Viruvius Cauchy plate
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Viruvius Cauchy plateDESCRIPTION
Domenica 29 giugno 2014. Vitruvius and Cauchy region. Vitruvius Cauchy domes termed Vitruvius Vi 1-6 and Cauchy C1-19. Vitruvius domes termed Vi1-Vi6. 58 0.5. 63 0.5. 60 0.5. 60 0.5. 50 0.5. 90 10. 130 15. 70 10. 50 5. 17 0.2. 23 0.2. 27 0.2. 13 0.1. 11 0.1. 73 0.5. 90 10. 15 0.2. Pa s, effusion rates of E 45-100. Duration of the effusion processes of 0.6-2.0 years. The domes Vi1, Vi2, Vi3 and Vi6 in northern Mare Tranquillitatis belong to class C. 81 0.5. 70 1.CONTENT
This web page vitruviuscauchy.blogspot.com states the following, "Vitruvius Cauchy domes termed Vitruvius Vi 1-6 and Cauchy C1-19." We saw that the webpage said " Pa s, effusion rates of E 45-100." It also said " Duration of the effusion processes of 0. The domes Vi1, Vi2, Vi3 and Vi6 in northern Mare Tranquillitatis belong to class C."SEEK SIMILAR DOMAINS
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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Yerkes 1 is characterized by the presence of rilles in the summit. It has a height of 110. A flank slope of 1. Ye1, with its low flank slope and rather low edifice volume, belongs to class B. If the effusion of lava continues over a long period of time, a steep flank slope and high edifice volume may occur as in the case of class B.
Doppelmayer 2 is a typical effusive mare dome, with a shallow flank slope, and low edifice volume. It was formed of lavas of a viscosity of 10. Pa s, which is between the ranges of values typically observed for lunar mare domes and highland domes, respectively, erupting at moderate rates over a long period of time of nine years. Is situated between classes C.
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