The item is a photograph depicting the remaining lumber beams after the fire at the Bank of Montreal in Prince George.
The item is a CDR containing seven jpg images for a property presentation by Kent Sedgwick.
Photograph depicts an Alberni Pacific tourist railway locomotive backing onto its train of passenger cars (3 opened, 2 closed, all CN transfer cabooses, now remodelled).
Photograph taken on the Esquimalt & Nanaimo Railway main line out of Port Alberni with run-around siding over the right out of sight. Yard is found towards the rear. On the left, there was private trackage of the Nordeske paper mill that was in daily use until December 31, 2001 when Rail America stopped runnning freights because the mill went to road transport.
Photograph depicts an Alberni Pacific railway train that was just coming into a run-around loop at the end of a sawmill spur. Trackage built 2000/01.
Photograph depicts Esquimalt & Nanaimo Railway trackage in Port Alberni only used by the Alberni Pacific tourist railway. Visible is an interesting throw-type switch.
Photograph depicts a water tank car used for fighting line side fires. Propery of Alberni Pacific tourist railway. Sat in a yard in Port Alberni. Formerly owned by Crown Zellerbach of Ladysmith.
Photograph depicts an old tank car owned by a logging railway on Vancouver Island, parked at the end of a spur behind a locomotive shed of the Alberni Pacific Railway.
Photograph depicts a tiny switcher that belonged to the McLean sawmill and was buily by Buda of New Westminster, circa 1927. Sat on unconnected trackage adjacent to the Alberni Pacific Railway and was part of a sawmill exhibit.
Includes a copy of B.C. Bookworld, vol. 21, no.4, winter 2007-2008 with a feature interview with Ann Walsh.
This document contains pedon descriptions for sites BC07-03 & BC07-04 for Sanborn's comparative study of grassland soils in the Boreal Cordillera ecozone.
This document contains transcribed August 2007 field notes from 5 observation sites for Sanborn's comparative study of grassland soils in the Boreal Cordillera ecozone.
File consists of thin section micrograph images from the Boreal Cordilleran grassland soils study (2007 & 2008).
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
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).