| dbo:abstract |
Das Uzboi-Ladon-Morava-System, kurz auch ULM-System genannt, ist eine etwa 8000 Kilometer lange Oberflächenstruktur auf dem Mars. (de) The Uzboi-Landon-Morava (ULM) outflow system is a long series of channels and depressions that may have carried water across a major part of Mars. It starts with channels that drain into the Argyre basin in the Argyre quadrangle. Water ponded in the Argyre basin, then the overflow is believed to have traveled northward through Uzboi Vallis, into , through , to the floor of . Some of the water may have helped to carve Ares Vallis. Altogether, the total area drained for this watershed may have been about 11 X 106 km2 or about 9% of Mars. Pictures below show the Argyre basin which was once full of water. Also, the wider view shows the distance the water traveled, which was south of Argyre basin to Margaritifer Terra. (en) 乌斯钵-拉冬-摩拉瓦 (Uzboi-Landon-Morava) 溢道系统是一长串的河床和洼地，可能曾携带着水流穿过了火星大部分的地区。它启源于流入阿耳古瑞区中阿耳古瑞盆地的河道。积蓄在阿耳古瑞盆地中的大水，据说随后漫溢而出向北奔流，一路穿过乌斯钵谷，进入拉冬盆地，再穿越摩拉瓦谷，最后抵达珍珠湾盆底。其中部分水流可能冲刷蚀刻了阿瑞斯谷 。总之，该流域的总溢流面积可能约为 11 X 106公里2或约火星9% 的表面。 下面的图片显示了曾经被水注满的阿耳古瑞盆地。此外，更广阔的视图显示了水流穿越的距离，从阿耳古瑞盆地以南一直到珍珠高地。 (zh) |
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wiki-commons:Special:FilePath/Margaritifer_Sinus.png?width=300 |
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dbr:Uzboi_Vallis dbc:Argyre_quadrangle dbc:Margaritifer_Sinus_quadrangle dbr:Margaritifer_Terra dbr:Ares_Vallis dbr:Argyre_quadrangle dbc:Valleys_and_canyons_on_Mars dbr:Argyre_basin dbr:Morava_Valles dbr:Landon_basin dbr:Margaritifer_basin |
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dbt:Geography_of_Mars dbt:Annotated_link dbt:Reflist dbt:Short_description |
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dbc:Argyre_quadrangle dbc:Margaritifer_Sinus_quadrangle dbc:Valleys_and_canyons_on_Mars |
| rdfs:comment |
Das Uzboi-Ladon-Morava-System, kurz auch ULM-System genannt, ist eine etwa 8000 Kilometer lange Oberflächenstruktur auf dem Mars. (de) 乌斯钵-拉冬-摩拉瓦 (Uzboi-Landon-Morava) 溢道系统是一长串的河床和洼地，可能曾携带着水流穿过了火星大部分的地区。它启源于流入阿耳古瑞区中阿耳古瑞盆地的河道。积蓄在阿耳古瑞盆地中的大水，据说随后漫溢而出向北奔流，一路穿过乌斯钵谷，进入拉冬盆地，再穿越摩拉瓦谷，最后抵达珍珠湾盆底。其中部分水流可能冲刷蚀刻了阿瑞斯谷 。总之，该流域的总溢流面积可能约为 11 X 106公里2或约火星9% 的表面。 下面的图片显示了曾经被水注满的阿耳古瑞盆地。此外，更广阔的视图显示了水流穿越的距离，从阿耳古瑞盆地以南一直到珍珠高地。 (zh) The Uzboi-Landon-Morava (ULM) outflow system is a long series of channels and depressions that may have carried water across a major part of Mars. It starts with channels that drain into the Argyre basin in the Argyre quadrangle. Water ponded in the Argyre basin, then the overflow is believed to have traveled northward through Uzboi Vallis, into , through , to the floor of . Some of the water may have helped to carve Ares Vallis. Altogether, the total area drained for this watershed may have been about 11 X 106 km2 or about 9% of Mars. (en) |
| rdfs:label |
Uzboi-Ladon-Morava-System (de) Uzboi-Landon-Morava (en) 乌斯钵-拉冬-摩拉瓦谷 (zh) |
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wikidata:Uzboi-Landon-Morava dbpedia-de:Uzboi-Landon-Morava dbpedia-zh:Uzboi-Landon-Morava https://global.dbpedia.org/id/zkKh |
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wikipedia-en:Uzboi-Landon-Morava?oldid=1096928579&ns=0 |
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wiki-commons:Special:FilePath/Argyre_basin_topo.jpg wiki-commons:Special:FilePath/Wikimolaargyre.jpg wiki-commons:Special:FilePath/Margaritifer_Sinus.png |
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