“…Thickened salt was the preferred interpretation of Joesting and others, because the Needles faults are commonly regarded as caused by downslope sliding of the rocks above the salt toward the Colorado River. Lewis and Campbell (1965), Stromquist (1976), Huntoon (1979), and Hildenbrand and Kucks (1983) interpreted the anomaly source as low-density, moderately magnetized Precambrian rocks because of small magnetic highs in the area of the low (not shown on fig. 5).…”