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<p>It was likewise used by American geologist <a href="page.php?w=G._K._Gilbert">G. K. Gilbert</a> to explain the uplifted shorelines of <a href="page.php?w=Lake_Bonneville">Lake Bonneville</a>. The concept was further developed in the 1950s by the Dutch geodesist <a href="page.php?w=Vening_Meinesz">Vening Meinesz</a>.</p>

<p><big> Models </big></p>
<p>Three principal models of isostasy are used:<br/>
# The Airy-Heiskanen model - where different topographic heights are accommodated by changes in <a href="page.php?w=Crust_%28geology%29">crustal</a> thickness,</p><p>
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