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Surficial Geology of Seagull Creek (parts of NTS 105F/10 and 7), Yukon (1:50,000 scale)

Physiography: The Seagull Creek map area includes the upper two-thirds of the Seagull Creek drainage area. The creek rises at a high divide (1372 m) in the Pelly Mountains and flows southsoutheast for approximately 30 km in a broad, U-shaped valley before joining the McConnell River (1067 m). The drainage area contains summits of up to 2162 metres elevation with numerous cirques on north and east-facing aspects. The evidence of glaciation in this landscape is ubiquitous. Most high peaks have been eroded into knife-edge aretes or horn peaks and cirque basins are currently occupied by active or extinct rock glaciers, tarn lakes, or glacial debris. Valley sides have been over-steepened by glacial erosion and are susceptible to mass movements.

Data and resources

FieldValue
Publisher
Modified
2021-07-06
Release Date
2019-05-10
Frequency
Irregularly
Homepage URL
Temporal Coverage
Wednesday, December 31, 1969 - 16:00
Licence
Public Access Level
Public
Department
Energy, Mines and Resources
Publication type
Organizational responsibilities and functions
Additional Info: 
FieldValue

Document Type

Open File (Geological - Surficial)

NTS

105F07, 105F10

Year Published

2005

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