Geology of the Haliburton and Bancroft Areas, Province of Ontario (Classic Reprint)

Angebote / Angebote:

Excerpt from Geology of the Haliburton and Bancroft Areas, Province of OntarioThe average gradient of the snuthwartl slnping hut'tlen of the plain eannnt. He t'ertainly with the data at present availahle. The exaet height. At a stttlieient ntltnhei' ui' peints nut heing knewa. If. However. A line is taken t't'mn the height of land whieh here farms the divide hetween the lttsknka antl latlawaska rivers. At the nurthe't'n edge 44 the llalihttt'tnn sheet in the township of Peek feet), in a tlit'eetinn S. 19° Ii. Tu the surface ml the plain at a pnin-t two miles snath ut' (iumler hatn feet). In the township of (ilanmrgan - a distance of 46 miles - the gt'atlient will he t'ntttnl to he 6-4 feet to the mile. If a lnnget' line 'is taken.. Emssing the entite eensitletetl in this report, running.r a little to the west of that just. Tnentinnetl and parallel to it. From t'anue lake in the tuwnship of l'eek feet). Jttst nm'th f the limit of the llalihttrtnn sheet. To lleet' ha\' (792, feet). In the township of Harvey. At the extreme smithet'n lintit ut' the llanereft sheet, the total tleseent will he 5st} feet, and the gradient Sol l'eet tn the mile.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.