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This file contains the following photographs in both print photograph and negative format:

Thorsen Bay
Print roll 11, #01-2A
Corresponding slides: slide roll 6, #12-10

Y04-19 (27.5 km on Cultus Bay Rd., near Thorsen Bay)
Date: July 22, 2004
Location Coordinates: 61º 12’ 3.0” N, 138º 28’ 58.3’ W, 819 m asl (± 18.9 m)
Site Description: Roadcut at base of 30º, E-facing slope. Colluviated loess overlies sandy glaciofluvial at 120 cm. Prominent paleosol with “cumulic” B horizon at 80-120 cm, with strong effervescence throughout exposure.
Print roll 11, #3A-5A (profile), #6A-10A (landscape)
Corresponding slides: slide roll 6, #9-7 (profile), #6-1 (landscape)

Sample Depths & Descriptions: Y04-19-01 – charcoal at 95 cm
Roadcut opposite ~ 30 m to NE on grassy S aspect (10° slope) with 15-20 cm of calcareous loess and sand over 2 cm White River ash; strongly effervescent throughout.
Print roll 11, #11A-12A (profile)
Corresponding slides: slide roll 7, #36-35 (profile)

Thorsen Bay landscape
Print roll 11, #13A-16A
Corresponding slides: Slide roll 7, #34-32

Y04-20B
Date: July 22, 2004
Location Coordinates: 61º 10’ 16.5” N, 138º 26’ 18.7’ W, 797.5 m asl (± 5.9 m)
Site Description: wind-eroded Slims soil on glaciolacustrine with contorted bedding (exposed on blown-out roadcut); calcareous to surface; White R ash pockets at 10-20 cm; S aspect, 5° slope.
Print roll 11, #17A-21A
Corresponding slides: Slide roll 7, #31-26

Y04-22
Date: July 22, 2004
Location Coordinates: 61º 9’ 39.24” N, 138º 25’ 7.8’ W, 790.6 m asl (± 6.4 m)
Site Description: toe of 30° slope, W aspect (grassy slope with poplar at toe); 1.0-1.2 of colluviated loess over gravelly glaciofluvial with buried soil at 70-80 cm
Print roll 11, #22A-24A
Corresponding slides: Slide roll 7, #25-24

During the 1980s, Agriculture Canada pedologists Scott Smith (retired from Summerland Research Station, formerly based in Whitehorse) and Charles Tarnocai (retired from Central Experimental Farm, Ottawa) had a large field program which addressed the trends in soil development in the central Yukon. Across this region, particularly between Whitehorse and Dawson City, the land surfaces and surficial deposits vary greatly in age due to the differing extents of glaciations over the past ~2 million years.

Tarnocai and Smith shared the unpublished data and soil samples from this work with Dr. Paul Sanborn, and this resulted in a student project published as:
Daviel, E., P. Sanborn, C. Tarnocai, and C.A.A. Smith. 2011. Clay mineralogy and chemical properties of argillic horizons in central Yukon paleosols. Canadian Journal of Soil Science 91: 83-93. https://doi.org/10.4141/cjss10067

This file consists of photocopies of lab data sheets for Tarnocai & Smith Yukon soil samples from the Land Resource Research Institute, Agriculture Canada.

These lab data sheets were transcribed into an Excel spreadsheet (see item 2023.2.2.6.3).