And yet, widely accepted and deeply rooted as it is, it seems to me that this theory does not tally with obvious facts. For, if wages depend upon the ratio between the amount of labor seeking employment and the amount of capital devoted to its employment, the relative scarcity or abundance of one factor must mean the relative abundance or scarcity of the other. Thus, capital must be relatively abundant where wages are high, and relatively scarce where wages are low. Now, as the capital used in paying wages must largely consist of the capital constantly seeking investment, the current rate of interest must be the measure of its relative abundance or scarcity. So, if it be true that wages depend upon the ratio between the amount of labor seeking employment and the capital devoted to its employment, then high wages, the mark of the relative scarcity of labor, must be accompanied by low interest, the mark of the relative abundance of capital, and reversely, low wages must be accompanied by high interest. This is not the fact, but the contrary. Eliminating from interest the element of insurance, and regarding only interest proper, or the return for the use of capital, is it not a general truth that interest is high where and when wages are high, and low where and when wages are low? Both wages and interest have been higher in the United States than in England, in the Pacific than in the Atlantic States. Is it not a notorious fact that where labor flows for higher wages, capital also flows for higher interest? Is it not true that wherever there has been a general rise or fall in wages there has been at the same time a similar rise or fall in interest? In California, for instance, when wages were higher than anywhere else in the world, so also was interest higher. Wages and interest have in California gone down together. When common wages were $5 a day, the ordinary bank rate of interest was twenty-four per cent. per annum. Now that common wages are $2 or $2.50 a day, the ordinary bank rate is from ten to twelve per cent.