Proceedings of the Canadian Institute

Cover Proceedings of the Canadian Institute
Proceedings of the Canadian Institute
Canadian Institute 1849 1914
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Ocean currents flow for the most part of their course through water and having a bed of water between the current and the bottom, thereby protecting it from any corrading influence the current might have. Whatever planed off the sub-carboniferous and other beds to the level of the Highland lim, or hollowed out the basin, ocean currents had nothing to do with the work.
Transportation as we have already stated is chiefly carried on by running water. It is also carried on to a small extent by the
...aid of the wind and atmospheric currents. The latter is more or less con- N fined to the sandy shores of the sea and arid sandy districts.
Disintegration is earned on by weathering and slightly, in a mechanical way, by ininning water. This action of running water has been called corrasion.
The chief agents in weathering are changes of temperature, rain as^ a solvent and as a mechanical agent, gravity and vegetation.
Sudden changes of temperature affect material of every sort. Frost following a saturated condition will by freezing fracture the hardest rock wherever water has been enabled to penetrate.


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