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1)  Laochangpo
老长坡
2)  Changpo
长坡
1.
Geochemical Characteristics for Anomaly Zonality and Prospecting Model of Changpo Super Sn Polymetallic Deposit in Guangxi;
广西长坡锡多金属矿床地球化学异常分带特征及找矿模式
2.
Geological characteristics of tin polymetallic deposit in Changpo district and tts ore forming condition;
长坡区锡多金属矿床地质特征与成矿条件分析
3.
Tin Polymetallic ore deposit of Changpo has clear zoning distribution on the space, there are three parts from bottom to top The layer like mineral vein→The thin ( or likely net) ore vein →fissure vein, we call it "three storeys".
长坡锡多金属矿床的空间分布自下而上呈似层状→细 (网 )脉状、裂隙脉状。
3)  slope length
坡长
1.
Experimental study on impacts of slope length treated with polyacrymide on sediment yield;
施加聚丙烯酰胺后坡长对侵蚀产沙过程的影响
2.
Hillslope soil erosion prediction based on WEPP model under different slope lengths in hilly-gully region of the loess area;
基于WEPP的黄土丘陵区不同坡长条件下坡面土壤侵蚀预测
3.
Based on observation data of experiment plots at the City of Zhangjiakou,analysis was made on the effect of rainfall intensity on the relationship among slope length,runoff and soil loss.
张家口市水保试验站坡长小区五年观测资料表明,降雨强度影响径流量、侵蚀量随坡长的变化。
4)  old landslide
老滑坡
1.
The cause of this landslide is the rainfall that forced the old landslides existing under the road construction cut-slope to lose its balance.
通过对贵阳南江峡谷滑坡的现场调查、钻孔勘探资料的分析,阐明该滑坡发生的主要原因是以老滑坡为基础,公路施工切坡使其失去支撑,降雨又为滑坡提供了诱发条件。
2.
Study on Inspiring Effect of Landslide Experiment on Condition of Rainfall ——Example of slope piled by old landslide in Jiangjiagou valley;
蒋家沟部分滑坡是在老滑坡的基础上 ,经过后期条件改变如坡脚流水切割、降雨入渗激发而再次发生规模不等和形式不一的滑动。
5)  olders(geroutes)
长老
1.
After a great adjustment in Lycurgusian reform it comprises 28 olders(geroutes) and 2 kings(basileis).
斯巴达元老院起源于荷马时代的长老会议,在莱库古改革时期经过了巨大的调整。
6)  reactivation of old landslide
老滑坡复活
补充资料:长乐老
1.五代宰相冯道一生仕唐晋汉周四朝﹐相六帝﹐因自号"长乐老"。《新五代史.杂传十六.冯道》﹕"当是时﹐天下大乱﹐戎夷交侵﹐生民之命﹐急于倒悬。道方自号'长乐老'﹐著书数百言﹐陈己更事四姓及契丹所得阶勋官爵以为荣。"后世常借指凭靠阿谀取荣而长保禄位的人。
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