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康格里夫环形山

康格里夫环形山
月球轨道器1号拍摄的图像
纬度0.28°S
经度167.84°W
直径57.61公里
深度2.450公里
余经日出时168°
命名来源威廉·康格里夫

康格里夫环形山(Congreve)是位于月球背面赤道上一座古老的大型撞击坑,约形成于酒海纪[1],其名称取自英国发明家火箭武器先驱威廉·康格里夫爵士(1772年-1828年),1970年被国际天文联合会批准接受。

描述

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该陨坑西侧紧邻利普斯基环形山、西北偏西是克拉索夫斯基环形山茹科夫斯基环形山坐落在它的北面;东北为恩格尔伽特陨石坑,在它的东侧和西南面分别是巨大的科罗廖夫环形山伊卡洛斯环形山[2]。陨坑中心月面坐标0°17′S 167°50′W / 0.28°S 167.84°W / -0.28; -167.84,直径57.61公里[3],深度2.450公里[1]

康格里夫环形山外观呈多边形状,因存续期长而受撞击侵蚀严重,部分区域已磨损的难以辨识。陨坑坡壁平缓,北侧和西侧坑沿及内壁较明显,东侧则坐落着一对较大的陨石坑,而东南边缘仅剩为一弯浅浅的山脊。它的坑壁最大高出周边地形1190米[1],内部容积约2775.413[1]。坑底表面相对平坦,在东部可看到三座明显的撞击坑,其余地表上散落着一些细小的陨坑。

卫星陨石坑

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按惯例,最靠近康格里夫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。

LAC-68、LAC-69、LAC-86及LAC-87拼接图
康格里夫 纬度 经度 直径
G 0.89° S 163.88° W 17.50公里
H 1.31° S 165.74° W 37.96公里
L 3.73° S 166.83° W 29.91公里
N 3.66° S 168.57° W 29.93公里
Q 1.74° S 169.56° W 55.35公里
U 0.40° S 170.75° W 54.72公里
  • 卫星坑“康格里夫 H”、“康格里夫 L”、“康格里夫 Q”和“康格里夫 U”形成于酒海纪[1]

参考文献

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  1. ^ 1.0 1.1 1.2 1.3 1.4 Lunar Impact Crater Database
  2. ^ Crater Congreve on the LAC-87 map (PDF). [2016-06-25]. (原始内容存档 (PDF)于2013-02-20). 
  3. ^ Directory of the International Astronomical Union. [2016-06-25]. (原始内容存档于2022-01-08). 

外部链接

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康格里夫环形山
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