Recently it has become apparent that teleseismic detection has decreased substantially in many regions of the world. The major decrease was related to the closure of the VELA arrays in the United States during the later 1960's. This detection decrease has been recognized in South and Central America, Mexico, the Kuriles, the Caribbean, Tonga, and the New Hebrides. In this paper the effect of the closure of these arrays on the reporting of events in the Aleutian Island Arc is examined. In the Aleutians, the detection history is complicated by the short-term installation of a local network on and near Amchitka Island during the early 1970's. The temporal coincidence of the installation of this network and the closure of the VELA arrays delayed the detection decrease in the central Aleutians until the Amchitka network was closed in early 1973. Reporting in the eastern Aleutians was unaffected by the installation of the Amchitka network. In that region the detection decreased between 1968 and 1970, the times of the closure of the VELA arrays. New techniques have been developed which make it possible to determine the effect of station installation of closure on the reporting in some regions. These techniques rely on plots which show the distribution of an observed seismicity rate change in the magnitude domain. These plots make it possible to recognize probable detection changes and to determine quantititively magnitude cutoffs which avoid these changes. The magnitude level at which these cutoffs are made is termed the minimum magnitude of homogeneity (mminb)Ih. The reporting of events with mb≤4.6 in the Aleutians decreased substantially during the mid-1970's, so mminh in the region is 4.7. This is different from the magnitude of completeness (mminc) which is mb=5.0¿0.1. If one is interested in examining seismicity rates for changes which may be precursors to earthquakes, then awareness of detection-related changes and magnitude cutoffs which avoid these changes are essential for meaningful results.