Rümker plateau is composed of a series of overlapping domes, lava flows and to a ring surrounding the central portion. The examined domes on the Rümker plateau are typical mare domes morphometrically similar to the class B. Representing domes with lower slopes.

Birt and Rupes Recta region. 1 , while Birt 2 belongs to class C. 1 with a tendency towards class C. 2 due to its smaller diameter and lower edifice volume.

With an average slope of 1. The edifice volume is determined to 3. 5 belongs to class B. Rheologic modelling indicates that it was built by lava of moderate viscosity of 2. Pa s, erupting at a high effusion rate of 110 m.

Duration of the effusion processes of 0. The domes Vi1, Vi2, Vi3 and Vi6 in northern Mare Tranquillitatis belong to class C.

The heights of Wollaston 1-3 correspond to 50 m, 55 m and 40 m, respectively, resulting in average flank slopes of 1. Based on the inferred rheologic properties and morphometric properties the domes Wollaston 2 and 3 belong to the class C. While the smaller dome Wollaston 1 belongs to class C.