Geological Mapping in the Campbell Range, Southeastern Yukon was produced by the Government of Yukon. It details five lithological units and structural features of the Finlayson Lake fault zone, based on mapping at a 1:50,000 scale. The dataset was last updated on April 17, 2026.
Use Cases
- Analyze fault kinematics based on descriptions of thrust and strike-slip faults.
- Correlate lithological units with regional terranes like the Slide Mountain terrane.
- Study rock type distributions based on identified units of schist, metachert, greenstone, and serpentinite.
- Model structural relationships based on inferred bounding faults and thrust contacts.
Strengths
- Mapping conducted at a detailed 1:50,000 scale.
- Five distinct lithological units are identified and described.
- Structural analysis includes specific fault orientations (e.g., northwest-striking, east-striking).
Limitations
- Column-level documentation is absent; field semantics must be inferred after download.
- Row count is unknown, which may limit suitability assessment.
- Freshness should be verified as the last update date is in the future (2026).
Provenance
- Source
- Government of Yukon
- Collection Method
- Geological field mapping at 1:50,000 scale.
- Freshness
- Last updated 2026-04-17 15:40:37.105767
- Geography
- Campbell Range, Southeastern Yukon (Parts of 105 G/8, G/9 and 105 H/5, H/12)