We investigate how integration of bank ownership across states has affected economic volatility within states. In theory, bank integration could cause higher or lower volatility, depending on whether credit supply or credit demand shocks predominate. In fact, year-to-year fluctuations in a state’s economic growth fall as its banks become more integrated (via holding companies) with banks in other states. As the bank linkages between any pair of states increase, fluctuations in those two states tend to converge. We conclude that interstate banking has made state business cycles smaller, but more alike. I. INTRODUCTION The United States banking system was once anything but united. Until 1978, every state in the union barred banks from other states, so instead of one national banking system, we had more like 50 little banking systems, one per state. 1 Once states opened their borders to out-of-state banks, bank holding companies marched in and bought up (or merged with) banks all over the country. In 1975, just 10 percent of the bank assets in the typical state were owned by a multistate bank holding company. By 1994 this interstate bank asset ratio had risen to 60 percent (Figure I). Our paper investigates how the advent of interstate banking integration in the United States has affected economic volatility within states. With the United States’ balkanized banking system, the fate of a state and its banks were closely tied; as went the state, so went the banks. The farm price deflation in the early 1980s bankrupted many farmers and many farm banks. Falling oil prices in the mid-1980s wiped out a lot of Texans and a lot of Texas banks. Shocks to commodity prices probably caused these contractions, but frictions in the banking sector may have aggravated them. By allowing a freer flow of bank capital and lending among states, we maintain that interstate banking will reduce the drag that banking frictions can have on economic contractions.
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