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Oakwood Aeolians sing at Corliss High Chicago Defender (04/11/2000)
Oakwood Aeolians sing at Corliss High Under the directionLloyd Mallory Jr. the Oakwood College Aeolians are scheduled to perform at Corliss HighSaturday, April 15 at 7 p.m. On Friday, the Aeolians will appear at the Independence SDA Church

In The Aeolian Islands, A September Song - New York Times The New York Times (09/29/2002)
boat is practically the only way to reach the Aeolians, a sprinkling of dark volcanic cones that risevolcano in Europe. Invasion is nothing new to the Aeolians. Like their Sicilian sister hanging hazy on themetallurgy, that first attracted settlers to the Aeolians near the end of the fifth

Climate, sediment supply and tectonics as controls on the deposition and preservation of the aeolian-fluvial Etjo Sandstone Formation,...... Journal of the Geological Society (07/01/1999)
Abstract: Deposition and subsequent preservation of the Jurassic-Cretaceous Etjo Sandstone Formation of Namibia represents a complex interplay between climatic and tectonic factors and related variations in extrabasinal sediment supply. The aeolian and fluvial deposits indicate semi-arid to arid

Reviews/Music; Aeolian Players In a Celebration Of Summers - New York Times The New York Times (11/16/1988)
violinist. This year, Bowdoin and the Aeolians, along with a few guest performers whoviolinist. This year, Bowdoin and the Aeolians, along with a few guest performers whoEchoes of Autumn, 1965'' composed for the Aeolians in 1966, and played by Mr. Kaplan, Peter

Stromboli Calling: Where Aeolus Blows and Vulcan Fumes.(Aeolian Islands ) World and I (08/01/2004)
s northern coast. They rose from the deep relatively recently; Stromboli, the youngest, formed 40,000 years ago. The Aeolians were settled by 4000 B.C., and in some centuries the islanders knew great prosperity. Homer said King Aeolus, who gavepacks were helped into the boat and went off to Ginostra. The Carpaccio

The red clay mantle in the Wagga Wagga region, New South Wales: evaluation of an aeolian dust deposit (Yarabee Parna) using methods...... Australian Journal of Soil Research (01/01/2001)
Introduction Aeolian dust deposits are widely distributed in south-eastern Australia. Butler (1956) first used the word parna (Aboriginal word for dust) to refer to the aeolian clay deposits in the Riverine Plain. Since Butler (1956), and Butler and Hutton (1956), similar deposits have been

Using radiometric data to identify aeolian dust additions to topsoil of the Hillston district, western NSW.(New South Wales) Australian Journal of Soil Research (12/15/2003)
Introduction Although Australia lacks the thick loess mantles that are found on most other continents, Butler's (1956) parna model of dust deposition and related features in southern New South Wales (NSW) and northern Victoria has achieved considerable currency over the last 45 years. However, it

Symposium report: Aeolian dust--implications for Australian mineral exploration and environmental management. Australian Journal of Soil Research (01/01/2001)
synthesis of existing information should include all models, and information from various sites, e.g. Wagga Wagga, geomorphic maps, profile characteristics, geochemical information, and radiometric data. Further research is required on sediment flux calculations

An aeolian component in Pleistocene and Holocene valley aggradation: evidence from Dicks Creek catchment, Yass, New South Wales.(Statistical...... Australian Journal of Soil Research (01/01/2001)
Introduction The study of Quaternary processes within the Southern Highlands of New South Wales has evoked considerable interest during the past 40 years. More recently, the occurrence of extensive dryland salinity in the area has led to further detailed investigations into the origin of salts

The stratigraphic role of marine deposits in the geological evolution of the Panarea volcano (Aeolian Islands, Italy) Journal of the Geological Society (09/01/2007)
Abstract: Using reconstructed unconformity-bounded stratigraphy, the geological evolution of Panarea and surrounding islets can be described in terms of the interaction between the growing volcano and sea-level fluctuations. From the recognition of marine deposits corresponding to marine oxygen

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