Caption describing photograph: "Leaf morphology of Betula papyrifera. Revels garden."

Caption describing photograph: "Leaf morphology of Betula glandulosa. General distribution in sphagnum bogs and muskeg through Northeast B.C. Quesnel North."

Photograph depicts several men and a dog stand on snowy ground, a canvas tent on the left. A rough hewn table on the right background.

Photograph depicts a skiff of fresh snow covering a fallen tree in the foreground. Tents and suspended tarps in the midground. A haze of wood smoke drifts into the snowy forest in the background.

Caption describing photograph: "Larix larciana (Tamarack). Wildling transplanted Autumn 1964 from Tamarack Lake 30 miles West of Prince George. Age 6 years. Height 29", 65 leader 4", 66 growth 9". All measurement taken June 23, 1966."

Photo depicts a large sled loaded with large metal tubing, a tent and a pile driver(?)

Photographic print contains the following writing on verso:
"Larch and Douglas fir seed trees under (?) seed bed preparation, 1986 Nelson BC, J Revel"

Photograph depicts a landscape perspective featuring construction of two water flumes across a narrow valley between a forested landscape.

Photograph depicts a landscape perspective featuring a water flume in the shape of a horseshoe built along a forested hillside. Handwritten annotation on verso of photograph reads: "Horshoe Creek"

Photograph depicts one man standing on the bank of a river, forest in the background. The image is not in focus or possibly a double exposure.

Image depicts the Lakeland Sawmill in Prince George, B.C, identified by the beehive burners; the one with white smoke belonged to Pas Lumber Co. which was bought out by Lakeland in 1987.

Image depicts the Lakeland Sawmill in Prince George, B.C.

Photograph depicts a small inland lake, trees and low hills border the lake.

Item is an original "Kwadacha Park 1976" trip report by W.G. Hazelwood. Includes original photographic prints pasted into the report. Also includes a "Kwadacha Wilderness Park Proposal" accompanying map.

File consists of an original draft copy of the "Kokanee Glacier Park Master Plan", as well as the "Background Report for Kokanee Glacier Park Master Plan" and the "Kokanee Glacier Park Master Plan: Public Handout and Questionnaire". These items are accompanied by correspondence related to the Master Plan.

This image is part of the outbound sequence of aerial images obtained on the helicopter flight to the Klutlan Glacier study site. The sequence starts from the base camp at the White River crossing on the Alaska Highway and heads south, to a point just upvalley of the debris-covered terminus (approx. 10-15 km from Alaska border), and turning back north to the landing spot on the Generc River floodplain close to the study site (see Fig. 1 in paper).

This image is part of the outbound sequence of aerial images obtained on the helicopter flight to the Klutlan Glacier study site. The sequence starts from the base camp at the White River crossing on the Alaska Highway and heads south, to a point just upvalley of the debris-covered terminus (approx. 10-15 km from Alaska border), and turning back north to the landing spot on the Generc River floodplain close to the study site (see Fig. 1 in paper).

This image is part of the outbound sequence of aerial images obtained on the helicopter flight to the Klutlan Glacier study site. The sequence starts from the base camp at the White River crossing on the Alaska Highway and heads south, to a point just upvalley of the debris-covered terminus (approx. 10-15 km from Alaska border), and turning back north to the landing spot on the Generc River floodplain close to the study site (see Fig. 1 in paper).

This image is part of the outbound sequence of aerial images obtained on the helicopter flight to the Klutlan Glacier study site. The sequence starts from the base camp at the White River crossing on the Alaska Highway and heads south, to a point just upvalley of the debris-covered terminus (approx. 10-15 km from Alaska border), and turning back north to the landing spot on the Generc River floodplain close to the study site (see Fig. 1 in paper).

File contains the following data sets:

• S925finl.xls [chemical analysis data, Ministry of Forests & Range, Analytical Chemistry Laboratory for pedons Y07-06 & Y07-07; also includes data for BC07-03 & BC07-04 (Boreal Cordillera grassland soils – see associated file note)]
• S1007finl_revised2.xls [chemical analysis data, Ministry of Forests & Range, Analytical Chemistry Laboratory for pedons Y07-06 & Y07-07: oxalate & dithionite extractions, P retention; also includes P retention data for Nazko pedons BC07-07 & BC07-09]
• CANTEST lab report 90206003.pdf [particle size analyses for Klutan Glacier pedons Y07-06 & Y07-07; also Tuya pedons BC07-03 & BC07-04 &]

With the assistance of the Yukon Geological Survey, Dr. Paul Sanborn was able to visit the terminus of the Klutlan Glacier, a major outlet glacier which originates in the Alaska portion of the St. Elias Mountains. The stagnant terminus has a thick cover of debris, including a large component of White River tephra, providing enough soil material to support a boreal forest. Field work occurred on July 8, 2007, and results were published as:

Sanborn, P. 2010. Soil formation on supraglacial tephra deposits, Klutlan Glacier, Yukon Territory. Canadian Journal of Soil Science 90: 611-618. https://doi.org/10.4141/cjss10042