Bouldery craters are primarily the result of bolides impacting solid material.
Learn about the moon’s most fascinating objects, understand how the moon was formed and the names of many of the craters … and why they honor individuals who have changed the course of history.
It is about 275 miles (~440 km) across. These lavas also extend past the
Mare Humorum - WordReference English dictionary, questions, discussion and forums. Mare Humorum is a scientifically interesting area because it allows the study of the relationships among lunar mare filling, mare basin tectonics, and global thermal evolution to the major mascon maria – regions of the moon's crust which contain a large amount of material denser than average for that area (Solomon, Head, 1980).
Several rilles in the southeast section can be easily seen with a 4-inch scope. This gives you a clear indication of the sequence of activity. Mare Humorum (the "Sea of Moisture") is a lunar mare.The impact basin it is located in is 825 kilometers across. Tags.
Moon. What features appeared after subsidence took place?Three generations of crater age can be easily observed on Mare Humorum. is a small circular mare on the lunar nearside. These lavas also extend past the basin rim in several places. lunar surface due to the weight of Mare Humorum. basin has been flooded and filled by mare lavas. This week we will highlight the area around Mare Humorum.Look closely at the Hippalus rilles just east of the mare. (Both Gassendis taken together are sometimes referred to as the Gassendi is considered to be one of the Moon’s most beautiful and interesting objects. Draw a map of what you can see, then come back later and try to improve on the count. Mare Humorum is a scientifically interesting area because it allows the study of the relationships among lunar mare filling, mare basin tectonics, and global thermal evolution to the major mascon maria – regions of the moon's crust which contain a large amount of material denser than average for that area (Solomon, Head, 1980).
Several have been reported here.It is highly recommended that you get a copy of Sky and Telescope’s Note the large fractures arcing around
In the upper right are several such flows which extend
It was not sampled by the Apollo program, so a precise age has not been determined.
However, geological mapping indicates that it is intermediate in age between the Imbrium and Nectaris Basins, suggesting an age of about 3.9 billion years. (See how close you can get to 30.) This image shows Mare Humorum and the western edge of Mare Nubium. Mare Humorum, the “Sea of Moisture” Mare Humorum is located just south of Oceanus Procellarum. Notice how some of them plough through both mountain ridges and craters, and some are interrupted completely by small craters but continue on the other side. Such a sinking of the mare may also MARE HUMORUM (EP) Padelezh hollek : 31 mn Testennoù, mouezhioù ha kan, holl vinvioù sonerezh, logo, mennozhioù gant Arnev, programmiñ taboulinoù, advouezhioù, sonskeudenniñ ha meskañ gant Mornoz; Skeudennoù sevenet gant Rom diwar mennozhioù Arnev Trugarekaat evit …
Mare Nubium, the “Sea of Clouds” Mare Nubium is east of Mare Humorum. Full Moon Atlas: Sector F-2 Mare Humorum/ Western Mare Nubium. It was not sampled by the Apollo program, so a precise age has not been determined. The mountains surrounding Mare Humorum mark the edge of an old impact basin. Mare Humorum. Mare Humorum: [SW/M6] The Humorum basin is one of the best examples of subsidence that you can see on the Moon. The mountains surrounding Mare Humorum mark the edge of an old impact basin. From crater statistics, in the year 2000 Hiesinger and colleagues found that in Humorum there was a peak of eruptions at about 3.3-3.5 thousand million years ago.You have already liked this page, you can only like it once!
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