Issued Under Title, Message from . . . the Governor General, with Reports on Geological Survey Presented to the Legislative AssemblyGeological Survey of Canada, 1872 Contents of each report may be found in "List of publications of the Geological survey of Canada. 1900." |
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Results 1-5 of 93
Page 7
... road through the townships of Arundel and Harrington , on which a single team can draw from eight to nine hundred pounds , and a light car can travel from Grenville Village to the rear of the Township of Arundel without encounter ...
... road through the townships of Arundel and Harrington , on which a single team can draw from eight to nine hundred pounds , and a light car can travel from Grenville Village to the rear of the Township of Arundel without encounter ...
Page 31
... road from Spruce Lake to Musquash , while the limestones and the quartzites of the upper series are well exposed on the eastern shore of the peninsula of Pisarinco . Both portions cross the latter to Musquash Harbor , of which they form ...
... road from Spruce Lake to Musquash , while the limestones and the quartzites of the upper series are well exposed on the eastern shore of the peninsula of Pisarinco . Both portions cross the latter to Musquash Harbor , of which they form ...
Page 34
... Road , especially near where the latter passes from St. John into Albert county . They may be in part intrusive . DETAILS OF THE LAURENTIAN SYSTEM . The general range and distribution of the supposed Laurentian rocks in St. John County ...
... Road , especially near where the latter passes from St. John into Albert county . They may be in part intrusive . DETAILS OF THE LAURENTIAN SYSTEM . The general range and distribution of the supposed Laurentian rocks in St. John County ...
Page 37
... road , a short distance to the north- Peninsula . west . Some portions here represented are without visible stratification , while others exhibit a gneissic structure , and are succeeded at Mosquito Cove Hollow by well marked gneiss ...
... road , a short distance to the north- Peninsula . west . Some portions here represented are without visible stratification , while others exhibit a gneissic structure , and are succeeded at Mosquito Cove Hollow by well marked gneiss ...
Page 38
... road , the section was extended in a northerly direction over the calcareo - silicious strata in the centre of the Lau- rentian area , as follows : - Section on Green Head road . Traverse measure . Space , occupied mostly by slate ...
... road , the section was extended in a northerly direction over the calcareo - silicious strata in the centre of the Lau- rentian area , as follows : - Section on Green Head road . Traverse measure . Space , occupied mostly by slate ...
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Common terms and phrases
appear argillites bands beds belt Brook Brunswick calcareous Carboniferous Charlotte County chloritic clay-slates coarse Coastal group Coldbrook color conglomerate Cove Creek crystalline crystals dark grey Dawson described Devonian diorite distance district Division east eastern side eastward epidotic exposed extending feet feldspar feldspathic felsites fossils geological gneiss grained granite granitoid green greenish greenish-grey grey feldspathic grey sandstones grey shales grits Harbor hard grey Hartt hills hornblende Huronian Island John County John group John River Kingston group last named latter Laurentian ledges Lepreau limestone Long Lake Lower Carboniferous mass mica mica-schists micaceous miles mineral Musquash nearly Nerepis Nerepis River northern side northward Nova Scotia numerous observed occur parish pebbles peninsula petrosilicious porphyritic portage portion probably pyrites quartz quartzites reddish resembling ridge road sandstones sandy schistose schists sediments seen shales shore silicious Silurian similar slates slaty southern strata stream syenitic thickness Upper Silurian valley veins
Popular passages
Page 277 - The attempts frequently made to enhance the value of the stock by declaring dividends, sometimes paid out of capital, but often by means of a process commonly known as " picking the eyes out of the mine...
Page 175 - ... conglomerate having a red slaty paste filled with large subangular fragments of a grey altered rock, like the lower slate of the Coldbrook group. It also contains fragments of reddish sandstone and a few pieces of impure slaty limestone. The conglomerate is overlaid by thick beds of purple clay slate, which by the accession of coarser materials becomes a slaty sandstone and grit filled with white particles. The highest member on the line of section is a slaty conglomerate holding fragments of...
Page 62 - Works the rocks of the more northerly anticlinal ridge present the following succession : — Hard greenish-grey petrosilicious rock, with very obscure stratification ; conglomerate with bright red slaty paste ; grey conglomerate ; coarse reddish grit and conglomerate, with purple sandstone : apparent thickness of the whole, 5,000 feet. From the Coldbrook valley, through which the above strata (which are chiefly of Nos. 3 and 4) pass northward to the valley of Hammond...
Page 342 - The timber consists mostly of spruce, balsam-fir, white ce.dar, tamarack, white birch and aspen. Some of the larger spruces and tamaracks measured between five and six feet in girth at five feet from the ground ; but the average diameter of the larger trees would be about eighteen inches. In the last twenty or thirty miles explored, the ground became swampy on going back to a short distance from the river on either side, the timber consisting of small spruces, cedars and tamaracks. The...
Page 278 - The disregard of the natural features of the ground, shown in locating the crushing and dressing machinery without reference to the easy delivery of the material from the mine and the fall required for the perfect treatment of the ores, and for getting rid of the tailings.
Page 135 - The actual thickness, however, may be much less than this, for while there are numerous faults and folds for which allowance is made in the above estimate, a repetition of similar sediments on either side of the trough of these rocks upon which the city of St. John stands, would appear to indicate that the entire series, with the undei lying Huronian strata, is here folded upon itself in a sharp synclinal, overturned to Overturn, the northwest. In this case, the aggregate thickness of the series,...
Page 291 - Bands of crystalline limestone are easily distinguished from bands of gneiss, but it is scarcely possible to know, from mere local inspection, whether any mass of limestone in one part is equivalent to a certain mass in another. They all resemble one another more or less lithologically, and although masses are met with, running for considerable distances rudely parallel to one another, it is not yet INVESTIGATIONS OF SIR W. LOGAN'.
Page 282 - ... manufacture." Concerning the use of formaldehyde. — " Inasmuch as milk, of all ordinary foods, is the most prone to deterioration and requires the most careful treatment, the temptation to use such an efficient preservative as formaldehyde is proportionately greater, especially during the summer months. " It seems not out of place to call attention to the fact that apart from the injurious effects of formaldehyde itself its use as a preservative would be especially inadvisable in milk or cream,...