Wd. Kalkreuth et al., GEOLOGICAL, ARCHAEOLOGICAL, AND HISTORICAL OCCURRENCES OF COAL, EAST-CENTRAL ELLESMERE ISLAND, ARCTIC CANADA, Arctic and alpine research, 25(4), 1993, pp. 277-307
Coal, once widely distributed over most of east-central Ellesmere Isla
nd, is only present in restricted outcrops of Eureka Sound Group sedim
ents that survive in the Bache Peninsula Graben (BPG) on eastern Bache
Peninsula. The discovery of coals similar to those of Bache Peninsula
in modern moraine sediments at the Jewell, Leffert, and Alfred Newton
glaciers on Johan Peninsula to the south, provide evidence that(I) th
e Eureka Sound Group was more extensive in the past and is present tod
ay beneath modern glaciers and (2) the glaciers are likely filling gra
bens similar to the BPG. Twelve samples of coal were recovered from Th
ule culture house ruins dating from the 12th to 17th centuries A.D. Fo
ur samples have huminite reflectance levers and compositional features
of lignites, and most likely originated in nearby seams of the Tertia
ry Eureka Sound Group. The remaining eight pieces were either boghead
coal, cannel shale, or jet materials that are as yet unknown in the Eu
reka Sound Group coal-bearing strata. There is no evidence that coal w
as burned by the early native peoples. At the turn of the century expl
oration of the area and the quest for the North Pole saw the importati
on of coal into the area from Nova Scotia. Many references to coal can
be found in journals and other literature from the period, and its us
e was an important element in the exploration period. Caches of coal b
rought by the explorers Robert Peary and Robert Stein are found in the
Cape Herschel area and at Pim Island. In 1905, Peary also cached a la
rge quantity of coal at Bartlett Bay, 5 km to the east of the coal out
crops on eastern Bache Peninsula. Peary, who travelled widely in the a
rea on hunting expeditions, likely knew of the local coal but did not
choose to use it. Samples of coals from the caches proved to be identi
cal to Nova Scotia bituminous coals and very different from the Eureka
Sound lignites and sub-bituminous coals. The R.C.M.P. manned a post o
n Bache Peninsula from 1926 to 1933 and later at Alexandra Fiord (unti
l 1962). The coal, used for cooking and heating, was purchased from a
company that imported high rank (anthracite) coal from Wales. Samples
of coals from the two posts and a way-station at Rice Strait are very
different from both the local and the Nova Scotia coals in terms of ra
nk.