Page:Principles of Political Economy Vol 2.djvu/108

88 mortgages or other private debts of old standing, a percentage corresponding to the estimated amount of the depreciation.

To this doctrine, the following was the answer usually made. Granting that, by returning to cash payments without lowering the standard, an injustice was done to debtors, in holding them liable for the same amount of a currency enhanced in value, which they had borrowed while it was depreciated; it is now too late to make reparation for this injury. The debtors and creditors of to-day are not the debtors and creditors of 1819: the lapse of years has entirely altered the pecuniary relations of the community; and it being impossible now to ascertain the particular persons who were either benefited or injured, to attempt to retrace our steps would not be redressing a wrong, but superadding a second act of wide-spread injustice to the one already committed. This argument is certainly conclusive on the practical question; but it places the honest conclusion on too narrow and too low a ground. It concedes that the measure of 1819, called Peel's Bill, by which cash payments were resumed at the original standard of 3l. 17s. 10½d., was really the injustice it was said to be. This is an admission wholly opposed to the truth. Parliament had no alternative; it was absolutely bound to adhere to the acknowledged standard; as may be shown on three distinct grounds, two of fact, and one of principle.

The reasons of fact are these. In the first place, it is not true that the debts, private or public, incurred during the Bank restriction, were contracted in a currency of lower value than that in which the interest is now paid. It is indeed true that the suspension of the obligation to pay in specie, did put it in the power of the Bank to depreciate the currency. It is true also that the Bank really exercised that power, though to a far less extent than is often pretended; since the difference between the market price of gold and the Mint valuation, during the greater part of the interval,