Annual Report, 1890-91, Vol. 5

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Excerpt from Annual Report, 1890-91, Vol. 5: Part II, Reports P, Q, R, S, SsAlong the northern part of Pictou and Colchester counties, from Big Island, Merigomish, to Brulé and Tatamagouche, there is a wide belt of Permian rocks, the conglomerate at the base forming Fraser's Permian. Mountain, Green Hill, Roger's Hill, Fitzpatrick's Mountain, Dal housie Mountain, the Biorachin and other highlands on its course. The conglomerate is overlaid by grey sandstones, like those of Pictou and West River, containing one or more thin coal seams, and these are succeeded in turn by brownish and red sandstones and marls with thin layers of limestone. Dark red, crumbly, Triassic Triassic. Sandstone and conglomerate, generally in nearly horizontal attitude, occupy a basin which extends westward from near Valley station, one rim fringing the south side of Mines Basin, the other reaching much further inland on the north side. Two principal intrusions of igneous rock have been determined within the area. In one red Igneous rocks. Syenite, diorite, felsite and similar rocks cut no strata newer than the Devonian, in the other Triassic sandstones are intersected and intermixed with great masses of basalt and amygdaloid which furnish the celebrated trap minerals of the Bay of Fundy.About the PublisherForgotten Books publishes hundreds of thousands of rare and classic books. Find more at www.forgottenbooks.comThis book is a reproduction of an important historical work. Forgotten Books uses state-of-the-art technology to digitally reconstruct the work, preserving the original format whilst repairing imperfections present in the aged copy. In rare cases, an imperfection in the original, such as a blemish or missing page, may be replicated in our edition. We do, however, repair the vast majority of imperfections successfully, any imperfections that remain are intentionally left to preserve the state of such historical works.