gassendidomes blogspot.com
Gassendi Hansteen plate
Mercoledì 9 luglio 2014. Gassendi and Hansteen domes termed Gassendi 1 and Hansteen 1-2. 78 0.5. 250 0.5. 21 x 17 0.5. 95 10. 1070 100. 85 10. 14 0.1. 49 0.5. 052 0.05. Gassendi 1 is another bisected dome, like the domes located near Rima Birt. The dome has a diameter of 7.8 0.5 km, a height of 95 10 m and resulting flank slope of 1.40 0.10. It belongs to class C. 2 in the classification scheme of possible lunar intrusive domes. Iscriviti a Post Atom.
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Gassendi Hansteen plateDESCRIPTION
Mercoledì 9 luglio 2014. Gassendi and Hansteen domes termed Gassendi 1 and Hansteen 1-2. 78 0.5. 250 0.5. 21 x 17 0.5. 95 10. 1070 100. 85 10. 14 0.1. 49 0.5. 052 0.05. Gassendi 1 is another bisected dome, like the domes located near Rima Birt. The dome has a diameter of 7.8 0.5 km, a height of 95 10 m and resulting flank slope of 1.40 0.10. It belongs to class C. 2 in the classification scheme of possible lunar intrusive domes. Iscriviti a Post Atom.CONTENT
This web page gassendidomes.blogspot.com states the following, "Gassendi and Hansteen domes termed Gassendi 1 and Hansteen 1-2." We saw that the webpage said " 21 x 17 0." It also said " Gassendi 1 is another bisected dome, like the domes located near Rima Birt. The dome has a diameter of 7. 5 km, a height of 95 10 m and resulting flank slope of 1. It belongs to class C. 2 in the classification scheme of possible lunar intrusive domes."SEEK SIMILAR DOMAINS
Herodotus Aristarchus plate
Herodotus 1, with its moderate to steep slope of 2. 5 km, large edifice volume of 21 cubic km, belongs to class B. 1 of the effusive lunar domes. It is characterized by a shallow vent about 200 m depth and 3 km long. The steep Herodotus 1 dome formed out of lava of high viscosity and over longer period of time than lower class B.
Hyginus plate
Hyginus region Hyginus 2 dome by Raffaello Lena B.
Kepler plate
Kepler 1, with its moderate slope of 1. 5 km, lies in an area of relatively thin lavas fails to completely cover hummocky Imbrian basin ejecta. It is a degraded dome with several craterlets on its summit. The rheologic model indicates a moderate lava viscosity and belongs to class C.