The vast majority of theses in this collection are open access and freely available. There are a small number of theses that have access restricted to the WWU campus. For off-campus access to a thesis labeled "Campus Only Access," please log in here with your WWU universal ID, or talk to your librarian about requesting the restricted thesis through interlibrary loan.
Date Permissions Signed
Date of Award
Master of Science (MS)
Ross, Charles A., 1933-
Suczek, Christopher A., 1942-2014
Pevear, David R.
The Tulameen Coalfield lies in a small, southeast plunging syncline in the Intermontane Belt of the Canadian Cordillera in south central British Columbia. The coal is interbedded with fluvial and lacustrine sediments of the Eocene Allenby Formation of the Princeton Group. The abundance of tephra and bentonite indicates volcanic activity was contemporaneous with coal and sediment deposition.
Although coal occurs on both sides of the basin, its economic importance is currently restricted to a 15-21 meter thick coal seam on the southwestern limb of the syncline. The coal is predominantly vitrain and clarain composed of greater than 90 percent vitrinite. Clean coal has 14 percent ash (mostly kaolinite and quartz) and low sulphur. The coal is interbedded with bentonite, mudstone and shale partings which increase in number from south to north. The partings are montmorillonite and/or kaolinite rich.
Coal rank along the southwestern limb of the basin was determined by measuring the percent maximum reflectance of vitrinite. Vitrinite reflectance increases laterally from .62 in the north to .86 in the south but shows no significant vertical variation. According to the A.S.T.M. classification, coal rank ranges from High Volatile C Bituminous to High Volatile B Bituminous. Field relations indicate partial post-deformation coalification.
Petrographic study of the coal suggests the coal-forming peat developed in a predominantly forest moor swamp environment.
Tulameen Coalfield, British Columbia, Coal petrology
Western Washington University
Subject – LCSH
Coal--British Columbia--Tulameen region; Petrology--British Columbia--Tulameen region
Tulameen Region (B.C.)
Copying of this thesis in whole or in part is allowable only for scholarly purposes. It is understood, however, that any copying or publication of this thesis for commercial purposes, or for financial gain, shall not be allowed without the author's written permission.
Williams, V. Eileen, "Coal Petrology of the Tulameen Coalfield, South Central British Columbia" (1978). WWU Graduate School Collection. 810.