ni, V, and Sc, but enriched in Mg, Fe, La, and Ce relative to E-MORBs. Petrographic group I, containing fine-grained garnet showed slight losses in Y and Yb, whereas petrographic group III with very coarse-grained garnet showed significant gains of these elements. These results suggest that the E-MORBs were affected by hydrothermal alteration on the seafloor, which in turn suggests the existence of a small ocean basin between the Mars Hill terrane and Laurentia."

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


2 valid minerals.

Detailed Mineral List:

Almandine
Formula: Fe2+3Al2(SiO4)3
Colour: red
Description: found in green chlorite schist, crystals up to 6 inches in size
'Chlorite Group'
Habit: none, found in schist form
Colour: green
Description: host rock for garnets
Quartz
Formula: SiO2
Habit: none, masive
Colour: clear to white
Description: found in veins with garnets

List of minerals arranged by Strunz 10th Edition classification

Group 4 - Oxides and Hydroxides
Quartz4.DA.05SiO2
Group 9 - Silicates
Almandine9.AD.25Fe2+3Al2(SiO4)3
Unclassified
'Chlorite Group'-

List of minerals for each chemical element

OOxygen
O AlmandineFe32+Al2(SiO4)3
O QuartzSiO2
AlAluminium
Al AlmandineFe32+Al2(SiO4)3
SiSilicon
Si AlmandineFe32+Al2(SiO4)3
Si QuartzSiO2
FeIron
Fe AlmandineFe32+Al2(SiO4)3

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.

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