A thesis from the Government of Yukon details the late Cenozoic glacial history of the McQuesten map area. The work characterizes glaciations from the pre-Reid (>200 ka) to McConnell (<29.6 ka BP) and reconstructs interglacial climates. The thesis links the distribution of surficial deposits to the occurrence of placer gold deposits.
Use Cases
- Modeling paleoclimate reconstructions based on descriptions of interglacial periods.
- Mapping placer gold deposit potential based on the distribution of surficial deposits.
- Studying glacial sequence stratigraphy based on the chronology of Reid and McConnell glaciations.
- Analyzing soil development over time based on comparisons of Holocene and paleosol characteristics.
Strengths
- Provides specific chronological markers for glaciations (Reid >200 ka, McConnell <29.6 ka BP).
- Identifies a specific geographic study area (McQuesten map area, Yukon).
- Links geological processes (glaciations, fluvial order) to a resource outcome (placer gold distribution).
Limitations
- Row count is unknown, which may limit suitability assessment.
- Column-level documentation is absent; field semantics must be inferred after download.
- Data format is a thesis (PDF/HTML), which may require manual extraction for structured analysis.
Provenance
- Source
- Government of Yukon
- Time Range
- Late Cenozoic, with specific references to Pleistocene (>200 ka) and Holocene periods.
- Freshness
- Last updated 2026-04-17 16:00:38.506899; freshness should be verified.
- Geography
- McQuesten map area, Yukon Territory, Canada.