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Roderick Dhu Prospect, Jewel Lake Area, Greenwood Mining Division, British Columbia, Canadai
| Regional Level Types | |
|---|---|
| Roderick Dhu Prospect | Prospect |
| Jewel Lake Area | Exploration Area |
| Greenwood Mining Division | Division |
| British Columbia | Province |
| Canada | Country |
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Latitude & Longitude (WGS84):
49° 11' 10'' North , 118° 37' 17'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Sion | 658 (2019) | 21.0km |
| Grand Forks | 4,208 (2008) | 21.7km |
| Curlew | 118 (2011) | 33.5km |
| Orient | 115 (2011) | 46.9km |
Other/historical names associated with this locality:
“Rhoderick Dhu” (Thomson, 1937) ; “Rhoderic Dhu” (Thompson, 1949)
About 11 kilometres north-northeast of Greenwood, British Columbia, north of the north-east end of Jewel (Long) Lake; Greenwood Mining Division.
The correct spelling of the name of this prospect is “Roderick Dhu”, but it has been called “Rhoderick Dhu” (Thomson, 1937) and “Rhoderic Dhu” (Thompson, 1949). Note that Jewel Lake was originally known as Long Lake, and the occurrence is in what was known in the early years as the “Long Lake Camp”. And for any literary/history buffs, there is an adjacent claim called “Lady of the Lake”!
The following quote is from B.C. Government site “Minfile”- Minfile No. 082ESE125:
“On the Roderick Dhu claim (L.598) a quartz fissure-vein is hosted in north-northeast striking and east dipping metasedimentary rocks of Group. These rocks are schistose quartz wackes or lithic wackes and are intruded by a Lower Tertiary pulaskite dyke. The quartz vein appears to be in a prominent fracture zone that roughly parallels the bedding foliation planes of the host metasedimentary rocks. At the southern extremity of the vein, widths range from 5 to 30 centimetres and is mineralized with galena, pyrite and telluride. Limonite occurs in fractures within the quartz. A shaft was sunk to 23 metres depth and stoping carried out 30 metres south. The quartz vein has been traced 152 metres northeast where a second shaft was sunk 7.6 metres in the vein, but mineralization is sparse. To the north of this point, the vein has been displaced by a 61 metre wide pulaskite dyke.”
Comments by Giles Peatfield regarding minerals reported:
Altaite: This mineral was reported by Thomson (1937, and subsequently by (Thompson, 1949). There are no details of where Thomson received his information, and the identification should be regarded as tentative.
Tetradymite: This mineral was reported by Thomson (1937, and subsequently by (Thompson, 1949). There are no details of where Thomson received his information, and the identification should be regarded as tentative.
One last comment. For many of the occurrences in this area, most workers simply report “telluride”, “rich tellurides”, etc. Specific mineral species data are few and far between.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsDetailed Mineral List:
| ⓘ Altaite Formula: PbTe References: |
| ⓘ Galena Formula: PbS References: |
| ⓘ Pyrite Formula: FeS2 References: |
| ⓘ Quartz Formula: SiO2 References: |
| ⓘ Tetradymite Formula: Bi2Te2S References: |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 2 - Sulphides and Sulfosalts | |||
|---|---|---|---|
| ⓘ | Altaite | 2.CD.10 | PbTe |
| ⓘ | Galena | 2.CD.10 | PbS |
| ⓘ | Tetradymite | 2.DC.05 | Bi2Te2S |
| ⓘ | Pyrite | 2.EB.05a | FeS2 |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Quartz | 4.DA.05 | SiO2 |
List of minerals for each chemical element
| O | Oxygen | |
|---|---|---|
| O | ⓘ Quartz | SiO2 |
| Si | Silicon | |
| Si | ⓘ Quartz | SiO2 |
| S | Sulfur | |
| S | ⓘ Galena | PbS |
| S | ⓘ Pyrite | FeS2 |
| S | ⓘ Tetradymite | Bi2Te2S |
| Fe | Iron | |
| Fe | ⓘ Pyrite | FeS2 |
| Te | Tellurium | |
| Te | ⓘ Altaite | PbTe |
| Te | ⓘ Tetradymite | Bi2Te2S |
| Pb | Lead | |
| Pb | ⓘ Altaite | PbTe |
| Pb | ⓘ Galena | PbS |
| Bi | Bismuth | |
| Bi | ⓘ Tetradymite | Bi2Te2S |
Other Databases
| Link to British Columbia Minfile: | 082ESE125 |
|---|
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