Isostatic correction The long wavelengths of the Bouguer gravity field correlate inversely with the long wavelengths of topography. Masses or "roots" at the base of the crust supporting the topography cause this correlation according to the theory of isostasy. These regionalscale anomalies are especially prominent in mountainous areas and near the edges of continents (i.e. continental shelves) and often obscure anomalies caused by upper crustal structures. Polynomial fitting or wavelength-filtering techniques have been routinely used for the removal of topography-induced regional and the enhancement of gravity anomalies related to shallow geologic features. However, these techniques suffer from the fact that they eliminate all wavelengths longer than some threshold, whether of not they are related to topographic features In fact, long-wavelength anomalies due entirely to lateral variations in crustal density will be eliminated by these techniques. The isostatic correction is preferable because the isostatic regional accounts for the effect of the topographic "roots", thereby removing the observed correction between Bouguer values and topography. Isostatic residual gravity maps reveal more clearly than most gravity maps the density distributions within the upper crust that are of 1 interest in most kinds of geologic and tectonic analyses. (A) Analogue of Airy isostasy: taller wood blocks float higher in water. (B) Analogue of Pratt isostasy: less dense wood blocks (lighter shading) float higher in water than denser wood blocks (darker shading). All blocks have the same mass and have even bases. (C) A topographically high region is underlain by a lower-density crustal root. Every column of material weighs the same, indicating isostatic equilibrium. Airy model In most cases a better approximation to earth structure applies well to mountain ranges, variable thickness of continental crust Pratt model applies to mid-ocean ridges: ridges elevated compared to rest of ocean floor. Reason: crust+uppermost mantle hot under ridges and therefore less dense than surroundings The principle of isostasy states that mass excesses, represented by topographic loads at the surface, are compensated by mass deficiencies at depth which are referred to as isostatic roots. The effect of these mass deficiencies are not accounted for in the Bouguer reduction and there exists an inverse correlation between broad Bouguer anomaly lows and positive topography. The isostatic correction removes the gravity effect of the isostatic roots. 2