Rupes Altai Piccolomini plate
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Rupes Altai Piccolomini plateDESCRIPTION
Rupes Altai Piccolomini plate. Giovedì 14 agosto 2014. Rupes Altai and Piccolomini region. Piccolomini dome termed Pi1. 14 0.5. 350 30. 29 0.3. 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.CONTENT
This web page piccolominidome.blogspot.com states the following, "Rupes Altai and Piccolomini region." We saw that the webpage said " 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." It also said " 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."SEEK SIMILAR DOMAINS
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.
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.