Unnamed prospects East of North Peak, North Peak (North Sisters Peak), Tres Hermanas Mining District, Tres Hermanas Mountains, Luna County, New Mexico, USAi
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Latitude & Longitude (WGS84):
31° 55' 30'' North , 107° 42' 45'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Columbus | 1,625 (2017) | 12.8km |
| Puerto Palomas | 5,659 (2015) | 18.0km |
| Sunshine | 420 (2011) | 24.0km |
| La Hacienda | 725 (2017) | 31.2km |
| Pulpotio Bareas | 120 (2017) | 33.0km |
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 |
|---|---|---|
| Deming Gem & Mineral Society | Deming, New Mexico | 38km |
Pb occurrences/prospects located about 0.8 km (0.5 mile) NE of North Peak (coordinates of record).
NOTE: The geographic coordinates presented are taken from the topo map at a point about halfway between the group of shafts and other prospects described in the reference, as reflected on the topo map.
A few prospects are located in an arroyo leading East from North Sister Peak. This peak is defined as the northwesternmost of the group of three peaks for which the Tres Hermanas Mountains are named. The prospects are located near the center of the S1/2 sec. 25, T. 27 S., R. 9 W. The area can be reached by a dirt road branching off to the west from State Highway 11 approximately 51/2 miles north of Columbus. The dirt road leads west to the base of South Sister Peak, and thence northward to the prospects; the total distance from the highway is approximately 4 miles.
The prospects are located in a narrow belt of east-dipping Permian(?) limestones bounded on the southwest by the Tres Hermanas quartz monzonite stock and on the northeast by intrusive andesite porphyry. The limestones were strongly metamorphosed by both of these intrusions of igneous rock.
The first prospect reached in going up the arroyo to the area is on the north side. Here a short adit was driven in a northerly direction along a faulted contact between andesite porphyry on the west and Permian (?) limestones on the East. Little important mineralization was developed by this excavation; the fault zone contains only moderate amounts of iron and manganese oxides, without detectable amounts of any ore minerals.
Immediately South, on the other side of the arroyo, steeply east-dipping limestones are exposed. One bed within this sequence has been highly silicated by the formation of garnet, epidote, and probably other silicate minerals. This bed contains scattered grains of magnetite and a few cubes of galena.
The several other prospects are located to the west about a quarter of a mile farther up the arroyo. Three closely spaced shafts, one timbered, but all considered unsafe to enter, are located where two smaller arroyos join to form the main channel. Outcrops are poor, but the shafts appear to be located along a northeast-striking contact between intrusive andesite porphyry to the north and east-dipping limestones to the south. The limestones are strongly marbleized and silicated. The shaft dumps contain only a few ore samples; these were highly oxidized specimens containing some cerussite.
Two other prospects are located nearby, one about 500 feet South and another about the same distance southeast from the shafts. The latter consists of several pits made along an east-striking contact between Permian (?) limestone on the north and intrusive andesite on the south. Considerable magnetite has replaced the limestone near this contact. The other prospect is within the andesite and does not offer visible signs of ore mineralization.
The prospects are located in a narrow belt of east-dipping Permian(?) limestones bounded on the southwest by the Tres Hermanas quartz monzonite stock and on the northeast by intrusive andesite porphyry. The limestones were strongly metamorphosed by both of these intrusions of igneous rock.
The first prospect reached in going up the arroyo to the area is on the north side. Here a short adit was driven in a northerly direction along a faulted contact between andesite porphyry on the west and Permian (?) limestones on the East. Little important mineralization was developed by this excavation; the fault zone contains only moderate amounts of iron and manganese oxides, without detectable amounts of any ore minerals.
Immediately South, on the other side of the arroyo, steeply east-dipping limestones are exposed. One bed within this sequence has been highly silicated by the formation of garnet, epidote, and probably other silicate minerals. This bed contains scattered grains of magnetite and a few cubes of galena.
The several other prospects are located to the west about a quarter of a mile farther up the arroyo. Three closely spaced shafts, one timbered, but all considered unsafe to enter, are located where two smaller arroyos join to form the main channel. Outcrops are poor, but the shafts appear to be located along a northeast-striking contact between intrusive andesite porphyry to the north and east-dipping limestones to the south. The limestones are strongly marbleized and silicated. The shaft dumps contain only a few ore samples; these were highly oxidized specimens containing some cerussite.
Two other prospects are located nearby, one about 500 feet South and another about the same distance southeast from the shafts. The latter consists of several pits made along an east-striking contact between Permian (?) limestone on the north and intrusive andesite on the south. Considerable magnetite has replaced the limestone near this contact. The other prospect is within the andesite and does not offer visible signs of ore mineralization.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsMineral List
4 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 DiagramDetailed Mineral List:
| ⓘ Cerussite Formula: PbCO3 |
| ⓘ Epidote Formula: (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| ⓘ Galena Formula: PbS |
| ⓘ 'Garnet Group' Formula: X3Z2(SiO4)3 |
| ⓘ Magnetite Formula: Fe2+Fe3+2O4 |
| ⓘ 'Manganese Oxides' |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 2 - Sulphides and Sulfosalts | |||
|---|---|---|---|
| ⓘ | Galena | 2.CD.10 | PbS |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Magnetite | 4.BB.05 | Fe2+Fe3+2O4 |
| Group 5 - Nitrates and Carbonates | |||
| ⓘ | Cerussite | 5.AB.15 | PbCO3 |
| Group 9 - Silicates | |||
| ⓘ | Epidote | 9.BG.05a | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Unclassified | |||
| ⓘ | 'Garnet Group' | - | X3Z2(SiO4)3 |
| ⓘ | 'Manganese Oxides' | - | |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| C | Carbon | |
| C | ⓘ Cerussite | PbCO3 |
| O | Oxygen | |
| O | ⓘ Cerussite | PbCO3 |
| O | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| O | ⓘ Magnetite | Fe2+Fe23+O4 |
| O | ⓘ Garnet Group | X3Z2(SiO4)3 |
| Al | Aluminium | |
| Al | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Si | Silicon | |
| Si | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Si | ⓘ Garnet Group | X3Z2(SiO4)3 |
| S | Sulfur | |
| S | ⓘ Galena | PbS |
| Ca | Calcium | |
| Ca | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Fe | Iron | |
| Fe | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Fe | ⓘ Magnetite | Fe2+Fe23+O4 |
| Pb | Lead | |
| Pb | ⓘ Cerussite | PbCO3 |
| Pb | ⓘ Galena | PbS |
Other Regions, Features and Areas containing this locality
North AmericaContinent
North America PlateTectonic Plate
- Basin and Range BasinsBasin
- Mazatzal DomainDomain
- Sierra Madre OrientalWide Rift
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