Geostatistical Modeling of Sediment Abundance in a Heterogeneous Basalt Aquifer at the Idaho National Laboratory, Idaho

Scientific Investigations Report 2006–5316

U.S. GEOLOGICAL SURVEY
Scientific Investigations Report 2006–5316
DOE/ID-22201

Figure - refer to figure caption for alternative text description

Figure 19. Distribution of sediment-rich and sediment-poor areas in the model domain. (A) as currently implemented in the U.S. Geological Survey subregional ground-water flow model, based on an 11-percent sediment threshold, regardless of depth; and (B) median sediment content of the uppermost 300 feet of the aquifer, as determined by multiple-indicator kriging. The extent of the Big Lost Trough (dashed polygon) and the boundary between sediment-rich and sediment-poor areas in (A) are shown for comparison.

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