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甘斯文特环形山

甘斯文特环形山
月球轨道器4号拍摄的图像
纬度79.42°S
经度111.17°E
直径77.5公里
深度2.77公里
余经日出时256°
命名来源赫尔曼·甘斯文特英语Hermann Ganswindt
克莱门汀号拍摄的图像,甘斯文特环形山位于中间,下方是艾德尔森环形山。

甘斯文特环形山(Ganswindt)是月球背面南极区一座古老的大撞击坑,约形成于39.2-38.5亿年前的酒海纪[1],其名称取自德国发明家火箭先驱赫尔曼·甘斯文特英语Hermann Ganswindt(Hermann Ganswindt ,1856年-1934年),1970年被国际天文学联合会批准接受。

描述

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该陨坑西南偏西毗邻海代尔瓦里环形山、北面靠近里滕豪斯陨石坑、巨大的薛定谔环形山位于它的东北、东南偏东坐落了尼菲德耶夫环形山、而它的南面则部分覆盖了艾德尔森环形山的北侧壁[2]。该陨坑中心月面坐标79°25′S 111°10′E / 79.42°S 111.17°E / -79.42; 111.17,直径77.5公里[3],深度2.77公里[1]

甘斯文特环形山边缘大致呈圆形,但有些不规则,尤其是南侧坑壁。坑壁平均高出周边地形1340米[1],内部容积约为5509.63公里3[1]。坑底大部分被崎岖的山脊所覆盖,靠东南坐落一座醒目的小陨坑。由于太阳光只能斜射至该陨坑内,因此,它的坑底北部几乎总是笼罩在阴影中,因此,该部分的地形难以被观察到。

赫尔曼·甘斯文特早在1881年就提出了使用反推力运输工具作为太空旅行的手段,他也曾提出了包含时间在内的四维空间理论。

参考资料

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  1. ^ 1.0 1.1 1.2 1.3 Lunar Impact Crater Database
  2. ^ Crater Ganswindt on LAC-140 map. (PDF). [2016-11-05]. (原始内容存档 (PDF)于2021-03-28). 
  3. ^ Directory of the International Astronomical Union. [2016-11-05]. (原始内容存档于2021-06-14). 

另请参阅

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外部链接

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甘斯文特环形山
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