The data below represent everything available in the MBMG Abandoned and Inactive Mines (AIM) database.
AIM Id | Name | Alternate Name | District | County |
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FH004363 | UNAWAH CREEK PROSPECTS | FLATHEAD |
MRDS | AMLI | MILS | Latitude | Longitude | Datum |
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300290074 | 48.186 | -113.6867 |
Township | Range | Section | QSection | UTM Northing | UTM Easting | UTM Zone | UTM Datum |
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28N | 17W | 13 | CDBC | 5340243 | 300307 | 12 |
Average Elevation | Elev Units | Land Owner | 250K Quad | 100K Quad | 24K Quad |
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F | CUT BANK | HUNGRY HORSE | FELIX PEAK |
Property Type | Update Date | Who Updated |
---|---|---|
LODE | 12/28/2000 | KBM |
Commodities Identified |
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COPPER |
Information |
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Agency: NF Region District: R1 Ranger District: HUNGRY HORSE Forest Service Tract: Watershed Code: 17010209 Forest or Resource Area: FLATHEAD Owner: N Impact: Report: Unawah Creek Prospects FH004363 The Unawah Creek prospects are located in section 13, T28N, R17W (Felix Lake quadrangle). The site was visited in October 2000. Workings consisted of a partially caved adit with a small 1' x 1' opening and two trenches. The adit trended N 36 W and extended into the hillside approximately 30 feet. The floor of the adit was flooded but there was no evidence of discharge. The small dump was partially vegetated. Johns (1942) and Marks (1978) described the deposit as a 2"-5" quartz vein containing scattered blebs and vugs of malachite, chalcocite, and iron oxides. A selected dump sample assayed at 1.33 percent copper and 0.35 ounce silver a ton. Host rock is reddish-purple argillite of the Grinnell Formation (Precambrian Ravalli Group). Unawah Creek Prospects FH004363 The Unawah Creek prospects are located in section 13, T28N, R17W (Felix Lake quadrangle). The site was visited in October 2000. Workings consisted of a partially caved adit with a small 1' x 1' opening and two trenches. The adit trended N 36 W and extended into the hillside approximately 30 feet. The floor of the adit was flooded but there was no evidence of discharge. The small dump was partially vegetated. Johns (1942) and Marks (1978) described the deposit as a 2"-5" quartz vein containing scattered blebs and vugs of malachite, chalcocite, and iron oxides. A selected dump sample assayed at 1.33 percent copper and 0.35 ounce silver a ton. Host rock is reddish-purple argillite of the Grinnell Formation (Precambrian Ravalli Group). |
Information |
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Mill Tailings: N Adit Discharge: N Metal Leaching: N Water Erosion: N Residence: N Hazardous Materials: N Open Adit: Y Visit: Y Comments: PARTIALLY COLLAPSED ADIT WITH 1' X 1' OPENING, STANDING WATER IN ADIT WIT NO EVIDENCE OF DISCHARGE. |
End of report. Retrieved 5/4/2024 3:04:16 AM.
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