Fowler is a large lunar impact crater that lies in the northern hemisphere on the Moon’s far side. It lies to the south-southwest of the crater Esnault-Pelterie, and north of Gadomski. Overlying the eastern rim and intruding into the interior is Von Zeipel. The outer rim of this crater has become worn and rounded by impact erosion until it has become little more than an irregular
Fleming is a large lunar impact crater that is located on the Moon’s far side, and cannot be seen from the Earth. It lies about a crater diameter to the east-northeast of Hertz, and to the northwest of Lobachevskiy. The low rim of this formation is heavily eroded and overlaid by multiple smaller craters. The most notable of these is Fleming along the southern
Finsen is a lunar impact crater that is located in the southern hemisphere, on the Moon’s far side. It is attached to the southeastern exterior of the walled plain Leibnitz, and the ejecta from Finsen covers the southeastern part of Leibnitz’s interior floor. To the southwest of Finsen is another walled plain, Von Kármán, partly overlain by Leibnitz. This is a relatively young impact
Ellerman is a lunar impact crater on the far side of the Moon. It lies within the outer blanket of ejecta that surrounds the Mare Orientale impact basin, and is located to the west of the Montes Cordillera mountain range. To the northwest of Ellerman is the larger crater Gerasimovich. Probably due to its location amidst rugged surroundings, the otherwise circular rim of this crater is somewhat
Emden is a lunar impact crater that is located in the northern hemisphere on the far side of the Moon. It is named after Jacob Robert Emden (1862-1940). The crater lies to the northwest of the larger crater Rowland, and to the east-northeast of Tikhov. It has been heavily damaged by subsequent impacts, leaving the rim worn and irregular and the interior partly covered by craters. The western
Esnault-Pelterie is a lunar impact crater on the far side of the Moon, named after French rocketry and astronautics pioneer Robert Esnault-Pelterie. It is located in the northern hemisphere, to the south of the crater Carnot. Esnault-Pelterie overlies the western side of the crater Schlesinger. To the south is the crater Von Zeipel and to the southwest is Fowler. The rim of this crater are somewhat worn, but still retain some
Dyson is a lunar impact crater, 63 kilometers in diameter, that lies on the far side of the Moon, past the northwest limb. It is located in the northern part of the surface, to the northwest of the crater Coulomb, and east of van’t Hoff.[1] The most unusual aspect of this crater is the asymmetry of the inner wall. To the northeast the
Delporte is a lunar impact crater on the far side of the Moon. It overlies part of the northwestern rim of the huge walled plain Fermi, and the crater Litke is nearly attached to the southeastern rim. The rim of this crater is only marginally worn, although it is not quite circular and the edge is somewhat uneven. There is a shelf running along the
Davisson is a lunar impact crater that is located on the far side of the Moon from the Earth. This crater lies across the eastern rim of the huge walled plain Leibnitz, and the rim and outer rampart intrudes into the interior floor of Leibnitz. To the east-northeast of Davisson is the walled plain Oppenheimer, a formation only somewhat smaller than Leibnitz. The rim of Davisson has been
Daedalus is a prominent crater located near the center of the far side of the Moon. The inner wall is terraced, and there is a cluster of central peaks on the relatively flat floor. Because of its location (shielded from radio emissions from the Earth), it has been proposed as the site of a future giant radio telescope, which would be scooped