Baldwin Place Farm, Asheboro, Randolph County, North Carolina, USAi
| Regional Level Types | |
|---|---|
| Baldwin Place Farm | Deposit (Active) |
| Asheboro | City |
| Randolph County | County |
| North Carolina | State |
| USA | Country |
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Latitude & Longitude (WGS84):
35° 41' 45'' North , 79° 42' 10'' West
Latitude & Longitude (decimal):
Type:
Deposit (Active) - last checked 2026
Deposit first discovered:
1998
Age:
630 to 535 Ma
Geologic Time:
Dating method:
Geology data and references
Reference for age:
North Carolina Geological Survey
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Franklinville | 1,157 (2017) | 5.4km |
| Ramseur | 1,701 (2017) | 6.2km |
| Asheboro | 26,103 (2017) | 10.1km |
| Randleman | 4,153 (2017) | 16.3km |
| Staley | 395 (2017) | 17.6km |
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
Local clubs are the best way to get access to collecting localities
| Club | Location | Distance |
|---|---|---|
| Greensboro Gem & Mineral Club | Greensboro, North Carolina | 43km |
Other/historical names associated with this locality:
Lost Cause Prospect
Site appears to contain a preserved and exposed "fossil" low-sulfidation (LS) epithermal (Hot Spring/Geothermal) "boiling chamber" (composed of many small boiling chambers or low pressure open space filled dilations where fluid boiled) hosted within a mineralized brittle fault or fault zone(s). Fault strike is NW 310 degrees dipping approximately 70 degree NE and assumed to be a sinistral fault. Primary targets appear to be at open space filled dilations at intersections of fault fractures and pre-existing NE 28 degrees trending veins or contacts. Dilated pockets (small boiling chambers) appear to be organized as fault fracture foot wall laterals. Top of overall "boiling chamber" is exposed at certain elevation which appears to be estimated 550 to 570 feet AMSL. Visible gold in samples appears to begin at approximately 550 feet AMSL (top going down), along with other common LS Epithermal gangue minerals and textures. A fault core has been identified along with some of the associated proximal and distal fault splays out to 700 feet laterally from core. Known alteration halos are very narrow, key mineral and metallic targets are bound to faulting fractures and intersection lateral open space filled dilations. The site is not developed and lode deposit remains "in place".
Site in private family ownership since 1849 with modern day research starting in 1998 after discovering a section width with anomalous gold count in pan samples. This followed by later discovery of gold, silver, adularia, sericite, calaverite alteration and precipitation within open space filled pockets. In 2012 an area of "in place" bladed quartz was uncovered in a parcel section which led to discovery and exposure of brittle fault structure(s) and underlying geologic system definition(s). Historical family lore exist of small scale gold prospecting on the property and a gold vein running SW to NE through the width of the parcel. This "gold vein" can now be interpreted as an inline series of SW to NE trending open space filled pockets or laterals stemming from SE to NW trending fault zone fractures.
Site in private family ownership since 1849 with modern day research starting in 1998 after discovering a section width with anomalous gold count in pan samples. This followed by later discovery of gold, silver, adularia, sericite, calaverite alteration and precipitation within open space filled pockets. In 2012 an area of "in place" bladed quartz was uncovered in a parcel section which led to discovery and exposure of brittle fault structure(s) and underlying geologic system definition(s). Historical family lore exist of small scale gold prospecting on the property and a gold vein running SW to NE through the width of the parcel. This "gold vein" can now be interpreted as an inline series of SW to NE trending open space filled pockets or laterals stemming from SE to NW trending fault zone fractures.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsDetailed Mineral List:
| ⓘ Acanthite Formula: Ag2S References: Randy Davis CollectionIdentified by Randy Davis: Visual Identification |
| ⓘ Calaverite Formula: AuTe2 References: |
| ⓘ Hematite Formula: Fe2O3 References: |
| ⓘ 'K Feldspar' References: |
| ⓘ 'K Feldspar var. Adularia' Formula: KAlSi3O8 References: |
| ⓘ 'Limonite' References: Randy Davis CollectionIdentified by Randy Davis: Visual Identification |
| ⓘ Muscovite Formula: KAl2(AlSi3O10)(OH)2 References: |
| ⓘ Muscovite var. Sericite Formula: KAl2(AlSi3O10)(OH)2 References: |
| ⓘ Native Gold Formula: Au Description: Identified by owner Randy Davis. References: |
| ⓘ Native Silver Formula: Ag References: |
| ⓘ Orthoclase Formula: K(AlSi3O8) References: |
| ⓘ Pyrite Formula: FeS2 References: |
| ⓘ Quartz Formula: SiO2 Colour: white Description: Site of angle-plated quartz deposit. References: |
| ⓘ Quartz var. Amethyst Formula: SiO2 References: |
| ⓘ Quartz var. Smoky Quartz Formula: SiO2 References: |
List of minerals arranged by Strunz 10th Edition classification
| Group 1 - Elements | |||
|---|---|---|---|
| ⓘ | Native Gold | 1.AA.05 | Au |
| ⓘ | Native Silver | 1.AA.05 | Ag |
| Group 2 - Sulphides and Sulfosalts | |||
| ⓘ | Acanthite | 2.BA.35 | Ag2S |
| ⓘ | Calaverite | 2.EA.10 | AuTe2 |
| ⓘ | Pyrite | 2.EB.05a | FeS2 |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Hematite | 4.CB.05 | Fe2O3 |
| ⓘ | Quartz var. Amethyst | 4.DA.05 | SiO2 |
| ⓘ | 4.DA.05 | SiO2 | |
| ⓘ | var. Smoky Quartz | 4.DA.05 | SiO2 |
| Group 9 - Silicates | |||
| ⓘ | Muscovite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
| ⓘ | var. Sericite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
| ⓘ | Orthoclase | 9.FA.30 | K(AlSi3O8) |
| Unclassified | |||
| ⓘ | 'K Feldspar var. Adularia' | - | KAlSi3O8 |
| ⓘ | 'Limonite' | - | |
| ⓘ | 'K Feldspar' | - | |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| H | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| O | Oxygen | |
| O | ⓘ K Feldspar var. Adularia | KAlSi3O8 |
| O | ⓘ Quartz var. Amethyst | SiO2 |
| O | ⓘ Hematite | Fe2O3 |
| O | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| O | ⓘ Orthoclase | K(AlSi3O8) |
| O | ⓘ Quartz | SiO2 |
| O | ⓘ Quartz var. Smoky Quartz | SiO2 |
| O | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Al | Aluminium | |
| Al | ⓘ K Feldspar var. Adularia | KAlSi3O8 |
| Al | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Al | ⓘ Orthoclase | K(AlSi3O8) |
| Al | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Si | Silicon | |
| Si | ⓘ K Feldspar var. Adularia | KAlSi3O8 |
| Si | ⓘ Quartz var. Amethyst | SiO2 |
| Si | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Si | ⓘ Orthoclase | K(AlSi3O8) |
| Si | ⓘ Quartz | SiO2 |
| Si | ⓘ Quartz var. Smoky Quartz | SiO2 |
| Si | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| S | Sulfur | |
| S | ⓘ Acanthite | Ag2S |
| S | ⓘ Pyrite | FeS2 |
| K | Potassium | |
| K | ⓘ K Feldspar var. Adularia | KAlSi3O8 |
| K | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| K | ⓘ Orthoclase | K(AlSi3O8) |
| K | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Fe | Iron | |
| Fe | ⓘ Hematite | Fe2O3 |
| Fe | ⓘ Pyrite | FeS2 |
| Ag | Silver | |
| Ag | ⓘ Acanthite | Ag2S |
| Ag | ⓘ Native Silver | Ag |
| Te | Tellurium | |
| Te | ⓘ Calaverite | AuTe2 |
| Au | Gold | |
| Au | ⓘ Calaverite | AuTe2 |
| Au | ⓘ Native Gold | Au |
Other Regions, Features and Areas containing this locality
North AmericaContinent
North America PlateTectonic Plate
- Carolina TerraneVolcanic Arc
- Carolinia DomainDomain
USA
- Carolina Slate BeltGeologic Region
- ⭔Southeastern United StatesArea
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References
Moye, Robert J. (2013) Advanced Argillic Epithermal Alteration systems (AES) in the Carolina terrane of central North Carolina: Possible structural controls and association with Neoproterozoic Uwharrie felsic magmatism. Carolina Geological Society Annual Meeting 2013, Carolina Geological Society.System fault referenced in Figure 3 of paper along with associated geologic information





Baldwin Place Farm, Asheboro, Randolph County, North Carolina, USA