rumkerdomes blogspot.com

Rumker plate

Domenica 15 giugno 2014. Rümker domes termed Rümker 1-6. 84 0.5. 91 0.5. 91 0.5. 73 0.5. 55 0.5. 200 20. 130 15. 240 25. 170 20. 70 10. 27 0.2. 16 0.2. 30 0.2. 27 0.2. 15 0.2. 69 0.5. 100 10. 17 0.2. 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.
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Rumker plate

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Domenica 15 giugno 2014. Rümker domes termed Rümker 1-6. 84 0.5. 91 0.5. 91 0.5. 73 0.5. 55 0.5. 200 20. 130 15. 240 25. 170 20. 70 10. 27 0.2. 16 0.2. 30 0.2. 27 0.2. 15 0.2. 69 0.5. 100 10. 17 0.2. 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.

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This web page rumkerdomes.blogspot.com states the following, "Rümker domes termed Rümker 1-6." We saw that the webpage said " Rümker plateau is composed of a series of overlapping domes, lava flows and to a ring surrounding the central portion." It also said " The examined domes on the Rümker plateau are typical mare domes morphometrically similar to the class B. Representing domes with lower slopes."

SEEK SIMILAR DOMAINS

Birt and Rupes Recta plate

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.

Sinus Iridum plate

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.

Viruvius Cauchy plate

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

Wollaston plate

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.

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