Messier plate
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Messier plateDESCRIPTION
Mercoledì 16 luglio 2014. Domes termed Messier 1-2. 77 0.5. 87x64 0.5. 85 10. 80 10. 126 0.1. 112 0.1. Two domes near Messier, which are similar to each other with respect to their morphometric, rheologic, and spectral properties, belong to class C. With a tendency towards class C. Due to their moderate R. Value With their inferred moderate lava viscosities these domes share the properties of rheologic group R. Accordingly, the inferred magma rise speed amounts to several 10.CONTENT
This web page messierdomes.blogspot.com states the following, "Two domes near Messier, which are similar to each other with respect to their morphometric, rheologic, and spectral properties, belong to class C." We saw that the webpage said " With a tendency towards class C." It also said " Due to their moderate R. Value With their inferred moderate lava viscosities these domes share the properties of rheologic group R. Accordingly, the inferred magma rise speed amounts to several 10."SEEK SIMILAR DOMAINS
Petavius 1, with its moderate slope of 1. 5 km, large edifice volume of 19 cubic km.
Rupes Altai and Piccolomini region. It is located about 85 km northwest of the crater Piccolomini inside the Nectaris basin, about 30 km closer to its centre than the Altai Scarp. The dome Pi1 is characterised by a high lava viscosity of 10. Pa s Its rheologic properties are similar to those of the comparably steep domes north of Hortensius in Mare Insularum. Pi1 belongs to class B.
The domes R1, R3 and R5 are part of the Procellarum group and belong to class C. 2 , while the dome R4 with its smaller diameter, height and lower edifice volume is situated between classes C.
La chèvre de Mr Seguin .
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.