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Sable Resources Ltd.
Summary
| Project: | Baker | |
|---|---|---|
| Deposit: | Baker | |
| Location: | Canada | |
| Commodities: | Gold-Silver | |
| Date: | 8/25/2017 | |
| Report Code: | NI43-101 | |
| Report Type: | Exploration/Drilling Update | |
| Project Stage: | Pursuing Resources Definition | |
| Report details: | 25-8-2017: Sable Resources Ltd. announces an Exploration/Drilling Update report for its Baker deposit at the Baker project. Summary of exploration work on the Baker Gold Project. The Baker Gold Project (the “Baker Project” or “Property”) is located in the | |
| Resources: | (historic estimate only) | |
| CP/QP: | [Overall Report]: Adrian Smith (Divitiae Resources Ltd.) | |
| ABSTRACT: | The Baker Gold Project (the “Baker Project” or “Property”) is located in the Toodoggone region of the Omineca Mining Division, 430 km northwest of Prince George, British Columbia. The Property is situated 35 km northwest of the former Kemess South open pit gold-copper mine. The Baker Project consists of 54 mineral claims, and 2 mining leases, all 100%-owned by Multinational Mining Inc., a 100% owned subsidiary of Sable Resources Ltd. The claims cover 6,601 hectares of land that encompass the Baker Gold Project which includes the past-producing Dupont-Baker ‘A’ and Multinational ‘B’ underground gold-silver mine, and the past-producing Shasta open pit/underground gold-silver mine, as well as multiple gold, silver, and copper showings. Access to the project is provided by a series of branching gravel roads, including the Finlay Forest Service Road that begins south of the town of Mackenzie, then connects to the Omineca Resource Access Road (ORAR). The ORAR continues beyond the end of the Kemess South mine access road, past the Sturdee River gravel airstrip located 10 km south, to the Project. Road access is currently seasonal and the driving time to the property from Prince George is 9 hours. The Property lies within the Toodoggone region within a portion of the Stikine Terrane. The Stikine Terrane is comprised of Paleozoic to Mesozoic island arc assemblages and overlying Mesozoic sedimentary sequences within the lntermontane Belt. The oldest rocks exposed in the Toodoggone region consist of crystalline limestone of the Devonian Asitka Group. They are unconformably overlain by mafic volcanic rocks of the Upper Triassic Takla Group. Takla Group volcanic rocks are in turn overlain by bimodal volcanic and sedimentary strata of the Lower Jurassic Toodoggone Formation of the Hazelton Group. | |
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