The federal farm loan system, new method of farm mortgage finance, under national supervision; a practical manual upon organizing and conducting national farm loan associations, also joint stock land banks... /

Mode of access: Internet.

Journal of a trip to the Shepherd, Banks, and Torres Islands and to Espiritu Santo and Efate in the New Hebrides, November 15, 1963, to December 25, 1963 /

Reprint, with new indexes, of the 1965 ed.

The Multilateral development banks : increasing U.S. exports and creating U.S. jobs.

Shipping list no.: 94-0175-P.

The changing business of banking : a study of failed banks from 1987 to 1992.

"June 1994"--Cover.

Digest of decisions relating to national banks, 1864-1926 - [1864-1936]

"The digest of decisions relating to national banks was for many years included as part of the comptroller's Annual report. Prior to 1902 this was confined to decisions by the federal courts, but in that year a large number of state decisions were added. Since that date all decisions of the federal courts have been included and a few selected state decisions added thereto." Pref., vol. II p. iv

Federal laws affecting national banks, including provisions of U. S. Revised statutes, Federal reserve act, Deposit insurance law, Emergency banking act, Bank conservation act, Banking act of 1933, Banking act of 1935 and other laws affecting the national banking system as of January 1, 1950.

"Compiled to supersede and bring up to date the previous edition, published in 1940."

Federal laws affecting national banks, including provisions of U. S. Revised statutes, Federal reserve act, Deposit insurance law, Emergency banking act, Bank conservation act, Banking act of 1933, Banking act of 1935 and other laws affecting, directly or indirectly, the national banking system, as of January 1, 1936.

On cover: National bank laws as of Jan. 1, 1936

An evaluation of results and effectiveness of job banks /

"Contract no. 83-06-72-01."

Annual report of the Superintendent of Banks /

Mode of access: Internet.

Federal reserve banks : inaccurate reporting of currency at the Los Angeles Branch : report to the Ranking Minority Member, Committee on Banking and Financial Services, House of Representatives /

"B-274060"--P. 1.

Why do US banks borrow from the Fed? A fresh look at the ‘reluctance’ phenomenon

The role of several theoretical factors in determining the demand of US banks for borrowed reserves from the Fed is empirically investigated. The main objective is to isolate the candidate(s) most likely responsible for the recent observed phenomenon of banks reluctance to borrow from the Fed, particularly since the mid-1980s. The results indicate that the declining number of banks due to mergers and consolidations holds much of the weight for explaining the weakened demand for borrowed reserves since the mid-1980s. Consistent evidence is found suggesting that US banks may have been unlawfully exploiting the discount window service for profit-taking purposes. This finding proves credible and suggests the need for further loan scrutiny at the Federal discount window.

Anomalous magnetic susceptibility values and traces of subsurface microbial activity in carbonate banks on San Salvador Island, Bahamas

Pure limestones beneath the paleosols on San Salvador Island, Bahamas, contain strong positive magnetic susceptibility anomalies, although the iron content is generally very low. These magnetic phenomena differ from those associated with disconformities, which are marked by accumulation of paramagnetic airborne dust deposits with relatively high iron content. The strength and characters of the magnetic response in these subsurface zones correspond to the presence of magnetite, particularly small single-domain magnetite crystals of microbial origin. These crystals are not present elsewhere in the intergranular rock pores or microvugs. They are preferentially concentrated in capillary microborings, which developed concurrently with formation of calcite cements that have soil-related C and O isotope compositions. These magnetic zones occur several meters below the overlying soil horizons. Very thin and long linear microborings may be attributable to cyanobacterial microborers. The single-domain magnetites in these micrometer-size tunnels plugged by calcite appear to result from later occupation of these tiny holes by magnetotactic bacteria. Inorganic origin of the magnetite seems unlikely. Numerous traces that suggest subsurface microbial activity provide evidence that may be used to develop possible scenarios for subsequent biological studies of the precise bacteria involved.