The interaction of contaminated sites with meltwater/groundwater and aeolian processes did not significantly change the hydrocarbon distribution at the former base site during the monitoring period (1992- 96).
Coal, aeolian deposits, evaporites, red beds, palaeosols or mineralogy of clay minerals are usually used for such analyses since it is believed their formation is climate-dependent.
The aeolian mode differs from the phrygian in that the latter includes a flat second.
Aeolian practices are site specific, difficult to control and take much time to understand.
Aeolian inputs of silicate and more soluble minerals appears to be an important process in all soils based on surface horizon characteristics.
The sounds of aeolian harps and wind chimes depend on the direction and amount of wind in the natural environment.
Aeolian fractionation can lead to downwind changes in the chemical composition of distal ash fall deposits, connected to changes in the mineralogical composition.
Our appreciation of aeolian depositional processes and products in carbonate systems has been, with some notable exceptions, poor until now.
