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A French blunderbuss, called an espingole, 1760, France Musketoon, blunderbuss and coach gun from the American Civil War era. The flared muzzle is the defining feature of the blunderbuss, differentiating it from large caliber carbines; the distinction between the blunderbuss and the musketoon is less distinct, as musketoons were also used to fire shot, and some had flared barrels.
Sinus Iridum is one of the largest craters of Upper (Late) Imbrian age. [ 2 ] The selenographic coordinates of the bay's center are 45.01° N, 31.67° W, and the diameter is 249 km. [ 1 ] It was the planned landing site of Chang'e 3 , China's 2013 lunar exploration mission, which instead landed nearby in Mare Imbrium .
Lunar maria (singular mare) are large, dark, regions of the Moon. They do not contain any water, but are believed to have been formed from molten rock from the Moon's mantle coming out onto the surface of the Moon. This list also includes the one oceanus and the features known by the names lacus, palus and sinus.
Minecraft is a media franchise developed from and centered around the video game of the same name. Developed by Mojang Studios (formerly known as Mojang AB) and Xbox Game Studios , which are owned by Microsoft Corporation , the franchise consists of six video games, along with various books, merchandise, events, and an upcoming theatrical film.
This is not a list of the highest places on the Moon, meaning those farthest from the CoM. Rather, it is a list of peaks at various heights relative to the relevant datum. This is because the Moon has mass asymmetries: the highest point , located on the far side of the Moon, is approximately 6,500 meters higher than Mons Huygens (usually listed ...
Montes Apenninus is the most prominent remnant of the outer ring of the Imbrium basin, which also includes Montes Carpatus to its south and Montes Caucasus to its north.. The Montes Apenninus range forms the southeastern border of the large Mare Imbrium lunar mare and the northwestern border of the Terra Nivium highland region.
More than 135 mountains have been identified on the surface of Jupiter's moon Io. [1] Despite the extensive active volcanism taking place on Io, most mountains on Io are formed through tectonic processes. These structures average 6 km (4 mi) in height and reach a maximum of 17.5 ± 1.5 km (10.9 ± 1 mi) at South Boösaule Montes. [2]
The Pre-Nectarian period is defined from the point at which the lunar crust formed, to the time of the Nectaris impact event. Nectaris is a multi-ring impact basin that formed on the near side of the Moon, and its ejecta blanket serves as a useful stratigraphic marker. 30 impact basins from this period are recognized, the oldest of which is the South Pole–Aitken basin.