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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.
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Immediately to the north of the remnants of the northern crater wall lies a large and elongated lunar dome termed Fracastorius 1, with an evident vent on its surface.
1 , while Gambart 3 is situated between classes C.