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COAL - Clpdigital.org

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Another meritorious feature of these pumps, as<br />

well as in all types of Cameron pumps, is found<br />

in the design and construction of their operating<br />

mechanism, which has but few working parts, and<br />

no outside valve gear or rods to become broken or<br />

to get out of alignment.<br />

Floating timbers and debris, which are often<br />

times the cause of damage to submerged pumps,<br />

can do no harm to Cameron pumps, as the working<br />

parts are not exposed. Often a Cameron pump<br />

has been submerged under water for weeks and<br />

has kept right on pumping to the limit of its<br />

capacity until it has cleared the shaft or mine.<br />

New Coal Field in Nova Scotia.<br />

The recent discovery of coal about 20 miles south<br />

of Springhill is the most important mining event<br />

in many years in Nova Scotia. It is the direct<br />

result of deduction from painstaking investigations<br />

of the geological conditions at Springhill.<br />

Dawson, who stood in the front rank of Canadian<br />

geologists and whose conclusions were generally<br />

accepted without reserve, judged that the conglomerate<br />

rock that appears at Springhill and extends<br />

south was deposited before the coal measures;<br />

hence, where the conglomerate appears at<br />

the surface the conclusion was that no coal existed.<br />

THE <strong>COAL</strong> TRADE BULLETIN. 4!)<br />

under the conglomerate. It was on this theory<br />

Coal prospectors have, since his day, generally<br />

accepted the conglomerate district, as not productive.<br />

Mr. Fletcher, of the geological survey of<br />

Canada, undertook a long and laborious examination<br />

of the surface indications, and arrived at conclusions<br />

directly at variance with Dawson's,<br />

namely, that the conglomerate was of a later age<br />

than the coal, and that there was no apparent reason<br />

why there were not coal seams at Springhill<br />

Fig. 3. Outside Construction of Pumps.<br />

that a number of coal men formed an association<br />

to bore at a spot indicated by Mr. Fletcher. The<br />

work has resulted in the discovery of a fine coal<br />

field which, if not entirely new, is at least an extension<br />

of the Springhill field, embracing an area<br />

of 200 square miles or more. Mr. Fletcher assumed<br />

that coal would be reached at a depth of<br />

from 2,000 to 3,000 feet, and operations were commenced<br />

with that idea. The drill first pierced<br />

some 810 feet of reddish sandstone, etc., belonging<br />

to the upper Permian formation; then about<br />

1,500 feet of conglomerate was met; then some 19<br />

feet of sandstone, when the coal was struck. The<br />

drill went through some 12 feet of coal, but it<br />

made no core, and as the pitch of the seam is unknown<br />

its exact thickness cannot be determined<br />

as yet.

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