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The most significant variable that influences annual runoff ratio for both basin types is the average annual days of measurable precipitation.
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Documenting more of these basins types is the key to refining our understanding of the tectonic evolution of continental margins.
Spatial autocorrelation of ordinary least squares estimated residuals are reduced by geographically weighted regression (GWR) for all models in both basin types.
Given that there are only 3,131 ground surveys in the 5 million square kilometer Brazilian Amazon basin, precision identification of soils and vegetation types is only possible for the RADAM data records and even these may not be precise given local environmental heterogeneity within the area of the botanical survey.
A variety of basin types have been formed in the different types of glacial drift deposits, including basins in morainic material, kettle lakes, channels formed by water movement in tunnels beneath the ice masses, and lake basins formed by thawing in permafrost.
Both types are fatal.
Both types are represented here.
Both types are found throughout the world.
Both types are found in most bones.
Both types were important.
After the second major transgression (Apt 2), higher differences between sequence thicknesses as well as lithofacies types are due to intrashelf basin topographies.
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