Government of Yukon data describes evidence for a late-McConnell readvance of the Cassiar Lobe in Seagull Creek, Pelly Mountains. The dataset likely contains geomorphic landforms and sediment stratigraphy identified in the Seagull Creek valley. It was last updated on 2026-04-17.
Use Cases
- Model paleo-ice-flow reversals based on geomorphic landforms.
- Assess glacial transport and deposition processes based on sediment stratigraphy.
- Support mineral exploration programs based on implications for glacially transported materials.
Strengths
- Focuses on a specific glacial event (late-McConnell readvance) in a defined location (Seagull Creek valley).
- Provides an interpretation with implications for mineral exploration programs.
Limitations
- Column-level documentation is absent; field semantics must be inferred after download.
- Row count is unknown, which may limit suitability assessment.
Provenance
- Source
- Government of Yukon | Gouvernement du Yukon
- Freshness
- Last updated 2026-04-17 15:52:27.608105; freshness should be verified.
- Geography
- Seagull Creek valley, Pelly Mountains, central Yukon