The American Mycological Society

Abstract

The afternoon session was held in the university lecture room. The meeting was called to order by Professor Barrows, who addressed the society on 'Recent Advances in Ornithology.' The following program was then presented: LEON J. COLE: 'I n Memoriam-Albert Bowen Durfee' (read by J. Wilbur Kay in the absence of the author). NORMAN A. WOOD: 'Birds ..oted En route to Northern Michigan.' OTTO MCCREARY: 'Ecological Distribution of tiie Birds of the Porcupine Mountains, Michigan.' MAX M. PEET: 'Observations on the Nesting Habits of a Pair of House Wrens.' ALEXANDER WX. BLAIN, JR.: 'On the Use in Surgery of Tendons of the Ardeidoe and Gruide.' NORMAN A. WOOD: 'Some New and Rare Records for Michigan.' EARL H. FROTIIINGHAM: 'A List of Birds from the-Micnigan Forest Reserve, Crawford County.' LEON J. COLE: The Occurrence of Bewick's Wren, Thryomnanes bewickii (Aud.), at Grand Rapids (read by Wm. H. Dunham).

Remoblization and Injection in Deepwater Depositional Systems: Implications for Reservoir Architecture and Prediction

“…2A): (a) tectonic stress (e.g., Winslow, 1983), (b) earthquake induced liquefaction (e.g., Fuller, 1912;Obermeier, 1989), and (c) localized excess pore fluid pressures resulting from depositional processes, such as local loading due to mass movements and slumping (Truswell 1972), the passage of storm waves (Allen 1985;Martel and Gibling, 1993), or channel switching (e.g., Hiscott, 1979). In general, depositional event triggers tend to produce small-scale (cm-mscale) intrusions dominated by sills (e.g., the Ordovician of Quebec and Western Ireland documented by Hiscott,1979, andArcher, 1984, respectively).…”

Regional structure of the southeast Missouri and Illinois-Kentucky mineral districts

“…The New Madrid earthquake series of 1811-13 included hundreds of quakes, and several of these were among the most violent earthquakes ever recorded anywhere in the world (Fuller, 1912). The very large oval pattern of the epicenters of the earthquake series was elongated northeastward along the New Madrid fault zone across the IllinoisKentucky district, but a branching lobe of the epicenters extended northwestward up the Ste.…”

Effects of the March 1964 Alaska earthquake on the hydrology of the Anchorage area, Alaska

“…Dewatering is presumably desirable for engineering stability, but it may affect adversely the ground-water supply of the Anchorage area. If the formation is dewatered by pumping the sand and gravel aquifers Subsidence of unconsolidated material by compaction during earthquakes has been reported from many previous earthquakes, notably the New Madrid earthquake of 1811 (Fuller, 1912). The Alaska earthquake of 1964 caused subsidence in many of the areas underlain by unconsolidated deposits in south-central Alaska beneath or within the clay to reduce water leakage into the clay, the problem of decreased piezometric level in the artesian system near the estuary would arise immediately.…”