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弗里德曼环形山

弗里德曼环形山
纬度12.48°S
经度126.88°W
直径101.45公里
深度2861米
余经日出时128°
命名来源亚历山大·弗里德曼

弗里德曼环形山(Fridman)是月球背面的一座撞击坑残迹。其名称取自苏联数学家气象学家宇宙学家亚历山大·亚历山大洛维奇·弗里德曼(1888年-1925年),1970年被国际天文联合会正式批准接受。

描述

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弗里德曼环形山位于巨大的赫茨普龙环壁平原南面,西南连接了约费环形山的东北侧壁。其中心月面坐标12°29′S 126°53′W / 12.48°S 126.88°W / -12.48; -126.88,直径101.45公里[1],深度2861米[2]

该陨坑处于赫茨普龙环形山喷发物覆盖层之内,同时也位于环东海撞击盆地辽阔的喷发物覆盖层西北偏西区,因此,该环形山外侧壁损毁严重,坑壁平均高出周边地形1490米[2],内部容积约10256.97立方千米[2]; 环四周横跨着一些较小的撞击坑,陨坑东南侧边缘保存相对最完整。陨坑内西南地表部分被约费环形山的外壁垒覆盖,北部区坐落着数座小陨石坑,而东南部地表上留有众多撞击形成的小陨洞。

卫星陨石坑

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按惯例,最靠近弗里德曼环形山的卫星坑在月图上以字母标注在该坑中心点的旁边。

月球勘测轨道飞行器拍摄
弗里德曼 纬度 经度 直径
C 10.61° S 124.93° W 37.67 公里

参考资料

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另请参阅

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弗里德曼环形山
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