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Lucus Planum is a region on Mars, named after an albedo feature. Its name was approved by the IAU in 1997. The center latitude of the feature is 4.99 degrees S and the center longitude is 182.83 degrees It lies just to the east and north east of the volcano Apollinaris Patera. Lucus Planum lies in both the Memnonia quadrangle and the Aeolis quadrangles. It is part of a region called the "Medusae Fossae Formation" Part of this region is covered with yardangs. They are formed by the action of wind on sand sized particles; hence they often point in the direction that the winds were blowing when they were formed. Views of yardangs in this region are shown below.

AttributesValues
rdfs:label
  • Lucus Planum (ca)
  • Lucus Planum (fr)
  • Lucus Planum (it)
  • Lucus Planum (en)
  • 卢库斯高原 (zh)
rdfs:comment
  • Lucus Planum és una formació geològica de tipus planum a la superfície de Mart, localitzada amb el sistema de coordenades planetocèntriques a 2.25 latitud N i 190.43 ° longitud E, que fa 899.87 km de diàmetre. El nom va ser aprovat per la UAI l'any 1997 i fa referència a una característica d'albedo. (ca)
  • Lucus Planum est une étendue plane élevée (planum) située principalement dans l'hémisphère sud de la planète Mars. (fr)
  • Il Lucus Planum è una struttura geologica della superficie di Marte. (it)
  • 卢库斯高原(Lucus Planum)是火星上一处以反照率特征命名的区域,其名称于1997年被国际天文学联合会批准接受。该特征的中心坐标为南纬4.99度、东经182,83度,它坐落在门农尼亚区和埃俄利斯区之间,正对着阿波利纳里斯山东面及东北。它也是被称为“梅杜莎槽沟层”区的一部分,部分区域覆盖着风吹起的沙粒大小颗粒作用而成的雅丹地貌,因此,其外观通常指示了形成时的风向。该地区雅丹的视图如下所示。 * 背景相机拍摄的卢库斯高原的表面宽景图。 * 前一张照片中的雅丹地貌近景。 * HiWish计划下高分辨率成像科学设备显示的卢库斯高原雅丹地貌全景。 * 前一幅雅丹地貌图像的近景。 * HiWish计划下高分辨率成像科学设备显示的前一幅图像的雅丹近景。 (zh)
  • Lucus Planum is a region on Mars, named after an albedo feature. Its name was approved by the IAU in 1997. The center latitude of the feature is 4.99 degrees S and the center longitude is 182.83 degrees It lies just to the east and north east of the volcano Apollinaris Patera. Lucus Planum lies in both the Memnonia quadrangle and the Aeolis quadrangles. It is part of a region called the "Medusae Fossae Formation" Part of this region is covered with yardangs. They are formed by the action of wind on sand sized particles; hence they often point in the direction that the winds were blowing when they were formed. Views of yardangs in this region are shown below. (en)
foaf:depiction
  • http://commons.wikimedia.org/wiki/Special:FilePath/44777_1725yardangsclose.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/ESP_044777_1725yardangs.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/
44777_1725yardangs2.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/44777yardangcontext.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/44777yardangcontextclose.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Lucusplanummap.jpg
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  • Lucus Planum és una formació geològica de tipus planum a la superfície de Mart, localitzada amb el sistema de coordenades planetocèntriques a 2.25 latitud N i 190.43 ° longitud E, que fa 899.87 km de diàmetre. El nom va ser aprovat per la UAI l'any 1997 i fa referència a una característica d'albedo. (ca)
  • Lucus Planum est une étendue plane élevée (planum) située principalement dans l'hémisphère sud de la planète Mars. (fr)
  • Lucus Planum is a region on Mars, named after an albedo feature. Its name was approved by the IAU in 1997. The center latitude of the feature is 4.99 degrees S and the center longitude is 182.83 degrees It lies just to the east and north east of the volcano Apollinaris Patera. Lucus Planum lies in both the Memnonia quadrangle and the Aeolis quadrangles. It is part of a region called the "Medusae Fossae Formation" Part of this region is covered with yardangs. They are formed by the action of wind on sand sized particles; hence they often point in the direction that the winds were blowing when they were formed. Views of yardangs in this region are shown below. * Wide context view of surface of Lucus Planum, as seen with CTX. * Closer view of yardangs from previous image, as seen with CTX. * Wide view of yardangs in Lucus Planum, as seen by HiRISE under HiWish program * Close view of yardangs in previous image, as seen by HiRISE under HiWish program * Close view of yardangs from a previous image, as seen by HiRISE under HiWish program (en)
  • Il Lucus Planum è una struttura geologica della superficie di Marte. (it)
  • 卢库斯高原(Lucus Planum)是火星上一处以反照率特征命名的区域,其名称于1997年被国际天文学联合会批准接受。该特征的中心坐标为南纬4.99度、东经182,83度,它坐落在门农尼亚区和埃俄利斯区之间,正对着阿波利纳里斯山东面及东北。它也是被称为“梅杜莎槽沟层”区的一部分,部分区域覆盖着风吹起的沙粒大小颗粒作用而成的雅丹地貌,因此,其外观通常指示了形成时的风向。该地区雅丹的视图如下所示。 * 背景相机拍摄的卢库斯高原的表面宽景图。 * 前一张照片中的雅丹地貌近景。 * HiWish计划下高分辨率成像科学设备显示的卢库斯高原雅丹地貌全景。 * 前一幅雅丹地貌图像的近景。 * HiWish计划下高分辨率成像科学设备显示的前一幅图像的雅丹近景。 (zh)
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