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Over a period of time of 4. Dome in the classification scheme of effusive lunar domes. While Hux2 is a typical representative of class In.
Aristoteles 1, with its moderate slope of 1. 5 km, edifice volume of 1. 2 cubic kms, lies near the crater Aristoteles N and belongs to class B. 2 of the effusive lunar domes. According to the classification scheme, if the effusion process continues over a long period of time, steep flank slope and higher edifice volume may occur as in the case of B.
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Based on the inferred rheologic properties and morphometric properties the domes Capuanus 1 and Capuanus 2 belong to the class C. While the smaller dome Capuanus 3 is a typical exemplar of the class E. Capuanus 1 and Capuanus 2 were formed from lava of viscosities of 3.